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航运排放的突然减少作为一种意外的地球工程终止冲击会产生显著的辐射变暖。

Abrupt reduction in shipping emission as an inadvertent geoengineering termination shock produces substantial radiative warming.

作者信息

Yuan Tianle, Song Hua, Oreopoulos Lazaros, Wood Robert, Bian Huisheng, Breen Katherine, Chin Mian, Yu Hongbin, Barahona Donifan, Meyer Kerry, Platnick Steven

机构信息

GESTAR-II, University of Maryland, Baltimore County, MD USA.

Sciences and Exploration Directorate, Goddard Space Flight Center, Greenbelt, MD USA.

出版信息

Commun Earth Environ. 2024;5(1):281. doi: 10.1038/s43247-024-01442-3. Epub 2024 May 30.

Abstract

Human activities affect the Earth's climate through modifying the composition of the atmosphere, which then creates radiative forcing that drives climate change. The warming effect of anthropogenic greenhouse gases has been partially balanced by the cooling effect of anthropogenic aerosols. In 2020, fuel regulations abruptly reduced the emission of sulfur dioxide from international shipping by about 80% and created an inadvertent geoengineering termination shock with global impact. Here we estimate the regulation leads to a radiative forcing of Wm averaged over the global ocean. The amount of radiative forcing could lead to a doubling (or more) of the warming rate in the 2020 s compared with the rate since 1980 with strong spatiotemporal heterogeneity. The warming effect is consistent with the recent observed strong warming in 2023 and expected to make the 2020 s anomalously warm. The forcing is equivalent in magnitude to 80% of the measured increase in planetary heat uptake since 2020. The radiative forcing also has strong hemispheric contrast, which has important implications for precipitation pattern changes. Our result suggests marine cloud brightening may be a viable geoengineering method in temporarily cooling the climate that has its unique challenges due to inherent spatiotemporal heterogeneity.

摘要

人类活动通过改变大气成分影响地球气候,进而产生驱动气候变化的辐射强迫。人为温室气体的变暖效应已被人为气溶胶的冷却效应部分抵消。2020年,燃料法规突然将国际航运中二氧化硫的排放量减少了约80%,并造成了具有全球影响的意外地球工程终止冲击。在此,我们估计该法规导致全球海洋平均辐射强迫为Wm。与1980年以来的变暖速率相比,辐射强迫量可能导致2020年代的变暖速率翻倍(或更多),且具有强烈的时空异质性。这种变暖效应与2023年近期观测到的强烈变暖一致,并预计会使2020年代异常温暖。该强迫在量级上相当于自2020年以来测量到的行星热量吸收增加量的80%。辐射强迫在半球上也有强烈的对比,这对降水模式变化具有重要意义。我们的结果表明,海洋云增亮可能是一种暂时冷却气候的可行地球工程方法,但由于其固有的时空异质性而面临独特挑战。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8039/11139642/d67e9204deea/43247_2024_1442_Fig1_HTML.jpg

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