ocean temperature 中文意思是什麼

ocean temperature 解釋
海水溫度
  • ocean : n 1 洋，大海；（有別于內海的）外洋。 ★ 英國用 sea 的地方，美國常用 ocean 如：spend some weeks by ...
  • 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. Decadal variability and abrupt change of upper - ocean temperature in the pacific

    太平洋次表層海溫年代際變率及其突變特徵
  3. Inter - decadal change of sea surface temperature and its interaction between tropical pacific and indian ocean in summer and winter

    印度洋海表溫度年際異常的年代際變化
  4. The variations of sea ice in the arctic ocean are simulated by using a improved high resolution hibler dynamic - thermodynamic sea ice model during 1979 - 1998. the model is driven by surface atmospheric and oceanic forcing consists of geostrophic winds, surface air temperature, specific humidity, and longwave and shortwave radiative fluxes provided by international arctic buoy program ( iabp ). the simulated results show that arctic sea ice have noticeable seasonal and annual variability

    利用一個hibler海冰熱動力模式，在改進了其熱力部分和改變模擬范圍以及提高解析度的基礎上，以北極國際浮標計劃（ iabp ）提供的1979 - 1998年間逐日變化的日平均海平面氣溫場，濕度場，長短波輻射場，風場，洋流場，海洋熱流量場為強迫場，模擬了上述20年間北極海冰的時空演變。
  5. It is found that mld based on a temperature change from the ocean surface of 0. 5 degree celsius is deeper, especially from jan. to apr., while mld based on a variable density change from the ocean surface with a temperature change of 0. 5 degree celsius is shallower

    分析表明，基於溫度階躍0 . 5得到的mld較深，尤其在1 4月，這可能主要是因為沒考慮mld此時受到的鹽度變化的影響；基於溫差為0 . 5對應的密度定義的mld最淺。
  6. Relation of winter temperature anomaly in dalian to prophase sst over indian ocean

    大連地區冬季氣溫異常與前期印度洋海溫的關系
  7. The same period, the ocean thermal slow, relatively high temperature, air density changes smaller solipsism relative area of low pressure

    同一時期，海洋散熱較慢，溫度相對地較高，空氣密度變化較小，遂形成相對的低壓區。
  8. In this paper, features of decadal variability and the possible mechanism of sea - air system in the pacific are investigated by using upper - ocean temperature, heat storage and wind stress data, the main results are as follows : the most pronounce decadal sign exists at about 160 meter in depth in the western pacific. there are significant decadal abrupt changes in temperature from surface to deep in the subsurface at about 1980. with different depth in the subsurface, there exist 4 types of abrupt change modes, their generation is closely related to the decadal sign which originates from the east of north pacific and propagates along the south - west subduct ion route

    研究表明，太平洋次表層海溫最強的年代際信號在熱帶西太平洋約160m深處，此信號在1980年前後從上至下，先後經歷了一次顯著的年代際突變過程，而且隨深度的不同存在著四種不同的空間突變模態，這四種模態的形成與北太平洋海溫異常的西南潛沉路徑有著密切的聯系。
  9. On the surface of msta, there exists true dipole mode in the indian ocean, that ' s to say that if the temperature anomaly in the western indian ocean is positive, it is much likely that there is negative anomaly in the eastern indian ocean. dipole mode also exists in the pacific as that in the indian ocean. by virtue of the walker circulation and the similar circulation above the indian ocean, it is showed that the air - sea interaction events in the tropical pacific and the indian ocean develop with each other at the same time

    由於在次表層海溫距平極值面上，熱帶西、東印度洋的海溫距平呈真正意義的偶極子模態，即當西印度洋海溫距平為正（負）時，東印度洋海溫距平為負（正） ，偶極子模態的海溫距平分佈在熱帶太平洋同樣存在，兩大洋海溫距平的偶極子模態間有密切的聯系，結合walker環流和印度洋上空的類似walker環流，進而指出熱帶印度洋和太平洋海氣相互作用事件是協調發展的。
  10. It also explain that the correlation between ssta of kuroshio and the change of wind field in equaroral mid - pacific is results of air - sea interaction ; however, when time comes into summer, the instance status of ocean is different from the last winter to next early springtime, the sea surface temperature turn into the definitive factor, so the increase of heat flux in may to jun month which is realized by absorbing more heat from the sun radiation results in the decrease of sst in kuroshio in the season of jun - jul. finally, during the aug to dec season of next year, the sst of kuroshio is increasing again

    最後分析了黑潮海溫與夏季東亞大氣環流及我國降水的時滯關系，發現：當前冬黑潮區域海溫異常偏高時，後期夏季亞洲低壓的強度減弱，西北太平洋副熱帶高壓強度加強，而且位置西伸、偏北，梅雨鋒位置偏南，長江中下游地區降水偏多，北太平洋冬季海域的海溫分佈呈+ 、 - 、 +趨勢（順序為赤道中東太平洋、西北太平洋、我國近海） ；反之亦然。
  11. Temperature and salinity structures in summer marginal ice zone of arctic ocean and an analytical study on their thermodynamics

    夏季北冰洋海冰邊緣區海水溫鹽結構及其形成機理
  12. 17 levitus s. and t. p. boyer, 1994 : world ocean atlas 1994 volume 4 : temperature. noaa atlas nesdis 4, u. s. department of commerce, washington, d. c. 117 pp

    18赫崇本，汪國祥，雷宗友等，黃海冷水團的形成及其性質的初步探討，海洋與湖沼， 1959 ， 2 ： 1 ~ 14
  13. Tectonic movement in interaction with the ocean, atmosphere and living things form the carbon cycle, adjusting the carbon dioxide content in the atmosphere and stabilizing the surface temperature on earth

    板塊運動在與海洋大氣及生物互動下形成碳循環，調節大氣中二氧化碳的含量，從而穩定地球的氣溫。
  14. The thermocline reflects the ocean temperature field ' s important physics characteristics. it has important influence on underwater communication, submarine activity as well as fishery farming and fishing. it has close relations with branch subjects such as ocean current, water mass, inside wave, sea and air exchange

    溫度躍層是反映海洋溫度場的重要物理特性指標，對水下通訊、潛艇活動及漁業養殖、捕撈等有重要影響，並與海洋環流、水團、內波、海氣交換等分支學科關系密切。
  15. This is very odd. there ' s a buoy registering a 1 3 - degree drop in ocean temperature

    真奇怪，有一個浮標顯示13度的海洋溫度下降
  16. The north and south poles greatly influence the atmosphere and ocean temperature, and therefore affect climatic changes throughout the world

    南北兩極對大氣及海洋溫度均有影響，導致全球氣候的轉變。
  17. The researchers have seen what they describe as a “ stunning ” correlation between a rise in ocean temperature over the past 40 years and pollution of the atmosphere

    研究人員已在過去四十年來海水溫度上升和大氣層污染之間，找到他們所描述的令人目瞪口呆的相互關系。
  18. On the basis of saltzman ' s model, we add in aerosol parameter, and modify the cloud feedback mechanism, then set up a sea - ice, ocean temperature nonlinear coupled climatic model which involving aerosol, co2 and cloud parameters

    在saltzman模式的基礎上引入了氣溶膠參數化方案，並對原模式中的雲反饋機制進行了修正，從而建立了一個含氣溶膠、 co _ 2和雲參數的海冰?海溫非線性耦合氣候模式，提高了模式階次。
  19. Then a non - linear model is developed, which includes mechanism of how the concentration of greenhouse gas, especially carbon dioxide, influences the ocean temperature, the atmosphere temperature, and the

    然後，針對描述溫室污染氣體濃度，即二氧化碳濃度對大氣系統，尤其是因此而對海溫、氣溫以及雲量產生影響的非線性模式進行了數值模擬。
  20. He therefore gave his models a series of decade - long tests beginning with the real climatic conditions ( level of solar radiation, ocean temperature and so on ) on 80 different start dates from 1982 to 2001

    於是，他就對自己的模型進行了一系列十年期的試驗，這些試驗開始於從1982年到2001年間的80個不同的起始時間的真實氣候條件（太陽輻射程度、海洋溫度等等） 。
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