在未来气候条件下,更多的人口暴露于安潘规模的飓风中

Dann Mitchell, Laurence Hawker, James Savage, Rory Bingham, Natalie S. Lord, Md Jamal Uddin Khan, Paul Bates, Fabien Durand, Ahmadul Hassan, Saleemul Huq, Akm Saiful Islam, Yann Krien, Jeffrey Neal, Chris Sampson, Andy Smith, Laurent Testut
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引用次数: 8

摘要

南亚经历了世界上一些最具破坏性的气候事件,一些气旋造成数十万人丧生。尽管如此,与世界其他地区相比,该地区对极端气候的研究基本上缺乏。为了了解该地区极端事件未来可能发生的变化,我们考虑了超级气旋安潘,它于2020年5月登陆,给印度和孟加拉国的海岸线带来了2-4米的风暴潮。利用最新的CMIP6气候模式预测,结合风暴潮、水文和社会经济模型,我们考虑了人口暴露于安潘规模风暴潮的未来变化。我们将海平面上升和人口变化与2100年之前的预测相一致,但保持其他因素不变。印度和孟加拉国都将受到负面影响,在高排放情景下,印度遭受极端风暴潮洪水(3米)的风险增加了200%,孟加拉国遭受低排放洪水(0.1米)的风险增加了80%。只有当我们遵循低排放情景,与《巴黎协定》目标2°C一致时,我们才会看到孟加拉国的风暴潮风险没有真正的变化。主要是由于人口和气候信号相互抵消。对印度来说,即使在这种低排放的情况下,洪水暴露的增加仍然很大(50%)。虽然这里我们只将风暴潮洪水部分归因于气候变化,但我们强调,热带气旋是多方面的,损害往往是物理和社会因素的综合。我们建议未来的气候风险评估明确考虑潜在的复合因素。
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Increased population exposure to Amphan-scale cyclones under future climates

Southern Asia experiences some of the most damaging climate events in the world, with loss of life from some cyclones in the hundreds of thousands. Despite this, research on climate extremes in the region is substantially lacking compared to other parts of the world. To understand the narrative of how an extreme event in the region may change in the future, we consider Super Cyclone Amphan, which made landfall in May 2020, bringing storm surges of 2–4 m to coastlines of India and Bangladesh. Using the latest CMIP6 climate model projections, coupled with storm surge, hydrological, and socio-economic models, we consider how the population exposure to a storm surge of Amphan's scale changes in the future. We vary future sea level rise and population changes consistent with projections out to 2100, but keep other factors constant. Both India and Bangladesh will be negatively impacted, with India showing >200% increased exposure to extreme storm surge flooding (>3 m) under a high emissions scenario and Bangladesh showing an increase in exposure of >80% for low-level flooding (>0.1 m). It is only when we follow a low-emission scenario, consistent with the 2°C Paris Agreement Goal, that we see no real change in Bangladesh's storm surge exposure, mainly due to the population and climate signals cancelling each other out. For India, even with this low-emission scenario, increases in flood exposure are still substantial (>50%). While here we attribute only the storm surge flooding component of the event to climate change, we highlight that tropical cyclones are multifaceted, and damages are often an integration of physical and social components. We recommend that future climate risk assessments explicitly account for potential compounding factors.

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