intraseasonal 中文意思是什麼

intraseasonal 解釋
季內
  1. Furthermore, the zonal propagation of the intraseasonal oscillation ( iso ) of the sh subtropical high is also documented. results show that the australia high ( ah ) is influenced by the mascarene high ( mh ) through the eastward propa gation of the quasi - biweekly oscillation

    另外還分析了南半球副熱帶高壓低頻振蕩的緯向傳播，指出馬斯克林高壓（馬高）對澳大利亞高壓（澳高）的影響主要通過準雙周低頻振蕩的東傳得以實現。
  2. In contrast, the out - of - phase vacillation in summertime ao covers the arctic region and mid - latitude asian continent. though the summertime ao exists on intraseasonal as well as interannual time scale, its asian active center abates on the intraseasonal pattern, thus awarding it more conspicuous zonal symmetric structure. interannually, summertime ao exhibits the zonal asymmetric and baroclinic features, and its seesaw mode is significant only in the lower troposphere

    在年際時間尺度上，夏季北極濤動表現出比冬季北極濤動更強的緯向非對稱性和對流層高、低層位相不一致的斜壓性，其極地中心和亞洲中心的反位相濤動關系在對流層低層比較顯著，向上逐漸減弱，到對流層高層不能表現明顯的亞洲中心。
  3. ( 4 ) the epwp climatologic sst has a clear intraseasonal variability, which is very similar to el nino growth process, i. e., occurring in spring, developing in summer, maturing in autumn and decaying in winter

    進一步分析表明，東太平洋暖池及異常經向風僅對日nino （ lanina ）事件發生、發展起促進（抑制）作用而不起決定作用。
  4. To diagnose the climate changes and anomalies on different time scales ( intraseasonal, seasonal, interannual, decadal and interdecadal ) in climate system, to investigate the formation mechanisms of the climate changes and climate anomalies from the point of view of land - sea - atmosphere interactions in climate system, and to understand the dynamical processes in the climate changes and climate anomalies

    通過動力學診斷方法揭示大氣中時間尺度為一周以上的各種異常氣象現象及其變化，從氣候系統各子系統之間相互作用的角度研究異常氣候的產生機制，增加對氣象異常現象形成的動力學過程的認識。
  5. 5 intraseasonal discrepancy exists in the extremely temperature decrease corresponding with the four type of spring temperature. the cold wave incidence of the heilongjiang type tend to be more in may, while the others in april

    5 、春季氣溫4種空間分佈型態極端降溫過程的分佈存在月際差異，黑龍江地區多出現在5月份，其它地區多出現在4月份。
  6. Based on the ncep / ncar reanalysis products, the sea ice concentration data and the observation rainfall data in china, the seasonal, intraseasonal and interannual variations of the atmospheric circulation in the southern hemisphere ( sh ) are systematically analyzed together with their influences on east asian summer monsoon ( easm ). the major conclusions are summarized as follows : ( 1 ) in the lower level of the troposphere, the semi - annual oscillation ( sao ) is most active along 40 s and 65 s in the extratropics of the sh. over these latitudes, the variance percentages of sao exceed 70 %, and the anti - phase variation of the sea level pressure ( slp ) between the two latitudes is primarily caused by their sao components

    利用ncep ncar再分析資料、南半球海冰密度資料及中國臺站降水資料，本文系統分析了南半球大氣環流的季節、季節內和年際變化特徵及其對東亞夏季風的影響，主要結論歸納如下： （ 1 ）對南半球熱帶外大氣環流而言， 40 s和65 s是低層大氣準半年振蕩最為顯著的兩個緯帶，在這兩個緯帶上，半年波的貢獻都超過了70 ，二者季節變化的反位相主要體現為半年波分量的反位相。
  7. The relationship between the intraseasonal oscillations in the northern hemisphere during the boreal winter in the stratosphere and troposphere

    平均環流場的氣候特徵及其與我國夏季降水關系的初步分析
  8. 2 the intraseasonal variation features of summer precipitation in northeast china are that the 24 percent of summer precipitation concentrate on late - july and first dek of august, i. e. the 12th, 13th and 14th pen of summertime

    2東北地區夏季降水的季內演變特徵為：東北地區夏季降水量的近24集中在7月末期到8月上旬即主要集中在夏季第12 、 13 、 14候。
  9. 6, the intraseasonal discrepancy exists in the temporal distribution of extreme rainfall in northeast china. while extreme rainfall appears in august in the east of liaoning and the northeast of heilongjiang, so does june in other three areas

    6東北地區不同區域極端降水的時間分佈存在月季差異，遼寧東部和黑龍江東北部地區主要出現在8月份，其它3個地區則出現在6月份。
  10. In terms of diagnostic analysis chiefly, including of lanczos filter, single value decomposition ( svd ), ceof, composite and correlation analysis etc., and numerical modeling, the temporal and spatial characteristics of the intraseasonal oscillation ( mjo ) of the air - sea system and the causes are investigated in this paper

    本文對海氣系統季內振蕩的時空特徵及其成因作了氣候學研究。主要採用診斷方法（ lanczos濾波、奇異值分解、復自然正交函數分析、合成分析及相關分析等） ，並結合數值模擬。
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