...
  • 主题
高级搜索  >
历史搜索 清空历史
首页> 外文期刊>Geophysical Research Letters >Weakened Submesoscale Eddies in the Equatorial Pacific Under Greenhouse Warming
【24h】

Weakened Submesoscale Eddies in the Equatorial Pacific Under Greenhouse Warming

机译：Weakened Submesoscale Eddies in the Equatorial Pacific Under Greenhouse Warming

获取原文
获取原文并翻译 | 示例
           
页面导航
  • 摘要
  • 著录项
  • 相关主题

摘要

Abstract Submesoscale eddies in the equatorial Pacific induce a pronounced upward heat flux from the subsurface to the surface ocean. Yet their response to greenhouse warming and feedback on the mean‐state change remain unknown. Using a long‐term high‐resolution climate simulation under a high carbon emission scenario, we show that submesoscale eddies in the central and eastern equatorial Pacific weaken, leading to an ∼50% reduction in their upward heat flux at the end of the 21st century, compared to its mid‐20th century level. This reduction is caused by an intensified stratification and a weakened cold tongue thermal front associated with a projected El Niño‐like warming pattern. The reduced vertical submesoscale eddy heat flux plays an important role in the anomalous heat budget of the surface layer over the central and eastern equatorial Pacific under greenhouse warming, acting as negative feedback on the El Niño‐like warming pattern.

著录项

获取原文

客服邮箱：kefu@zhangqiaokeyan.com

京公网安备：11010802029741号 ICP备案号：京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有

  • 客服微信

  • 服务号