But even in wealthy countries like the UK, there are warnings of carbon inequality. Amy Norman, a researcher at the think-tank, The Social Market Foundation, says politicians need to level with voters on what the transition to net zero will mean for the way we live. There's potential for a public and political backlash over issues of unfairness, she says, which could damage trust and ultimately the wider transition to net zero (removing as many emissions as we produce). Have countries kept their climate change promises? "This is an entire economical, societal shift and transition that we need to make," she says. "Politicians need to have the public on board and bringing them alongside - if you're hitting lower incomes where it hurts with their finances you're going to lose support quickly and especially if that's seen to be unfair." Anyone driving around in a clapped-out car they rely on for the school run might well wonder how to afford a shiny new electric car. And if you live in a tower block, where would you even charge one? And those dreading a hefty bill to fix a faulty boiler will be shuddering at the thought of an expensive heat pump. These are some of the issues politicians must wrestle with as they work out how to deliver on their promises for curbing emissions. Amy Norman says there needs to be a package of support for low-income households to help meet the costs of electric vehicles and funding for local authorities to install public charging points. Issues of climate justice are thrown into even sharper relief when looking at emissions through a global lens. Studies show that the combined emissions of the richest 1% of the global population account for more than the poorest 50%. The global south will bear the brunt of economic impacts from rising temperatures, with those on lower incomes more vulnerable to the likes of floods, drought and extreme heat. In Nigeria, for instance, the poorest 20% of people are 50% more likely to be affected by a flood, 130% more likely to be affected by a drought, and 80% more likely to be affected by a heat wave than the average Nigerian. And in Bangladesh, India, and Honduras, poor people are losing two to three times more than the wealthy when hit by a flood or storm. One recent study found that enacting policies to fight climate change will push an additional 50 million people into poverty by 2030.https://www.bbc.com/news/science-environment-56941979
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A 50,000-year history of current flow yields new climate clues A 50,000-year history of current flow yields new climate clues by Sarah Stanley , Eos New research confirms the central role of a major ocean circulation system in driving sudden climate changes during the last ice age. Here an iceberg floats off of Baffin Island, Nunavut, Canada, in the North Atlantic Ocean, a region that plays a key role in ocean circulation. Credit: National Snow and Ice Data Center , CC BY 2.0 From 50,000 to 15,000 years ago, during the last ice age, Earth's climate wobbled between cooler and warmer periods punctuated by why not try here occasional, dramatic ice-melting events. Previous research has suggested that these oscillations were likely influenced by changes in the Atlantic Meridional Overturning Circulation (AMOC), a pattern of currents that carry warm, tropical water to the North Atlantic, where it cools, sinks, and flows back south. However, the precise role played by the AMOC in ancient climate fluctuations has been unclear. Now Toucanne et al. have reconstructed the historical flow of a key current in the upper part (the northward flow) of the AMOC, the Glacial Eastern Boundary Current (GEBC), shedding new light on how the AMOC can drive sudden changes in climate. The GEBC flowed northward along Europe's continental margin during the last ice age (it persists today as the European Slope Current). To better understand the GEBC's role in the AMOC, the researchers collected six seafloor sediment cores off the coast of France. Analysis of grain sizes and isotope levels in the core layers revealed the current's strength when each layer was deposited, yielding the first high-resolution, 50,000-year historical record of the current. This new historical record shows that the GEBC flowed faster during warmer intervals of the last ice age but weakened during the coldest periods. The timing of these changes aligns well with previously established records on AMOC speed and the southward return flow of deep waters to the west. Comparing the history of the GEBC with other records also shows that major ice-melting events, in which ice age glaciers released huge amounts of freshwater into the Atlantic, correspond with periodic weakening of the current and of the AMOC in general. Drawing on these findings, the researchers outline a mechanism by which the GEBC could have carried cold glacial meltwater northward and contributed to changes in the AMOC that may have driven warm-cold climate oscillations in the North Atlantic. More information: Samuel Toucanne et al. The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability, Paleoceanography and Paleoclimatology (2021). DOI: 10.1029/2020PA004068 Provided by Eos This story is republished courtesy of Eos, hosted by the American Geophysical Union. Read the original story here .https://phys.org/news/2021-05-year-history-current-yields-climate.html