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运动增强的英文

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"运动增强"怎么读用"运动增强"造句

英文翻译手机手机版

  • hyperkinesia
  • hyperkinesis

例句与用法

  • Take more exercises , strengthen body and prevent from catching a cold
    3加强运动增强体质。预防感冒。
  • The motion divergence body resistivity , decreases the opportunity which is sick
    运动增强身体抵抗力,减低患病的机会。
  • Such exercises as weight - lifting are anaerobic , which require brief urts of inte e effort . they improve muscle strength or build up eed
    比如举重就是无氧运动,他需要短时间内用力屏气,这种运动增强了肌肉的力量,加快了运动的速度。
  • Such exercises as weight - lifting are anaerobic , which require brief spurts of intense effort . they improve muscle strength or build up speed
    比如举重就是无氧运动,他需要短时间内用力屏气,这种运动增强了肌肉的力量,加快了运动的速度。
  • ( 5 ) the spring greenland sea - ice extent is larger ( smaller ) : then during the following summer the high of the japanese sea is stronger ( weaker ) , and the low of the asian land is stronger ( weaker ) , which make the pattern of low west and high east easily ( uneasily ) form ; the ascending movement over north china is strengthened ( weakened ) ; the summer monsoon of east asia is stronger ( weaker ) , then the southeastern , warm and damp airflow towards the north china is stronger ( weaker ) , and the cold airflow of the high level over the north china is also stronger ( weaker ) , which make the convergence of the cold and warm air over north china easily ( uneasily ) form ; the sst of the east pacific ocean is lower ( higher ) , while the sst of west wind drift is higher ( lower )
    ( 5 )春季格陵兰海冰面积偏大(小) :后期夏季日本海高压偏强(弱) ,而大陆上低压也偏强(弱) ,易(不易)形成西低东阻的形势;华北地区的上升运动增强(减弱) ;东亚夏季风偏强(弱) ,向华北地区输送的西南暖湿气流偏强(弱) ,而对应高空华北地区上空冷空气活动偏强(弱) ,利于(不利于)华北上空冷暖空气的交汇;夏季赤道东太平洋海温偏低(高) ,西风漂流区海温偏高(低) 。在以上的环流背景下,华北夏季降水偏多(少) ,易涝(旱) 。
  • In 1999 , the dipole existed in between the okhotsk high and the depression in the north of northeast china , thus the okhotsk high became active and maintained , the subh was located to an area quite further south than usual . the high persisted in the east region of nw china , the cold air flowed to the mid - lower reaches of the yangtze river along the high . in the east region of nw china , air steam under troposphere was strong sinking motion , and formatted the negative vorticity region , the vapour flux divergence was divgence . lt was apparently that the rain could n ' t occur in the eastern portin of nw china . in 2000 year , okhotsk high was very weak or did n ' t exist in , there was high in the east asia - japan , the subh is located to an area further north than usual . in the east region of nw china , the trough maintained , air stream under troposphere was strong ascending motion , the cycolonic circulation was prevailing , the vapour flux divergence was intensive convergences the rain easy happened in the east areas of northwest china
    4多梅雨1999年鄂霍茨克海阻塞高压与我国东北北部低压形成偶极子,使得阻塞高压稳定少动,西太副高位置偏南,西北地区东部持续受高压控制,冷空气沿此高压流经长江中下游地区上空;在西北地区东部对流层中下层气流下沉运动较强,呈反气旋涡度,水汽通量散度辐散,不利于西北地区东部降水。空梅雨2000年相反,鄂霍茨克海高压减弱甚至不存在,东亚-日本为高压,西太副高位置偏西偏北,西北地区东部处于西风槽中,对流层中下层气流上升运动增强,盛行低压环流,水汽通量散度强烈辐合,有利于降水生成。
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