thermohaline 中文意思是什麼

thermohaline 解釋
熱鹽的
  1. Based on the two ctd data sets from the cruise of the summertime in 2000 and wintertime in 2001 in bohai sea and the collected historic observed thermohaline data, we analyse systemically the distributional characteristics of temperature, salinity and density in wintertime and summertime in the bohai sea and the results reveal that the current hydrologic characteristics of the bohai sea have some obvious variances relative to the previous research results. in summer there are three low - temperature centers in the middle - layer and underlayer of the middle parts of the bohai strait, liaodong bay - mouth and bohai bay - mouth, but there is a uniform high - temperature center in the middle part of the bohai sea. in winter the isotherms extend westward and northward to the bohai sea from the warm core of the bohai strait and a cold - water tongue off the qinhuangdao spreads southeastward out, so the saddle - like isotherm pattern is formed in the middle part of the bohai sea

    利用2000年夏季和2001年冬季渤海兩次ctd資料和以前收集的渤海溫鹽調查資料,分析了渤海冬、夏季溫鹽密度的分佈特徵,結果表明,渤海現有的水文特徵與以往研究結果相比發生了明顯的變異:夏季在渤海海峽、遼東灣口和渤海灣口中部中、下層存在三個低溫中心,在渤海中部則出現一個上下均勻一致的高溫中心;冬季等溫線以渤海海峽暖中心向西和向北兩個方向伸入渤海,而從秦皇島外海有一冷水舌向東南方向伸展,在渤海中部海域形成「馬鞍狀」等溫線結構。
  2. On base of the data analysis, three - dimensional tide - induced residual currents, the wind - driven and thermohaline currents in the bohai sea are diagnostically computed with an orthogonal curvilinear grid system, by means of a three - dimensional ecomsed model. the winter and summer thermohaline structure and circulation characteristics in bohai sea are analysed, and the circulation variance is discussed preliminarily. the tides and tidal currents in bohai sea are well reproduced

    在資料分析的基礎上,應用三維斜壓ecomsed模式對渤海的潮致余流、風生環流和密度環流進行了診斷計算,分析了渤海冬夏季的溫鹽場結構和對應環流的特徵,並對渤海上述幾個不同時期的環流變異進行了初步的分析和探討。
  3. Based on the thermohaline data in august of 1958 and 2000, january of 2001, january and august in the marine atlas of bohai sea, yellow sea, east china sea ( hydrology, 1992 ), the normal annual wind field data in bohai sea, and the near forty years sss data observed in the four measurement stations beihuangcheng, tanggu, qinhuangdao, huludao of bohai sea : the thermohaline field ' s variance characteristics are analysed

    基於1958年8月、 2000年8月、 2001年1月、 《渤海、黃海、東海海洋圖集( 1992 ) 》中的1月和8月份溫鹽資料、渤海多年平均風場資料以及渤海北隍城、塘沽、秦皇島和葫蘆島4個水文測站近40年的sss觀測資料,分析了渤海溫鹽場的變異特徵。
  4. Review and perspectives of study on thermohaline circulation

    海洋環流模式研究回顧與展望
  5. Huang r x, and x. jin, 2002 : sea surface elevation and bottom pressure anomalies due to thermohaline forcing, part i : isolated perturbations. j phys oceanogr., 32, 2131 - 2150

    張學洪,李薇,金向澤,黃瑞新, 2002 :壓力坐標海洋環流模式的發展和應用前景,自然科學進展(已付印)
  6. Adjustment of the north atlantic thermohaline circulation to the atmospheric forcing in a global air - sea coupled model

    全球海氣耦合模式中熱鹽環流對大氣強迫的響應
  7. Proceeding of modelling studies on the stability and variability of the thermohaline circulation

    大洋溫鹽環流的穩定性及變率模擬研究進展
  8. 3. main control factors of the thermohaline structures in the northern ecs and their climatological variability were concluded as follows

    另外, 124 . 5oe以西及30on以南海域均對黑潮13年左右的年代變化發生響應,振幅越向北越弱。
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