autumn circulation 中文意思是什麼
autumn circulation
解釋
秋季循環- autumn : n. 1. 秋，秋季〈英國為八、九、十月；美國普通稱 fall, 指九、十、十一月〉。2. 成熟期；凋落期；晚年。
- circulation : n. 1. 循環；運行。2. 傳播；環流（量），流通（量）。3. （雜志等的）發行（額），銷數，銷路。4. 通貨，貨幣；流通證券。5. 【航空】環量，環流。
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The responses of asian monsoon circulation to the heat source annual anomalies over the bay of bengal and philippines in summer and the annual relationships between the heat sources over the bay of bengal and philippines and the precipitation of china in summer are studied emphatically, with the results as follows : ( 1 ) the coverage and intensity of atmospheric heat source are the largest and strongest in summer and then turn smaller and weaker in autumn and winter, and in turn begin to become larger and stronger in spring again
著重討論了夏季孟加拉灣和菲律賓熱源年際異常時，亞洲季風環流系統的響應，及其與中國夏季降水的年際關系。結果表明： （ 1 ）夏季大氣熱源的范圍最大，強度最強，以後以秋、冬季依次變小變弱，春季又開始變大變強。夏季亞洲季風區有三個強的大氣熱源中心，其中以孟加拉灣熱源最強，菲律賓熱源和印度半島西部熱源次之。 -
We classified flood and drought years of summer and autumn, it is pointed out in the paper that there are circulation anomaly in 500mb height field before flood or drought years. we also find out that there are intimated relation between autumn floods and droughts of zhejiang province and the macro - scale rain belt. the meteorological elements emergence abnormal features in summer before flood and drought years. we make out predictor to predicate summer precipation
論文結合三種排序方法劃分了夏秋旱澇年，研究表明，夏季、秋季旱澇年前期冬季和夏季500hpa高度場環流有明顯的異常特徵，夏秋旱澇與我國夏秋大尺度天氣氣候異常有密切的關系，旱澇前期我國氣象要素場有明顯的異常特徵。製作了浙江省夏季旱、澇預報工具。 -
It is expected to be available for circulation in the late summer and early autumn and will be released, subject to sufficient supplies being available, in response to public demand
新鈔目前在印製中，預計將於今年夏秋之間因應市民的需求開始分批推出市面流通。 -
The mesoscale circulation determines basic air flow patterns in this area, which is typical in spring - summer season and in calm weather of autumn - winter season
中尺度環流是該地區低層大氣流動的基本模態，春夏季和秋冬季弱系統條件下的區域流動大體按這種模態演變。 -
When the autumn kuroshio ssta is positive, the sea - land sea level pressure differences in the east asian region become large in winter, the east asian trough at 500hpa shifts eastward and is deep in its south and shallow in the northern, along with strong north winds in the above area and weak westerly circulation in the asian region
當秋季黑潮區域海溫異常偏高，東亞地區的海陸氣壓差異進一步加大，東亞大槽北部減弱、南部加深、位置東移，東亞地區的偏北風加強，亞洲地區西風環流減弱，即東亞冬季風加強；反之亦然。
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