基于敏感性策略的海洋云增亮太阳气候干预对气候的影响

IF 3.4 2区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Journal of Geophysical Research: Atmospheres Pub Date : 2025-01-10 DOI:10.1029/2024JD041245
C.-C. Chen, J. H. Richter, Walker R. Lee, Mari Tye, Douglas G. MacMartin, Ben Kravitz
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引用次数: 0

摘要

利用社区地球系统模式第2版(CESM2)的综合模拟研究了海洋云增亮在降低地球表面温度方面的效率。我们采用了一种基于敏感性的云播策略,该策略以前是在社区气候系统模型第3版(CCSM3)下开发的,以抵消二氧化碳加倍的变暖,其中我们以最容易变亮的海洋区域为目标,以确定在SSP2-4.5下诱导1°C冷却所需的面积范围。结果表明,在CESM2中,超过5%的海洋面积的播云能够实现这一目标。在这种播云方案下,播云主要部署在低纬度地区,导致La Niña-like响应模式,这是一个主要的意外后果。提出并讨论了这些副作用背后的潜在机制。模拟还显示,5%的人工降雨方案导致全球降水总体减少,陆地降水增加,海洋降水减少。
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Climate Impact of Marine Cloud Brightening Solar Climate Intervention Under a Susceptibility-Based Strategy Simulated by CESM2

The efficiency of marine cloud brightening in cooling Earth's surface temperature is investigated using an ensemble of simulations with the Community Earth System Model version 2 (CESM2). We employ a susceptibility-based cloud seeding strategy, previously developed under the Community Climate System Model version 3 (CCSM3) to counteract the warming of CO2 doubling, in which we target the regions of the ocean most easily brightened, to determine what area extent will be required to induce 1°C cooling under SSP2-4.5. The results indicate that cloud seeding over 5% of the ocean area is capable of achieving this goal in CESM2. Under this seeding scheme, cloud seeding is mainly deployed over lower latitudes which leads to a La Niña-like pattern of response which is a major unintended consequence. Potential mechanisms behind such side effects are presented and discussed. The simulations also reveal that the 5% cloud seeding scheme induces an overall reduction in global precipitation, with an increase over land and a decrease over the ocean.

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来源期刊
Journal of Geophysical Research: Atmospheres
Journal of Geophysical Research: Atmospheres Earth and Planetary Sciences-Geophysics
CiteScore
7.30
自引率
11.40%
发文量
684
期刊介绍: JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.
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