江淮流域 的英文怎麼說

中文拼音 [jiānghuáiliúyù]
江淮流域 英文
jiang huai basin
  • 江 : 名詞1. （大河） （large） river 2. （指長江） the changjiang [yangtze] river 3. （姓氏） a surname
  • 淮 : 名詞1. （淮河） the huaihe river （我國大河之一, 全長1000公里）2. （姓氏） a surname
  • 流 : 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...
  • 域 : 名詞（在一定疆界內的地方; 疆域） land within certain boundaries; territory; region
  • 流域 : [水文] watershed; basin; drainage area; catchpit; catchment area; drainage basin; feeding ground;...
  1. May and during the 1st. - 7th. october. no matter during 1st. - 7th. may or 1st. - 7th. october, the persistent rain and sun weather is all related with the quasi - biweekly oscillation of vortex

    1977 、 1985年五一期間和1983 、 1984年十一期間江蘇省極端異常降水都是與長江流域或江淮地區大范圍降水異常相聯系的。
  2. Mineral composition and chemical characteristics of albic soils in jianghuai drainage basin

    江淮流域白漿化土壤的礦物組成與化學特性的研究
  3. Analyzing the physics structure of vorticity, divergence, vertical velocity, frontogenesis " function, apparent heat source and apparent moist sink etc. indicated the physics fields are favorable for the occurance of the heavy rain over changjiang - huaihe river basin where the physics values are well according to the heavy rainstorm positions ; the low level jet is closely subject to the moisture and the coupled system of the low and the upper level jetstreams induced the strongly " ascending motion ; the intensity of the frontogenesis varies with the development of the rainfall system and reacts the rainfall intensity

    主要分析了這次過程中的多種物理量，包括渦度、散度、垂直速度、鋒生函數、視熱源、視水汽匯等，對這一暴雨過程有了比較系統的認識。結果表明：在江淮流域存在著有利於發生暴雨的物理量場配置，渦度、散度、垂直速度等物理量，與暴雨的落區都很吻合的；低空急流的產生不僅有利於水汽的輸送，而且高低空急流的耦合造成了有利於強上升運動的配置；鋒生強度隨著降水系統的發展變化，並影響降水強度。
  4. Both composite and correlation analyses show that the 150hpa asia - australia cef ( aacef ) in boreal spring has important influences on easm. when aacef is weaker, the summer wpsh tends to be stronger with a southwestward extension, and the south asia high ( sah ) will be stronger too. this circulation pattern will lead to more rainfall in the yangtze and huaihe river valley and less rainfall outside of this region

    相關分析和合成分析的結果還顯示，春季150hpa亞澳越赤道氣流對東亞夏季風有重要影響：當春季該氣流偏弱時，北半球夏季西太平洋副高強度偏強，位置偏南偏西，南亞高壓強度也偏強，這樣的環流背景使江淮流域6 ? 7月降水偏多，華南華北降水偏少；反之，當春季該氣流偏強時，夏季西太副高強度偏弱，位置偏北偏東，南亞高壓強度也偏弱，江淮流域夏季降水偏少，華南華北降水偏多。
  5. During recent decade and more, major and super floods have taken place frequently in the yangtse river and huai river. the natural phenomenon of flooding is inevitable. it is not a surefire plan only to take engineering measures for flood control while climatic variation is far from being known

    近十多年來在我國長江、淮河流域連續不斷發生的大洪水或特大洪水再次向我們展示了這樣一個道理，洪水是一種自然現象，當環球大的氣候因素及其變化規律遠未被認識時，試圖僅依靠工程措施來控制洪水並非萬全之策，逐步運用非工程措施，常常能起到「以柔克剛」 、 「以弱勝強」之功效。
  6. ( 4 ) the correlations are significant between the sth position index and the general circulation. in the westerly ( easterly ) year, equatorial westerly is weaker ( stronger ), cross - equatorial flow is weaker ( stronger ), south china sea summer monsoon is weaker ( stronger ), the yangtze river valley westerly is stronger ( weaker ), which has the positive ( negative ) effect on the maintenance of rain band over the yangtze river valley, so the rainfall is more ( less ) in this area and it is hit by floods ( droughts ), vice versa

    （ 4 ）本文運用定義的副高指數研究了六月份副高偏東偏西年份的大型環流特徵及其對我國東部天氣的影響，風矢量場和相關場分析結果表明：副高偏西（東）年，赤道西風減弱（增強） ，越赤道氣流偏弱（增強） ，南海夏季風偏弱（強） ，而長江流域西風增強（減弱） ，有（不）利於雨帶在江淮流域維持，該地區降水偏多（少）易澇（旱） 。
  7. There are certain relations between circulation pattern index ' s decadal variance characteristic and decadal variation tendency of the precipitation of china : in the 1960s and the 1970s, in which the negative index are relatively more, the precipitation are abundant, and in 1980s in which positive index dominant the precipitation over north china are obvious deficient ; the situation of the yangtse river and huaihe river basin is opposite

    流型指數的年代際變化特徵與我國降水的年代際變化趨勢有一定的關系，負指數偏多的60 、 70年代華北降水偏多，而正指數占優勢的80年代華北降水則明顯偏少；江淮流域的情況則相反。
  8. A study on the variation and forecasting models of groundwater level and draining waterlogging in cultivated soil layers in the jianghuai valley

    江淮流域地下水位變化規律及預報模型與耕作層排漬模型研究
  9. It is obvious that semi - quantitative was a scientific and practical method in water quality bio - assessment for macro - invertebrate assemblage sampling. ii the calculation of the tolerance value of benthic macro - invertebrate taxa 1. ninety - two samples were obtained from mountain streams in jixi, ningguo, xouning, qimeng and susong counties, anhui province, and plain waterbodies in qinghuaihe river and small water bodies in zijingshan, nanjing city, jiangsu province from 1998 - 2002

    從1998年至2002 ，在位於安徽績溪縣、休寧縣境內的新安江水繫上游支流、寧國縣的青陽河、九華山九華河上游、祁門縣境內的閶江水系和大北河水系以及宿松縣趾風河，南京秦淮河流域和紫金山地區小水體設點採集大型底棲無脊椎動物樣本，共獲92個樣本。
  10. Abstract : through analysis and comparison of the climatic conditions of the main sandy pear ( pyrus pyrifolia nakai ) producing areas in china and japan it is clear that the ecological conditions in the areas where the japanese pears have been extensively grown in japan are quite similar to the ecological conditions of the areas from the line of qinling mountains, huai river, and yangtze river southward in china, where the ecological conditions are suitable to be grown the cultivars of pyrus pyrifolia nakai, including the japanese pear cultivars

    文摘:通過對砂梨在我國的生態適應性與日本梨在日本主產區的氣候條件的分析和比較，認為秦嶺、淮河、長江流域及其以南的廣大地區與日本國梨產區氣候條件相似，都適合砂梨及日本梨的生長發育，主要差異在栽培技術水平和新技術的應用上。
  11. Through analysis and comparison of the climatic conditions of the main sandy pear ( pyrus pyrifolia nakai ) producing areas in china and japan it is clear that the ecological conditions in the areas where the japanese pears have been extensively grown in japan are quite similar to the ecological conditions of the areas from the line of qinling mountains, huai river, and yangtze river southward in china, where the ecological conditions are suitable to be grown the cultivars of pyrus pyrifolia nakai, including the japanese pear cultivars

    通過對砂梨在我國的生態適應性與日本梨在日本主產區的氣候條件的分析和比較，認為秦嶺、淮河、長江流域及其以南的廣大地區與日本國梨產區氣候條件相似，都適合砂梨及日本梨的生長發育，主要差異在栽培技術水平和新技術的應用上。
  12. There are 6 dominant spatial patterns : same distribution allover the country ; the seesaw between the regions of south of the yangtze river and mid - lower reaches of the yellow river ; the seesaw between the regions over the yangtze river and the yellow river and the south part of south china ; coherent variations over the yangtze - huaihe river basin and north - east china and opposite variations in the regions of north china and north - west china and south - east part of china ; the seesaw between the east part and the west part of china ; coherent variations over mid - lower reaches of the yellow river and south china and opposite variations in the yangtze river basin

    近44年來我國逐旬降水量年變化特徵主要存在六種空間分佈型：全國大范圍地區年變化特徵一致的分佈；長江以南地區和黃河中下游地區降水量分佈相反；長江、黃河流域和華南沿海降水量分佈相反；長江、淮河流域和東北地區與華北、西北和東南沿海降水量分佈相反；我國東西部地區降水量分佈相反；長江流域與黃河中下游和華南降水量分佈相反。
  13. It ` s in the middle of henan, shandong, jiangsu, zhejiang, jiangxi, hubei, across yangtze river and thehuaihe river

    分別與河南、山東、江蘇、浙江、江西、湖北接壤，跨長江、淮河流域，緊靠以上海為中心的長江三角洲經濟區，是臨江近海的內陸省份。
  14. The huai - si area, sitting between these two great rivers, occupied a unique place during this transferring of economic center

    地處黃河流域和長江流域之間的淮泗地區在唐代經濟發展過程中以及在我國經濟重心南移過程中都有著非常重要的地位。
  15. On the basis of the typical weather situation in huaihe river basin in 1998, the paper analyses the features of the land temperature of huaihe river basin in the four stages of the 1998 s meiyu of yangtze

    最後結合1998年淮河流域試驗加密觀測期間的主要天氣形勢，分析了江淮梅雨4個階段相對應的地面溫度的特徵。
  16. According to natural conditions of the area, natural rules and systematic engineering principle, a series of countermeasures were propased such as improving forest cover degree, enhancing water conservancy project, adjusting agricultural production constitution, combining engineering measures with ecological measures to restore mine ecosystem and to take comprehensive measures to control soil erosion so as to improve ecological environmental quality in watershed between the yangtze river and the huaihe river

    針對研究區域的自然環境條件和社會經濟狀況，按照系統工程的原理，從遵守自然規律的角度出發提出了提高森林覆蓋率，加強水利工程建設，改良土壤，因地制宜調整農業產業結構，工程措施與生物措施相結合進行礦山修復，治理水土流失，搞好生態環境保護規劃，大力發展生態旅遊，提高公眾的環境意識，依靠科技進步促進地方經濟發展的一系列改善江淮分水嶺地區生態環境問題的對策。
  17. The key area of the first eigenvector of eof for summer precipitation decadal change in china allots in south and north of changjiang river which vary contrary ; the second one ' s allots in middle valley of changjiang river and jianghuai valley ; the third one ' s allots almost in total china. ( 3 ) tropic and north pacific summer ssta ' s decadal change has good correlation with china summer precipitation ' s decadal change

    中國年平均與汛期平均降水eof分析的前三個特徵向量基本一致，第一特徵向量表現為長江南北反向的形態，第二特徵向量表現為中部為正，其餘為負的分佈形態，第三特徵向量表現為長江中游、江淮流域為正，其南北兩側為負的分佈形態。
  18. A meso - scale numerical weather forecast system based on dawning 1000 and its applicability to jianghua basin

    基於曙光1000的中尺度數值氣象預報系統及其在江淮流域的適用性研究
  19. This scheme was finally tested by a typical meso - scale severe rainstorm process which happened on the middle - lower parts of the yangtze river in china during the period of july 4th - 5th, 2003

    並以2003年7月4日? 5日發生在江淮流域的特大暴雨過程為例，對該方案進行了驗證。
  20. During the lasting course of type e, 850hpa, 500hpa and 200hpa wind field is obviously different from that during the lasting course of type c. the same is true of the precipitation deviation distribution of china, and during type e course the monthly precipitation deviation is positive over the yangtse river and huaihe river basin and negative over north china. the situation of type c is opposite. the result is mainly to reflect the situation in june

    E 、 c型持續過程期間， 850hpa 、 500hpa 、 200hpa風場存在明顯差異。我國降水量距平分佈也有明顯差異， e型過程江淮流域月降水量為正距平，華北為負距平， c型則相反，而這個結果主要是反映了6月份的情況。
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