海洋大氣環流 的英文怎麼說

中文拼音 [hǎiyánghuánliú]
海洋大氣環流 英文
general circulation of the ocean
  • : 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...
  • : Ⅰ名詞1 (氣體) gas 2 (空氣) air 3 (氣息) breath 4 (自然界冷熱陰晴等現象) weather 5 (氣味...
  • : Ⅰ名詞1 (環子) ring; hoop 2 (環節) link 3 (姓氏) a surname Ⅱ動詞(圍繞) surround; encircle;...
  • : Ⅰ動1 (液體移動; 流動) flow 2 (移動不定) drift; move; wander 3 (流傳; 傳播) spread 4 (向壞...
  • 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...
  • 環流 : [氣象學] circulation; circulating current; circumferential motion; circular current; ring current...
  1. The atmospheric circulation of the wet year deviate from enso year to no - enso year. in enso year, the subtropical high is strong with the deepening of trough over south of baikal lake while in no - enso year, the subtropical high is weak with the high incidence of typhoons over northwest of pacific and south china sea

    多雨年發生在enso年和no - enso年形式的不同主要表現在: enso年副熱帶高壓較強,貝加爾湖地區南部低壓槽容易加深;在no - enso年副熱帶高壓強度減弱,在西北太平和南地區多熱帶系統活動。
  2. The severe sand dust not only has great effects on the quality of atmosphere environment in cities and on people ' s health, but also can be transported by northwest current to the sea, and exert baneful effects on marine ecosystem

    強沙塵天不僅對城市境質量和人體健康產生影響,而且會經西北輸送和沉降,對中營養鹽的供給和生態系統造成影響。
  3. Sichuan is one of the agricultural province, locates in the area between the continental climate and oceanic climate, the distribution of precipitation is always disproportional due to the influence of atmosphere circumfluence, the existence of drought and floodwater plus water pollution have produced huge menace to agriculture, water resources utilization, soil erosion and even the life and properties of human being

    解決水資源的諸多問題,是擺在全黨、全社會和全國人民面前一項刻不容緩的重戰略任務。四川作為貧水國的一個農業省,由於地處候與陸性候交接地帶,受影響,降水時空分佈不均,水旱災害極為頻繁,尤其是乾旱對農業生產的威脅最
  4. Blue sky : the resplendence of china civilization once again

    西太平溫和北極冰異常對的影響
  5. The relationship between sea surface temperature anomaly in pacific and the circulation of northern hemisphere is the focus of air - sea interaction research in recent years. the ssta in pacific contributes to remote response in mid - latitude atmosphere, and is connected with climate changes in global. the cycling of enso is typical phenomena of large scale in pacific air - sea interaction system

    太平溫異常對北半球異常有重要影響,而enso循是太平耦合系統中典型的異常演變過程,不僅描述了熱帶地區異常現象,而且與中高緯度的候異常變化相聯系。
  6. 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

    最後分析了黑潮溫與夏季東亞及我國降水的時滯關系,發現:當前冬黑潮區域溫異常偏高時,後期夏季亞洲低壓的強度減弱,西北太平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,北太平冬季域的溫分佈呈+ 、 - 、 +趨勢(順序為赤道中東太平、西北太平、我國近) ;反之亦然。
  7. Based on the analysis mentioned above, a conceptual diagram explaining the physical process is put forward : stronger ( weaker ) convective activities in tropical areas stronger upward ( downward ) vertical anomaly stream in tropical areas more ( less ) moisture transports from " key regions " to shandong stronger ( weaker ) hadley and walker circulation stronger ( weaker ) east asian summer monsoon eap ( negative eap ) in 500hpa upward ( downward ) vertical anomaly stream rise in shandong subtropical high abnormally located northward ( southward ) more ( less ) rain in shandong province

    弱季風年與山東夏旱年則相反。通過分析山東夏季降水與東亞夏季風以及異常的物理過程,得出了如下物理概念模型:熱帶印度以及南-熱帶西太平地區對加強(減弱)吟熱帶地區垂直上升(下沉)增強崢熱帶印度和南一西太平地區水汽輸送通量增加。
  8. In order to study the anomaly pattern of summer rainfall in north china and the cause responsible for the anomaly, the climate characteristics of summer rainfall in north china and related circulation pattern, water vapor transport and outgoing long - wave radiation ( olr ) were analyzed in detail in this paper. more attention was paid on studying the relationship between sea surface temperature anomaly ( ssta ) over the north pacific and summer precipitation anomaly in north china and an agcm was utilized to confirm the affection of ssta on the summer rainfall of the north china

    為了揭示華北夏季降水異常規律及其成因,本文詳細分析了華北夏季降水的候特徵及有關的特徵、水汽輸送特徵和向外長波輻射( olr )特徵,著重研究了北太平溫異常與華北夏季降水異常的關系,並應用模式初步驗證了北太平溫異常對華北夏季降水的影響。
  9. This was due largely to the development of an el nino in the year, which was characterized by above normal sea surface temperatures in the equatorial eastern and central pacific. the associated change in atmospheric steering flow caused tropical cyclones over the western north pacific to turn towards the north before entering the south china sea

    厄爾尼諾是指在赤道太平東部及中部出現面溫度異常變暖的現象,它導致的改變,將北太平西部的熱帶旋引導向北移動,相對減少了它們向西移入南的機會。
  10. The sst anomaly of the equatorial eastern pacific and west wind drift region both have influence on the general circulation and summer rainfall in north china, and the influence is nonlinear, which is not only manifested through the intensity change of anomaly of general circulation and summer rainfall in north china, but also through the spatial distribution pattern of the anomaly

    赤道東太平、西風漂溫的異常都會對和華北夏季降水產生影響,這種影響是非線性的,這種非線性關系不僅僅體現在和華北夏季降水異常的強度變化上,也體現在異常的空間分佈形態上。
  11. On base of results above, composite model of ssta in pacific and circulation anomaly are constructed for analysis their evolution. during mature phase of el nino usually in winter, positive ssta dominates in tropical eastern ocean and negative ssta dominates in west wind drift district in mid - latitude ocean, correspondingly the pna index of 500 hpa geopotential height is positive which means the aleutian low gets strong, and the situation is somewhat inversely during la nina phase of ssta

    合成位相反映了太平ssta演變特徵,以及相對應的異常特徵:當西風漂區處于暖態而熱帶中東太平溫偏低時,合成模型當中阿留申低壓減弱, 500hpapna指數為負異常;當西風漂區處于冷態,熱帶中東太平處于暖態( elnino峰值?成熟期ssta典型分佈) ,合成模型中阿留申低壓加強, 500hpapna指數為正異常。
  12. Because the system error is ineluctable for mode, it is necessary to correct the simulation fielde effectively. in this paper, based on the idea of combined eof correction, the interannual simulation of sea surface wind stress anomalies of the tropical pacific ocean by lap two - level atmosphereic model have been corrected, result of corrected erperiment shows that the corrected field is more similar to the observation field, especially on the distribution of the space. three prediction experiments also shew that correcting scheme of combined eof can improve the interannual prediction veracity of model

    在本文中,基於「聯合自然正交展開誤差訂正」的思想,將中科院物理研究所兩層模式輸出的熱帶太平表風應力異常的跨年度模擬場進行訂正,訂正試驗的分析結果表明,訂正後的熱帶太平表風應力距平場與相應觀測場年際變率分量的相似程度遠遠好於模式模擬的結果,尤其是在空間分佈方面的改善非常顯著;三組跨年度訂正檢驗結果也表明,訂正後的跨年度預測結果明顯好於模式的預測結果。
  13. 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,西太平副熱帶高壓以及太平熱帶狀況都有顯著的差異。
  14. Response of the general circulation to western pacific sea surface temperature anomalies and north pole sea ice area anomalies in summer

    西太平溫和北極冰異常對的影響
  15. Based on summer precipitation in north china and the northern hemisphere sea level pressure ( slp ) and the pacific sea surface temperature anomaly ( ssta ) from 1900 to 2001 and ncep data from 1950 to 1999, this paper studies inter - decadal variations of summer precipitation in north china and linkage of it and general circulation of atmosphere ( gca ) and enso cycle using eof and wavelet transform and composite analysis and correlation analysis and so on

    本文採用1900 2001年華北夏季降水量、北半球平面壓( slp ) 、太平表溫度距平( ssta ) 、 1950 1999年ncep資料等,利用eof 、小波變換、合成分析、相關分析等方法,研究了華北夏季降水的年代際變化及其與東亞、 enso循的聯系。
  16. The precipitation character of the middle part of viet nam and its relation to the atmospheric circle. the autumn precipitation of the middle part of viet nam has obvious variations in inter - annual and inter - decade scale with clearly quasi 6a, 10a, 15a period ; in heavy rainfall years, there are a positive anomaly over the north - west pacific and a negative anomaly over japan ; while in deficient rainfall years, the anomaly distribution is on the contrary ; 4. the precipitation character of the south part of viet nam and its relation to the atmospheric circle. the research finds that the rainfall of the south part of vietnam usually concentrates in the autumn every year and a clear difference of atmosphere condition exists between that of flood and drought years

    越南中部降水變化特徵及其與溫的關系越南中部秋季降水具有明顯的年際、年代際變化特徵,具有明顯的準6a 、 10a 、 15a左右的周期;越南中部多雨年, 500hpa高度距平場在熱帶西北太平為正距平,日本附近上空為負距平;而少雨年則相反;越南中部多雨年,熱帶中東太平溫異常偏高,西太平溫異常偏低;少雨年則相反;越南中部多雨年,登陸越南的臺風頻數偏多;而少雨年則相反。
  17. By use of noaa sst and atmosphere circulation datasets, the relation between ssta in pacific and anomaly in circulation is studied

    12間noaa資料集,分析太平ssta與北半球冬季異常的關系,並著重研究溫異常影響下的變化特徵。
  18. By using multi - channel observations of olr, hirs - tb12, erb, vis, ssmr and ssm i on the us satellites, it is analyzed that the global general atmospheric circulation features related to the anomaly of cold vortex over northeast china and it s premonitors are also revealed. it is found that there is an effected chain, which consists of sea ice over northern hemisphere, sea surface temperature in the mid - east equatorial pacific, asia monsoon and local budget of earth radiation in northeast china, on the anomaly of northeast cold vortex. the impacts of each factor in the chain are discussed. the results indicate that the applications of multi - channel satellite observations on research of climate change are of significance

    利用美國象衛星olr , hirs - tb12 , erb , vis , ssmr和ssm i多通道的觀測資料,分析了東北冷渦異常年的全球特徵及其關鍵地區的先兆特徵對于東北冷渦異常,發現了有一個由北半球的冰,赤道東太平溫,亞洲的季風以及東北地區地系統輻射收支組成的影響鏈存在。由此討論了影響鏈上的各因子對東北冷渦異常的作用。結果表明多通道衛星觀測資料的綜合應用在候變化的研究和預測中有著重要的意義。
  19. A study on the relationships between the onset of the south china sea summer monsoon and the anomalies of tropical ocean and atmospheric circulations

    夏季風爆發與熱帶溫和異常變化關系的研究
  20. This thesis is divided into two parts, the first part is the design of the correcting scheme of combined eof for wind stress anomalies simulation field on surface of tropical pacific of lap general circulation model. the second part is. the correcting and exam of the tropical pacific wind stress anomalies for two - level general circulation model

    本論文分為兩部分:第一部分為針對iap兩層模式輸出的熱帶太平表風應力異常的模擬場設計的誤差訂正方案,第二部分為對熱帶太平表風應力異常的模擬場進行訂正試驗及訂正檢驗。
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