08/03/2018

Climate Change 'Impacts Women More Than Men'

BBC - Mary Halton

Over 70% of those displaced by flooding in Pakistan in 2010 were women and children. Getty Images
Women are more likely than men to be affected by climate change, studies show.
UN figures indicate that 80% of people displaced by climate change are women.
Roles as primary caregivers and providers of food and fuel make them more vulnerable when flooding and drought occur.
The 2015 Paris Agreement has made specific provision for the empowerment of women, recognising that they are disproportionately impacted.
Millions in Nigeria, Cameroon, Chad, Niger and the Central African Republic rely on Lake Chad. Getty Images
In central Africa, where up to 90% of Lake Chad has disappeared, nomadic indigenous groups are particularly at risk. As the lake's shoreline recedes, women have to walk much further to collect water.
"In the dry season, men go to the towns... leaving women to look after the community," explains Hindou Oumarou Ibrahim, coordinator of the Association of Indigenous Women and People of Chad (AFPAT).
With dry seasons now becoming longer, women are working harder to feed and care for their families without support. "They become more vulnerable... it's very hard work," Ibrahim recently told the BBC's 100 Women initiative.

A global problem
It is not just women in rural areas who are affected. Globally, women are more likely to experience poverty, and to have less socioeconomic power than men. This makes it difficult to recover from disasters which affect infrastructure, jobs and housing.
Shanika Reaux with her baby Tatiana were displaced by Hurricane Katrina. Getty Images
After Hurricane Katrina in 2005, African American women were among the worst affected by flooding in Louisiana. As sea levels rise, low-lying cities like New Orleans will be increasingly at risk.
"In New Orleans, there was much higher poverty among the African American population before Katrina," says Jacquelyn Litt, professor of women's and gender studies at Rutgers University.
"More than half the poor families in the city were headed by single mothers," she told BBC News.
"[They] are reliant on interdependent community networks for their everyday survival and resources. The displacement that happened after Katrina essentially eroded those networks. It places women and their children at much greater risk."
In the immediate aftermath of extreme events, emergency shelters can be inadequately equipped to support women. The Superdome, in which evacuees were temporarily housed after Hurricane Katrina, didn't have enough sanitary products for the women accommodated there.
Katrina impact: Women and children waiting to be evacuated outside the New Orleans Superdome. Getty Images
Increased incidences of violence against women, including sexual assault and rape, have also been documented in the wake of disasters.

'Natural' disasters?
Much as climate change is accelerated by human behaviours, the impact of weather and climate events is influenced by societal structures. Disasters do not affect all people equally.
In the wake of the 2004 tsunami, an Oxfam report found that surviving men outnumbered women by almost 3:1 in Sri Lanka, Indonesia and India.
While no one cause was clear, there were similar patterns across the region. Men were more likely to be able to swim, and women lost precious evacuation time trying to look after children and other relatives.
Another study spanning 20 years noted that catastrophic events lowered women's life expectancy more than men; more women were being killed, or they were being killed younger. In countries where women had greater socioeconomic power, the difference reduced.

Half the world
In recognition of this vast disparity, governments and organisations working on climate change are gradually moving to include women's voices in policy and planning.
Women farmers in Durban protesting the impact of climate change on their livelihoods. Getty Images
The UN has highlighted the need for gender sensitive responses to the impacts of climate change, yet the average representation of women in national and global climate negotiating bodies is below 30%.
The numbers don't improve at the local level.
"Women are often not involved in the decisions made about the responses to climate change, so the money ends up going to the men rather than the women," environmental scientist Diana Liverman told the BBC's Science in Action programme on the World Service this week.
As an author for the Intergovernmental Panel on Climate Change (IPCC), whose reports influence climate change policy, Liverman has been monitoring the numbers of women involved.
Twenty-five percent of those nominated to participate in the next report are women. "IPCC has been very receptive to this and is actually discussing how they can support women better," explains Liverman.
"Women are half the world. It's important they participate in all major decisions,"
"Climate change is not a fight for power," points out Hindou Oumarou Ibrahim, "it's a fight for survival."

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US Government Can Be Sued By Children Over Climate Change: Court

Fairfax - Jonathan Stempel (Reuters)

New York: A US federal appeals court has rejected the American government's bid to halt a lawsuit by young people claiming that President Donald Trump and his administration are violating their constitutional rights by ignoring the harms caused by climate change.
Students at a climate rally in San Francisco last week. Photo: AP
By a 3-0 vote, the 9th US Circuit Court of Appeals in San Francisco said the administration had not met the "high bar" under federal law to dismiss the Oregon lawsuit, which was originally brought in 2015 against the administration of Barack Obama.
The lawsuit started during the Obama administration. Photo: AP
The potentially far-reaching case is one of a handful seeking to have courts address global warming and its causes.
Twenty-one plaintiffs, now aged 10 to 21, accused federal officials and oil industry executives of knowing for decades that carbon dioxide emissions from the burning of fossil fuels destabilise the climate, but refusing to do anything about it.
They said this has deprived them of their due process rights to life, liberty and property, including to live in a habitable climate.
Students at a rally for clean energy in San Francisco last week. California opposes a Trump administration plan to scrap a policy slashing climate-changing emissions from power plants. Photo: AP
US District Judge Ann Aiken in Eugene, Oregon in November 2016 refused to dismiss the lawsuit, saying a quick dismissal without addressing the merits could sanction the government's alleged "knowing decision to poison the air."
In seeking to overturn that ruling, the government said letting the case proceed could lead to burdensome litigation, and provoke a "constitutional crisis" by pitting courts against Trump and the many other Executive Branch officials named as defendants.
A South Korean environmental activist protests against the US withdrawal from the Paris climate accord last year. Photo: AP
But in Wednesday's decision, Chief Judge Sidney Thomas said the dismissal request was premature, and deciding whether the plaintiffs' claims were too broad could be addressed through the normal legal process.
"Litigation burdens are part of our legal system, and the defendants still have the usual remedies before the district court for non-meritorious litigation," Thomas wrote. "Claims and remedies often are vastly narrowed as litigation proceeds; we have no reason to assume this case will be any different."
The US Department of Justice, which handled the government appeal, did not immediately respond to requests for comment.
Julia Olson, who represented the plaintiffs and is executive director of Our Children's Trust, which advocates for improving the climate, in an interview welcomed the decision.
"It's very exciting," she said. "It will be the first time that climate science and the federal government's role in creating its dangers will go on trial in a US court."
The lawsuit was returned to Aiken for further proceedings.

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New Scenarios Show How The World Could Limit Warming To 1.5c In 2100

Carbon Brief - Zeke Hausfather

Civil Society 1.5C protest at COP21. Credit: Takver.
In the 2015 Paris Agreement on climate change, nearly every country on Earth pledged to keeping global temperatures “well below” 2C above pre-industrial levels and to “pursue efforts to limit the temperature increase even further to 1.5C”.
However, at the time, scientists had only modelled energy system and carbon mitigation pathways to achieve the 2C target. Few studies had examined how the world might limit warming to 1.5C.
Now a paper in Nature Climate Change presents the results from a new modelling exercise using six different “integrated assessment models” (IAMs) to limit global temperatures in 2100 to below 1.5C.
The results suggest that 1.5C is achievable if global emissions peak in the next few years and massive amounts of carbon are sucked out of the atmosphere in the second half of the century through a proposed technology known as bioenergy with carbon capture and storage (BECCS).

Defining the 1.5C target
One challenge with the goal of limiting warming to 1.5C above pre-industrial levels is that it was not clearly defined in the text of the Paris Agreement. For example, scientists disagree on what, exactly, pre-industrial temperatures were and how best to define them, as well as what dataset to use.
There is also not a clear consensus if the target should be to aim to have even odds of the world reaching 1.5C warming by 2100, or seek to try and avoid having temperatures exceed 1.5C by aiming for an even lower warming amount. Because uncertainties in climate sensitivity mean that we could have anything between 1.5C and 4.5C warming per doubling of CO2 emissions, scientists tend to plan to avoid the worst case where climate sensitivity ends up being on the higher end of the range.
In the case of the 2C target, the Paris Agreement’s “well below” language has been interpreted as ensuring that there is no more than a 33% chance of exceeding 2C – and, therefore, a 66% chance of staying below it. But the 1.5C target could be interpreted as either aiming for a 50% chance of staying below 1.5C, or a 66% chance similar to the 2C target. This may sound like a small distinction, but it has large impacts on the resulting carbon budget and ease of meeting the target.
In their new paper, a team of 23 energy researchers choose the stricter interpretation of the target, aiming for a 66% chance of avoiding more than 1.5C warming in the year 2100. However, they allow for temperatures to exceed 1.5C over the course of the century as long as they fall back down to below 1.5C by the year 2100. This is known as an “overshoot” scenario.

1.5C only possible in some future pathways
To assess viable pathways to limit warming to 1.5C, the researchers use the new Shared Socioeconomic Pathways (SSPs) developed in preparation for the next Intergovernmental Panel on Climate Change (IPCC) assessment report due early next decade. These SSPs – which Carbon Brief will explore in more depth in the coming weeks – present five possible future worlds that differ in their population, economic growth, energy demand, equality and other factors.
Each world could have multiple different climate trajectories, though some will have a much easier time reducing emissions than others. The new climate trajectory associated with avoiding more than 1.5C warming in 2100 is called Representative Concentration Pathway 1.9 (“RCP1.9”), which is a world where the radiative forcing from greenhouse gases is limited to no more than 1.9 watts per meter squared (W/m2) above pre-industrial levels. This is lower than the range of RCPs previously used by climate modellers, which went from 2.6 up to 8.5W/m2.
The six IAMs all find viable 1.5C scenarios in SSP1, which is a pathway that focuses on “inclusive and sustainable development”. Four of the six models find pathways in SSP2, which is a middle of the road scenario where trends largely follow historical patterns. No models show viable 1.5C pathways in SSP3, which is a world of “regional rivalry” and “resurgent nationalism” with little international cooperation.
Finally, only one of the models has a 1.5C pathway in SSP4, which is a world of “high inequality”, while two models have viable pathways in SSP5, a world of “rapid economic growth” and “energy intensive lifestyles”.

Emissions must peak quickly
To limit warming to below 1.5C, all the models that the researchers examined require that global emissions peak by 2020 and decline precipitously thereafter. After 2050, the world must reduce net CO2 emissions to zero and emissions must be increasingly negative throughout the second half of the 21st century.
Even with these rapid reductions, all the scenarios considered still overshoot 1.5C warming in the 2040s, before declining to around 1.3-1.4C above pre-industrial levels by 2100. Models with more rapid reductions – generally associated with SSP1 – have less temperature overshoot than those with more gradual reductions.
The figure below shows both CO2 emissions (left) and global warming above pre-industrial (right) across all the 1.5C models examined. The lines are coloured based on the SSP used.
CO2 emissions in gigatons (Gt) CO2 (left) and global mean surface temperature relative to preindustrial (right) across all RCP1.9/1.5C scenarios included in Rogelj et al 2018. Data available in the IIASA SSP database. Chart by Carbon Brief using Highcharts.

The models show a remaining 1.5C “carbon budget” from 2018 to 2100 of between -175 and 400 gigatonnes of CO2 (GtCO2). This range is consistent with estimates from the IPCC’s 5th Assessment Report.
The wide range is largely a result of differences in emissions of non-CO2 greenhouse gases, such as methane and nitrous oxide, which vary by a factor of between two and three across the models by 2100. Some models with higher non-CO2 emissions have a remaining carbon budget of less than zero, requiring more CO2 to be removed from the atmosphere than added by the end of the century. In these simulations, the carbon budget for 1.5C has already been used up.
The central estimate across the models is that the remaining 2018-2100 carbon budget is around 230 GtCO2. At the current rate of emissions, this would allow roughly six years until the entire 1.5C budget is exhausted, with a range of zero to 11 years across all the models.

Replacing fossil fuels with renewables
The study explores the different ways that global energy needs can be met, while also cutting GHG emissions in order to meet the 1.5C goal. Limiting warming to below 1.5C requires that the world rapidly phase out all types of fossil fuels – or at least those without accompanying carbon capture and storage (CCS). At the same time, the world need to quickly ramp up the use of zero and net-negative carbon energy sources – things such as BECCS that generate energy while actually removing CO2 from the atmosphere.
The figure below shows the use of renewables (left), net-negative BECCS (centre) and coal without CCS (right) across all the 1.5C models. The colours show which SSPs the model simulations use.
Global primary energy use in exajoules (EJ) for non-renewable biomass (left), BECCS (center), and coal without CCS (right) across all RCP1.9/1.5C scenarios. Adapted from Figure 2 in Rogelj et al 2018. LARGE IMAGE
In most models, overall energy use actually increases between 2018 and 2100, by between -22% and +83%, with a central increase of 22%.
However, the models also show that energy efficiency is quite important in the short term – at least, while most energy comes from fossil fuels. This is particularly important in the transportation and building sectors, where rapid decarbonisation is more difficult than in power generation.
The models show an estimated 60-80% of all energy coming from renewables globally by 2050. Some models also show a much larger role for nuclear power, though others do not.
To limit warming to 1.5C, coal use without carbon capture declines by around 80% by 2040, with oil similarly mostly phased out by 2060. This would require most petrol or diesel vehicles to be phased out by 2060, with electric or other low-carbon alternative fuel vehicles making up the vast majority of sales well before that date. Future natural gas use is more mixed in the models, with some showing increases and some decreases by mid-century.

Emissions must go negative
Negative emissions are needed in the latter half of the century to pull the extra CO2 out of the atmosphere. This is because emissions cannot fall fast enough in the models to avoid exceeding the allowable carbon budget to avoid 1.5C warming.
Most of the models emit roughly 50-200% more CO2 than the allowable carbon budget over the course of the century, before pulling the extra CO2 back out.
The models assume widespread adoption of BECCS starting between 2030 and 2040 and then rapidly scaling up. By 2050, many models have BECCS producing more than 100 exajoules (EJ), roughly the same amount of energy globally as coal provides today. By 2100, BECCS will be around 200EJ compared to 300EJ for all non-biomass renewable energy.
The figure below shows the amount of CO2 sequestered by CCS (both from BECCS and fossil fuels) across all the models. Carbon capture ramps up after 2020 and could be 20 GtCO2 or higher by the end of the century, which is around half of global CO2 emissions in 2018.
Annual CO2 sequestered by carbon capture and storage in gigatons (Gt) CO2 by year and SSP across all RCP1.9/1.5C scenarios. Adapted from Figure 3 in Rogelj et al 2018.
The models produce estimates of global forest cover changes between -2% and 26% between today and 2100, with most models showing significant increases in forest cover. Both BECCS and afforestation require a lot of land. Most models show a decline in global cropland scenarios roughly equal to the area currently used for agriculture across the entire European Union.
However, most of the models used in the study do not include afforestation as an explicit mitigation option, so afforestation and other “natural” negative emissions technologies could potentially play a larger role in the future. The specific technologies used for future negative emissions may be different and somewhat less reliant on BECCS, but non-BECCS approaches are largely excluded from the models due to remaining uncertainties in cost and effectiveness at scale.
Similarly, the amount of BECCS used differs quite a bit between models and across SSPs, with SSP1 requiring the least negative emissions and SSP5 requiring the most due to its slower emissions reductions and higher overall energy use.
Dr Joeri Rogelj, the paper’s lead author from the International Institute for Applied Systems Analysis (IIASA) in Austria, tells Carbon Brief:
“This indicates that a focus on sustainable lifestyles that limit energy demand can strongly reduce the reliance on BECCS.”
One interesting consequence of the 1.5C target is a reduced use of fossil fuels combined with CCS, compared to what is found in 2C scenarios. This is because fossil fuels with CCS still results in methane emissions from coal mining or gas handling, as well as CO2 emissions due to imperfect capture and leakage. These extra emissions can become too important to allow at a large scale in a 1.5C world.

Much more difficult to reach 1.5C than 2C
In addition to exploring the details of what it would take to limit warming to 1.5C, the paper also compares it to existing 2C scenarios across a number of different categories. The figure below shows the difference between 1.5C and 2C scenarios across both economic and CO2 reduction metrics. Each dashed line represents a 100% increase in cost or effort in a 1.5C world compared to a 2C world.
Relative increases in cost and CO2 reduction metrics for 1.5C scenarios compared to 2C scenarios for various SSPs. Each dashed line represents a 100% increase in cost or reduction amount, up to a 500% increase. Taken from figure 4 in Rogelj et al 2018. LARGE IMAGE
The largest increases are in carbon prices, which must be between 200% and 400% higher, and in near-term costs, which are 200% to over 300% higher. These increases in short-term costs are driven by the more severe near-term emission reductions needed. Long-term costs are also expected to be around 200% higher.
For CO2 reduction metrics, a 1.5C world requires approximately two to three times larger reductions in CO2 from buildings and transport than in a 2C world. These sectors are more difficult to decarbonise than power generation as they involve the direct combustion of fossil fuels that are less easily replaced.

Difficult, but possible?
The new scenarios in this study are important because they show that there are possible trajectories and technological pathways that can limit warming to below 1.5C in 2100. However, all of the models included overshoot 1.5C of warming in the middle of the century. Most also rely on massive amounts of still-unproven negative emissions later in the century to allow a more feasibly gradual reduction in emissions in the near-term.As Dr Glen Peters, a senior researcher at the CICERO Center for International Climate Research in Norway who was not involved in the study, tells Carbon Brief:
“Limiting temperature to 1.5C is getting close to what models can deliver, with only certain socioeconomic, technological and resource assumptions amenable to 1.5C pathways. How to transform the model results into a viable society transformation remains the elephant in the room. The 1.5C scenarios require radical reductions in unabated fossil fuel use, rapid expansion of non-fossil energy sources and planetary-scale carbon dioxide removal. Failing to meet any of those core building blocks will make 1.5C quickly infeasible.”

Note: Accompanying the publication of the study is a newly updated SSP emissions and scenario database, which includes data for all SSP scenarios.

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