降溫異常 的英文怎麼說

中文拼音 [jiàngwēnyìcháng]
降溫異常 英文
cooling anomaly
  • 降 : 降動詞1. （投降） surrender; capitulate 2. （降伏） subdue; vanquish; tame
  • 溫 : Ⅰ形容詞（不冷不熱） warm; lukewarm; hot; gentle; mild Ⅱ名詞1 （溫度） temperature 2 （瘟） acute ...
  • 異 : 形容詞1 （有分別; 不相同） different 2 （奇異; 特別） strange; unusual; extraordinary 3 （另外的;...
  • 降溫 : 1 （降低溫度） lower the temperature （as in a workshop）; cooling; hypothermia; hypothermy 2 [氣...
  1. The activity of cold air and interannual variation of low level jet are important cause of interannual variation of the rainfall in april. interannual variation of subtropic high is the main cause of interannual variation of the rainfall in may over north china. there is significant negative correlation between interdecadal variation of the rainfall in april and that of sst in the areas of equatorial indian ocean and tropic middle - east pacifi

    華北4月降水與熱帶中東太平洋、赤道印度洋海溫年代際變化呈明顯的負相關:華北5月降水與熱帶中東太平洋、赤道印度洋海溫年代際變化存在明顯的正相關:熱帶海溫的年代際異常引起的副熱帶高壓的年代際異常可能是影響華北4 、 5月降水異常的重要原因。
  2. 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。
  3. This pattern of ssta distribution is related to summer rainfall anomaly of north china by means of the tropical convection activity and general circulation in the middle and high latitude

    這種海溫異常分佈型可通過夏季熱帶對流活動和中高緯大氣環流與華北夏季降水異常產生聯系。
  4. Further, correlation analysis is used to the summer rainfall and four seasonal north pacific ssta, the results suggest north pacific ssta which notability cause the summer rainfall anomaly over eastern china are prophase winter ssta of kuroshio region of northwestern pacific, prophase spring ssta of middle and eastern equatorial pacific and summer ssta of west wind drift region

    進一步對上述東部夏季降水異常區夏季降水與春夏秋冬太平洋海溫異常作相關分析，表明對中國東部夏季降水有顯著影響是：西北太平洋黑潮海區前期冬季海溫異常、赤道中東太平洋前期春季海溫異常、中高緯太平洋西風漂流區同期夏季海溫異常。
  5. 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氣候特徵及有關的環流特徵、水汽輸送特徵和向外長波輻射（ olr ）特徵，著重研究了北太平洋海溫異常與華北夏季降水異常的關系，並應用大氣環流模式初步驗證了北太平洋海溫異常對華北夏季降水的影響。
  6. The temporal and spatial variations of summer precipitation anomaly in northeast china ( nespa ) are studied, and its relations with contemporary circulation anomalies over north pacific ( np ) and sst departure of pacific on the interdecadal and interannual scale are discussed by means of harmonic analysis, reof and svd

    採用諧波分析、 reof 、 svd等方法分析了東北夏季降水異常的時空特徵，並按年代際、年際尺度分析了它與同期北太平洋區域對應尺度環流、相關海表溫度異常的聯系。
  7. Data used in this work are north pacific ssta, 160 stations precipitation of china, and ncep reanalysis data. main results are as follow : ( 1 ) it is found that a apparent transition of north pacific ssta in later 1970 ' s : eastern and middle - equatorial pacific ssta turns from cold to warm with area extending, and mid - latitude pacific ( west wind drift zone ) turns from warm to cold. during this transition of ssta, different characters also appear in el nino and la nina : before 1976, la nina happens more frequently, and its duration is longer, el nino zone develops from negative ssta in the early stage ; after 1976, el nino happens a little bit frequent and longer with more intensity than before, el nino zone develops from positive ssta in the early stage ; the course of ssta variation has an enso cycle of 2 - 6 years, annual oscillation of 8 - 9 years, and decadal variation of about 22 years

    本文採用1950 - 1999年北太平洋海表溫度（ sst ） 、中國160站夏季降水和ncep再分析的歐亞500hpa高度場等資料，利用eof 、 svd 、小波分析、合成分析和相關分析等方法，在分析北太平洋海溫時空分佈特徵的基礎上，著重探討了海溫異常及其年代際變化對我國東部降水的影響，並對降水、高度場和海溫三者之間的關系進行了分析，以試圖尋找三者異常之間可能的聯系，主要結論如下： （ 1 ） 1976年前後，北太平洋海溫經歷了一次明顯的轉變，赤道中、東太平洋厄爾尼諾海區由冷轉暖，暖水范圍增大，中緯度西風漂流區海溫由暖轉冷；在這樣的年代際背景下，厄爾尼諾、拉尼娜事件在不同的時期也有不同的特徵：在76年前，拉尼娜事件發生頻率高，持續時間長，事件起始於負海溫距平；而76年後，則是厄爾尼諾事件發生頻率略高，持續時間長，強度增大，事件起始於正海溫距平。
  8. 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

    赤道東太平洋、西風漂流區海溫的異常都會對大氣環流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大氣環流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。
  9. ( 4 ) flood season precipitation anomalies has a good correlations with southwest and southeast summer monsoon, polar vortex, west wind trough and west pacific high ( 5 ) the ssta anomalies of west pacific key regions combine with south atlantic key regions has a good predict to the flood season precipitation anomalies in liaoning areas

    遼寧夏季多雨水汽來源於西南夏季風和我國東部海域，汛期降水異常與西南、東南夏季風，極渦，西風槽以及西太平洋副高活動關系密切。西太平洋和南大西洋海溫關鍵區冷暖水年結合對遼寧汛期多少雨年有很好的指示作用。
  10. Using monthly mean rainfall and temperature data in north - west of china ( nwc ), the characteristics of rainfall anomaly at rainy season in nwc and the inter - annual varieties of drought / flood are diagnosed by means of eof, reof and wavelet analysis et al. and the ncep / ncar monthly reanalyzed data are employed to analyse the evolution character of water vapor flux and it ' s divergence flux, 500hpa height and u, v wind field. results show that ( a ) the space distribution of rainfall anomaly can be separated into seven climate sensitive areas, the first and the third region have the same rought / flood trend

    本文使用西北（區） 168個站1961 2000年6 9月（主汛期）月平均降水、溫度資料，運用eof 、 reof 、小波分析等方法診斷了主汛期月降水異常和旱澇的年代際變化；同時利用ncep ncar月平均資料，分析了強（弱）季風年西北空中水汽通量及其散度場、 500hpa高度場、 u 、 v風場的演變特徵，結果表明： （ a ）西北汛期降水可分為七個氣候異常區，第一、三異常區旱澇趨勢相同。
  11. The approaches establish a relationship between monthly precipitation abnormality and monthly circulation, soil moisture and temperature on the shallow and deep layers. the relationship is the precipitation diagnostic equation and its coefficients and dimensions are determined by using the observed data of huai river basin. then we select the main soil moisture and temperature attributing factors by the dimensional analysis to establish a forecasting equation of summer precipitation over huai river basin with the statistic approach

    通過將大氣中的熱量、水汽收支方程與一個簡化的兩層土壤溫度、濕度方程相結合，並依據月尺度大氣環流的演變特徵，推導出月降水距平與500hp月平均高度距平場、土壤深淺兩層溫、濕度的關系；利用臺站觀測資料，使用統計反演方法確定方程中各項的系數和量級，從而找出影響降水的主要土壤溫、濕因子；利用統計方法建立這些因子與淮河流域夏季降水異常之間的簡單線性預報方程，並對1992 - 2000年淮河流域夏季降水趨勢進行回報。
  12. ( 5 ) the " seesaw " type of ssta distribution is the dominate ssta distribution in equator and south pacific ocean correlating with the floods season precipitation anomalies in tpnes

    （ 5 ）與青藏高原東北側區汛期降水異常相關的主要海溫型是赤道及其以南太平洋的「翹翹板」型。
  13. ( 6 ) there is apparent positive correlation between floods season precipitation in northeast china and ssta ( 3 - 5 monthly averaged in present year ) in the " key regions " ( 21 n - 27 n, 61 w - 75 w ) of north atlantic. the " seesaw " type of ssta distribution is the dominate ssta distribution in north atlantic correlating with the floods season precipitation anomalies in northeast china

    （ 6 ）東北汛期降水與當年3 5月北大西洋key海區（ 21 n 27 n ， 61 w 75 w ）有較好的正相關關系，與東北汛期降水異常相關的北大西洋主要海溫分佈型是南北「翹翹板」型。
  14. The results indicate that those soil factors, which are selected by the blending method of dynamical and statistical approaches, are useful for forecasting monthly summer precipitation and can expressly discover their dynamical relationships

    結果表明對淮河流域夏季降水趨勢的預測有很好的效果，且更加明確了土壤溫、濕因子與降水異常之間的動力學聯系。
  15. Using ncep / ncar 40 - year reanalysis, gisst2. 3b data - set, cru south oscillation index along with in situ the 160 station data of surface air temperature / rainfall records in china, the inter - decadal variations in the relationship between equatorial western and eastern pacific variabilities are examined. the possible relations to the surface air temperature / rainfall in china are also investigated

    利用ncep / ncar再分析資料、全球海溫海冰gisst2 . 3b資料、英國cru提供的南方濤動指數以及中國160站降水和氣溫資料，分析了熱帶太平洋地區海氣系統內部聯系的年代際變化特徵及其與中國降水/氣溫異常的聯系。
  16. In the study of the mechanism of precipitation anomalies, the discovery is then chiefly to study the effect of ssta on precipitation and temperature in pre - floods period in south of china, concluding that there is a high con - elation between season precipitation in south of china and ssta ssta distribution

    本文利用國家氣候中心整編的1951 - 2000年中國160個站的月平均降水和月平均氣溫資料，重點分析了華南前汛期降水和氣溫異常的時空變化特徵及其與海溫異常的關系。
  17. When the winter kuroshio ssta is high, there is high ( low ) pressure ( compared with mean ) in the asia and weak ( strong ) easterly jet at high level in summer. at the same time, the west - northern pacific high becomes strong ( weak ) and shifts westward ( eastward ) and northward ( southward )

    當冬季黑潮區域海溫異常偏高時，亞洲熱低壓強度減弱，西北太平洋副熱帶高壓位置西伸且偏北，強度明顯偏強，梅雨鋒位置偏南，長江中下游地區降水偏多。
  18. Relationships between ssta of tropical indian ocean and summer rainfall in southern china

    中國南方夏季降水與熱帶印度洋偶極型海溫異常的聯系
  19. With the analysis methods of eof, reof, wavelet, correlation, running mean, and synthesis, sanxia summer precipitation ( sxsp ) anomaly rules and its reasons is studied. the results show that : ( 1 ) sxsp anomalies exhibit remarkable variation cycle of 15 years, 6 - 7 years and 2 ~ 3 years. the distribution of sxsp is in phase with the middle - low reaches of the yangtze river, while it is out of phase with that of middle and west of sichuan basin

    本文採用1959 2001年三峽庫區44個觀測站夏季（ 6 8月）降水量資料、 1959 2001年ncep ncar逐月、逐日資料， 1959 2000年中國160站降水資料、全球逐月海溫資料等，利用eof 、 reof 、小波變換、合成分析、相關分析、滑動平均等方法，研究了三峽庫區夏季降水異常規律及其成因。
  20. 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大氣環流和海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洋為正距平，日本附近上空為負距平；而少雨年則相反；越南中部多雨年，熱帶中東太平洋海溫異常偏高，西太平洋海溫異常偏低；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。
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