northwest pacific 中文意思是什麼
northwest pacific
解釋
西北太平洋-
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年大氣環流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，在西北太平洋和南海地區多熱帶系統活動。 -
The master chorale has also appeared as a guest chorus in the kennedy center concert hall with such noteworthy organizations as joffrey ballet, virginia symphony, washington chamber symphony, richmond symphony, and northwest pacific ballet
大師合唱團現在也經常以嘉賓的身份出現在肯尼迪中心音樂堂中，參加演出的主要團體有喬夫里芭蕾舞團，弗吉尼亞交響樂團，華盛頓室內交響樂團，里奇蒙交響樂團和西北太平洋芭蕾舞團。 -
In the northwest pacific domain, the folding age is from late jurassic to middle eocene, and in the tethys domain it is between middle and late eocene
主要褶皺時代很晚，在南北太平洋大地構造域是晚侏羅世至中始新世，在特提斯大地構造域是中晚始新世之交。 -
Preliminary analysis on the relationship between the distribution of fishing ground of pacific saury cololabis saira and sst in northwest pacific
西北太平洋秋刀魚漁場分佈及與海水表層溫度的關系分析 -
The variation in the early aao beget the rainband latitudinal discrepance of the china summer monsoon by means of impacting on the intensity and position of northwest pacific subtropical high in the late summer
前期aao偏強時，後期6 ? 7月長江流域降水將增加，反之亦然。前期aao的變化通過影響後期夏季西北太平洋副高的強度和位置，引起中國夏季風雨帶位置的南北偏差。 -
The climatic characteristics of explosive cyclogenesis in the northwest pacific
西北太平洋爆發性海洋氣旋發生發展的氣候學特徵 -
( 4 ) in summer, tropic west pacific ssta decadal change infect precipitation decadal change in south and north of changjiang river maybe by : positive ssta in tropic west pacific weaken the summer monsoon circulation, lead more precipitation in south of changjiang river and less precipitation in north of it, vice versa ; middle north pacific ssta decadal change infect precipitation decadal change in mid - down valley of changjiang river maybe by : when ssta is negative in middle north pacific, the height field in tropic rises obviously, the subtropical high strengthens and extends westward, the northern limit retreats southward, leads upper trough retreats northward and move eastward, meiyu front moves northward, then leads more precipitation in mid - down valley of changjiang river, vice versa ; middle northwest pacific - low latitude mid - east pacific infects precipitation in north china possibly by change the activity of northeast china cyclone
（ 4 ）熱帶西太平洋ssta年代際變化影響夏季中國長江南北降水年代際變化的可能機制是熱帶西太平洋海表溫度正（負）異常減弱（加強）東亞夏季風環流，從而使江南降水增加（減少） ，江北降水減少（增加） ；夏季中部北太平洋ssta年代際變化影響中國長江中下游地區夏季降水年代際變化的可能機制是中部北太平洋海表溫度負異常，將導致熱帶地區高度場普遍增高，副高加強西伸，副高北界南退，致使高空槽北縮東移，梅雨鋒西移北進，中國長江游中游、中卜游降水增多，反之亦反；夏季中高緯西北太平洋一低緯中東太平洋反向距平分佈結構影響中國東北降水的可能機制是低緯中東太平洋海表溫為負異常。 -
The relationship between cef and china summer rainfall and that between cef and tropical cyclone frequence ( tcf ) in the northwest pacific ( nwp ) are investigated. lt is found that the several branches of cross - equatorial flow have different interannual variability. periodicity and interdecadal variability. the five channels in the lower troposphere in the monsoon region of the eastern hemisphere have different relationships with china summer rainfall. the results also show that there are obvious relation between the interannual variatin of cef and tcf from july to october in the northwest pacific
確定了東半球季風區對流層高低層各支越赤道氣流通道的位置，並探討了越赤道氣流與我國夏季降水和西北太平洋上熱帶氣旋發生頻數的年際變化之間的關系。結果表明：季風區夏季的幾支越赤道氣流具有不同的年際變率、周期以及年代際的變化特徵。夏季季風區對流層低層的5支越赤道氣流的強度與我國夏季降水呈不同的相關型。 -
Origin of mesozonic basins on the northwest pacific margin and the north tethys margin
兩種不同類型的活動大陸邊緣及其動力學機制 -
However, in july 2002, the subtropical ridge did not extend to southern china and the steering flow over the northwest pacific had a more northerly direction than usual. as a result, the tropical cyclones in the region were carried northwards and did not enter the south china sea (
但今年同期副熱帶高壓脊並沒有西伸至華南，使西北太平洋上引導氣流的方向比正常偏北，在該區的熱帶氣旋因此偏向北移，而不向西進入南海（ -
In terms of the ncep reanalysis data, rainfall and temperature data from sixteen stations of china and the tbb data provided by the meteorological research institute of japan, the main features and basic rules of westward extension and withdrawal processes of the northwest pacific subtropical high ( sth ) and its effect on the weather of the east china are investigated in this paper, by composite analysis, theoretical analysis and dynamical diagnosis. based on the relation between the heating and sth, the effects of the distribution of apparent heat source beside the sth on its maintenance and westward extension are also discussed, using the apparent heating to quantitative calculate the complete vorticity equation ( cve ). major results are as follows : ( 1 ) the variation of 500hpa vorticity in the key area ( 115 - 125 e, 20 - 30 n ) is used to indicate the westward extension process of sth
本文利用ncep再分析資料和國家氣象局提供的160站降水和溫度資料以及日本氣象廳提供的t _ （ bb ）資料，通過合成分析、理論分析、動力診斷等方法，詳細分析了六月份西太平洋副熱帶高壓的西伸過程特徵，以及西太平洋副熱帶高壓西進東退的規律及其對我國東部天氣的影響，並圍繞加熱場與西太平洋副熱帶高壓的相互關系這一主題，重點討論了大氣視熱源分佈對西太平洋副高維持與西伸的影響，並運用全型垂直渦度方程對副高形態變異的可能機理進行了研究，得到了以下主要結論： （ 1 ）本文選取了關鍵區（ 115 ? 125 e ， 20 ? 30 n ）內的渦度值來表示副高的西伸過程。 -
Tropic west pacific is the key area which infect precipitation in north of changejiang river greater ; middle north pacific is the key area compacting precipitation in middle and down changjiang river valley and heavier ; and middle northwest pacific - low latitude mid - east pacific are key areas infecting precipitation in north china more obviously
江北降水的關鍵岡影響中國長江中下游地區及其兩側降水的關鍵區在中緯中部北太平洋；影響中國東北降水的關鍵區是中緯西北太平洋與低緯中東太平洋的反向耦合結構。 -
In 2002, none of the tropical cyclones forming over the northwest pacific moved into the south china sea
於二零零二年，所有在西北太平洋上形成的熱帶氣旋都沒有移入南海。 -
Each year, an average of 30 tropical cyclones form over the northwest pacific and the south china sea. of these, about one sixth come close to the south china coast and pose a threat to hong kong
在西北太平洋及南中國海，每年平均有30個熱帶氣旋形成，其中大約有六分之一會移近華南海岸，對香港構成威脅。 -
Usually, the subtropical ridge over the pacific extends westwards to southern china in july, steering the tropical cyclones over the northwest pacific to move westwards and enter the south china sea (
太平洋上的副熱帶高壓脊通常會在七月份向西伸延至華南，這有利西北太平洋上的熱帶氣旋向西移動進入南海（ -
2 ) the olr mjo intensity anomaly for the four key areas of the pacific, namely, the tropical western pacific, the middle and eastern pacific, the northwest pacific and the southwest pacific, is significantly and positively related to the local ssta
2 ）太平洋四關鍵區（熱帶西太平洋、熱帶東中太平洋、西北太平洋、西南太平洋）的olr季內振蕩強度與sst異常呈顯著局地同時性正相關關系。 -
China has kept a close cooperative relationship with the un economic and social commission for asia and the pacific and other relevant organizations, and has made contributions to environmental causes and the development of the asian and pacific regions through participating in the northeast asia environmental cooperation, the northwest pacific action plan, and the regional coordinating unit for the east asian seas action plan
中國與聯合國亞太經社會等組織保持了密切的合作關系，並通過參加東北亞地區環境合作、西北太平洋行動計劃、東亞海洋行動計劃協調體等，對亞太地區的環境與發展作出了貢獻。 -
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。 -
The tropical eastern pacific ( for the whole year ), northwest pacific ( for the boreal spring, summer and autumn ) and southwest pacific ( for the austral summer around ) are the strong mjo regions of sst with the conditions of shallow climatic mixed layer depth
Sst季內振蕩高強度區存在於熱帶東太平洋（終年存在） ，西北太平洋（北半球春夏秋季存在、夏季最強）和西南太平洋（南半球夏季前後存在） ；氣候薄混合層（ mld ）是其存在條件。 -
It is of great importance, for the discussion of global carbon cycle and for the consummation of the global carbon database, to study the coi flux over the east china sea since it is one of the important marginal seas in northwest pacific
東海是西北太平洋邊緣海中最重要的組成部分之一，研究東海海氣界面的co _ 2通量，對于更完整、準確地探討邊緣海區對全球碳循環的貢獻，以及完善全球碳系統參數數據庫有重要意義。
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