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首页> 外文期刊>ournal of the Meteorological Society of Japan >Variations of Large-Scale Characteristics Associated with the Increment of Baiu Precipitation around 1950
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Variations of Large-Scale Characteristics Associated with the Increment of Baiu Precipitation around 1950

机译:1950年左右随着Baiu降水增加而引起的大规模特征变化

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The characteristics of the inter-decadal variations of Baiu-precipitation after 1900, and their relationships to the large-scale characteristics were analyzed with the use of the data of precipitation amounts, surface temperature and sea-level pressure. The Baiu precipitation averaged over Japan tended to show small amounts from 1924 to 1944 (called “Period I”). But it increased around 1950 and showed relatively large amounts from 1952 to 1972 (called “Period II”). This inter-decadal variation had large amplitudes in the south-western part of Japan.The following meteorological components showed significant changes between the two periods; 1) the meridional temperature gradient on the western side of Japan (increased), 2) the sea-level pressure between 30°N and 40°N in Japan (decreased) and 3) the precipitation amount at Manila, Philippines (decreased). No significant changes were found in the meridional pressure gradient on the north-eastern side of Japan and in the first EOF component of the surface temperature in Japan, although they were correlated with year-to-year variations of Baiu precipitation.The results of the analysis suggest that the increment of Baiu precipitation from Period I to Period II was associated with long-term variations of sub-tropical circulation. An hypothetical process is proposed for the increment of Baiu precipitation around 1950.
机译:利用降水量,地表温度和海平面压力等资料分析了1900年以后Baiu降水年代际变化特征及其与大尺度特征的关系。从1924年到1944年,日本全境的平均Bayu降水量往往呈现少量(称为“时期I”)。但是它在1950年左右有所增加,并且在1952年到1972年之间显示出相对较大的金额(称为“时期II”)。在日本西南部,这种年代际变化幅度较大。 1)日本西侧的子午温度梯度(升高),2)日本30°N到40°N之间的海平面压力(降低),3)菲律宾马尼拉的降水量(降低)。尽管与Baiu降水量的年际变化相关,但日本东北侧和日本地表温度的第一个EOF分量的子午压力梯度没有发现显着变化。分析表明,Baou降水从第一期到第二期的增加与亚热带环流的长期变化有关。提出了一个关于1950年左右Baiu降水增加的假设过程。

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