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The Interdecadal Variation of the Western Pacific Subtropical High as Measured by 500 hPa Eddy Geopotential Height

机译:用500 hPa涡旋位势高度测量的西太平洋副热带高压年代际变化。

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The interdecadal variation of the summer western Pacific subtropical high (WPSH) during 1948–2009 is investigated in this study. Compared with most previous works, which focused on the 500 hPa geo-potential height, the interdecadal variation of the horizontal winds, relative vorticity, and eddy geopotential height over the western Pacific are all analyzed. The weakened anticyclone and decreased negative relative vorticity at middle-low levels over the western Pacific suggest that the WPSH weakened during 1979–2009 relative to 1948–78. After subtracting the zonal belt mean height between 0° and 40°N, the 500 hPa eddy geopotential height with significant negative anomalies over the western Pacific can correctly depict this weakened interdecadal variation of the WPSH. The illusory westward extension signal reflected by the 500 hPa geopotential height may derive from the significant increment of the geopotential height at middle and lower latitudes in the late 1970s under global warming.
机译:本文研究了1948–2009年夏季西太平洋副热带高压(WPSH)的年代际变化。与以往大多数关注500 hPa地势高度的工作相比,分析了西太平洋水平风的年代际变化,相对涡度和涡旋地势高度。西太平洋的反气旋减弱,中低水平的负相对涡度降低,表明WPSH在1979-2009年相对于1948-78年减弱了。减去纬向带平均高度(介于0°和40°N之间)后,西太平洋上500 hPa涡旋位势高度具有明显的负异常,可以正确地描述WPSH的年代际变化减弱。 500 hPa地势高度所反映的虚幻的向西延伸信号可能来自1970年代后期全球变暖下中低纬度的地势高度的显着增加。

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