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夏季西北太平洋副热带高压指数

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利用在特定区域上平均的夏季(6、7、8月)平均850 hPa位势高度异常,我们定义了两种指数,分别用来描述夏季北太平洋副热带高压在东西方向和南北方向上的偏移.对于东西向指数,平均的区域为副高的西侧(110°-150°E,10°-30°N);对于南北向指数,平均的区域为副高的西北侧(120°-150°E,30°-40°N).发现这两种指数是相互独立的.基于南北向指数的合成分析结果与以往的研究结果吻合得相当好.在年际时间尺度上,将这两种指数与国家气候中心公布的副高指数进行了比较,发现尽管有一些微弱的差别,本文定义的指数与国家气候中心的副高指数大致具有相似的年际变化,因而本文的指数与国家气候中心的指数也对应着相似的环流和降水型.进而,对本文的指数与国家气候中心的指数对应的环流(降水)型之间的不同进行了分析,表明本文的指数比国家气候中心的指数能够更好地描述对应的环流和降水型.一个重要的结果是,不论根据本文指数,还是根据国家气候中心指数,东西向指数(或西伸指数)都比南北向指数(或北界指数)对应着更显著的降水异常,特别是在东亚地区和菲律宾海.这两种指数还可以用来描述副高在夏季里的季节推进,即,北移和东退.副高在7月中旬迅速北移和东退.发现在副高平均处于偏北或偏东的夏季里,北移或东退的幅度明显偏强.这两种指数和本文的结果可用于对大气环流模式的评估.
Indices of the Summertime Western North Pacific Subtropical High
By averaging June-July-August (JJA) mean geopotential height anomalies at 850 hPa over the specified areas, the author proposes two innovative and succinct parameters to objectively define the zonal and meridional displacements of the western North Pacific subtropical high (WNPSH) in summer, respectively.Thus, these two indices and the present results may provide a basis for validating atmospheric general circulation models simulating the WNPSH. For the zonal index, the specified area is the west edge (110°-150°E,10°-30°N) of the WNPSH. For the meridional index, the specified area is the northwest edge (120°-150°E,30°-40°N) of the WNPSH. The interannual variations of these two indices are found to be independent. The results from a composite analysis based on the meridional index are in good agreement with previous studies based on case analyses.The two indices are compared with the existing indices announced by the National Climate Center (NCC) in China, on the interannual timescale. Despite slight differences, the interannual variations of the presented indices are basically similar to those of the NCC indices, and thus the circulation and precipitation associated with the present indices exhibit similar features to those associated with the NCC indices.Furthermore, an analysis of the differences between the associations of the present indices and the NCC indices shows that the presented indices are better than the NCC indices. An important result is that the zonal index is related to a more outstanding anomaly of precipitation, especially in East Asia and the Philippine Sea,both based on the presented indices and the NCC indices.The two indices can also be used to describe the seasonal march of the WNPSH during summer,namely, the poleward and eastward shifts. It is found that climatologically, the WNPSH shifts poleward and eastward rapidly in middle July, but the amplitudes of the poleward and eastward shifts are more remarkable in the summers when the WNPSH is located poleward and eastward in average.

WNPSH indicesinterannual variabilityseasonal evolution

陆日宇

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LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029

副高指数 年际变化 季节演变

国家重点基础研究发展计划(973计划)国家自然科学基金

G1998040900 Part 140075016 and 40023001

2002

大气科学进展(英文版)
中国科学院大气物理研究所

大气科学进展(英文版)

CSCDSCI
影响因子:0.741
ISSN:0256-1530
年,卷(期):2002.19(6)
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