温多的英文

• winda

• "温"英文翻译    warm; lukewarm; hot; gentle; ...
• "多"英文翻译    many; much; more
• "奥温多" 英文翻译 :    owendo
• "本温多" 英文翻译 :    benvindo
• "比温多" 英文翻译 :    biundo
• "胡温多" 英文翻译 :    jubindo
• "尼温多" 英文翻译 :    nhundo; niundo
• "温多夫" 英文翻译 :    wendorfof; windoff; windorf
• "温多拉" 英文翻译 :    windorah
• "温多雷" 英文翻译 :    undory
• "希温多" 英文翻译 :    chivundo
• "奥温多利" 英文翻译 :    ovindoli
• "低温多硅晶" 英文翻译 :    low temperature poly-silicon tft-lcd
• "低温多晶硅" 英文翻译 :    ltps
• "低温多晶矽" 英文翻译 :    low temperature poly silicon (ltps)
• "格施温多娃" 英文翻译 :    geschwindova
• "格温多林" 英文翻译 :    gwendoline
• "格温多伦" 英文翻译 :    gwendolen
• "古尔温多" 英文翻译 :    gurbindo
• "卡萨温多山" 英文翻译 :    casabindo cerro de; cerro de casabindo
• "马多卡温多" 英文翻译 :    madokawando
• "斯温多尔" 英文翻译 :    swindall
• "温多德鸡" 英文翻译 :    wyandotte
• "温多尔夫" 英文翻译 :    windolf; windolph
• "温多费尔" 英文翻译 :    windorfer

• The lady gwendolen dubedat bursts through the throng , leaps on his horse and kisses him on both cheeks amid great acclamation
  格温多林杜比达特小姐239推开人群，跳上他的马，在掌声雷动中吻他的双颊。
• You may think some animations are a bit simple . actually , the animators took a lot of time to make them . it ' s time to revisit these everlasting animations
  有些动画看似简单,背后却可能花了一段颇长的时间制作,就让我们一次过重温多部长青的定格及其他动画作品
• As a special group of ewenki ethnic minority , with a population of 232 , they speak olguya dialect , a branch of manchu tungus language family . according to the historical documents , as early as back in 2000 bc , their ancestors already lived in wender forest tundra , over of nibuchu river , north - east part of out baigal lake and baigal lake from 16th century to the mid - 17 century , following wild deer , they came to the area near weile river , branch of lena river and weitmu , north - west of baigal lake . during 18th century , along silik river , this group of people reached big sin ' an mountain . the rich natural resources there became the sources of their livelihood
  驯鹿鄂温克人是指居住在内蒙古自治区呼伦贝尔市所辖根河市敖鲁古雅鄂温克民族乡的鄂温克人，史称“使鹿部” ，使用的语言是满?通古斯语族鄂温克语敖鲁古雅方言，人口在2001年乡统计为232人，是我国鄂温克族中的独特群体。据史书记载，驯鹿鄂温克人的祖先在公元前2000年就居住在外贝加尔湖和贝加尔湖东北部尼布楚河上游的温多山林苔原高地。到了16世纪至17世纪中叶，他们追随野生驯鹿至贝加尔湖西北列拿河支流威吕河和维提姆河一带。
• Abstract : monthly rainfall data from 1951 to 1995 for june , july and august in 13 meteorological stations of the north china were used for accounting z index and discussing serious flood and drought featureas in these months . serious flood mainly happened in july and august , and sevious drought mainly happened in august . there were more flood in 1950 ' s to 1960 ' s and more drought since 1970 ' s in the north china . meanwhile , the deeper trough which covered the regions from the ural mts . to the balkhash lake play an important role in serious rainstom in rainy season in the north china . there often happened serious flood ( drought ) when the northwester pacific subtropical high was by west and north ( east and south ) , and the sea surface temperature in the equatorial central and eastern pacific was mainly in dropping ( raising ) stage
  文摘:利用华北平原地区的13个站点, 45年（ 1951 1995 )的降水资料,对夏季4个时段（ 6月、 7月、 8月、 6 8月）进行了z指数计算,确定了该地区各个时段的严重涝年和严重旱年.发现华北地区雨季的严重洪涝主要集中在7 , 8月,严重干旱则主要发生在8月,并可明显看出由50 60年代的多水期向70年代中期以后的少水期的转变,另外,乌拉尔山到巴尔喀什湖附近的低压槽加深和西北太平洋副热带高压的北抬,对华北地区雨季持续性暴雨的产生起着决定性的作用.严重洪涝年的夏季（ 6 8月） ,西北太平洋副热带高压偏西、偏北,赤道东太平洋海温多处于下降阶段;严重干旱年西北太平洋副高偏东、偏南,赤道东太平洋海温则处于上升阶段
• Monthly rainfall data from 1951 to 1995 for june , july and august in 13 meteorological stations of the north china were used for accounting z index and discussing serious flood and drought featureas in these months . serious flood mainly happened in july and august , and sevious drought mainly happened in august . there were more flood in 1950 ' s to 1960 ' s and more drought since 1970 ' s in the north china . meanwhile , the deeper trough which covered the regions from the ural mts . to the balkhash lake play an important role in serious rainstom in rainy season in the north china . there often happened serious flood ( drought ) when the northwester pacific subtropical high was by west and north ( east and south ) , and the sea surface temperature in the equatorial central and eastern pacific was mainly in dropping ( raising ) stage
  利用华北平原地区的13个站点, 45年（ 1951 1995 )的降水资料,对夏季4个时段（ 6月、 7月、 8月、 6 8月）进行了z指数计算,确定了该地区各个时段的严重涝年和严重旱年.发现华北地区雨季的严重洪涝主要集中在7 , 8月,严重干旱则主要发生在8月,并可明显看出由50 60年代的多水期向70年代中期以后的少水期的转变,另外,乌拉尔山到巴尔喀什湖附近的低压槽加深和西北太平洋副热带高压的北抬,对华北地区雨季持续性暴雨的产生起着决定性的作用.严重洪涝年的夏季（ 6 8月） ,西北太平洋副热带高压偏西、偏北,赤道东太平洋海温多处于下降阶段;严重干旱年西北太平洋副高偏东、偏南,赤道东太平洋海温则处于上升阶段