Siyu Zhao, Long Cao, Yu Fang, Panxi Dai, Jiaying Zhang
{"title":"Unintended winter–early spring warming over North America caused by tropical and subtropical deployment of marine cloud brightening","authors":"Siyu Zhao, Long Cao, Yu Fang, Panxi Dai, Jiaying Zhang","doi":"10.1038/s41612-026-01525-2","DOIUrl":null,"url":null,"abstract":"Marine cloud brightening (MCB) aims to reduce global warming, but its regional impacts remain uncertain. Using the Community Earth System Model, we implement MCB over a portion of tropical and subtropical oceans under SSP2-4.5. Despite overall cooling, MCB induces significant warming over mid-eastern North America in winter-to-early spring. The response originates mainly in the tropical and subtropical eastern Pacific, where MCB cools the atmosphere by reflecting solar radiation. This change modifies extratropical circulations through Gill-type and Rossby wave responses. The circulation changes warm mid-eastern North America via two pathways: suppressed synoptic disturbance activity, which reduces cloud cover and increases downward shortwave radiation, and enhanced positive temperature advection. This MCB-induced warming resembles that associated with a strong La Niña event, with implications for snowpack and water resources. Our results highlight potential unintended risks of regional MCB and the need for a better understanding of process-level teleconnection response to climate intervention strategies.","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"1 1","pages":""},"PeriodicalIF":9.6000,"publicationDate":"2026-08-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"npj Climate and Atmospheric Science","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1038/s41612-026-01525-2","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
Marine cloud brightening (MCB) aims to reduce global warming, but its regional impacts remain uncertain. Using the Community Earth System Model, we implement MCB over a portion of tropical and subtropical oceans under SSP2-4.5. Despite overall cooling, MCB induces significant warming over mid-eastern North America in winter-to-early spring. The response originates mainly in the tropical and subtropical eastern Pacific, where MCB cools the atmosphere by reflecting solar radiation. This change modifies extratropical circulations through Gill-type and Rossby wave responses. The circulation changes warm mid-eastern North America via two pathways: suppressed synoptic disturbance activity, which reduces cloud cover and increases downward shortwave radiation, and enhanced positive temperature advection. This MCB-induced warming resembles that associated with a strong La Niña event, with implications for snowpack and water resources. Our results highlight potential unintended risks of regional MCB and the need for a better understanding of process-level teleconnection response to climate intervention strategies.
期刊介绍:
npj Climate and Atmospheric Science is an open-access journal encompassing the relevant physical, chemical, and biological aspects of atmospheric and climate science. The journal places particular emphasis on regional studies that unveil new insights into specific localities, including examinations of local atmospheric composition, such as aerosols.
The range of topics covered by the journal includes climate dynamics, climate variability, weather and climate prediction, climate change, ocean dynamics, weather extremes, air pollution, atmospheric chemistry (including aerosols), the hydrological cycle, and atmosphere–ocean and atmosphere–land interactions. The journal welcomes studies employing a diverse array of methods, including numerical and statistical modeling, the development and application of in situ observational techniques, remote sensing, and the development or evaluation of new reanalyses.