sea ice concentration 中文意思是什麼

sea ice concentration 解釋
海冰密集度
  • sea : SEA = Southeast Asia 東南亞。n 1 海;海洋;內海;大(淡水)湖。2 〈pl 或與不定冠詞連用〉海面(狀...
  • ice : n 1 冰,冰塊。2 〈英國〉冰淇淋,冰淇淋 (= ice cream); 〈美國〉冰涼飲料[點心]。3 冰狀物,糖衣。...
  • concentration : n. 1. 集中。2. 【化學】提濃,蒸濃,濃縮;濃度;稠密度;【礦物】汰選,選礦,富化。3. 集中注意,專心。
  1. Based on the arctic sea ice concentration data and the ncep / ncar reanalysis data, the contemporaneous relationship of the winter sea ice in the sea of okhotsk and its adjacent sea areas with the northern pacific storm track is investigated by statistical analysis methods

    摘要利用北極海冰密集度資料和ncep / ncar再分析資料,運用統計方法討論了冬季鄂霍次克海及其鄰近海區海冰異常與同期北太平洋風暴軸的聯系。
  2. Concentration or arrangement of sea ice

    -海冰密集度或排列狀況
  3. ( 3 ) using the csim4, the arctic sea ice equilibrium state was simulated reasonably. the simulated ice thickness distribution pattern very like that detected by submarine investigations. the simulated ice concentration and motion are similar to the observation

    模擬的海冰厚度分佈與潛艇探測的海冰厚度分佈具有一致性;模擬的海冰密集度、海冰流速與觀測相近,模擬的海冰氣候態是合理的。
  4. Based on observed sea ice concentration data and simulated results, there has been noticeable downward trend in the extent of arctic sea ice during 1979 - 1998. the model shows a substantial reduction of ice advection into the eastern arctic from the canada basin, and an increase of ice export through fram strait, both of which tend to deplete the sea ice of arctic

    模擬結果表明北極海冰有很明顯的季節變化和年際變化,實測的海冰密集度資料和模式模擬結果都證明1979 - 1998這20年間北極海冰的一個最明顯的變化是海冰在不斷減少。
  5. 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。
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