海洋溫差 的英文怎麼說

中文拼音 [hǎiyángwēnchā]
海洋溫差 英文
ocean thermal gradients
  • 洋 : Ⅰ名詞1 （海洋） ocean 2 （洋錢） silver coin 3 （姓氏） a surname Ⅱ形容詞1 （盛大; 豐富） vast; m...
  • 溫 : Ⅰ形容詞（不冷不熱） warm; lukewarm; hot; gentle; mild Ⅱ名詞1 （溫度） temperature 2 （瘟） acute ...
  • 差 : 差Ⅰ名詞1 （不相同; 不相合） difference; dissimilarity 2 （差錯） mistake 3 [數學] （差數） differ...
  • 海洋 : seas and oceans; ocean; [詩歌用語] blue海洋霸權 maritime hegemony; 海洋保護區 marine preserve; 海...
  • 溫差 : [物理學] difference in temperature; range of temperature
  1. Areas that are well protected from the ocean experience a more continental type of climate with warmer summers, colder winters, greater daily and seasonal tempe - rature ranges, and generally lower relative humidity

    種植區域逐漸由海洋性氣候變為大陸性氣候，夏天炎熱，冬季寒冷，每日和季節性的溫差較大，並且濕度相對較低。
  2. The waters of the western equatorial pacific are warmer than in the eastern equatorial pacific, and the difference in temperature between these two areas could produce greater temperature swings between the normal weather pattern and el nino, they wrote

    西赤道太平洋的海表溫度高於東赤道太平洋，這兩個地區的溫度差會加大地球溫度在正常模式和"厄爾尼諾"之間的變化。
  3. ( 2 ) ln winter of the northern hemisphere, because of the difference in the land - ocean distribution, the temperature nowadays is lower than that of 14mab. p. simulated in the upper layer but higher in the middle layer ( about 200 - 1500m ). in deep ocean the discrepancy of temperature seems hardly to be obvious

    （ 2 ）北半球冬季，由於海陸分佈的差異使得海溫在海洋上層古海溫要暖于現代，在海洋中上層（約200 ? 1500米）現代的海溫則要暖於14mab
  4. 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。
  5. The paper delineates the general principles, the state of art and development tendencies of power generation by making use of oceanic temperature differences, wave rocking energy and tidal energy

    闡述了海洋溫差發電、海洋波浪發電及潮汐潮流發電的原理、現狀及發展趨勢。
  6. The experimental models not only can be introduced into low temperature waste - heat power generation, but also can be available in the geothermal, solar and ocean thermal gradient power generation

    該項研究的實驗模型不僅可以利用在低溫余熱發電系統，而且對地熱、太陽能及海洋溫差發電均有參考價值。
  7. The differences of some physical components including the atmospheric index, anomalous height at 500 hpa geopotential in northern hemisphere and anomalous ssts for spring ( february april ), between typical spring chilling years and typical spring warm years are obvious

    典型的春季低溫和高溫年份，亞洲中高緯度大氣環流，西太平洋副熱帶高壓以及太平洋熱帶海洋狀況都有顯著的差異。
  8. Monsoons are large - scale wind systems caused by differences in the temperatures of land and sea over the seasons

    隨著季節演變，陸地和海洋出現溫度差距，因而形成的大尺度風系統，就是季候風。
  9. In this text we make a diagnosis of linear and nonlinear response of quasi - quadrennial ( qq ) and quasi - biennial ( qb ) component of nino3. 4 index by using reanalyzed ncep / ncar data of sst, wind stress ( pseudo stress ) field, ssp, then have a time and spatial analysis of wind stress field by using mssa, and finally find the importance and contrast the effect of different wind stress field forcing the sea so as to find the cause ofenso irregularity

    本文首先分析海表溫度（ sst ） 、風應力場、海表面氣壓（ slp ）等ncep ncar再分析的月距平場對于nino3 . 4指數的準4a （ qq ）和準2a （ qb ）振蕩成分的線性和非線性響應，接著用mssa （多通道奇異譜分析）對風應力場進行時空特徵分析，最後用一個熱帶太平洋動力海洋模式研究具有不同振蕩性質的風應力場對海洋強迫作用的重要性及差異，尋找enso不規則性的原因。
  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. In this paper, decadal variability of tropic and north pacific ' s ssta and of precipitation in china, correlations between them and the possible mechanisms of the ssta decadal change compacting on the precipitation decadal change are analyzed by using ncep globe temperature, wind and height data ( 1948 - 2001 ), coads ssta data ( 1900 - 2001 ) and 147 stations " precipitation data in china. results show that : ( 1 ) mid - high latitude north pacific and tropic west pacific ssta have obvious decadal change, the prior ' s decadal change has great variance and the latter ' s has great contribution in total variance, the main eigenvectors " distribution are stable in eof of tropic and north pacific ssta ' s decadal variability, the key area of the first eigenvector allots in two sides of tropic pacific ; the second one ' s allots in mid - high latitude northwest pacific and low latitude mid - east pacific which vary contrary ; the third one ' s allots in middle north pacific

    本文利用ncep資料（ 1948 - 2001年）中的全球表面溫度場、風場、高度場資料， coads （ 1900 - 2001年）海表面溫度距平資料及中國147個站點1951 - 2001年共51年的降水資料，探討了熱帶及北太平洋ssta 、中國降水的年代際變化特徵，夏季熱帶及北太平洋ssta年代際變化與中國夏季降水年代際變化的耦合相互關系以及夏季熱帶及北太平洋ssta年代際變化影響中國夏季降水年代際變化的可能機制，結果表明： （ 1 ）北太平洋中高緯與熱帶西太平洋均有明顯的年代際變化，北太平洋中高緯年代際變化方差顯著，而熱帶西太平洋年代際變化方差貢獻顯著。
  12. After examining more than 40 years of temperature data taken from roughly 10, 000 surface stations, researchers from the national oceanic and atmospheric administration and from the university of reading in the u. k. found that temperature differences between day and night appear to follow distinct five - days - on, two - days - off patterns

    英國國家海洋及大氣管理局和英國國立瑞丁大學的研究員分析了約一萬個地面氣象站40多年來採集的氣溫數據。他們發現晝夜溫差出現明顯的五天大兩天小的變化規律。
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