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基于数据的全球变暖与海平面上升的路径分析和预测。

Data driven pathway analysis and forecast of global warming and sea level rise.

机构信息

Department of Applied Mathematics and Statistics, State University of New York at Stony Brook, Stony Brook, NY, 11794-3600, USA.

Duke University, 2080 Duke University Road, Durham, NC, 27708, USA.

出版信息

Sci Rep. 2023 Apr 4;13(1):5536. doi: 10.1038/s41598-023-30789-4.

DOI:10.1038/s41598-023-30789-4
PMID:37015939
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC10073234/
Abstract

Climate change is a critical issue of our time, and its causes, pathways, and forecasts remain a topic of broader discussion. In this paper, we present a novel data driven pathway analysis framework to identify the key processes behind mean global temperature and sea level rise, and to forecast the magnitude of their increase from the present to 2100. Based on historical data and dynamic statistical modeling alone, we have established the causal pathways that connect increasing greenhouse gas emissions to increasing global mean temperature and sea level, with its intermediate links encompassing humidity, sea ice coverage, and glacier mass, but not for sunspot numbers. Our results indicate that if no action is taken to curb anthropogenic greenhouse gas emissions, the global average temperature would rise to an estimated 3.28 °C (2.46-4.10 °C) above its pre-industrial level while the global sea level would be an estimated 573 mm (474-671 mm) above its 2021 mean by 2100. However, if countries adhere to the greenhouse gas emission regulations outlined in the 2021 United Nations Conference on Climate Change (COP26), the rise in global temperature would lessen to an average increase of 1.88 °C (1.43-2.33 °C) above its pre-industrial level, albeit still higher than the targeted 1.5 °C, while the sea level increase would reduce to 449 mm (389-509 mm) above its 2021 mean by 2100.

摘要

气候变化是我们这个时代的一个关键问题,其原因、途径和预测仍然是更广泛讨论的话题。在本文中,我们提出了一种新的数据驱动途径分析框架,以确定导致全球平均温度和海平面上升的关键过程,并预测从现在到 2100 年它们的增长幅度。仅基于历史数据和动态统计建模,我们就确定了将温室气体排放增加与全球平均温度和海平面上升联系起来的因果途径,其中间环节包括湿度、海冰覆盖和冰川质量,但不包括太阳黑子数量。我们的结果表明,如果不采取行动遏制人为温室气体排放,到 2100 年,全球平均气温将上升到比工业化前水平高约 3.28°C(2.46-4.10°C),而全球海平面将比 2021 年平均水平高约 573mm(474-671mm)。然而,如果各国遵守 2021 年联合国气候变化大会(COP26)规定的温室气体排放法规,全球温度上升将减缓到平均比工业化前水平升高 1.88°C(1.43-2.33°C),尽管仍高于 1.5°C 的目标,而海平面上升将减少到比 2021 年平均水平高约 449mm(389-509mm)。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7f/10073234/eb30bb289dd8/41598_2023_30789_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7f/10073234/a1f312e6c3a4/41598_2023_30789_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7f/10073234/7647901d08e2/41598_2023_30789_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7f/10073234/edc4d8dfe465/41598_2023_30789_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7f/10073234/1dd489306c40/41598_2023_30789_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7f/10073234/eb30bb289dd8/41598_2023_30789_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7f/10073234/a1f312e6c3a4/41598_2023_30789_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7f/10073234/7647901d08e2/41598_2023_30789_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7f/10073234/edc4d8dfe465/41598_2023_30789_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7f/10073234/1dd489306c40/41598_2023_30789_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7f/10073234/eb30bb289dd8/41598_2023_30789_Fig5_HTML.jpg

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