反气旋涡度的英文

• anticyclonic vorticity

• "反气旋"英文翻译    anticyclone
• "涡"英文翻译    eddy; whirlpool; vortex
• "度"英文翻译    surmise; estimate
• "气旋涡度" 英文翻译 :    cyclonic vorticity
• "反气旋涡旋" 英文翻译 :    anticyclonic eddies; anticyclonic eddy; anticylonic vortex
• "反气旋旋涡" 英文翻译 :    anticyclonic swirl
• "旋涡度" 英文翻译 :    vorticity
• "反气旋" 英文翻译 :    anti cyclone; anticyclone; high area
• "气旋式涡度" 英文翻译 :    cyclonic vorticity
• "北极反气旋" 英文翻译 :    arctic anticyclone
• "冰原反气旋" 英文翻译 :    glacial anticyclone; glacial high
• "大陆反气旋" 英文翻译 :    continental anti-cyclone
• "反气旋（高压）" 英文翻译 :    anticyclone
• "反气旋的" 英文翻译 :    anticyclonic
• "反气旋发生" 英文翻译 :    anticyclogenesis
• "反气旋风" 英文翻译 :    anticyclonic winds
• "反气旋风暴" 英文翻译 :    anticyclonic storm
• "反气旋辐散" 英文翻译 :    anticyclonic divergence
• "反气旋逆温" 英文翻译 :    anticyclonic inversion
• "反气旋区" 英文翻译 :    anticyclone; high
• "反气旋区域" 英文翻译 :    anticyclone
• "反气旋曲律" 英文翻译 :    anticyclonic curvature
• "反气旋生成" 英文翻译 :    anti cyclogenesis; anticyclogenesis
• "反气旋下沉" 英文翻译 :    anticyclone subsidence
• "反气旋消散" 英文翻译 :    anticyclolysis

• 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。