teleconnection 中文意思是什麼

teleconnection 解釋
遙聯；遙相關
  1. The positive and negative anomaly centers at 500hpa level formed the anomaly " wave train " from lower latitude to higher latitude over east asia. the teleconnection pattern called east asia - pacific pattern ( eap ) plays important roles in the summer rainfall in shandong area. study shows that weaker okhotsk sea high, northward location of subtropical high and stronger indian low, are likely to lead to more rain in shandong province in summer

    分析對比旱澇年不同層次高度場以及高低層散度場，結果發現，在春夏季旱澇年，高度場幾個主要的距平中心以及115 130 e區域高（ 200hpa ）低（ 925hpa ）層散度場基本呈現出反位相分佈特徵，北半球夏季存在的東亞-太平洋遙相關型（ eap型）對山東夏季降水產生重要影響。
  2. As a result, we find that in winter when the kuroshio is cooler than the normal, at following summer, the continental cyclone deepen and the east asia monsoon strengthen, that the mid - latitude blocking high weaken and zonal circulation develop, the east asia teleconnection of " - + - " is stired up, so that subtropical high weaken and diminish, and tend to east north, tropical monsoon trough strengthen and mei - yu front weaken, and tend to north, meanwhile south asia high weaken and diminish, and tend to eastvnorth, is easy to form eastern region type

    結果發現當黑潮海溫冷異常時，後期夏季大陸熱低壓加深，東亞夏季風偏強。中緯度阻塞高壓減弱，東亞地區緯向環流發展，在東亞-西太平洋地區激發「 - + - 」的東亞遙相關型，從而西太平洋副高強度偏弱，面積偏小，位置偏東、偏北，東亞梅雨鋒也偏弱，季風槽則變強，位置偏北。同時南亞高壓偏弱，位置偏北、偏東，易形成東部型。
  3. There is teleconnection relations between shandong summer rainfall and the convective activities happening in tropical areas in spring and summer accomplished by rossby waves

    通過分析強弱季風年春、夏季熱帶地區olr場的分佈特徵，發現熱帶地區的對流活動與山東夏季降水之間存在著遙相關關系。
  4. Longitude circulations exist in the soohpa height fields in wet. springs and latitude circulations exist in dry springs. the composite : differences of the atmospheric circulation exist in wet springs and dry springs, which appears to be the eu teleconnection pattern of the general circulation

    結果表明，山東省春季澇年與旱年的環流形勢存在明顯的差異：異常多雨年，貝加爾湖以西的廣大中高緯地區高度場降低，我國東部到日本的高度場明顯升高，亞洲中高緯地區呈現緯向環流。
  5. We divided the global june - august precipitation field into 34 subareas and pointed out that there exists evident teleconnection among the june - august precipitation in these subareas

    用reof方法將全球陸地6 - 8月降水場分成34個大尺度降水分區。
  6. 3 ) the teleconnection between winter sst of north pacific and summer precipitation is the areas of equator east pacific and black current with the areas of middle and lower reaches of yangtze river and hetao

    3 ）冬季太平洋sst與我國東部夏季極端降水量的遙相關型主要表現在，赤道東太平洋及黑潮海域的冬季海溫與長江中下游地區和河套地區的遙相關型。
  7. Characteristics of winter atmospheric teleconnection patterns in northern hemisphere and their effects on climate in china

    北半球冬季大氣環流遙相關型特徵與我國區域氣候
  8. 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。
  9. 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。
  10. 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。
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