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NPCC4:尾部风险、极端高温的气候驱动因素,以及极端事件预测的新方法。

NPCC4: Tail risk, climate drivers of extreme heat, and new methods for extreme event projections.

机构信息

Department of Atmospheric, Oceanic, and Earth Sciences, George Mason University, Fairfax, Virginia, USA.

CUNY Institute for Demographic Research (CIDR), City University of New York, New York City, New York, USA.

出版信息

Ann N Y Acad Sci. 2024 Sep;1539(1):49-76. doi: 10.1111/nyas.15180. Epub 2024 Aug 19.

DOI:10.1111/nyas.15180
PMID:39159316
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11438572/
Abstract

We summarize historic New York City (NYC) climate change trends and provide the latest scientific analyses on projected future changes based on a range of global greenhouse gas emissions scenarios. Building on previous NPCC assessment reports, we describe new methods used to develop the projections of record for sea level rise, temperature, and precipitation for NYC, across multiple emissions pathways and analyze the issue of the "hot models" associated with the 6th phase of the Coupled Model Intercomparison Project (CMIP6) and their potential impact on NYC's climate projections. We describe the state of the science on temperature variability within NYC and explain both the large-scale and regional dynamics that lead to extreme heat events, as well as the local physical drivers that lead to inequitable distributions of exposure to extreme heat. We identify three areas of tail risk and potential for its mischaracterization, including the physical processes of extreme events and the effects of a changing climate. Finally, we review opportunities for future research, with a focus on the hot model problem and the intersection of spatial resolution of projections with gaps in knowledge in the impacts of the climate signal on intraurban heat and heat exposure.

摘要

我们总结了纽约市(NYC)历史气候变化趋势,并根据一系列全球温室气体排放情景提供了有关未来变化的最新科学分析。在前 NPCC 评估报告的基础上,我们描述了用于为海平面上升、温度和降水的记录预测开发新方法的过程,这些预测涵盖了多种排放途径,并分析了与耦合模型比较计划第 6 阶段(CMIP6)相关的“热门模型”问题及其对 NYC 气候预测的潜在影响。我们描述了 NYC 内部温度变化的科学现状,并解释了导致极端高温事件的大规模和区域动态,以及导致极端高温暴露分布不均的局部物理驱动因素。我们确定了三个潜在风险领域及其可能的错误描述,包括极端事件的物理过程和气候变化的影响。最后,我们回顾了未来研究的机会,重点关注热门模型问题以及预测的空间分辨率与气候信号对城市内部热和热暴露影响的知识差距之间的交叉。

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本文引用的文献

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NPCC4: Advancing climate justice in climate adaptation strategies for New York City.NPCC4:推进纽约市气候适应战略中的气候正义。
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NPCC4: Climate change and New York City's health risk.NPCC4:气候变化与纽约市的健康风险。
Ann N Y Acad Sci. 2024 Sep;1539(1):185-240. doi: 10.1111/nyas.15115. Epub 2024 Jun 25.
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NPCC4: New York City climate risk information 2022-observations and projections.NPCC4:纽约市气候风险信息 2022-观测与预测。
Ann N Y Acad Sci. 2024 Sep;1539(1):13-48. doi: 10.1111/nyas.15116. Epub 2024 Jun 3.
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Overshooting the critical threshold for the Greenland ice sheet.格陵兰冰原的关键阈值被突破。
Nature. 2023 Oct;622(7983):528-536. doi: 10.1038/s41586-023-06503-9. Epub 2023 Oct 18.
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Localized uplift, widespread subsidence, and implications for sea level rise in the New York City metropolitan area.纽约市大都市区的局部隆起、广泛沉降及其对海平面上升的影响。
Sci Adv. 2023 Sep 27;9(39):eadi8259. doi: 10.1126/sciadv.adi8259.
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Atlantic meridional overturning circulation increases flood risk along the United States southeast coast.大西洋经向翻转环流增加了美国东南沿海的洪水风险。
Nat Commun. 2023 Aug 22;14(1):5095. doi: 10.1038/s41467-023-40848-z.
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Increasingly Sophisticated Climate Models Need the Out-Of-Sample Tests Paleoclimates Provide.日益复杂的气候模型需要古气候提供的样本外测试。
J Adv Model Earth Syst. 2022 Dec;14(12):e2022MS003389. doi: 10.1029/2022MS003389. Epub 2022 Dec 18.
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Heterogeneous melting near the Thwaites Glacier grounding line.斯维茨冰川的基底融线附近的异质融化。
Nature. 2023 Feb;614(7948):471-478. doi: 10.1038/s41586-022-05691-0. Epub 2023 Feb 15.