Restricting global warming to 1.5C could ‘halve’ risk of biodiversity loss

This is a re-post from Carbon Brief by Daisy Dunne

Limiting global warming to 1.5C above pre-industrial levels rather than 2C could halve the number of vertebrate and plant species facing severe range loss by the end of the century, a study finds.

The analysis of more than 115,000 species finds that keeping warming at 1.5C – which is the aspirational target of the Paris Agreement – instead of 2C could also cut the number of insects facing severe range loss by two-thirds.

However, if countries fail to ramp up their efforts to address climate change, around a quarter of all vertebrates (animals with a spine), half of insects and 44% of plants could face severe range loss, the lead author tells Carbon Brief.

The greatest range losses are expected to occur in some of the world’s biodiversity hotspots, the author adds, including in the Amazon and southern Africa.

Although the findings are significant, the research does not explore all the factors relevant to species survival, including the impact of evolution, another scientist tells Carbon Brief.

Hostile planet

Climate change threatens wildlife in a host of ways. One way is by reducing a species’ geographical range – the extent of the area where it is able to survive.

This can occur when local temperatures become too hot for species to tolerate or when changing rainfall patterns affect the types of food available, for example. As a species’ range contracts, its risk of extinction can increase.

The new study, published in Science, uses a set of global climate models to explore how warming this century could affect the ranges of more than 115,000 species that live on land.

For the analysis, the researchers used four scenarios, including where warming is limited to, in order, 1.5C, 2C, 3.2C (which is the amount of warming anticipated if countries stick to their national pledges to cut emissions) and to 4.5C, the amount of warming expected under a “business as usual” scenario (“RCP8.5”).

The research finds that, if warming is limited to 2C, 8% of vertebrates, 18% of insects and 16% of plants could lose at least half of their current range by 2100.

However, if warming is limited to 1.5C, this risk is halved for vertebrates and plants, and cut by two-thirds for insects.

Unequal losses

The charts below show how future global warming is expected to affect the ranges of invertebrates (A), vertebrates (B) and plants (C) , and also a further breakdown of how warming could affect insects (D), mammals (E) and birds (F).

The x-axis shows temperature rise above pre-industrial levels, while the y-axis shows the proportion of species expected to lose more than half of their range.

On the charts, results for “no dispersal” (yellow) and “realistic dispersal” (blue) are shown. The “realistic dispersal” results consider the ability of animals to move away from their site of birth into new areas, explains lead author Prof Rachel Warren, a researcher of global change and environmental biology at the Tyndall Centre for Climate Change Research. She tells Carbon Brief:

“​’No dispersal’ means that we assume the animals don’t move. ‘Dispersal’ means species can move at rates they’ve been observed to move at in response to the climate change that has happened so far.”

The proportion of species expected to lose more than half of their range by 2100 under different levels of temperature rise. Results are shown for invertebrates (A), vertebrates (B), plants (C), insects (D), mammals (E) and birds (F). Source: Warren et al. (2018)

The results show how invertebrates (A), such as insects, spiders and worms, are expected to lose a larger proportion of their range than vertebrates (B), such as mammals, birds and reptiles.

Insect species at a particularly high risk include key crop pollinators, including bees, hoverflies and blowflies, the research notes. This is due to a range of factors linked to insect physiology and lifestyle, says Warren:

“It is probably because they are ectothermic, which means that their body temperature is controlled externally, not internally, as in humans. Also they have life stages – eggs, larvae, pupae, as well as adults. Each of these stages might be vulnerable to different things, such as eggs drying out if there is too little rainfall.”

BMKF99 Green Hairstreak Butterfly perched on a fern, Devon Coast, UK.

Green Hairstreak Butterfly perched on a fern, Devon Coast, UK. Credit: Steve Bloom Images/Alamy Stock Photo.

For mammals (E) and birds (F), risks remain low at 1.5C but grow significantly larger as warming increases, the research finds. Mammals most at risk include critically endangered species such as the black rhino, which also faces significant challenges from habitat loss and poaching.

Warming hotspots

The maps below show how different levels of warming could affect global species diversity for vertebrates. The charts show the proportion of species expected to remain by 2100 – from 90-100% remaining (blue) down to just 0-10% of species remaining (red) – with and without the impact of dispersal.

The proportion of vertebrate species expected to remain in world regions by 2100 under different levels of temperature rise (from top to bottom: 1.5, 2, 3.2, 4.5C). Red shows 0-10% of species remaining while dark blue shows 90-100% remaining. Source: Warren et al. (2018)

The maps reveal that, if future global warming reaches 3.2-4.5C, striking biodiversity loss could occur in some of the world’s wildlife hotspots, including southern Africa and the Amazon – which is home to 30% of the world’s species.

HNWCNF Giraffe, Giraffa camelopardalis, with Mount Kilimanjaro in the background, Chyulu Hills National Park, Kenya.

Giraffe in front of Mount Kilimanjaro, Chyulu Hills National Park, Kenya. Credit: Lucas Vallecillos/Alamy Stock Photo.

This could be because temperatures in the tropics and subtropics are relatively consistent from one season to the next, which means resident species are less used to large swings in temperature, says Warren:

“Here in the UK, we can have terrible summers and very nice ones – whereas in the tropics it’s much more predictable. This means that, in temperate lands, species are likely to be buffered against quite large natural climate variability. Whereas in the tropics, as the average climate changes, it could get quickly outside the range of natural variability that species are adapted to.”

Other regions expected to suffer species losses include Australia, the last remaining habitat of marsupials, and the high Arctic, home of the polar bear, the Arctic fox and caribou.

BECCS trade-off

The results show that meeting the Paris Agreement’s aspirational target of limiting warming to 1.5C would bring “substantial benefits” for wildlife, the scientists write in their research paper:

“Successful implementation of the Paris Agreement could lead to substantial benefits for global terrestrial [land] biodiversity…However, restricting warming to 1.5C may be difficult.”

This difficulty lies in the assumption that “negative emissions technologies” will be able to help the world meet the 1.5C target, the researchers say. Most scenarios envisaging how the world could limit warming 1.5C incorporate a negative emissions technology known as bioenergy with carbon capture and storage (BECCS).

Put simply, BECCS involves burning biomass – such as trees and crops – to generate energy and then capturing the resulting CO2 emissions before they are released into the air.

The technology has yet to be demonstrated on a commercial basis, and recent researchshows its potential may be more limited than previously thought.

Even if BECCS is developed on a wide scale, the researchers say, it could pose a significant threat to biodiversity.

That is because large scale BECCS could require up to 18% of the land surface to be converted to biomass plantations, they say, which would drive up competition for land.

This could lead to more deforestation and habitat loss to meet bioenergy and agriculture requirements, they say:

“New studies are exploring scenarios in which BECCS is produced from secondary biofuels, or in which there are dietary changes in humans, resulting in greatly reduced effects of indirect land-use change.”

Survival of the fittest

The study provides “phenomenal coverage” of how climate change could impact biodiversity, says Colin Carlson, a postdoctoral fellow at Georgetown University, who was not involved in the research. Carlson previously published a study looking at the impact of climate change on the world’s parasites. He tells Carbon Brief:

“I expect it’ll be one of the most significant papers in this discipline soon. The focus on climate change mitigation ties into a lot of hot button issues right now – not just Paris, but also alternative solutions for mitigation, like CO2 removal.”

However, the study does not include many of the factors that are key to species survival, says Prof Georgina Mace, director of the Centre for Biodiversity and Environment Research at University College London, who was not involved in the research. She tells Carbon Brief:

“For example, the presence of critical resources, such as food, prey and nest sites; extreme events, pressures from habitat loss, or changes to biotic interactions, often overwhelm climate change effects. So the range loss estimates in this paper have a lot of uncertainty that is not represented.”

The research also does not consider the possibility that some species may be able to evolve new adaptations to cope with climate change, she adds:

“The year 2100 is a long way ahead and species are continuously adapting and evolving; the strong selective pressures mean that many will adapt to deal with climate change. Over this period of time, several hundred generations for many insects, we can expect evolutionary adaptation.”

 

Warren, R. et al. (2018) The projected effect on insects, vertebrates, and plants of limiting global warming to 1.5C rather than 2C, doi/10.1126/science.aar3646



from Skeptical Science https://ift.tt/2J5NaQ0

This is a re-post from Carbon Brief by Daisy Dunne

Limiting global warming to 1.5C above pre-industrial levels rather than 2C could halve the number of vertebrate and plant species facing severe range loss by the end of the century, a study finds.

The analysis of more than 115,000 species finds that keeping warming at 1.5C – which is the aspirational target of the Paris Agreement – instead of 2C could also cut the number of insects facing severe range loss by two-thirds.

However, if countries fail to ramp up their efforts to address climate change, around a quarter of all vertebrates (animals with a spine), half of insects and 44% of plants could face severe range loss, the lead author tells Carbon Brief.

The greatest range losses are expected to occur in some of the world’s biodiversity hotspots, the author adds, including in the Amazon and southern Africa.

Although the findings are significant, the research does not explore all the factors relevant to species survival, including the impact of evolution, another scientist tells Carbon Brief.

Hostile planet

Climate change threatens wildlife in a host of ways. One way is by reducing a species’ geographical range – the extent of the area where it is able to survive.

This can occur when local temperatures become too hot for species to tolerate or when changing rainfall patterns affect the types of food available, for example. As a species’ range contracts, its risk of extinction can increase.

The new study, published in Science, uses a set of global climate models to explore how warming this century could affect the ranges of more than 115,000 species that live on land.

For the analysis, the researchers used four scenarios, including where warming is limited to, in order, 1.5C, 2C, 3.2C (which is the amount of warming anticipated if countries stick to their national pledges to cut emissions) and to 4.5C, the amount of warming expected under a “business as usual” scenario (“RCP8.5”).

The research finds that, if warming is limited to 2C, 8% of vertebrates, 18% of insects and 16% of plants could lose at least half of their current range by 2100.

However, if warming is limited to 1.5C, this risk is halved for vertebrates and plants, and cut by two-thirds for insects.

Unequal losses

The charts below show how future global warming is expected to affect the ranges of invertebrates (A), vertebrates (B) and plants (C) , and also a further breakdown of how warming could affect insects (D), mammals (E) and birds (F).

The x-axis shows temperature rise above pre-industrial levels, while the y-axis shows the proportion of species expected to lose more than half of their range.

On the charts, results for “no dispersal” (yellow) and “realistic dispersal” (blue) are shown. The “realistic dispersal” results consider the ability of animals to move away from their site of birth into new areas, explains lead author Prof Rachel Warren, a researcher of global change and environmental biology at the Tyndall Centre for Climate Change Research. She tells Carbon Brief:

“​’No dispersal’ means that we assume the animals don’t move. ‘Dispersal’ means species can move at rates they’ve been observed to move at in response to the climate change that has happened so far.”

The proportion of species expected to lose more than half of their range by 2100 under different levels of temperature rise. Results are shown for invertebrates (A), vertebrates (B), plants (C), insects (D), mammals (E) and birds (F). Source: Warren et al. (2018)

The results show how invertebrates (A), such as insects, spiders and worms, are expected to lose a larger proportion of their range than vertebrates (B), such as mammals, birds and reptiles.

Insect species at a particularly high risk include key crop pollinators, including bees, hoverflies and blowflies, the research notes. This is due to a range of factors linked to insect physiology and lifestyle, says Warren:

“It is probably because they are ectothermic, which means that their body temperature is controlled externally, not internally, as in humans. Also they have life stages – eggs, larvae, pupae, as well as adults. Each of these stages might be vulnerable to different things, such as eggs drying out if there is too little rainfall.”

BMKF99 Green Hairstreak Butterfly perched on a fern, Devon Coast, UK.

Green Hairstreak Butterfly perched on a fern, Devon Coast, UK. Credit: Steve Bloom Images/Alamy Stock Photo.

For mammals (E) and birds (F), risks remain low at 1.5C but grow significantly larger as warming increases, the research finds. Mammals most at risk include critically endangered species such as the black rhino, which also faces significant challenges from habitat loss and poaching.

Warming hotspots

The maps below show how different levels of warming could affect global species diversity for vertebrates. The charts show the proportion of species expected to remain by 2100 – from 90-100% remaining (blue) down to just 0-10% of species remaining (red) – with and without the impact of dispersal.

The proportion of vertebrate species expected to remain in world regions by 2100 under different levels of temperature rise (from top to bottom: 1.5, 2, 3.2, 4.5C). Red shows 0-10% of species remaining while dark blue shows 90-100% remaining. Source: Warren et al. (2018)

The maps reveal that, if future global warming reaches 3.2-4.5C, striking biodiversity loss could occur in some of the world’s wildlife hotspots, including southern Africa and the Amazon – which is home to 30% of the world’s species.

HNWCNF Giraffe, Giraffa camelopardalis, with Mount Kilimanjaro in the background, Chyulu Hills National Park, Kenya.

Giraffe in front of Mount Kilimanjaro, Chyulu Hills National Park, Kenya. Credit: Lucas Vallecillos/Alamy Stock Photo.

This could be because temperatures in the tropics and subtropics are relatively consistent from one season to the next, which means resident species are less used to large swings in temperature, says Warren:

“Here in the UK, we can have terrible summers and very nice ones – whereas in the tropics it’s much more predictable. This means that, in temperate lands, species are likely to be buffered against quite large natural climate variability. Whereas in the tropics, as the average climate changes, it could get quickly outside the range of natural variability that species are adapted to.”

Other regions expected to suffer species losses include Australia, the last remaining habitat of marsupials, and the high Arctic, home of the polar bear, the Arctic fox and caribou.

BECCS trade-off

The results show that meeting the Paris Agreement’s aspirational target of limiting warming to 1.5C would bring “substantial benefits” for wildlife, the scientists write in their research paper:

“Successful implementation of the Paris Agreement could lead to substantial benefits for global terrestrial [land] biodiversity…However, restricting warming to 1.5C may be difficult.”

This difficulty lies in the assumption that “negative emissions technologies” will be able to help the world meet the 1.5C target, the researchers say. Most scenarios envisaging how the world could limit warming 1.5C incorporate a negative emissions technology known as bioenergy with carbon capture and storage (BECCS).

Put simply, BECCS involves burning biomass – such as trees and crops – to generate energy and then capturing the resulting CO2 emissions before they are released into the air.

The technology has yet to be demonstrated on a commercial basis, and recent researchshows its potential may be more limited than previously thought.

Even if BECCS is developed on a wide scale, the researchers say, it could pose a significant threat to biodiversity.

That is because large scale BECCS could require up to 18% of the land surface to be converted to biomass plantations, they say, which would drive up competition for land.

This could lead to more deforestation and habitat loss to meet bioenergy and agriculture requirements, they say:

“New studies are exploring scenarios in which BECCS is produced from secondary biofuels, or in which there are dietary changes in humans, resulting in greatly reduced effects of indirect land-use change.”

Survival of the fittest

The study provides “phenomenal coverage” of how climate change could impact biodiversity, says Colin Carlson, a postdoctoral fellow at Georgetown University, who was not involved in the research. Carlson previously published a study looking at the impact of climate change on the world’s parasites. He tells Carbon Brief:

“I expect it’ll be one of the most significant papers in this discipline soon. The focus on climate change mitigation ties into a lot of hot button issues right now – not just Paris, but also alternative solutions for mitigation, like CO2 removal.”

However, the study does not include many of the factors that are key to species survival, says Prof Georgina Mace, director of the Centre for Biodiversity and Environment Research at University College London, who was not involved in the research. She tells Carbon Brief:

“For example, the presence of critical resources, such as food, prey and nest sites; extreme events, pressures from habitat loss, or changes to biotic interactions, often overwhelm climate change effects. So the range loss estimates in this paper have a lot of uncertainty that is not represented.”

The research also does not consider the possibility that some species may be able to evolve new adaptations to cope with climate change, she adds:

“The year 2100 is a long way ahead and species are continuously adapting and evolving; the strong selective pressures mean that many will adapt to deal with climate change. Over this period of time, several hundred generations for many insects, we can expect evolutionary adaptation.”

 

Warren, R. et al. (2018) The projected effect on insects, vertebrates, and plants of limiting global warming to 1.5C rather than 2C, doi/10.1126/science.aar3646



from Skeptical Science https://ift.tt/2J5NaQ0

New research, May 21-27, 2018

A selection of new climate related research articles is shown below.

Climate change mitigation

Climate change communication

Climate change as a polarizing cue: Framing effects on public support for low-carbon energy policies

"• We evaluate how framing affects support for four low-carbon energy policies among U.S. partisans.

• For Republicans, a climate change frame lowers support relative to pollution or security frames.

• We find framing effects for renewable energy, carbon tax, and fuel efficiency policies, but not nuclear power.

• No framing effects are observed among Democrats or Independents.

• Results support a motivated reasoning rather than heuristic processing mechanism."

Emission savings

Impact of cutting meat intake on hidden greenhouse gas emissions in an import-reliant city (open access)

Domestic energy consumption and climate change mitigation

Carbon footprints of grain-, forage-, and energy-based cropping systems in the North China plain

Exploring the development of electric vehicles under policy incentives: A scenario-based system dynamics model

Profiling energy efficiency tendency: A case for Turkish households

Rising wages and energy consumption transition in rural China

Framing policy on low emissions vehicles in terms of economic gains: Might the most straightforward gain be delivered by supply chain activity to support refuelling? (open access)

Climate change and the building sector: Modelling and energy implications to an office building in southern Europe

Energy production

Promises and limitations of nuclear fission energy in combating climate change

"In a strategy to eliminate all non-CCS coal power stations, some 1600 MW of nuclear power would be required and sufficient to cover the base load for the electrical energy supply system. This nuclear expansion should be accompanied by effective international safety assurances, including a mandate to stop construction of unsafe nuclear power plants. In the long term, after 2065, we expect inherently safe molten salt thorium reactors to compete with fusion reactors."

Has the relationship between non-fossil fuel energy sources and CO2 emissions changed over time? A cross-national study, 2000–2013

"Wind’s association with CO2 emissions became increasingly negative after the Great Recession (i.e., suppressed emissions at a greater rate). Nuclear’s association with CO2resembled a distorted U-shaped curve over time. Biomass’ elasticity fluctuated between positive and negative values. Solar and geothermal’s elasticity remained fairly consistent over the course of the analysis, and hydro’s elasticity increased over time but remained negative throughout the study’s temporal period."

Scarcity in abundance: The challenges of promoting energy access in the Southern African region

Insights into wind sites: Critically assessing the innovation, cost, and performance dynamics of global wind energy development

Analysis on the synergistic effect of sustainable development of coal industry under 1.5°C scenario

Palm oil supply chain complexity impedes implementation of corporate no-deforestation commitments

Expansion of nuclear power technology to new countries – SMRs, safety culture issues, and the need for an improved international safety regime

The burden of sustainability: Limits to sustainable bioenergy development in Norway

Estimating the EROI of whole systems for 100% renewable electricity supply capable of dealing with intermittency

Electricity generation technologies: Comparison of materials use, energy return on investment, jobs creation and CO2 emissions reduction

Steady state of energy: Feedbacks and leverages for promoting or preventing sustainable energy system development

The changing risk perception towards nuclear power in China after the Fukushima nuclear accident in Japan

Gone with the wind: A learning curve analysis of China's wind power industry

Explaining technological change in the US wind industry: Energy policies, technological learning, and collaboration

An information theory based robustness analysis of energy mix in US States

U.S. climate policy and the regional economics of electricity generation

Climate Policy

The global impacts of US climate policy: a model simulation using GCAM-TU and MAGICC

"Simulations by the Model for the Assessment of Greenhouse-gas Induced Climate Change (MAGICC) indicate that the temperature increase by 2100 would rise by 0.081°C–0.161°C compared to the three original RCPs (Representative Concentration Pathways) if US emissions were kept at their 2015 levels until 2100. The probability of staying below 2°C would decrease by 6–9% even if the US resumes mitigation efforts for achieving its Nationally Determined Contribution (NDC) target after 2025. It is estimated by GCAM-TU that, without US participation, increased reduction efforts are required for the rest of the world, including developing countries, in order to achieve the 2°C goal, resulting in 18% higher global cumulative mitigation costs from 2015 to 2100."

Striving for equivalency across the Alberta, British Columbia, Ontario and Québec carbon pricing systems: the Pan-Canadian carbon pricing benchmark

Can India grow and live within a 1.5 degree CO2 emissions budget?

Ecological modernization and responses for a low‐carbon future in the Gulf Cooperation Council countries

Whose carbon is burnable? Equity considerations in the allocation of a “right to extract”

The role of a low carbon fuel standard in achieving long-term GHG reduction targets

Achievability of the Paris Agreement targets in the EU: demand-side reduction potentials in a carbon budget perspective (open access)

Policy discussion for sustainable integrated electricity expansion in South Africa

Do electric vehicles need subsidies? Ownership costs for conventional, hybrid, and electric vehicles in 14 U.S. cities

Geoengineering

CESM1(WACCM) Stratospheric Aerosol Geoengineering Large Ensemble (GLENS) Project (open access)

Negative emissions: Part 1—research landscape and synthesis (open access)

Negative emissions—Part 2: Costs, potentials and side effects (open access)

Negative emissions—Part 3: Innovation and upscaling (open access)

Climate change

Temperature, precipitation, wind

Internal variability and regional climate trends in an Observational Large Ensemble

Detection of anthropogenic influence on fixed threshold indices of extreme temperature

Statistical analysis of trends in monthly precipitation at the Limbang River Basin, Sarawak (NW Borneo), Malaysia

Return times and return levels of July–September extreme rainfall over the major climatic sub-regions in Sahel

Extreme events

Rainfall–vegetation interaction regulates temperature anomalies during extreme dry events in the Horn of Africa (open access)

Hurricane Harvey Links to Ocean Heat Content and Climate Change Adaptation (open access)

Urbanization effects on heat waves in Fujian Province, Southeast China

Weathering Storms: Understanding the Impact of Natural Disasters in Central America

Forcings and feedbacks

Ocean Carbon Cycle Feedbacks Under Negative Emissions

Global Contributions of Incoming Radiation and Land Surface Conditions to Maximum Near‐Surface Air Temperature Variability and Trend (open access)

Memory of irrigation effects on hydroclimate and its modeling challenge (open access)

Cryosphere

Contrasting the Antarctic and Arctic atmospheric responses to projected sea ice loss in the late 21st Century

Atmospheric and oceanic circulation

Can the salt-advection feedback be detected in internal variability of the Atlantic Meridional Overturning Circulation?

Carbon cycle

Attributing the Carbon Cycle Impacts of CMIP5 Historical and Future Land Use and Land Cover Change in the Community Earth System Model (CESM1)

The impact of transport model differences on CO2 surface flux estimates from OCO-2 retrievals of column average CO2 (open access)

Multi-scale dynamics and environmental controls on net ecosystem CO2 exchange over a temperate semiarid shrubland

Climate change impacts

Mankind

Differences, or lack thereof, in wheat and maize yields under three low-warming scenarios (open access)

Economically robust protection against 21st century sea-level rise

Responding to multiple climate-linked stressors in a remote island context: the example of Yadua Island, Fiji (open access)

Climate variability and changes in the agricultural cycle in the Czech Lands from the sixteenth century to the present

Crop productivity changes in 1.5 °C and 2 °C worlds under climate sensitivity uncertainty (open access)

Drought and Distress in Southeastern Australia

Temporal and spatial variation in personal ambient temperatures for outdoor working populations in the southeastern USA

Biosphere

Ocean warming has a greater effect than acidification on the early life history development and swimming performance of a large circumglobal pelagic fish

Disentangling the effects of acidic air pollution, atmospheric CO2, and climate change on recent growth of red spruce trees in the Central Appalachian Mountains (open access)

Asymmetric effects of daytime and nighttime warming on spring phenology in the temperate grasslands of China

Temperature affects phenological synchrony in a tree-killing bark beetle

Scots pine radial growth response to climate and future projections at peat and mineral soils in the boreo-nemoral zone

Other papers

General climate science

SODA3: a new ocean climate reanalysis (open access)

A climatological study of air pollution potential in China

On the Identification of Ozone Recovery

Palaeoclimatology

The rise and fall of the Cretaceous Hot Greenhouse climate

Simulation of the Greenland Ice Sheet over two glacial–interglacial cycles: investigating a sub-ice-shelf melt parameterization and relative sea level forcing in an ice-sheet–ice-shelf model (open access)

How wet and dry spells evolve across the conterminous United States based on 555 years of paleoclimate data

 



from Skeptical Science https://ift.tt/2J4zG7m

A selection of new climate related research articles is shown below.

Climate change mitigation

Climate change communication

Climate change as a polarizing cue: Framing effects on public support for low-carbon energy policies

"• We evaluate how framing affects support for four low-carbon energy policies among U.S. partisans.

• For Republicans, a climate change frame lowers support relative to pollution or security frames.

• We find framing effects for renewable energy, carbon tax, and fuel efficiency policies, but not nuclear power.

• No framing effects are observed among Democrats or Independents.

• Results support a motivated reasoning rather than heuristic processing mechanism."

Emission savings

Impact of cutting meat intake on hidden greenhouse gas emissions in an import-reliant city (open access)

Domestic energy consumption and climate change mitigation

Carbon footprints of grain-, forage-, and energy-based cropping systems in the North China plain

Exploring the development of electric vehicles under policy incentives: A scenario-based system dynamics model

Profiling energy efficiency tendency: A case for Turkish households

Rising wages and energy consumption transition in rural China

Framing policy on low emissions vehicles in terms of economic gains: Might the most straightforward gain be delivered by supply chain activity to support refuelling? (open access)

Climate change and the building sector: Modelling and energy implications to an office building in southern Europe

Energy production

Promises and limitations of nuclear fission energy in combating climate change

"In a strategy to eliminate all non-CCS coal power stations, some 1600 MW of nuclear power would be required and sufficient to cover the base load for the electrical energy supply system. This nuclear expansion should be accompanied by effective international safety assurances, including a mandate to stop construction of unsafe nuclear power plants. In the long term, after 2065, we expect inherently safe molten salt thorium reactors to compete with fusion reactors."

Has the relationship between non-fossil fuel energy sources and CO2 emissions changed over time? A cross-national study, 2000–2013

"Wind’s association with CO2 emissions became increasingly negative after the Great Recession (i.e., suppressed emissions at a greater rate). Nuclear’s association with CO2resembled a distorted U-shaped curve over time. Biomass’ elasticity fluctuated between positive and negative values. Solar and geothermal’s elasticity remained fairly consistent over the course of the analysis, and hydro’s elasticity increased over time but remained negative throughout the study’s temporal period."

Scarcity in abundance: The challenges of promoting energy access in the Southern African region

Insights into wind sites: Critically assessing the innovation, cost, and performance dynamics of global wind energy development

Analysis on the synergistic effect of sustainable development of coal industry under 1.5°C scenario

Palm oil supply chain complexity impedes implementation of corporate no-deforestation commitments

Expansion of nuclear power technology to new countries – SMRs, safety culture issues, and the need for an improved international safety regime

The burden of sustainability: Limits to sustainable bioenergy development in Norway

Estimating the EROI of whole systems for 100% renewable electricity supply capable of dealing with intermittency

Electricity generation technologies: Comparison of materials use, energy return on investment, jobs creation and CO2 emissions reduction

Steady state of energy: Feedbacks and leverages for promoting or preventing sustainable energy system development

The changing risk perception towards nuclear power in China after the Fukushima nuclear accident in Japan

Gone with the wind: A learning curve analysis of China's wind power industry

Explaining technological change in the US wind industry: Energy policies, technological learning, and collaboration

An information theory based robustness analysis of energy mix in US States

U.S. climate policy and the regional economics of electricity generation

Climate Policy

The global impacts of US climate policy: a model simulation using GCAM-TU and MAGICC

"Simulations by the Model for the Assessment of Greenhouse-gas Induced Climate Change (MAGICC) indicate that the temperature increase by 2100 would rise by 0.081°C–0.161°C compared to the three original RCPs (Representative Concentration Pathways) if US emissions were kept at their 2015 levels until 2100. The probability of staying below 2°C would decrease by 6–9% even if the US resumes mitigation efforts for achieving its Nationally Determined Contribution (NDC) target after 2025. It is estimated by GCAM-TU that, without US participation, increased reduction efforts are required for the rest of the world, including developing countries, in order to achieve the 2°C goal, resulting in 18% higher global cumulative mitigation costs from 2015 to 2100."

Striving for equivalency across the Alberta, British Columbia, Ontario and Québec carbon pricing systems: the Pan-Canadian carbon pricing benchmark

Can India grow and live within a 1.5 degree CO2 emissions budget?

Ecological modernization and responses for a low‐carbon future in the Gulf Cooperation Council countries

Whose carbon is burnable? Equity considerations in the allocation of a “right to extract”

The role of a low carbon fuel standard in achieving long-term GHG reduction targets

Achievability of the Paris Agreement targets in the EU: demand-side reduction potentials in a carbon budget perspective (open access)

Policy discussion for sustainable integrated electricity expansion in South Africa

Do electric vehicles need subsidies? Ownership costs for conventional, hybrid, and electric vehicles in 14 U.S. cities

Geoengineering

CESM1(WACCM) Stratospheric Aerosol Geoengineering Large Ensemble (GLENS) Project (open access)

Negative emissions: Part 1—research landscape and synthesis (open access)

Negative emissions—Part 2: Costs, potentials and side effects (open access)

Negative emissions—Part 3: Innovation and upscaling (open access)

Climate change

Temperature, precipitation, wind

Internal variability and regional climate trends in an Observational Large Ensemble

Detection of anthropogenic influence on fixed threshold indices of extreme temperature

Statistical analysis of trends in monthly precipitation at the Limbang River Basin, Sarawak (NW Borneo), Malaysia

Return times and return levels of July–September extreme rainfall over the major climatic sub-regions in Sahel

Extreme events

Rainfall–vegetation interaction regulates temperature anomalies during extreme dry events in the Horn of Africa (open access)

Hurricane Harvey Links to Ocean Heat Content and Climate Change Adaptation (open access)

Urbanization effects on heat waves in Fujian Province, Southeast China

Weathering Storms: Understanding the Impact of Natural Disasters in Central America

Forcings and feedbacks

Ocean Carbon Cycle Feedbacks Under Negative Emissions

Global Contributions of Incoming Radiation and Land Surface Conditions to Maximum Near‐Surface Air Temperature Variability and Trend (open access)

Memory of irrigation effects on hydroclimate and its modeling challenge (open access)

Cryosphere

Contrasting the Antarctic and Arctic atmospheric responses to projected sea ice loss in the late 21st Century

Atmospheric and oceanic circulation

Can the salt-advection feedback be detected in internal variability of the Atlantic Meridional Overturning Circulation?

Carbon cycle

Attributing the Carbon Cycle Impacts of CMIP5 Historical and Future Land Use and Land Cover Change in the Community Earth System Model (CESM1)

The impact of transport model differences on CO2 surface flux estimates from OCO-2 retrievals of column average CO2 (open access)

Multi-scale dynamics and environmental controls on net ecosystem CO2 exchange over a temperate semiarid shrubland

Climate change impacts

Mankind

Differences, or lack thereof, in wheat and maize yields under three low-warming scenarios (open access)

Economically robust protection against 21st century sea-level rise

Responding to multiple climate-linked stressors in a remote island context: the example of Yadua Island, Fiji (open access)

Climate variability and changes in the agricultural cycle in the Czech Lands from the sixteenth century to the present

Crop productivity changes in 1.5 °C and 2 °C worlds under climate sensitivity uncertainty (open access)

Drought and Distress in Southeastern Australia

Temporal and spatial variation in personal ambient temperatures for outdoor working populations in the southeastern USA

Biosphere

Ocean warming has a greater effect than acidification on the early life history development and swimming performance of a large circumglobal pelagic fish

Disentangling the effects of acidic air pollution, atmospheric CO2, and climate change on recent growth of red spruce trees in the Central Appalachian Mountains (open access)

Asymmetric effects of daytime and nighttime warming on spring phenology in the temperate grasslands of China

Temperature affects phenological synchrony in a tree-killing bark beetle

Scots pine radial growth response to climate and future projections at peat and mineral soils in the boreo-nemoral zone

Other papers

General climate science

SODA3: a new ocean climate reanalysis (open access)

A climatological study of air pollution potential in China

On the Identification of Ozone Recovery

Palaeoclimatology

The rise and fall of the Cretaceous Hot Greenhouse climate

Simulation of the Greenland Ice Sheet over two glacial–interglacial cycles: investigating a sub-ice-shelf melt parameterization and relative sea level forcing in an ice-sheet–ice-shelf model (open access)

How wet and dry spells evolve across the conterminous United States based on 555 years of paleoclimate data

 



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June guide to the bright planets

Watch for the moon to sweep past both Saturn and Mars in early June 2018. Read more.

Click the name of a planet to learn more about its visibility in June 2018: Venus, Jupiter, Saturn, Mars and Mercury

Help EarthSky keep going! Please donate what you can to our annual crowd-funding campaign.

The waxing crescent moon will sweep by the planets Mercury and Venus from June 14 to 16. Read more.

Venus is the brightest planet, and it’s very prominent this month in the west after sunset. Throughout June, Venus appears as a dazzling evening “star.” Look for Venus to adorn the western evening sky until October 2018.

At mid-northern latitudes, Venus attains its highest altitude as the evening “star” in June 2018. That’s in spite of the fact that Venus’ greatest elongation (maximum angular distance from the setting sun) doesn’t occur until August 17, 2018. At mid-northern latitudes, Venus sets roughly 2 1/2 hours after the sun throughout the month.

In the Southern Hemisphere, Venus’ altitude will increase day by day all month long. At temperate latitudes in the Southern Hemisphere, Venus sets about 2 1/2 hours after the sun in early June. By the month’s end, that’ll increase to about 3 hours after sunset.

Circle June 15 and 16 on your calendar. That’s when the young moon will be sweeping past Venus in the evening sky. The western twilight will make the pairing all the more picturesque.

The moon appears much larger on our sky chart than it does in the real sky. Look for the moon close to Jupiter on June 22 and 23, and to the north of the star Antares on June 25. Read more.

Jupiter is still bright and beautiful throughout June 2018. Our planet Earth passed between the sun and Jupiter – bringing the planet to opposition – on the night of May 8-9, 2018. From anywhere around the globe, you’ll still find Jupiter in the eastern or southeastern part of the sky at nightfall – highest in the sky at early-to-mid evening – and setting in the west before dawn. Jupiter is brighter than any star, but it’s not brighter than Venus, which is in the west after sunset, while Jupiter is in the eastern half of sky.

Jupiter shines in front of the constellation Libra the Scales until November 2018. Look for Libra’s brightest stars near Jupiter, Zubenelgenubi and Zubeneschamali (both star names are pronounced with the same rhythm as Obi-Wan Kenobi, of “Star Wars”).

In any year, you can find the constellation Libra between the star Antares (to the east of Libra) and the star Spica (to the west of Libra, outside the chart). But in 2018, the planet Jupiter acts as your guide “star” to this fairly faint constellation. You’ll find Jupiter and the constellation Libra in your southern sky around midnight in May 2018, and around mid-evening in June 2018.

If you aim binoculars at Zubenelgenubi, you’ll see this star as two stars. Zubeneschamali, meanwhile, is said to appear green in color, although, astronomers say, stars can’t look green.

Let the moon guide your eye to Jupiter on the evenings of June 22 and 23.

Watch for the bright moon to swing near Saturn and then Mars from June 27-30, 2018 . Read more.

Saturn and Mars rise into the southeast sky after nightfall in early June. At the beginning of the month, Saturn rises at about the time that Venus sets; and by the month’s end, it’s Mars that rises when Venus sets. Throughout the month, Mars rises about two hours after Saturn does.

In early June, at mid-northern latitudes (U.S., Europe, Japan), Saturn rises about 9 to 10 p.m. local time (10 to 11 p.m. local daylight saving time) and Mars follows Saturn into the sky roughly two hours later. Near the month’s end, when Saturn reaches opposition on June 27, Saturn rises around sunset and Mars rises around nightfall (approximately two hours after sunset).

In early June at temperate latitudes in the Southern Hemisphere (South Africa, southern Australia, New Zealand), Saturn rises around 7 p.m. local time and Mars comes up about two hours later, around 9 p.m. local time. Near the end of the month, around the time of Saturn’s opposition, Saturn rises around sunset and Mars follows Saturn into the sky roughly two hours later.

Click here for recommended sky almanacs; they can give you the rising times of the planets.

The predawn hours before sunrise, especially in the first half of the month, might offer a better view of Saturn and Mars, as these worlds are seen much higher up in the sky than they are before midnight.

You can tell Mars from Saturn because Mars has a reddish color. Saturn looks golden. Binoculars show their colors better than the eye alone.

Early in the month, on the mornings of June 1-3, the moon is sweeping past these planets, as shown on the chart below. Then, again, at the end of the month, watch for the moon to again sweep by Saturn and Mars from June 27-29, as shown below as well.

Watch for the moon to sweep past both Saturn and Mars in early June 2018. Read more.

Watch for the bright moon to swing near Saturn and then Mars from June 27-30, 2018 . Read more.

At present, both Saturn and Mars shine more brilliantly than a 1st-magnitude star. However, Mars is brighter than Saturn. Saturn’s brilliance will increase until it peaks at its June 27 opposition, and Mars’ brilliance will also increase until it peaks at its July 27 opposition.

But Saturn’s brightness increase will be subtle, while Mars’ will be dramatic! At the beginning of June, Mars is about 3 1/2 times brighter than Saturn, whereas by the month’s end, Mars will be some 7 1/2 times brighter than the ringed planet.

It’s not often that Mars outshines Jupiter, normally the fourth-brightest celestial object to light up the sky, after the sun, moon and Venus. But, for a couple of months in 2018, Mars will outshine Jupiter from about July 7 to September 7, 2018.

Remember Mars’ historically close opposition of August 28, 2003? That year, it was closer and brighter than it had been in some 60,000 years. This upcoming July opposition will be the best since 2003.

Read more: Mars brighter in 2018 than since 2003

Click here for more about close and far Mars oppositions

Diagram by Roy L. Bishop. Copyright Royal Astronomical Society of Canada. Used with permission. Visit the RASC estore to purchase the Observer's Handbook, a necessary tool for all skywatchers.

Diagram by Roy L. Bishop. Copyright Royal Astronomical Society of Canada. Used with permission. Visit the RASC estore to purchase the Observers Handbook, a necessary tool for all skywatchers. Read more about this image.

Mercury, the innermost planet of the solar system, moves out of the morning sky and into the evening sky on June 6, 2018. However, this world probably won’t first become visible in the western evening twilight until mid-month or so, when the slim waxing crescent moon couples up with Mercury on or near June 14. More realistically, you may have till wait till the month’s end to view Mercury, when this world sets about 1 1/2 hours after sunset at mid-northern latitudes (and about 1 3/4 hours after the sun at temperate latitudes in the Southern Hemisphere).

Mercury will reach its greatest elongation from the sun on July 12, 2018, and its reign as the evening “star” will extend all the way through July 2018. If you miss seeing the moon with Mercury in mid-June, try again in mid-July.

Your chances of spotting Mercury in the western evening twilight will be much better by late June and early July 2018. Read more.

What do we mean by bright planet? By bright planet, we mean any solar system planet that is easily visible without an optical aid and that has been watched by our ancestors since time immemorial. In their outward order from the sun, the five bright planets are Mercury, Venus, Mars, Jupiter and Saturn. These planets actually do appear bright in our sky. They are typically as bright as – or brighter than – the brightest stars. Plus, these relatively nearby worlds tend to shine with a steadier light than the distant, twinkling stars. You can spot them, and come to know them as faithful friends, if you try.

Bottom line: In June 2018, at evening dusk, Venus appears in the west whereas Jupiter lords over in the eastern half of sky. In early June, Saturn rises as Venus sets; and by late June, it’ll be Mars that rises as Venus sets. Mercury may be seen in the evening sky, starting around mid-June 2018. Click here for recommended almanacs; they can help you know when the planets rise, transit and set in your sky.

Don’t miss anything. Subscribe to EarthSky News by email

Enjoy knowing where to look in the night sky? Please donate to help EarthSky keep going.

Get your EarthSky 2018 lunar calendar now, while they last.

Visit EarthSky’s Best Places to Stargaze, and recommend a place we can all enjoy.



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Watch for the moon to sweep past both Saturn and Mars in early June 2018. Read more.

Click the name of a planet to learn more about its visibility in June 2018: Venus, Jupiter, Saturn, Mars and Mercury

Help EarthSky keep going! Please donate what you can to our annual crowd-funding campaign.

The waxing crescent moon will sweep by the planets Mercury and Venus from June 14 to 16. Read more.

Venus is the brightest planet, and it’s very prominent this month in the west after sunset. Throughout June, Venus appears as a dazzling evening “star.” Look for Venus to adorn the western evening sky until October 2018.

At mid-northern latitudes, Venus attains its highest altitude as the evening “star” in June 2018. That’s in spite of the fact that Venus’ greatest elongation (maximum angular distance from the setting sun) doesn’t occur until August 17, 2018. At mid-northern latitudes, Venus sets roughly 2 1/2 hours after the sun throughout the month.

In the Southern Hemisphere, Venus’ altitude will increase day by day all month long. At temperate latitudes in the Southern Hemisphere, Venus sets about 2 1/2 hours after the sun in early June. By the month’s end, that’ll increase to about 3 hours after sunset.

Circle June 15 and 16 on your calendar. That’s when the young moon will be sweeping past Venus in the evening sky. The western twilight will make the pairing all the more picturesque.

The moon appears much larger on our sky chart than it does in the real sky. Look for the moon close to Jupiter on June 22 and 23, and to the north of the star Antares on June 25. Read more.

Jupiter is still bright and beautiful throughout June 2018. Our planet Earth passed between the sun and Jupiter – bringing the planet to opposition – on the night of May 8-9, 2018. From anywhere around the globe, you’ll still find Jupiter in the eastern or southeastern part of the sky at nightfall – highest in the sky at early-to-mid evening – and setting in the west before dawn. Jupiter is brighter than any star, but it’s not brighter than Venus, which is in the west after sunset, while Jupiter is in the eastern half of sky.

Jupiter shines in front of the constellation Libra the Scales until November 2018. Look for Libra’s brightest stars near Jupiter, Zubenelgenubi and Zubeneschamali (both star names are pronounced with the same rhythm as Obi-Wan Kenobi, of “Star Wars”).

In any year, you can find the constellation Libra between the star Antares (to the east of Libra) and the star Spica (to the west of Libra, outside the chart). But in 2018, the planet Jupiter acts as your guide “star” to this fairly faint constellation. You’ll find Jupiter and the constellation Libra in your southern sky around midnight in May 2018, and around mid-evening in June 2018.

If you aim binoculars at Zubenelgenubi, you’ll see this star as two stars. Zubeneschamali, meanwhile, is said to appear green in color, although, astronomers say, stars can’t look green.

Let the moon guide your eye to Jupiter on the evenings of June 22 and 23.

Watch for the bright moon to swing near Saturn and then Mars from June 27-30, 2018 . Read more.

Saturn and Mars rise into the southeast sky after nightfall in early June. At the beginning of the month, Saturn rises at about the time that Venus sets; and by the month’s end, it’s Mars that rises when Venus sets. Throughout the month, Mars rises about two hours after Saturn does.

In early June, at mid-northern latitudes (U.S., Europe, Japan), Saturn rises about 9 to 10 p.m. local time (10 to 11 p.m. local daylight saving time) and Mars follows Saturn into the sky roughly two hours later. Near the month’s end, when Saturn reaches opposition on June 27, Saturn rises around sunset and Mars rises around nightfall (approximately two hours after sunset).

In early June at temperate latitudes in the Southern Hemisphere (South Africa, southern Australia, New Zealand), Saturn rises around 7 p.m. local time and Mars comes up about two hours later, around 9 p.m. local time. Near the end of the month, around the time of Saturn’s opposition, Saturn rises around sunset and Mars follows Saturn into the sky roughly two hours later.

Click here for recommended sky almanacs; they can give you the rising times of the planets.

The predawn hours before sunrise, especially in the first half of the month, might offer a better view of Saturn and Mars, as these worlds are seen much higher up in the sky than they are before midnight.

You can tell Mars from Saturn because Mars has a reddish color. Saturn looks golden. Binoculars show their colors better than the eye alone.

Early in the month, on the mornings of June 1-3, the moon is sweeping past these planets, as shown on the chart below. Then, again, at the end of the month, watch for the moon to again sweep by Saturn and Mars from June 27-29, as shown below as well.

Watch for the moon to sweep past both Saturn and Mars in early June 2018. Read more.

Watch for the bright moon to swing near Saturn and then Mars from June 27-30, 2018 . Read more.

At present, both Saturn and Mars shine more brilliantly than a 1st-magnitude star. However, Mars is brighter than Saturn. Saturn’s brilliance will increase until it peaks at its June 27 opposition, and Mars’ brilliance will also increase until it peaks at its July 27 opposition.

But Saturn’s brightness increase will be subtle, while Mars’ will be dramatic! At the beginning of June, Mars is about 3 1/2 times brighter than Saturn, whereas by the month’s end, Mars will be some 7 1/2 times brighter than the ringed planet.

It’s not often that Mars outshines Jupiter, normally the fourth-brightest celestial object to light up the sky, after the sun, moon and Venus. But, for a couple of months in 2018, Mars will outshine Jupiter from about July 7 to September 7, 2018.

Remember Mars’ historically close opposition of August 28, 2003? That year, it was closer and brighter than it had been in some 60,000 years. This upcoming July opposition will be the best since 2003.

Read more: Mars brighter in 2018 than since 2003

Click here for more about close and far Mars oppositions

Diagram by Roy L. Bishop. Copyright Royal Astronomical Society of Canada. Used with permission. Visit the RASC estore to purchase the Observer's Handbook, a necessary tool for all skywatchers.

Diagram by Roy L. Bishop. Copyright Royal Astronomical Society of Canada. Used with permission. Visit the RASC estore to purchase the Observers Handbook, a necessary tool for all skywatchers. Read more about this image.

Mercury, the innermost planet of the solar system, moves out of the morning sky and into the evening sky on June 6, 2018. However, this world probably won’t first become visible in the western evening twilight until mid-month or so, when the slim waxing crescent moon couples up with Mercury on or near June 14. More realistically, you may have till wait till the month’s end to view Mercury, when this world sets about 1 1/2 hours after sunset at mid-northern latitudes (and about 1 3/4 hours after the sun at temperate latitudes in the Southern Hemisphere).

Mercury will reach its greatest elongation from the sun on July 12, 2018, and its reign as the evening “star” will extend all the way through July 2018. If you miss seeing the moon with Mercury in mid-June, try again in mid-July.

Your chances of spotting Mercury in the western evening twilight will be much better by late June and early July 2018. Read more.

What do we mean by bright planet? By bright planet, we mean any solar system planet that is easily visible without an optical aid and that has been watched by our ancestors since time immemorial. In their outward order from the sun, the five bright planets are Mercury, Venus, Mars, Jupiter and Saturn. These planets actually do appear bright in our sky. They are typically as bright as – or brighter than – the brightest stars. Plus, these relatively nearby worlds tend to shine with a steadier light than the distant, twinkling stars. You can spot them, and come to know them as faithful friends, if you try.

Bottom line: In June 2018, at evening dusk, Venus appears in the west whereas Jupiter lords over in the eastern half of sky. In early June, Saturn rises as Venus sets; and by late June, it’ll be Mars that rises as Venus sets. Mercury may be seen in the evening sky, starting around mid-June 2018. Click here for recommended almanacs; they can help you know when the planets rise, transit and set in your sky.

Don’t miss anything. Subscribe to EarthSky News by email

Enjoy knowing where to look in the night sky? Please donate to help EarthSky keep going.

Get your EarthSky 2018 lunar calendar now, while they last.

Visit EarthSky’s Best Places to Stargaze, and recommend a place we can all enjoy.



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2018 Atlantic hurricane season outlook

Help EarthSky keep going! Please donate what you can to our annual crowd-funding campaign.

The 2018 Atlantic hurricane season starts today (June 1) and runs through November 30. Last week (May 24, 2018) NOAA released its annual hurricane season outlook. Scientists at NOAA’s Climate Prediction Center are forecasting a 75-percent chance that the 2018 Atlantic hurricane season will be near- or above-normal.

Two of the factors driving this outlook are the possibility of a weak El Niño developing, along with near-average sea surface temperatures across the tropical Atlantic Ocean and Caribbean Sea. These factors, says the report,

.. are set upon a backdrop of atmospheric and oceanic conditions that are conducive to hurricane development and have been producing stronger Atlantic hurricane seasons since 1995.

NOAA will update the 2018 Atlantic seasonal outlook in early August, just prior to the peak of the season.

Infrared satellite image of Hurricane Harvey on August 25, 2017. Image via NOAA.

More specifically, the NOA forecasters predict a 35 percent chance of an above-normal season, a 40 percent chance of a near-normal season, and a 25 percent chance of a below-normal season for this hurricane season.

Hurricane season probability and numbers of named storms: NOAA’s forecasters predict a 70 percent likelihood of 10 to 16 named storms (winds of 39 mph or higher), of which 5 to 9 could become hurricanes (winds of 74 mph or higher), including 1 to 4 major hurricanes (category 3, 4 or 5; with winds of 111 mph or higher). An average hurricane season produces 12 named storms, of which 6 become hurricanes, including 3 major hurricanes. Image via NOAA.

Image via NOAA.

Bottom line: NOAA’s outlook for the 2018 Atlantic hurricane season.

Read more from NOAA.

Help EarthSky keep going! Please donate what you can to our annual crowd-funding campaign.



from EarthSky https://ift.tt/2J9Z5bS

Help EarthSky keep going! Please donate what you can to our annual crowd-funding campaign.

The 2018 Atlantic hurricane season starts today (June 1) and runs through November 30. Last week (May 24, 2018) NOAA released its annual hurricane season outlook. Scientists at NOAA’s Climate Prediction Center are forecasting a 75-percent chance that the 2018 Atlantic hurricane season will be near- or above-normal.

Two of the factors driving this outlook are the possibility of a weak El Niño developing, along with near-average sea surface temperatures across the tropical Atlantic Ocean and Caribbean Sea. These factors, says the report,

.. are set upon a backdrop of atmospheric and oceanic conditions that are conducive to hurricane development and have been producing stronger Atlantic hurricane seasons since 1995.

NOAA will update the 2018 Atlantic seasonal outlook in early August, just prior to the peak of the season.

Infrared satellite image of Hurricane Harvey on August 25, 2017. Image via NOAA.

More specifically, the NOA forecasters predict a 35 percent chance of an above-normal season, a 40 percent chance of a near-normal season, and a 25 percent chance of a below-normal season for this hurricane season.

Hurricane season probability and numbers of named storms: NOAA’s forecasters predict a 70 percent likelihood of 10 to 16 named storms (winds of 39 mph or higher), of which 5 to 9 could become hurricanes (winds of 74 mph or higher), including 1 to 4 major hurricanes (category 3, 4 or 5; with winds of 111 mph or higher). An average hurricane season produces 12 named storms, of which 6 become hurricanes, including 3 major hurricanes. Image via NOAA.

Image via NOAA.

Bottom line: NOAA’s outlook for the 2018 Atlantic hurricane season.

Read more from NOAA.

Help EarthSky keep going! Please donate what you can to our annual crowd-funding campaign.



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2017’s costliest hurricanes

Hurricane Harvey at peak intensity – August 25, 2017 – near the coast of Texas. Image via RAMMB-slider.

Meteorologists describe 2017’s hurricane season as hyperactive. It was the costliest Atlantic hurricane season on record, displacing the former record holder, 2005. Nearly all the damage was due to 3 storms – Harvey, Irma, and Maria – which together caused at least $282.16 billion (USD) in damages.

The first of these three monster storms was Hurricane Harvey. It was the eighth named storm, third hurricane, and the first major hurricane of the extremely active 2017 Atlantic hurricane season. Harvey is tied with Hurricane Katrina as the costliest tropical cyclone on record. Much of its damage came from flooding triggered by rainfall in the Houston metropolitan area. According to Popular Science on December 14, 2017, between 24 trillion and 34 trillion gallons of water fell on the Gulf Coast during Harvey, equivalent to the amount of water melted off the West Antarctic Ice Shelf in a single year. Harvey’s floods displaced more than 30,000 people and prompted more than 17,000 rescues. The Texas Tribune said on October 13, 2017, that there were 88 deaths from Harvey, 62 caused by wind, rain and floods (which led to drownings or trees falling on people) and 26 deaths from “unsafe or unhealthy conditions” related to the loss or disruption of services such as utilities, transportation and medical care.

Hurricane Irma at peak intensity – September 5, 2017 – approaching the Leeward Islands. Image via EOSDIS Worldview.

Coming directly after Harvey, Hurricane Irma was the ninth named storm, fourth hurricane, second major hurricane and first Category 5 hurricane of the 2017 Atlantic hurricane season. According to Google, Hurricane Irma was the No. 1 top trending search term of 2017. That’s because Irma had incredibly strong winds, the strongest maximum sustained winds seen in the Atlantic since 2005’s Wilma (which was the most intense tropical cyclone ever recorded in the Atlantic). Irma was the first Category 5 hurricane on record to strike the Leeward Islands in the Caribbean Sea. It became the second-costliest Caribbean hurricane on record, after Maria (see below). It was also the most intense hurricane to strike the continental U.S. since Katrina in 2005, the first major hurricane to make landfall in Florida since Wilma in 2005, and the first Category 4 hurricane to strike the state since Charley in 2004. Wikipedia lists 134 deaths (49 direct, 85 indirect) from Irma.

Hurricane Maria near peak intensity – September 19, 2017 – moving north towards Puerto Rico. Image via The Naval Research Lab/ NOAA.

Coming two weeks after Irma, Hurricane Maria was the thirteenth named storm, eighth consecutive hurricane, fourth major hurricane, second Category 5 hurricane, and the deadliest storm of the hyperactive 2017 Atlantic hurricane season. It’s now regarded as the worst natural disaster on record for Dominica and Puerto Rico. In Puerto Rico, electricity was cut off to 100 percent of the island, and access to clean water and food became limited for most. For months, most families and businesses remained without power, cell phone service was limited, and clean water, food, medicine and fuel were all in very short supply. Less than half of residents had their power restored two months after the storm had passed, and, even today, some communities still have a “boil water” advisory in place. Official estimates originally placed the number of dead at 64. But a new Harvard study – published in late May 2018 in the peer-reviewed New England Journal of Medicine – estimates that at least 4,645 deaths can be linked to the hurricane and its immediate aftermath, making the storm far deadlier than previously thought. Read about the new study in the Washington Post.

In all, 2017 had 17 named storms, 10 hurricanes and 6 major hurricanes. The 2017 season ranks alongside 1936 as the fifth-most active season. 2017 is also one of only six years on record to feature multiple Category 5 hurricanes. It’s the second after 2007 to feature two hurricanes making landfall at that intensity.

Hurricane season for 2018 begins June 1 and ends November 30.

Bottom line: 2017’s hurricane season was the costliest on record, with nearly all the damage due to 3 storms – Harvey, Irma, and Maria.



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Hurricane Harvey at peak intensity – August 25, 2017 – near the coast of Texas. Image via RAMMB-slider.

Meteorologists describe 2017’s hurricane season as hyperactive. It was the costliest Atlantic hurricane season on record, displacing the former record holder, 2005. Nearly all the damage was due to 3 storms – Harvey, Irma, and Maria – which together caused at least $282.16 billion (USD) in damages.

The first of these three monster storms was Hurricane Harvey. It was the eighth named storm, third hurricane, and the first major hurricane of the extremely active 2017 Atlantic hurricane season. Harvey is tied with Hurricane Katrina as the costliest tropical cyclone on record. Much of its damage came from flooding triggered by rainfall in the Houston metropolitan area. According to Popular Science on December 14, 2017, between 24 trillion and 34 trillion gallons of water fell on the Gulf Coast during Harvey, equivalent to the amount of water melted off the West Antarctic Ice Shelf in a single year. Harvey’s floods displaced more than 30,000 people and prompted more than 17,000 rescues. The Texas Tribune said on October 13, 2017, that there were 88 deaths from Harvey, 62 caused by wind, rain and floods (which led to drownings or trees falling on people) and 26 deaths from “unsafe or unhealthy conditions” related to the loss or disruption of services such as utilities, transportation and medical care.

Hurricane Irma at peak intensity – September 5, 2017 – approaching the Leeward Islands. Image via EOSDIS Worldview.

Coming directly after Harvey, Hurricane Irma was the ninth named storm, fourth hurricane, second major hurricane and first Category 5 hurricane of the 2017 Atlantic hurricane season. According to Google, Hurricane Irma was the No. 1 top trending search term of 2017. That’s because Irma had incredibly strong winds, the strongest maximum sustained winds seen in the Atlantic since 2005’s Wilma (which was the most intense tropical cyclone ever recorded in the Atlantic). Irma was the first Category 5 hurricane on record to strike the Leeward Islands in the Caribbean Sea. It became the second-costliest Caribbean hurricane on record, after Maria (see below). It was also the most intense hurricane to strike the continental U.S. since Katrina in 2005, the first major hurricane to make landfall in Florida since Wilma in 2005, and the first Category 4 hurricane to strike the state since Charley in 2004. Wikipedia lists 134 deaths (49 direct, 85 indirect) from Irma.

Hurricane Maria near peak intensity – September 19, 2017 – moving north towards Puerto Rico. Image via The Naval Research Lab/ NOAA.

Coming two weeks after Irma, Hurricane Maria was the thirteenth named storm, eighth consecutive hurricane, fourth major hurricane, second Category 5 hurricane, and the deadliest storm of the hyperactive 2017 Atlantic hurricane season. It’s now regarded as the worst natural disaster on record for Dominica and Puerto Rico. In Puerto Rico, electricity was cut off to 100 percent of the island, and access to clean water and food became limited for most. For months, most families and businesses remained without power, cell phone service was limited, and clean water, food, medicine and fuel were all in very short supply. Less than half of residents had their power restored two months after the storm had passed, and, even today, some communities still have a “boil water” advisory in place. Official estimates originally placed the number of dead at 64. But a new Harvard study – published in late May 2018 in the peer-reviewed New England Journal of Medicine – estimates that at least 4,645 deaths can be linked to the hurricane and its immediate aftermath, making the storm far deadlier than previously thought. Read about the new study in the Washington Post.

In all, 2017 had 17 named storms, 10 hurricanes and 6 major hurricanes. The 2017 season ranks alongside 1936 as the fifth-most active season. 2017 is also one of only six years on record to feature multiple Category 5 hurricanes. It’s the second after 2007 to feature two hurricanes making landfall at that intensity.

Hurricane season for 2018 begins June 1 and ends November 30.

Bottom line: 2017’s hurricane season was the costliest on record, with nearly all the damage due to 3 storms – Harvey, Irma, and Maria.



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Are you prepared for a hurricane?

In 2012, Hurricane Sandy destroyed this house in Jersey Shore, New Jersey. Image via Shayna Marie Meyer

In 2012, Hurricane Sandy destroyed this house in Jersey Shore, New Jersey. Sandy was the 2nd-costliest hurricane on record in the U.S. until 2017, when both Harvey and Maria surpassed it. Image via Shayna Marie Meyer.

June 1 is the start of the Atlantic hurricane season each year. The season ends on November 30. No one can predict exactly how many hurricanes we’ll get in a season, or how powerful they’ll be. Last year’s hurricane season was unusually intense. In 2018, scientists at NOAA’s Climate Prediction Center are forecasting a 75-percent chance for an Atlantic hurricane season that’s near- or above-normal, thanks in part to a weak El Niño. In the Eastern Caribbean and along the U.S. East Coast, the season tends to be busiest between mid-August and mid-September. Now, early in the season, is the time to make a plan to stay safe if a hurricane approaches your area. 

If you live along the U.S. East Coast or Gulf of Mexico – and don’t have a plan – I hope this post will prepare you. Sit down with your family and figure something out, now. 

This week’s fund-raising has been awesome. We’re so grateful. Please donate what you can to our annual crowd-funding campaign.

Be prepared. Image via National Hurricane Center.

How to create a supply kit. According to the National Hurricane Center, your family should have a supply kit. The kit includes:

  • One gallon of water per person daily for up to a week.
  • Food for a week.  Canned food and juices work really well.  Make sure you have a manual can opener and other utensils needed for cooking food.
  • Blankets and pillows
  • Clothing (including clothing that is water resistant)
  • First aid kit, medications, prescription drugs
  • Toiletries, hygiene items, moisture wipes, hand sanitizer and soap
  • Flashlight and batteries
  • NOAA weather radio
  • Cash, because debit and credit cards might not work
  • Full tank of gas/extra gasoline
  • Pet care items such as food, water, muzzle, leash, and a cage.
  • Charged cellphone
  • Matches or lighter
  • If you have babies, make sure you have a decent supply of baby food, diapers, etc.

Also, if you live along the coast, make sure you have the supplies (such as plywood) to board up windows to protect your house. Get plywood now instead of 2-3 days before a storm hits.

Figure out what needs to be taken inside in case floods or strong winds pick up any of your belongings.

Develop an evacuation plan now.

If a hurricane is imminent … First, understand the difference between watches and warnings. Hurricane watches mean hurricane conditions (74 mile per hour winds or greater) are possible within 48 hours. Hurricane warnings means hurricane conditions are expected. If a hurricane is imminent …

Turn down your freezer and refrigerator to the coldest settings possible. If you lose electricity, your perishable foods will last longer.

Turn off propane tanks and small electrical appliances.

Consider whether you really want to stay at your house. The worst damage from hurricanes usually comes from storm surge and flooding. However, stronger hurricanes can produce violent winds that can cause damage to buildings and structures. Also, tropical systems are capable of producing small tornadoes. Do you want all of these possible impacts to threaten you and your family?

Pay careful attention to hurricane forecasts.  Sometimes, Mother Nature can be unpredictable.  A forecast Category One hurricane could end up being a strong Category Two, causing more damage than predicted.  If you see hurricane watches or warnings for your area, that should be enough to influence you to leave.  Do you have relatives that you can visit?  Don’t be a brave soul and weather out the storm.

Galveston, Texas. Hurricane of 1900. Image via NOAA

More links and other things to consider. Is your house in an area prone to flooding? If so, do you have flood insurance for your house?  Check out Floodsmart.gov if you do not have flood insurance.

How does your community prepare for a hurricane? Is there a certain procedure the city follows in case of an evacuation?

The Red Cross has more information about being prepared for a hurricane.

The National Hurricane Center also has excellent information about hurricane preparedness and safety.

Meteorologists’ main goal is to not only accurately forecast the weather, but to protect lives. They offer watches and warnings to prepare the public for life-threatening storms. Please do not ignore watches or warnings! Take every storm seriously. Hope for the best, but expect the worst.

Bottom line: June 1 is the start of the 2018 hurricane season. Are you prepared for a hurricane if one approaches your area? If you live along the Gulf of Mexico or East Coast and don’t have a plan, this post can help you prepare.

Hurricane Survival Tips: How to Stay Safe During a Hurricane

9 Affordable Ways to Prep Your Home for Hurricane Season

Disaster Preparedness for Pets

Enjoying EarthSky? Sign up for our free daily newsletter today!



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In 2012, Hurricane Sandy destroyed this house in Jersey Shore, New Jersey. Image via Shayna Marie Meyer

In 2012, Hurricane Sandy destroyed this house in Jersey Shore, New Jersey. Sandy was the 2nd-costliest hurricane on record in the U.S. until 2017, when both Harvey and Maria surpassed it. Image via Shayna Marie Meyer.

June 1 is the start of the Atlantic hurricane season each year. The season ends on November 30. No one can predict exactly how many hurricanes we’ll get in a season, or how powerful they’ll be. Last year’s hurricane season was unusually intense. In 2018, scientists at NOAA’s Climate Prediction Center are forecasting a 75-percent chance for an Atlantic hurricane season that’s near- or above-normal, thanks in part to a weak El Niño. In the Eastern Caribbean and along the U.S. East Coast, the season tends to be busiest between mid-August and mid-September. Now, early in the season, is the time to make a plan to stay safe if a hurricane approaches your area. 

If you live along the U.S. East Coast or Gulf of Mexico – and don’t have a plan – I hope this post will prepare you. Sit down with your family and figure something out, now. 

This week’s fund-raising has been awesome. We’re so grateful. Please donate what you can to our annual crowd-funding campaign.

Be prepared. Image via National Hurricane Center.

How to create a supply kit. According to the National Hurricane Center, your family should have a supply kit. The kit includes:

  • One gallon of water per person daily for up to a week.
  • Food for a week.  Canned food and juices work really well.  Make sure you have a manual can opener and other utensils needed for cooking food.
  • Blankets and pillows
  • Clothing (including clothing that is water resistant)
  • First aid kit, medications, prescription drugs
  • Toiletries, hygiene items, moisture wipes, hand sanitizer and soap
  • Flashlight and batteries
  • NOAA weather radio
  • Cash, because debit and credit cards might not work
  • Full tank of gas/extra gasoline
  • Pet care items such as food, water, muzzle, leash, and a cage.
  • Charged cellphone
  • Matches or lighter
  • If you have babies, make sure you have a decent supply of baby food, diapers, etc.

Also, if you live along the coast, make sure you have the supplies (such as plywood) to board up windows to protect your house. Get plywood now instead of 2-3 days before a storm hits.

Figure out what needs to be taken inside in case floods or strong winds pick up any of your belongings.

Develop an evacuation plan now.

If a hurricane is imminent … First, understand the difference between watches and warnings. Hurricane watches mean hurricane conditions (74 mile per hour winds or greater) are possible within 48 hours. Hurricane warnings means hurricane conditions are expected. If a hurricane is imminent …

Turn down your freezer and refrigerator to the coldest settings possible. If you lose electricity, your perishable foods will last longer.

Turn off propane tanks and small electrical appliances.

Consider whether you really want to stay at your house. The worst damage from hurricanes usually comes from storm surge and flooding. However, stronger hurricanes can produce violent winds that can cause damage to buildings and structures. Also, tropical systems are capable of producing small tornadoes. Do you want all of these possible impacts to threaten you and your family?

Pay careful attention to hurricane forecasts.  Sometimes, Mother Nature can be unpredictable.  A forecast Category One hurricane could end up being a strong Category Two, causing more damage than predicted.  If you see hurricane watches or warnings for your area, that should be enough to influence you to leave.  Do you have relatives that you can visit?  Don’t be a brave soul and weather out the storm.

Galveston, Texas. Hurricane of 1900. Image via NOAA

More links and other things to consider. Is your house in an area prone to flooding? If so, do you have flood insurance for your house?  Check out Floodsmart.gov if you do not have flood insurance.

How does your community prepare for a hurricane? Is there a certain procedure the city follows in case of an evacuation?

The Red Cross has more information about being prepared for a hurricane.

The National Hurricane Center also has excellent information about hurricane preparedness and safety.

Meteorologists’ main goal is to not only accurately forecast the weather, but to protect lives. They offer watches and warnings to prepare the public for life-threatening storms. Please do not ignore watches or warnings! Take every storm seriously. Hope for the best, but expect the worst.

Bottom line: June 1 is the start of the 2018 hurricane season. Are you prepared for a hurricane if one approaches your area? If you live along the Gulf of Mexico or East Coast and don’t have a plan, this post can help you prepare.

Hurricane Survival Tips: How to Stay Safe During a Hurricane

9 Affordable Ways to Prep Your Home for Hurricane Season

Disaster Preparedness for Pets

Enjoying EarthSky? Sign up for our free daily newsletter today!



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Moon, Saturn, Mars before dawn June 1-3

Before daybreak on June 1 to 3, watch for the moon near Mars and Saturn. Because the moon moves eastward in front of the constellations of the zodiac at the rate of about 1/2 degree (one moon-diameter) per hour, or about 13 degrees per day, look for the moon to change its position from day to day. It’ll be closest to Saturn on the morning of June 1, approximately between Saturn and Mars on June 2, and closest to Mars on June 3.

Help EarthSky keep going! Please donate what you can to our annual crowd-funding campaign.

If you’re a night owl, staying up past the midnight hour, you might also catch Mars beneath the moon and Saturn before your bedtime. However, Mars is still rising late at night. It’s low in the east as seen from around the globe in the wee hours. The predawn hours present a better view of the moon, Saturn and Mars, at which time all these worlds will shine higher in the sky.

At present, Saturn lodges in front of the constellation Sagittarius the Archer. Meanwhile, Mars beams in front of the constellation Capricornus the Seagoat. Although Saturn will remain in front of Sagittarius for the rest of the year, Mars will stay in front of Capricornus only until November 2018. Because these two worlds will shine so brightly and beautifully in our sky for many months to come, you can use them to locate these two constellations of the zodiac.

This year, in 2018, you can use the planet Saturn, which shines as brilliantly as a 1st-magnitude star, to locate “The Teapot” and the constellation Scutum the Shield. The Teapot makes up the western half of the constellation Sagittarius the Archer.

The constellation Capricornus has the shape of an arrowhead. Image via AlltheSky.

There are a couple ways to distinguish Saturn from Mars. A telescope – even a modest backyard variety – will show you that Saturn has glorious rings whereas Mars does not. Want to see Saturn’s rings? Read this first.

No telescope? No problem. Notice with your unaided eye that Saturn appears golden in color while Mars exhibits a reddish hue. Also, Mars is now the brighter planet, and it’s soon to be much, much brighter. Mars will remain brighter than Saturn for the rest of 2018.

Opposition happens when Earth flies between an outer planet, like Jupiter, and the sun. This happens yearly for most of the outer planets (except Mars). Illustration via Heavens Above.

In the relatively near future, Saturn and Mars will be at their brightest for 2018, and in Mars’ case its brightest for some years. Saturn will reach opposition – when Earth will fly between this outer planet and the sun – on June 27, 2018. Opposition marks the middle of the best time of year to see an outer planet, like Saturn or Mars. That’s when these planets shine at their brightest best for the year and stay out all night long.

Mars will reach its opposition one month later, on July 27, 2018. This is a very special opposition of Mars. The planet will be brighter around late July than it’s been since 2003, when it was brighter than it had been in some 60,000 years!

Mars is closest to Earth about every 2 years, when Earth passes between this planet and the sun. That event is called Mars’ opposition because, at such times, Mars appears opposite the sun in our sky. There’s also a 15-year cycle of close and far Mars oppositions, and that’s what this chart is showing. Notice that, in 2018, Mars will be especially close. The reason is that Mars’ opposition is July 27 and its perihelion – when it’s closest to the sun is relatively soon afterwards, on September 16. In 2018, Mars will be closer and brighter than it’s been since 2003. Diagram by Roy L. Bishop. Copyright Royal Astronomical Society of Canada. Used with permission. Visit the RASC estore to purchase the Observer’s Handbook, a necessary tool for all skywatchers.

Bottom line: Use the waning gibbous moon to locate the planets Saturn and Mars before daybreak on the mornings of June 1 to 3, 2018.

Help EarthSky keep going! Please donate what you can to our annual crowd-funding campaign.



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Before daybreak on June 1 to 3, watch for the moon near Mars and Saturn. Because the moon moves eastward in front of the constellations of the zodiac at the rate of about 1/2 degree (one moon-diameter) per hour, or about 13 degrees per day, look for the moon to change its position from day to day. It’ll be closest to Saturn on the morning of June 1, approximately between Saturn and Mars on June 2, and closest to Mars on June 3.

Help EarthSky keep going! Please donate what you can to our annual crowd-funding campaign.

If you’re a night owl, staying up past the midnight hour, you might also catch Mars beneath the moon and Saturn before your bedtime. However, Mars is still rising late at night. It’s low in the east as seen from around the globe in the wee hours. The predawn hours present a better view of the moon, Saturn and Mars, at which time all these worlds will shine higher in the sky.

At present, Saturn lodges in front of the constellation Sagittarius the Archer. Meanwhile, Mars beams in front of the constellation Capricornus the Seagoat. Although Saturn will remain in front of Sagittarius for the rest of the year, Mars will stay in front of Capricornus only until November 2018. Because these two worlds will shine so brightly and beautifully in our sky for many months to come, you can use them to locate these two constellations of the zodiac.

This year, in 2018, you can use the planet Saturn, which shines as brilliantly as a 1st-magnitude star, to locate “The Teapot” and the constellation Scutum the Shield. The Teapot makes up the western half of the constellation Sagittarius the Archer.

The constellation Capricornus has the shape of an arrowhead. Image via AlltheSky.

There are a couple ways to distinguish Saturn from Mars. A telescope – even a modest backyard variety – will show you that Saturn has glorious rings whereas Mars does not. Want to see Saturn’s rings? Read this first.

No telescope? No problem. Notice with your unaided eye that Saturn appears golden in color while Mars exhibits a reddish hue. Also, Mars is now the brighter planet, and it’s soon to be much, much brighter. Mars will remain brighter than Saturn for the rest of 2018.

Opposition happens when Earth flies between an outer planet, like Jupiter, and the sun. This happens yearly for most of the outer planets (except Mars). Illustration via Heavens Above.

In the relatively near future, Saturn and Mars will be at their brightest for 2018, and in Mars’ case its brightest for some years. Saturn will reach opposition – when Earth will fly between this outer planet and the sun – on June 27, 2018. Opposition marks the middle of the best time of year to see an outer planet, like Saturn or Mars. That’s when these planets shine at their brightest best for the year and stay out all night long.

Mars will reach its opposition one month later, on July 27, 2018. This is a very special opposition of Mars. The planet will be brighter around late July than it’s been since 2003, when it was brighter than it had been in some 60,000 years!

Mars is closest to Earth about every 2 years, when Earth passes between this planet and the sun. That event is called Mars’ opposition because, at such times, Mars appears opposite the sun in our sky. There’s also a 15-year cycle of close and far Mars oppositions, and that’s what this chart is showing. Notice that, in 2018, Mars will be especially close. The reason is that Mars’ opposition is July 27 and its perihelion – when it’s closest to the sun is relatively soon afterwards, on September 16. In 2018, Mars will be closer and brighter than it’s been since 2003. Diagram by Roy L. Bishop. Copyright Royal Astronomical Society of Canada. Used with permission. Visit the RASC estore to purchase the Observer’s Handbook, a necessary tool for all skywatchers.

Bottom line: Use the waning gibbous moon to locate the planets Saturn and Mars before daybreak on the mornings of June 1 to 3, 2018.

Help EarthSky keep going! Please donate what you can to our annual crowd-funding campaign.



from EarthSky https://ift.tt/2LKG80Z