winter anomaly 中文意思是什麼
winter anomaly
解釋
冬季異常-
Relation of winter temperature anomaly in dalian to prophase sst over indian ocean
大連地區冬季氣溫異常與前期印度洋海溫的關系 -
Further, correlation analysis is used to the summer rainfall and four seasonal north pacific ssta, the results suggest north pacific ssta which notability cause the summer rainfall anomaly over eastern china are prophase winter ssta of kuroshio region of northwestern pacific, prophase spring ssta of middle and eastern equatorial pacific and summer ssta of west wind drift region
進一步對上述東部夏季降水異常區夏季降水與春夏秋冬太平洋海溫異常作相關分析，表明對中國東部夏季降水有顯著影響是：西北太平洋黑潮海區前期冬季海溫異常、赤道中東太平洋前期春季海溫異常、中高緯太平洋西風漂流區同期夏季海溫異常。 -
On base of results above, composite model of ssta in pacific and circulation anomaly are constructed for analysis their evolution. during mature phase of el nino usually in winter, positive ssta dominates in tropical eastern ocean and negative ssta dominates in west wind drift district in mid - latitude ocean, correspondingly the pna index of 500 hpa geopotential height is positive which means the aleutian low gets strong, and the situation is somewhat inversely during la nina phase of ssta
合成位相反映了太平洋ssta演變特徵，以及相對應的大氣環流異常特徵：當西風漂流區處于暖態而熱帶中東太平洋海溫偏低時，合成大氣模型當中阿留申低壓減弱， 500hpapna指數為負異常；當西風漂流區處于冷態，熱帶中東太平洋處于暖態（ elnino峰值?成熟期ssta典型分佈） ，合成大氣模型中阿留申低壓加強， 500hpapna指數為正異常。 -
Then by using of statistics and numerical simulation analysis, research abnormality of the main circulation system at following summer in east asia, and the influence of the abnormality on the rainfall and temperature in summer in china, when sst over the kuroshio area during winter show cold or warm anomaly
再分別通過統計和數值模擬的方法，系統的分析了冬季黑潮海溫冷暖異常時，後期夏季東亞地區高低空的主要環流系統的異常，以及這些異常又如何進一步影響了我國夏季的降水和氣溫。 -
In heavy snow years, there are marked anomaly of atmospheric circulation : on 500 height field trough of east asia is heavier, north - west flow after height trough is striver, so that cold air of eastern region is stronger following " cold winter '. spring rain answering to eurasia winter snow anomaly is notable, in heavy snow years, yangtse - river has negative rain anomaly
在歐亞冬季積雪異常偏重的年份，大氣環流出現顯著異常： 500hpa位勢高度場上徑向氣流占優勢，東亞大槽偏強，高度場槽后西北氣流偏強，造成影響我國東部地區的冷空氣偏強，出現「冷冬天氣」 。我國春季降水對歐亞冬季積雪異常的響應最為顯著，重雪年春季我國長江流域以南大部地區出現明顯的降水負異常。 -
3 ) the anomaly interaction of global sea thermal elements with climate elements is of persistence from previous summer / winter through current winter / summer with relative stable interaction areas on inter - decadal time scale. while their abrupt climate change did not occur simultaneously
3 ）在年代際尺度變化方面，海洋熱異常和氣候異常有較好的同期相關關系，相互作用的關鍵區也有較穩定的位置，不同要素的氣候躍變點不盡相同。 -
By using of eof analysis, distribution of sst over the kuroshio area during winter are identified, which show cold or warm anomaly
本文首先通過eof分析確定了冬季黑潮區sst的主要分佈形勢，發現冬季黑潮區海溫主要表現為冷異常或暖異常。 -
Its warming was the higher in china, ( 5 ) the current atmosphere circulation anomaly is the current factor influenced the winter air temperature in the north - east china, and it includes siberian high anomaly, the east asian trough anomaly, the acreage of polar vortex anomaly, the asian winter monsoon anomaly and the anomaly of the west - wind circulation in east - asian
（ 4 ）東北地區冬季增暖趨勢與中國大部分地區是一致的，是增暖最顯著的地區之一。 （ 5 ）影響東北冬季氣溫異常的同期因子是環流異常，它包括西伯利亞高壓、東亞大槽、東亞冬季風、極渦面積、東亞西風環流指數等的異常。 -
These make west - pacific subtropical height strengthen and extend westward and blocking form and develop in mid - high latitude, while its above west wind drift zone decreases. and around 1976, 500hpa anomaly field of winter and summer also changes
其中變化比較顯著的是貝加爾湖附近和副高，都是76年後增強，這有利於低緯副高的加強西伸和中高緯阻塞的形成和發展；並且在76年前後，厄爾尼諾和拉尼娜年冬、夏季500hpa距平場也有一定的差異。 -
Relationship of east siberian autumn sea ice anomaly with winter atmospheric cir culation and east asia climate
秋季區域海冰面積異常與冬季大氣環流及東亞區域氣候的關系 -
In this paper, climatic characteristics of air temperature in north china in the past fifty year are analyzed, and winter air temperature, current atmosphere circulation anomaly, forgoing loohpa geopotential height anomaly and sst anomaly in northwest indian ocean are particularly discussed
分析了華北地區近50年來氣溫的氣候特徵，重點討論華北冬季氣溫同期環流異常情況和前期100hpa高度場異常、西北印度洋海溫異常特徵，簡單闡述了關鍵海區海溫異常影響華北冬季氣溫的可能機制。 -
The sea surface high anomaly ( ssha ) indicates that winter and summer are dynamically active seasons
海面高度距平分佈表明冬夏季為動力上活躍的季節。 -
( 5 ). winter air temperature in north china has important relationship with the mongolia high anomaly, the east asian trough anomaly and the acreage of polar vortex anomaly
（ 5 ）華北冬季氣溫與蒙古冷高壓異常、東亞大槽異常、極渦面積異常密切相關。
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