热低压 meaning in Chinese
heat low
thermal depression
thermal low
Examples
- As a result , the meiyu front moves southward ( northward ) and brings on more ( less ) rainfall at the middle - lower reaches of the yangtze river and less ( more ) at north china
反之，亚洲热低压强度加强西北太平洋副热带高压位置东撤且偏南，强度明显偏弱，梅雨锋位置偏北，我国华北地区降水偏多。 - When the winter kuroshio ssta is high , there is high ( low ) pressure ( compared with mean ) in the asia and weak ( strong ) easterly jet at high level in summer . at the same time , the west - northern pacific high becomes strong ( weak ) and shifts westward ( eastward ) and northward ( southward )
当冬季黑潮区域海温异常偏高时，亚洲热低压强度减弱，西北太平洋副热带高压位置西伸且偏北，强度明显偏强，梅雨锋位置偏南，长江中下游地区降水偏多。 - The main relative systems of heavy - hard rainfall in northeast plateau are western pacific subtropical high , south asia high , low latitude systems , upper level jet ( ulj ) , low level greater wind speed axes , westerly trough and plateau trough , low level vortex , cold frontal , occluded front in qinghai lake , mesoscale low pressure , heat low - pressure in qinghai , shear line and convergence line , mesoscale cloud cluster , etc . the west subsidiary model of south asia high is the main circulation type of heavy - hard rainfall in this area
3 、西太平洋副高、南亚高压、低纬系统、高空急流、低空大风速轴；西风槽和高原槽、低涡、冷锋、青海湖锢囚锋以及中尺度低压、青海热低压、切变线与辐合线、中尺度云团等系统是高原东北部地区大到暴雨的主要相关系统。 100hpa上的南亚高压中心强度加强，位置东西摆动预示高原地区将有降水产生，中心强度减弱，降水过程结束。南亚高压西部副型是高原东北部地区大到暴雨的主要流型。 - As a result , we find that in winter when the kuroshio is cooler than the normal , at following summer , the continental cyclone deepen and the east asia monsoon strengthen , that the mid - latitude blocking high weaken and zonal circulation develop , the east asia teleconnection of " - + - " is stired up , so that subtropical high weaken and diminish , and tend to east north , tropical monsoon trough strengthen and mei - yu front weaken , and tend to north , meanwhile south asia high weaken and diminish , and tend to eastvnorth , is easy to form eastern region type
结果发现当黑潮海温冷异常时，后期夏季大陆热低压加深，东亚夏季风偏强。中纬度阻塞高压减弱，东亚地区纬向环流发展，在东亚-西太平洋地区激发“ - + - ”的东亚遥相关型，从而西太平洋副高强度偏弱，面积偏小，位置偏东、偏北，东亚梅雨锋也偏弱，季风槽则变强，位置偏北。同时南亚高压偏弱，位置偏北、偏东，易形成东部型。 - In dry ( wet ) year , mongolia high was stronger ( weaker ) , indian low was later ( sooner ) and weaker ( stronger ) , baikal blocking high was stronger ( weaker ) , asian summer monsoon was weaker ( stronger ) , west pacific subtropical high leaned toward north ( south ) , east ( west )
这些异常表现为：旱(涝)年蒙古高压异常偏强(弱) ，印度热低压建立晚(早)且较弱(强) ，贝加尔湖阻塞高压较强(弱) ，亚洲夏季风偏弱(强) ，西太平洋副热带高压偏南(北) ，偏东(西) 。