水團 的英文怎麼說

中文拼音 [shuǐtuán]
水團 英文
water mass; slug水團花葉素 adifoline; 水團類型 water type; 水團源地 water-mass source region
  • 水 : 名詞1 （由兩個氫原子和一個氧原子結合而成的液體） water 2 （河流） river 3 （指江、河、湖、海、洋...
  • 團 : Ⅰ名詞1 （團子） dumpling 2 （成球形的東西） sth shaped like a ball 3 （工作或活動的集體） group; ...
  1. And the benthos ecosystem also shows a seasonal cycle. the biomass of macrobenthos is higher in autumn while that of meiobenthos tends to be higher in both spring and autumn

    黃海冷水團水域大型底棲動物生物量秋季比較大，而小型底棲動物生物量存在春、秋兩季的高值。
  2. Benthic foraminifer fauna, ams14c dating and acoustic sub - bottom profile was analyzed in the core ey02 - 2 and ey02 - 1 drilled from the muddy deposit in the middle southern yellow sea and the mid - shelf of north east china sea. considering the results of core qc2 ? dz4 and the standard oxygen isotope curves, we discussed the late - quaterenary paleo - environment evolution, benthic foraminifer fauna, paleo - climate, the climate events and water mass in postglacial period, average sedimentation rates, paleo - water depth, origin of sediments, average sea level rise rate in the shelf of south yellow sea and east china sea. at last we discussed the condition of sea level rise in the east china, green house effect and the protection of coastal zone

    本文根據南黃海中部泥質區和東海中陸架的兩個鉆孔巖芯的古生物、 ams ~ （ 14 ） c測年、淺地層剖面等，參考qc _ 2 、 dz _ 4成果及標準氧同位素曲線探討了黃東海陸架晚第四紀古環境演化、底棲動物群特徵、古氣候、冰後期以來氣候事件、古水團、沉積速率、古水深、沉積物源、海平面平均上升率，討論目前中國東部海平面上升的狀況、溫室效應及海岸帶保護。
  3. The result of transport without mixing would be a series of small regions of dyed fluid interspersed with clear fluid.

    只有輸移而沒有摻混，其結果必將在清水中散布著一系列染色水團小塊。
  4. The stratification is very obvious in the vertical profiles of chlorophyll and dissolved oxygen, with high content in the subsurface layer when thermocline exists

    在溫躍層存在季節，黃海冷水團水域的葉綠素和溶解氧含量出現次表層最大值現象。
  5. Climatological analysis of water masses in zhoushan fishing ground and adjacent region

    舟山漁場及其鄰近海域水團的氣候學分析
  6. The yellow sea cold water mass ( yscwm ), as an important oceanic phenomenon in the marginal sea of china, is always the focus of oceanographers

    黃海冷水團是我國陸架淺海上一個重要的海洋現象，一直倍受我國物理海洋學家所關注。
  7. 3. some theories or means, such as box model, one - dimensional advection - difusion models, applied to study on the transportation and the relaionship of biogenic elements

    應用數理統計學的方法對南海垂向水團進行聚類分析，探討南海垂向水團化學要素基本特徵； 3
  8. However it seems that the distribution and abundance of euphausia superba was related to the cold water mass exist at 30 - 100 m, and with the confluence area between the high and the low chi a centers at 25 m depth

    調查期間大磷蝦的分佈與表層水溫、鹽度及葉綠素的關系不明顯，但似乎與30 - 100m處的冷水團和25m深度處的葉綠素高值中心和低值中心的交匯區有關。
  9. 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
  10. Based upon the analysis of the data obtained during the survey, it can be concluded that : 1 ) the number of biomass of macrobenthos in the yellow sea and the east china sea in autuma is higher than that in spring, while the number of density of macrobenthos in autumn is lower than that in spring ; 2 ) the number of biomass of macrobenthos in the yellow sea is higher than that in the east china sea ; 3 ) the number of species in the yellow sea is lower than that in the east china sea ; 4 ) one of the characteristics of distribution of macrobenthos in the east china sea is that the species richness increased from the coastal waters to the offshore deep waters, from the north to the south. 5 ) the species composition in the deeper part occupied by the cold water mass of the yellow sea is more stable than that in the coastal part of the yellow sea in the late 40 ~ 50 years

    通過以上幾方面的分析，結果表明： 1 ）黃東海調查海域的秋季總生物量均高於春季，總棲息密度則低於早春季； 2 ）黃東海春季生物多樣性指數高於秋季； 3 ）南黃海、東海的水文特點顯著不同：東海底溫顯著高於南黃海底溫，東海底鹽亦高於南黃海底鹽； 4 ）南黃海春秋季生物量分佈無一致規律，東海春秋季生物量除長江口外基本上自近岸向外海逐步降低； 5 ）東海大陸架大型底棲動物的種類組成較南黃海更豐富； 6 ）東海大型底棲動物的分佈特點之一為：種類數由北向南、由近岸（西部）向外海（東部）逐漸增多； 7 ）在黃海冷水團控制的海域，其底棲動物種類組成較近岸海域穩定； 8 ）幾個生物多樣性指數各有側重，都能較好地反映底棲動物的分佈特點
  11. Therefore, the surface mid east china sea is a sink of atmospheric co2 ( especially in summer ), even though there are abundant freshwater with high content of co2 input to it

    當然，在沖淡水與陸架水的交接處（包括水團的交接處和有上升流的地區）生物活動亦是強烈的，因此coz匯區的范圍進一步擴大。
  12. During the periods of 12ka, 60ka, 118 - 130ka, the decreasement of summer monsoon resulted in the decreasement of sw monsoon, then correspondingly, the less high salinity water mass make this area low salinity

    在12ka 、 60ka 、 118 - 130ka 、 240 - 250ka幾個時期由於夏季季風的減弱，引起西南季風流減少，從西邊過來的高鹽度水團的減少使該區鹽度降低。
  13. The bohai, yellow and east china seas connect together. they lie east to the largest continent and west of the deepest ocean. the water masses formation and variety have many characteristics and the synoptic become complex

    連綿一體的渤海、黃海、東海有著獨特的地理環境，它背靠全球最大最高的大陸，瀕臨最大最深的大洋，海域中水團水系的形成與變性有著諸多突出的特徵，所以該區域的氣候特徵和大氣變化因深受海洋的影響而更加復雜。
  14. The condition of profiles in outer station did n ' t change much in spring cruise, but showed more variable in near - shore stations when observed in different time. fluorescent characteristic per cell can be obtained by flowcytometric analysis. based on fluorescence data of synechococcus of all stations, two distinctly pigment - containing cell types coexisting can be found in some stations of east china sea, which located in all depth of p3, mixlayer of e7, 40 - meter depth of e6 of autumn cruise and in mixlayer of p2 of spring cruise

    通過對流式細胞計測量的細胞熒光結果來看，在秋季的p3 、 e7整個混合層、 e6站40米層，春季的p2站均發現有兩群不同色素含量的聚球藻（ high一pe和low一pe ）共存現象，極有可能分別屬于不同品系，春季共存站位位置比秋季時更靠外，表明在秋季p3 、 e7等站位的共存是季節性現象，可能與此季節黑潮次表層水沿陸架坡涌升入侵到中陸架有關，水團的運動及混合使從外海遷移而來的high一pe與近岸的low一pe得以共存，在春季，由於長江沖淡水的日漸強盛，在中陸架區的共存區域有所外移。
  15. 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。
  16. The shallow thermocline distributes in the areas of guangdong, guangxi, fujian and vietnam continental shelf, with obviously seasonal variabilily, and at the same time, in the south and middle areas of nanhai, even in winter when there is no thermocline in the coastal area, there also exists the shallow thermocline

    後者廣東、廣西、福建沿海陸架區則與黃、東海相同，表現為季節性溫躍層，有成長、強盛、消衰、無躍層的年周期變化過程。南海深溫度躍層基本屬於水團疊置型，躍層分佈范圍及躍層強度、上界深度、厚度與氣候關系不大。
  17. Generally, the model is competent for the simulation of energy flow characteristics of the ecosystem in the yscmw. the analysis of the sensitive tests suggests that the phytoplankton biomass is controlled

    對整個黃海冷水團水域營養鹽的循環收支分析結果表明:浮游植物光合作用的吸收是黃海冷水團水域營養鹽的最大損耗項，有機物分解是其重要源項。
  18. The numerical simulation with complete forcing produces the main characteristics of yellow and east china seas circulation in summer. baroclinic effect plays a important role on yellow seas circulation that yellow seas cold water mass induces a anticlockwise circulation. tide also strengthens it

    夏季黃海的環流結構體現了較強的斜壓性，主要以密度流為主，黃海冷水團在黃海中部誘導了一個氣旋式環流，潮汐作用亦對這一環流有貢獻。
  19. The vertical flux between compartments of the model system is also taken into account. basic characteristics of the seasonal variations of the pelagic - benthic coupling ecosystem in the yscmw are simulated. compared with the observations and the related studies in this region, it is found that the seasonal cycle of ecosystem is well represented and the relationships between variations and different layers are acceptable

    通過該模型對黃海冷水團水域生態系統各生態變量的季節變化進行了模擬，並同黃海冷水團水域的觀測資料及相關文獻分析對照，證明模擬結果能較好地反映出黃海冷水團水域生態系統的季節變化特徵，各個生態變量間的關系及不同水層間的生態變化差異是比較合理的。
  20. In this paper, zooplankton communities, their species composition and indicator species in the east china sea and the yellow sea were examined with multivariate methods. in the southern part of the yellow sea, where was known as an important spawning ground of anchovy, the seasonal variations of zooplankton were studied in details with respect to species composition, abundance, biomass and vertical distribution. furthermore zooplankton indication of the yellow sea warm current ( yswc ) in winter was discussed

    本論文用數理統計方法（包括：雙向指示種分析、多維定標序列分析、判別分析和多元回歸分析）對春、秋兩季東、黃海浮遊動物群落進行了劃分、確定各群落的指示種；對南黃海浮遊動物的種類組成、分佈及其時空變化進行了研究，並與歷史資料進行了比較；並探討了黃海冷水團對某些浮遊動物的意義，以及浮遊動物對黃海暖流指示。
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