sst china 中文意思是什麼
sst china
解釋
冠捷半導體-
The results show that the strong winter monsoon will decrease the gradient of ssh, and change the characteristics of sst, which has influence on the sea current, especially in a shallow and closed sea area such as the south china sea
結果表明：強冬季風會減弱海面高度梯度，普遍降低黑潮區海表溫度，對流場有一定的影響，尤其在南海這樣的封閉海區。 -
The activity of cold air and interannual variation of low level jet are important cause of interannual variation of the rainfall in april. interannual variation of subtropic high is the main cause of interannual variation of the rainfall in may over north china. there is significant negative correlation between interdecadal variation of the rainfall in april and that of sst in the areas of equatorial indian ocean and tropic middle - east pacifi
華北4月降水與熱帶中東太平洋、赤道印度洋海溫年代際變化呈明顯的負相關:華北5月降水與熱帶中東太平洋、赤道印度洋海溫年代際變化存在明顯的正相關:熱帶海溫的年代際異常引起的副熱帶高壓的年代際異常可能是影響華北4 、 5月降水異常的重要原因。 -
The temporal and spatial variations of summer precipitation anomaly in northeast china ( nespa ) are studied, and its relations with contemporary circulation anomalies over north pacific ( np ) and sst departure of pacific on the interdecadal and interannual scale are discussed by means of harmonic analysis, reof and svd
採用諧波分析、 reof 、 svd等方法分析了東北夏季降水異常的時空特徵，並按年代際、年際尺度分析了它與同期北太平洋區域對應尺度環流、相關海表溫度異常的聯系。 -
The sst anomaly of the equatorial eastern pacific and west wind drift region both have influence on the general circulation and summer rainfall in north china, and the influence is nonlinear, which is not only manifested through the intensity change of anomaly of general circulation and summer rainfall in north china, but also through the spatial distribution pattern of the anomaly
赤道東太平洋、西風漂流區海溫的異常都會對大氣環流和華北夏季降水產生影響，這種影響是非線性的，這種非線性關系不僅僅體現在大氣環流和華北夏季降水異常的強度變化上，也體現在異常的空間分佈形態上。 -
( 5 ) the spring greenland sea - ice extent is larger ( smaller ) : then during the following summer the high of the japanese sea is stronger ( weaker ), and the low of the asian land is stronger ( weaker ), which make the pattern of low west and high east easily ( uneasily ) form ; the ascending movement over north china is strengthened ( weakened ) ; the summer monsoon of east asia is stronger ( weaker ), then the southeastern, warm and damp airflow towards the north china is stronger ( weaker ), and the cold airflow of the high level over the north china is also stronger ( weaker ), which make the convergence of the cold and warm air over north china easily ( uneasily ) form ; the sst of the east pacific ocean is lower ( higher ), while the sst of west wind drift is higher ( lower )
（ 5 ）春季格陵蘭海冰面積偏大（小） ：後期夏季日本海高壓偏強（弱） ，而大陸上低壓也偏強（弱） ，易（不易）形成西低東阻的形勢；華北地區的上升運動增強（減弱） ；東亞夏季風偏強（弱） ，向華北地區輸送的西南暖濕氣流偏強（弱） ，而對應高空華北地區上空冷空氣活動偏強（弱） ，利於（不利於）華北上空冷暖空氣的交匯；夏季赤道東太平洋海溫偏低（高） ，西風漂流區海溫偏高（低） 。在以上的環流背景下，華北夏季降水偏多（少） ，易澇（旱） 。 -
The precursor in northern hemisphere circulation and sst fields for east china s ummer rain patterns
北半球冬季環流的特徵緯向波數及其時空演變 -
Finally, the possible physical mechanism by which the sst of the north pacific affecting eastern china summer rainfall was elementary discussed by numerical simulation using model ccm3
最後，運用數值模式ccm3對太平洋海表溫度對東部夏季降水的影響機制進行初步研究。 -
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 this article, based on the rainfall data over north china in spring and respective month, atmospheric circulation data ( ncep ) and the sea surface temperature data ( sst ), the methods of eof analysis, yamamoto analysis, mesa analysis, correlation analysis and composition analysis are used to study totau spatial and temporal distribution characteristics of the rainfall in spring and respective month over north china, investigate correlation with interannual andinterdecadal variation of sea surface temperature and atmospheric circulation, and analyse mechanism of influence
本文用華北春季及春季各月降水資料， ncep資料以及coads海溫資料，採用eof分解、 yamamoto分析、最大熵譜分析、相關分析、合成分析等方法研究了華北春季、各月降水的總體分佈特徵及時空分佈特徵，並從總體上探討了其與海溫、大氣環流年際、年代際變化的關系及其影響機制。 -
The main coupled mode of ssw and sst in the tropical pacific - south china sea - tropical indian ocean on interannual time scale
印度洋海面風與海面溫度年際變化整體耦合的主模態 -
Thesis gives cargo tracking mode and architecture as well as thoughts when enterprises carry out co - operation cargo tracking system. to state cargo tracking co - operation between china national foreign trade transportation ( group ) corporation ( sinotrans ) and guangdong south satellite telecommunication service co. ltd ( sst )
論文以中國外貿運輸總公司和廣東南方衛星通信服務有限公司進行協同跟蹤為例，提出了協同跟蹤模式，並給出了跨省際的物流運輸企業建設協同跟蹤系統的總體框架和思路。 -
This paper is concerned with the time - spatial characteristics of summer extreme precipitation over eastern china and with the teleconnection between summer extreme precipitation and sst of the north pacific and soi, based on the daily rainfall data of 59 stations from 1951 to 2000
本文利用我國東部（ 105e ~ 0以東） 59個測站1951 - 2000年的夏季逐日降水資料對我國東部夏季降水極值的時空特徵及其與北太平洋海溫和南方濤動指數（ soi ）的遙相關進行研究。 -
Results show, 1 ) the teleconnection between extreme precipitation of ease china and the same season sst of north pacific is mainly in nino area ( nino 1 - 2 area most ) ; the plus connection area between nino1 area and the next summer extreme precipitation is in middle and lower reaches of yangtze river
結果表明， 1 ）我國東部夏季極端降水量空間分佈與同期太平洋sst的遙相關型主要集中在整個nino海區（以nino1 - 2區為最） ； nino1區與次年夏季極端降水量的相關主要表現在與長江中下游區的正相關型。 -
Based on the empirical orthogonal function ( eof ), the characteristics of large scale variations of precipitation anomaly during rainy season ( from jun to aug ) in south - west china for the period 1961 1995 is analyzed, and the teleconnection distribution charac - teristics between sea surface temperature ( sst ) over india ocean and precipitation during rainy season in south - west china were studied by using the method of cca
用自然正交函數展開方法對1961 1995年西南汛期（ 6 8月）降水大尺度變化特徵進行分析，並在此基礎上用典型相關分析方法研究了1 8月印度洋海溫距平場與西南汛期降水場的遙相關分佈特徵。 -
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。 -
5 the positive correlation exists between the summer rainfall in northeast china and nino3 sst
5東北地區夏季降水同nino3區海溫場有較好的正相關關系。
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