sea temperature 中文意思是什麼

sea temperature 解釋
海水溫度
  • 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...
  • temperature : n. 1. 溫度，氣溫。2. 體溫。3. 〈口語〉發燒，高燒。
  1. Amore 2001 has successfully investigated the gakkel ridge and arctic ocean in vicinity of its geological and geophysical nature, as well as the nature of sea ice and biology in this area. the preliminary onboard petrology and bathymetry results show that the mantle beneath the gakkel ridge with low temperature has only encountered very low degree partial melting during the spreading and there is no any direct relationship between the crust nature and the spreading rate along the gakkel ridge in any simple petrologic way. mantle temperature and fracture zone density also play a major role on the crust nature, besides spreading rate

    對所取得資料的初步研究表明gakkel洋中脊之下的地幔僅經受了較低程度的部分熔融，具有較低的溫度。 gakkel洋中脊處的地殼性質和巖漿活動與擴張速率之間不存在任何直接的巖石學相關性，擴張而導致的巖石圈頂部的冷卻並不是決定洋脊處地殼性質的最重要因素。地幔溫度和斷裂帶的存在與否及其密度對地殼性質具有重要的影響意義。
  2. Genetic analysis shows that it may be caused by the difference of the response of each area to winter monsoon ' s abnormal, the kuroshio and our offshore is influenced mostly by heat flux between the sea and atmosphere, but in the other areas, the abnormal current incited by abnormal wind has decisive effect on the change of the sea temperature, at the same time, air pressure also has some impact on the sea temperature

    其區域性形成的原因主要可能是因為各海區對冬季風異常的響應方式不同，強冬季風使得黑潮與我國近海海洋過多散熱，海溫降低；在西北太平洋暖池北部，強冬季風引起西風異常，從而引發異常氣旋性環流，海水輻合下沉加熱其表層以下海水，同時異常環流使得更多東側異常暖水向西加熱其表層水；在黑潮與親潮交匯處的升溫也主要是由於強冬季風導致的流場異常，海水輻合下沉升溫。
  3. The kalman filter is introduced and explored by assimilating sea temperature observations into one - dimensional numerical temperature model, which is decomposed into two parts, one part is the certain, the other is the random. then a data assimilation model is set up, it can assimilate sea temperature continuous observations data

    在此基礎上，利用kalman濾波原理，以一維海溫垂直分佈的數值模式為例，通過對原模式進行分解，得到確定性模式和隨機過程兩部分，繼而建立了一個可同化海溫連續觀測資料的數據同化模式。
  4. But only for the closure of indonesia passage, warm pool can be formed under 150m with the center between 300m and 600m or so while in upper layer the modern sea temperature is still colder, so seen from the simulation, only the open of indonesia passage can not form the warm pool like the present

    P ）模擬的海溫要暖，形成淺層暖池。但單是上述通道關閉，暖池只形成在150米以下，中心在300 ? 600米深海洋層，而海洋上層（ 150米以上）仍為現代冷。依數值模擬來看，只有上述通道的開啟，並不能形成如現代淺層海洋暖池。
  5. The most obvious sea temperature difference appears between 500m and 600m and the variable amplitude in southern hemisphere is larger than that in northern hemisphere

    模擬的海溫，海溫溫差最明顯的地方出現在500 ? 600米之間。南半球的變化幅度要大於北半球，到海洋深層，海溫溫差變化不是很明顯。
  6. The salinity distribution characteristics are the high - salinity in the bohai bay and the low - salinity in the boahi strait. the density distribution shows that there is a large cyclonic density circulation in bohai sea and it is likely to exist some density current gyre in the middle part of the bohai sea. in winter the saddle - like pattern of the bohai sea temperature and salinity shows that the circulation structure is much complexer than the previous research results

    密度分佈表明：夏季渤海灣口已經由以前的低密度中心變為現在的高密度中心，相應的環流結構也必會發生大的變化；夏季渤海中部會存在一個反氣旋式的密度環流，並在局部可能存在多個密度流渦環；冬季渤海「馬鞍狀」溫鹽結構反映其密度環流結構要比以往研究結果復雜得多。
  7. The variation of sensible heat flux is dominated by air - sea temperature difference. interannual variability of turbulent heat fluxes is examined using svd, eof and mtm methods

    熱帶太平洋enso事件通過對walker環流的調整減小熱帶大西洋itcz區的風速值，湍動熱通量亦隨之減小。
  8. Workshop on the network system for monitoring and predicting enso event and sea temperature structure of the warm pool in west pacific ocean. 5 - 7 february, 2001, macao

    2002熱帶海洋環境與氣候變化研討會，三亞， 2月26日3月1日。王東曉（南海環流模式比較初步結果、太平洋年代際變化的強迫因子、南海環流的多渦結構） 。
  9. The surface of the maximum sea temperature anomaly ( msta ) was constructed from the subsurface sea temperature anomaly data in the tropical pacific from 1955 to 2002. it is quite similar to the depth distribution of the 20 ? c isotherm, which is usually used to represent the center of the thermocline layer

    利用1955 - 2002年48年熱帶、副熱帶太平洋地區次表層溫度距平資料，構造了溫度距平極值深度分佈的曲面圖（ msta ） ，它很接近20溫度面的深度分佈，因此有理由認為這一深度曲面很接近熱帶溫躍層的深度面。
  10. Results show that the interdecadal anomalies are more significant in the variance of the system anomaly in the north pacific ( np ), and the interannual and interdecadal anomalies are about equivaleut in the tropical pacific ( tp ) ; the interdecadal change characters of the surface ( shallow ) layer of the ocean and the atmosphere aloft are unanimous in the same season and region, and their transition from a low mode to a high mode both occurred from the end of 1970s to the beginning of 1980s, with an exception for july in the np, which is related to the stability of the stratification of sea temperature within the sub - surface layer ; the interannual scale air - sea anomalies are associated with enso, is most typical for january, then july in the tp, followed by january in the np, and there is no visible relationship for july in the np

    在海氣系統異常的方差構成中，北太平洋區域以年代際異常為主，熱帶太平洋區域年際和年代際異常相當；表（淺）層海洋與大氣的年代際變化特徵對同一季節、區域是一致的，且20世紀70年代後期到80年代初均發生由低模態向高模態的轉變；北太平洋區域的7月與此不同，這與該季節近表層海溫層結穩定有關；年際尺度的海、氣異常與enso有關，且以熱帶太平洋區域1月最典型， 7月次之，北太平洋區域1月再次之， 7月無明顯關系。
  11. There is marked correlation between snow anomaly and east pacific sea temperature, after heavy ( light ) snow years in eurasia, sea temperature increase ( chill ) gradually, we can find there is contact between eurasian snow cover and el nifio ( la nina ) event to a certainty

    異常與次年秋季、冬季赤道東太平洋海溫異常之間的相關顯著，赤道東太平洋海溫的年際變化也表現出了歐亞冬季出現重雪（輕雪）后的次年，從夏季到冬季赤道東太平洋海溫逐漸增暖（變冷） 。
  12. Sir david said " there is no question that intensity of hurricanes is dependent on surface sea temperature

    金說： 「毫無疑問，颶風強度的大小取決于海洋表面溫度的高低。
  13. At around 0642utc, almost 6 degrees above the sea temperature

    9度，比海面溫度高出近6度。
  14. 1961 - 1990 normals for hong kong graphical data : mean sea temperature

    香港氣象平均值1961 - 1990圖像資料:平均海水溫度
  15. Mean sea temperature

    平均海水溫度
  16. " the point is that there is nobody arguing that higher sea temperature does not create more intense hurricanes

    現在沒有誰會爭辯說較高的海面溫度不會造成強度更高的颶風。
  17. The closure of indonesia passage causes the modern simulated sea temperature warmer than that of 14mab. p

    印度尼西亞地區的海流通道的關閉，使得海溫在中層現代比古代（ 14mab
  18. If an area has been covered by clouds for a long period, the sea temperature over the area on the image may represent observation days ago

    如一個地區長時間被雲所覆蓋，則該區顯示的海水表面溫度可能代表多日前的觀測。
  19. J. cloud height above msl : few 1500 sct 2500 ft sct 8000 ft k. visibility : 8 km tempo 3000 m in mist haze rain l. 0 deg. c level : 16000 ft 10 deg. c level : 10000 ft m. turbulence : mod offshore n. sea state : 2. 0 - 2. 5 m sea temperature : 23 deg iv

    四雲量及雲底高度:少雲3000英尺疏雲8000英尺五能見度: 8公里，有薄霧煙霞可低至3000米六0 c高度: 16000英尺10 c高度: 10000英尺七湍流:離岸有中度湍流八海浪高度: 2 . 0 - 2 . 5米海水溫度: 23度攝氏iv .展望:吹和緩至清勁偏東風。
  20. As the sea temperature following the hatching time then in 2000 was too low for immediate release of this batch of baby turtles, the ocean park helped in taking care of the turtles for about a year before eventually releasing them back to the sea

    該批小海龜在孵出后未能即時放生，是由於當時海水溫度太低，故由海洋公園協助照顧海龜約一年，然後才放回大海。
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