冬季風 的英文怎麼說

中文拼音 [dōngjìfēng]
冬季風 英文
dry monsoon
  • 風 : Ⅰ名詞1 （空氣流動） wind 2 （風氣; 風俗） practice; atmosphere; custom 3 （景象） scene; view 4 ...
  1. You can sit in one of the modified high - powered jeeps of the professional operators, and drive through water, over rocks, whirl about on the sand, and then hurtle downwards from the top of a sand mound as high as a five - story building. your heart will really race - there s simply nothing to compare with it ! sand dunes rising and falling just near the beach are one of the masterpieces created by the chinook - type wind that blows down off pingtung s mountains

    九棚與港仔兩大沙漠，面積廣達二百多公頃，冬季時，屏東特有的落山風捲起狂沙，在海灘堆積出綿延的沙丘，坐在飆沙業者特製改裝的強力吉普車上，涉水越石在沙上橫沖直撞再從五層樓高的沙丘頂端垂直俯沖，直令人心跳加速，大呼過癮！
  2. The results show that the strong winter monsoon will decrease the gradient of ssh, and change the characteristics of sst, which has influence on the sea current, especially in a shallow and closed sea area such as the south china sea

    結果表明：強冬季風會減弱海面高度梯度，普遍降低黑潮區海表溫度，對流場有一定的影響，尤其在南海這樣的封閉海區。
  3. Vortex street appearing downwind of cheju island under wintry prevailing winds

    冬季盛行風下，濟州島下游出現的渦旋列。
  4. From the numerical modeling results, it can be found that there is a clockwise gyre in the middle part of bohai sea, whether in wintertime or in summertime. in summer, the clockwise gyre corresponding to the high - temperature and low - density center in the middle bohai sea is mainly dominated by the density circulation. and in winter, it is mainly dominated by the wind stress curl

    通過數值模擬結果發現，在渤海中部，無論冬季還是夏季，都存在一個順時針的渦旋運動，夏季，對應于渤海中部的高溫低密中心，其流場主體部分呈順時渤海冬夏季環流特徵及變異的初步研究針向旋轉，這主要是密度環流占優的結果，而冬季的順時針向的旋轉，主要是海面風應力旋度影響的結果。
  5. ( 3 ) the previously winter kuroshio ssta relates greatly to the east asian summer monsoon ( easm )

    （ 3 ）前期冬季黑潮區域海溫異常與東亞夏季風存在顯著的聯系。
  6. Conclusions are drawn as follows : ( 1 ) there is a closely relationship between the autumn kuroshio ssta and the east asian winter monsoon ( eawm )

    （ 1 ）秋季黑潮區域海溫異常與東亞冬季風有明顯的正相關關系。
  7. Zhoushan has a northern subtropical monsoon marine climate with clear four seasons ; leading wind directions are southeast wind in summer, northwest wind in winter. with an annual average wind speed of 3. 3m s ; and an average temperature of 15. 6 - 16. 6, and the frost free period reaches 251 - 303 days perannum, annual average sunshine time 1941 - 2257 hours, and the annual preeipitation is 927 - 1620 mm

    舟山屬北亞熱帶南緣季風海洋型氣候，四季分明主導風向，夏季為東南風，冬季為西北風，年平均風速3 . 3米秒年平均氣溫15 . 6 . - 16 . 6 ，冬季最低溫為- 1 ，夏季最高溫度為37無霜期251 - 303天，年日照時數1941 - 2257小時年降雨
  8. Winter is the best season to eat carp, in the cold wind howling, and air - conditioning attacks in winter, seed fertilizer carp meat, taste particularly tasty, minyan also have " winter carp xia lei, " said

    冬季是吃鯽魚的最佳季節，在寒風瑟瑟、冷氣襲人的冬季，鯽魚肉肥籽多，味尤鮮美，民諺也有「冬鯽夏鯉」之說。
  9. Setenaly according to the analyses from selected profiles, we know that, it is cold and dry in this region during the early holocene when east asian winter monsoon ' s influence is obvious, so, it is a transition period from sand deposit to sandy soil deposit, when the layers become thinner gradually from north to south. during middle holocene, it is warm and humid, influenced evidently by east asian summer monsoon, so, it is an obivious pedogenesis, when there are generally well - developped holecene palaeosol ( so ) from north to south, and the pedogenesis in the south is better than that in the north, the soil is also thicker than that of the north. from late holocene to now, the climate changes to be dry and cold, but its changing scope is smaller than that of last glacial period

    2 、就所選剖面分析來看，本區在全新世早期氣候回返，相對較寒冷乾燥，東亞冬季風影響較明顯，此時為沙層堆積向砂質土壤過渡，自北至南堆積的沙粒漸細；全新世中期氣候溫暖濕潤，東亞夏季風影響顯著，此時為明顯的成壤期，表現在自北至南普遍可見發育較好的黑壚土層，且南部的成壤作用比北部好，土壤的厚度也要大；全新世晚期至今，氣候向乾冷方向轉化，但變化幅度遠小於末次冰期。
  10. So, the ash content in peat sediment can be used as a proxy to indicate the winter monsoon intensity, higher ash content shows stronger winter monsoon, and the vice versa

    據此，作者認為該地區泥炭沉積中的灰分物質是風成堆積，進而提出該地區泥炭灰分含量可以指示冬季風強度的變化。
  11. Genetic analysis shows that it may be caused by the difference of the response of each area to winter monsoon ' s abnormal, the kuroshio and our offshore is influenced mostly by heat flux between the sea and atmosphere, but in the other areas, the abnormal current incited by abnormal wind has decisive effect on the change of the sea temperature, at the same time, air pressure also has some impact on the sea temperature

    其區域性形成的原因主要可能是因為各海區對冬季風異常的響應方式不同，強冬季風使得黑潮與我國近海海洋過多散熱，海溫降低；在西北太平洋暖池北部，強冬季風引起西風異常，從而引發異常氣旋性環流，海水輻合下沉加熱其表層以下海水，同時異常環流使得更多東側異常暖水向西加熱其表層水；在黑潮與親潮交匯處的升溫也主要是由於強冬季風導致的流場異常，海水輻合下沉升溫。
  12. ( 2 ) the anomalous eawm predominantly relates to the winter kuroshio ssta. the winter kuroshio ssta becomes positive ( negative ) when there is a strong ( weak ) eawm. the possible links might be the winter latent and sensible heat release in the west - northern pacific ocean

    （ 2 ）東亞冬季風異常對冬季黑潮區域海溫異常有密切的聯系，當東亞冬季風偏強時，冬季黑潮區域海溫偏低；反之，冬季黑潮區域海溫偏高。
  13. A 3d baroclinc ocean model is used to model the ocean current around the kuroshio area on the condition of successively anomalous east asia winter monsoon, some significant results are obtained, and the influence of strong ( weak ) winter monsoon on sea surface height ( ssh ), sea surface temperature ( sst ) and sea current around the kuroshio area is analyzed preliminarily

    摘要運用一個三維斜壓海洋模式對冬季風風場持續異常時期的黑潮區海洋進行了模擬，初步分析了冬季風風場持續異常對黑潮區海面高度、海流和海溫的影響。
  14. Its warming was the higher in china, ( 5 ) the current atmosphere circulation anomaly is the current factor influenced the winter air temperature in the north - east china, and it includes siberian high anomaly, the east asian trough anomaly, the acreage of polar vortex anomaly, the asian winter monsoon anomaly and the anomaly of the west - wind circulation in east - asian

    （ 4 ）東北地區冬季增暖趨勢與中國大部分地區是一致的，是增暖最顯著的地區之一。 （ 5 ）影響東北冬季氣溫異常的同期因子是環流異常，它包括西伯利亞高壓、東亞大槽、東亞冬季風、極渦面積、東亞西風環流指數等的異常。
  15. Based on the analysis of the features of asia winter monsoon and north - west pacific temperature ' s temporal and spatial variation, using simulation and statistic analysis methods such as correlation analysis, synthesis, svd and so on, this paper study priority the regional characters of asian winter monsoon ' s influence on north - west pacific temperature. statistic analysis and simulation all indicate that winter monsoon ' s impact on north - west pacific temperature contains regional characters positively, abnormal strong winter monsoon will causes the temperature ' s reducing of kuroshio and our offshore and increasing of the north of pacific warm pool synchronous, and the temperature of the adjacent area between the north of kuroshio and the oyashio will rise in later season

    在分析東亞冬季風與西北太平洋海溫時空變化特徵的基礎上，通過相關、合成以及svd等統計分析方法和數值模式模擬，本文重點研究了東亞異常冬季風對西北太平洋海溫影響的區域性特徵，統計分析與模式模擬結果都表明：東亞冬季風對西北太平洋海溫影響存在明顯的區域性特徵，主要分為三個區域，黑潮與我國近海、西太平洋暖池北部、日本東部的親潮與黑潮交界處。
  16. A mild winter storm

    溫和的冬季風雪
  17. Observational study of wind fields, temperature fields over beijing area in summer and winter

    北京區域夏冬季風場溫度場的觀測研究
  18. The midwest is recovering from a strong winter storm that dumped snow in some areas and produced tornados in others. storm disrupted air travel from denver to chicago

    中西部正從冬季風暴中復甦，它使一些地方大雪傾空而下，而其它一些地方則引起了龍卷風。暴風雪也阻斷了丹佛到芝加哥的航班。
  19. During the banpo man time or in the middle holocene, 5000 ~ 6000 bp, the climate within the modern glaciation best fitted vegetation and the intrusion of some sub - tropic trees was postulated to have taken place

    古土壤代表間冰期夏季風盛行的濕熱氣候，植被比較繁盛；黃土代表冰期冬季風盛行的乾冷氣候，植被凋凌。
  20. When the autumn kuroshio ssta is positive, the sea - land sea level pressure differences in the east asian region become large in winter, the east asian trough at 500hpa shifts eastward and is deep in its south and shallow in the northern, along with strong north winds in the above area and weak westerly circulation in the asian region

    當秋季黑潮區域海溫異常偏高，東亞地區的海陸氣壓差異進一步加大，東亞大槽北部減弱、南部加深、位置東移，東亞地區的偏北風加強，亞洲地區西風環流減弱，即東亞冬季風加強；反之亦然。
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