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Abstract
Ocean-onto-land droughts (OTLDs), droughts originating over oceans and migrating onto land, have intensified due to anthropogenic climate change over the past 60 years. Under a high-emissions scenario, OTLDs are projected to become more frequent, persistent, widespread, and severe globally. Intensified OTLDs are linked to reduced moisture transport driven by atmospheric thermodynamic responses to global warming and circulation pattern shifts.
Publisher
npj Climate and Atmospheric Science
Published On
Authors
Yansong Guan, Xihui Gu, Louise J. Slater, Jiabo Yin, Jianfeng Li, Solomon Hailu Gebrechorkos, Xiang Zhang, Dongdong Kong, Xuesong Yan
Tags
ocean-onto-land droughts
climate change
moisture transport
global warming
atmospheric responses
drought intensity
circulation patterns
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