冬季风的英文

• dry monsoon

• "冬季"英文翻译    winter
• "风"英文翻译    wind
• "冬季风暴" 英文翻译 :    wintergewitter
• "冬季季风" 英文翻译 :    winter monsoon
• "冬季风暴行动" 英文翻译 :    operation wintergewitter
• "冬季季风气候" 英文翻译 :    winter monsoon climate
• "季风" 英文翻译 :    [气象学] monsoon 冬季风 dry monsoon; 夏季风 wet monsoon; 季风气侯 monsoon climate; 季风区 monsoon region; 季风雨 monsoon rain; 季风云团 monsoon cluster
• "冬季" 英文翻译 :    1.(一年的第四季) winter 严寒[暖和]的冬季 hard [mild] winter2.peret (埃及古历一年三季之一); 冬季奥运会 the winter olympic games; 冬季攻势 [军事] winter offensive; 冬季全运会 national winter games; 冬季体育运动 winter sports; 冬季作物 winter crops
• "反季风" 英文翻译 :    antitrade wind; counter trade; counter-trades
• "季风槽" 英文翻译 :    monsoon trough
• "季风带" 英文翻译 :    monsoon zone
• "季风林" 英文翻译 :    mo oon forest; mo oonforest; monsoon forest
• "季风流" 英文翻译 :    monsoon drift
• "季风区" 英文翻译 :    monsoon region
• "季风雾" 英文翻译 :    monsoon fog
• "季风绪" 英文翻译 :    fengxu ji
• "季风雨" 英文翻译 :    monsoon rain
• "蜗季风" 英文翻译 :    southwest mo oon; southwest monsoon
• "夏季风" 英文翻译 :    summer monsoon; the summer wind
• "尤季风" 英文翻译 :    indian monsoon
• "季风, 吹季风的季节, 雨季" 英文翻译 :    monsoon
• "潮湿季风" 英文翻译 :    wet monsoon
• "赤道季风" 英文翻译 :    equatorial monsoon
• "地中海季风" 英文翻译 :    etesian wind; etesians; etesiens
• "东北季风" 英文翻译 :    north-east monsoon

• Observational study of wind fields , temperature fields over beijing area in summer and winter
  北京区域夏冬季风场温度场的观测研究
• Conclusions are drawn as follows : ( 1 ) there is a closely relationship between the autumn kuroshio ssta and the east asian winter monsoon ( eawm )
  ( 1 )秋季黑潮区域海温异常与东亚冬季风有明显的正相关关系。
• 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
  据此，作者认为该地区泥炭沉积中的灰分物质是风成堆积，进而提出该地区泥炭灰分含量可以指示冬季风强度的变化。
• 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
  古土壤代表间冰期夏季风盛行的湿热气候，植被比较繁盛；黄土代表冰期冬季风盛行的干冷气候，植被凋凌。
• 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
  结果表明：强冬季风会减弱海面高度梯度，普遍降低黑潮区海表温度，对流场有一定的影响，尤其在南海这样的封闭海区。
• ( 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 )东亚冬季风异常对冬季黑潮区域海温异常有密切的联系，当东亚冬季风偏强时，冬季黑潮区域海温偏低；反之，冬季黑潮区域海温偏高。
• 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 、就所选剖面分析来看，本区在全新世早期气候回返，相对较寒冷干燥，东亚冬季风影响较明显，此时为沙层堆积向砂质土壤过渡，自北至南堆积的沙粒渐细；全新世中期气候温暖湿润，东亚夏季风影响显著，此时为明显的成壤期，表现在自北至南普遍可见发育较好的黑垆土层，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，气候向干冷方向转化，但变化幅度远小于末次冰期。
• 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
  其区域性形成的原因主要可能是因为各海区对冬季风异常的响应方式不同，强冬季风使得黑潮与我国近海海洋过多散热，海温降低；在西北太平洋暖池北部，强冬季风引起西风异常，从而引发异常气旋性环流，海水辐合下沉加热其表层以下海水，同时异常环流使得更多东侧异常暖水向西加热其表层水；在黑潮与亲潮交汇处的升温也主要是由于强冬季风导致的流场异常，海水辐合下沉升温。
• 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 )东北地区冬季增暖趋势与中国大部分地区是一致的，是增暖最显著的地区之一。 ( 5 )影响东北冬季气温异常的同期因子是环流异常，它包括西伯利亚高压、东亚大槽、东亚冬季风、极涡面积、东亚西风环流指数等的异常。
• 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
  当秋季黑潮区域海温异常偏高，东亚地区的海陆气压差异进一步加大，东亚大槽北部减弱、南部加深、位置东移，东亚地区的偏北风加强，亚洲地区西风环流减弱，即东亚冬季风加强；反之亦然。