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摘要:
The relationship between sea surface temperature (SST) east of Australia and tropical cyclone frequency over the western North Pacific (WNPTCF) is analyzed by use of observation data.The WNPTCF from June to October is correlated negatively to spring SST east of Australia.When the spring SST is in the positive phase,a cyclonic circulation anomaly in the upper troposphere and an anticyclonic circulation anomaly in the lower troposphere prevail over the western North Pacific from June to October,concurrent with an anomalous atmospheric subsidence and an enlarged vertical zonal wind shear.These conditions are unfavorable for tropical cyclone genesis,and thus WNPTCF decreases.The negative phase of the spring SST east of Australia leads to more tropical cyclones over the western North Pacific.The spring SST east of Australia may give rise to simultaneous change in tropical atmospheric circulation via the teleconnection wave train,and then subsequently affect atmospheric circulation variation over the western North Pacific.
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Bottom water temperature measurements in the South China Sea,eastern Indian Ocean and western Pacific
海底底水温度(BWT)
南海(SCS)
东印度洋(EIO)
西太平洋(WPO)
大洋传送带模式
Cyclone Frequency over the Western North Pacific
Hadley环流
热带气旋频数
西北太平洋
大气本底
模型模拟
西部
对流层大气
投影
in the tropical western North Pacific in summer
西北太平洋夏季降水
东亚夏季降水
东亚高空急流
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篇名 Sea surface temperature east of Australia:A predictor of tropical cyclone frequency over the western North Pacific?
来源期刊 科学通报(英文版) 学科 地球科学
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年,卷(期) 2011,(2) 所属期刊栏目
研究方向 页码范围 196-201
页数 6页 分类号 P444
字数 语种 中文
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科学通报(英文版)
半月刊
1001-6538
11-1785/N
大16开
北京东黄城根北街16号
2-177
1950
eng
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9507
总下载数(次)
1
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58070
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