首页|基于CESM模式的4至6月热带西南印度洋海表异常增暖对印太气候影响的研究

基于CESM模式的4至6月热带西南印度洋海表异常增暖对印太气候影响的研究

扫码查看
热带西南印度洋温跃层深度较浅,该海域温跃层的变化与海表温度具有密切的联系,具有独特的海气相互作用.文章基于观测资料和模式资料分析了 4 至 6 月热带西南印度洋海表增暖对热带印度洋-西太平洋的气候影响.结果表明,4 至 6月热带西南印度洋海表增暖增强了当地的对流活动,导致热带西南印度洋降水的增加;热带印度洋的低空出现了关于赤道反对称的"C型"风场异常,即赤道以北为异常的东北风,赤道以南为异常的西北风;5月至 6月北印度洋低空异常的东北风会减弱亚洲夏季风,北印度洋海表潜热释放减少,北印度洋海表增暖.热带西南印度洋海表增暖的气候影响并不局限在热带印度洋地区,其增暖能加热对流层大气,激发东传的大气开尔文波,热带西北太平洋低层的东风响应在信风的背景下也能触发局地的海气正反馈,两者共同有利于热带西北太平洋地区低空反气旋式风场的维持.反气旋式风场异常在 5、6 月能增强季风水汽输送,使得我国长江流域的降雨显著增多.该研究结果揭示了热带西南印度洋加热异常可引起横跨北印度洋-热带西太平洋的海气相互作用,为我国东部地区夏季降水预报提供了有益参考.
Impacts of the anomalous southwest tropical Indian Ocean SST warming on Indo-Pacific climate from April to June based on the CESM model
The thermocline depth in the southwest tropical Indian Ocean(TIO)is shallow,and thermocline variations are closely related to the sea surface temperature,making southwest TIO feature a unique ocean-atmosphere interaction.Based on the observation and model data,this study analyzed the climatic effects of the southwest TIO SST warming on the tropical Indo-Western Pacific from April to June.The results show that the local convective activities are enhanced by the warming of the southwest TIO from April to June,and the precipitation in the southwest TIO increases.In the lower troposphere of the tropical Indian Ocean,a"C-shaped"wind anomaly pattern appears with abnormal northeast winds north of the equator and abnormal northwest winds south of the equator.From May to June,abnormal north-easterly winds in the North Indian Ocean can weaken the Asian summer monsoon,reduce the latent heat release of the North Indian Ocean,and warm the North Indian Ocean.The climatic effect of the southwest TIO SST warming is not limited to the tropical Indian Ocean region.The warming can heat the tropospheric atmosphere and stimulate the eastward atmospheric Kelvin wave,and the easterly wind response in the lower troposphere of the tropical northwest Pacific Ocean can also trigger local positive ocean-atmosphere feedback under the background of trade winds.Both are conducive to the maintenance of anticyclonic wind anomaly at the lower troposphere of the tropical northwest Pacific.The anticyclonic wind anomaly can enhance the monsoon water vapor transport in May and June,which makes the rainfall increase significantly over the Yangtze River Valley in China.This study reveals that the heating anomaly in the southwest TIO could cause ocean-atmosphere interaction across the north Indian Ocean and tropical western North Pacific Ocean,which would provide a useful reference for the summer precipitation forecast in eastern China.

trans-basin influenceocean-atmosphere interactionprecipitationanticyclone

陈泽生、李振宁、郭媛媛、王腾、杜岩

展开 >

热带海洋环境国家重点实验室(中国科学院南海海洋研究所),广东 广州 510301

环境与可持续发展学部(香港科技大学),香港 999077

大气与海洋科学系/大气科学研究院(复旦大学),上海 200438

跨洋盆影响 海气相互作用 降水 反气旋

国家重点研发计划项目中国科学院战略性先导科技专项(B类)国家自然科学基金项目中国科学院青年创新促进会项目热带海洋环境国家重点实验室自主项目

2019YFA0606703XDB42010305421750432022347LTOZZ2102

2024

热带海洋学报
中国科学院南海海洋研究所

热带海洋学报

CSTPCD北大核心
影响因子:0.513
ISSN:1009-5470
年,卷(期):2024.43(2)
  • 28