降水增加 meaning in Chinese
precipitation enhancement
Examples
- But if the temperature and precipitation increase at same time , the transfer of interlock area of farming - pastoral region will decrease , or keep unchanging
而在温度升高、同时降水增加的气候情景下，农牧交错带的移动变缓，甚至不变，视降水的情况而定。 - Different areas present different variation tendency of summer rainfall , among which the rainfall significantly decreases in the east of liaoning and increases in southeast of inner - mogolio
各区域降水的变化趋势不一致，其中辽宁东部地区降水减少最明显，内蒙古东南部降水增加趋势最明显。 - There is an apparent rainfall distribution of " floods in the south and droughts in the north " in 1990 ' s , total amount of rainfall in china has the slight decreasing trend
而华北区夏季降水减少趋势明显。 10年尺度振荡特征清楚， 90年代南涝北旱分布形式非常清晰。高原的降水增加在8个区里最显著。 - ( 4 ) in summer , tropic west pacific ssta decadal change infect precipitation decadal change in south and north of changjiang river maybe by : positive ssta in tropic west pacific weaken the summer monsoon circulation , lead more precipitation in south of changjiang river and less precipitation in north of it , vice versa ; middle north pacific ssta decadal change infect precipitation decadal change in mid - down valley of changjiang river maybe by : when ssta is negative in middle north pacific , the height field in tropic rises obviously , the subtropical high strengthens and extends westward , the northern limit retreats southward , leads upper trough retreats northward and move eastward , meiyu front moves northward , then leads more precipitation in mid - down valley of changjiang river , vice versa ; middle northwest pacific - low latitude mid - east pacific infects precipitation in north china possibly by change the activity of northeast china cyclone
（ 4 ）热带西太平洋ssta年代际变化影响夏季中国长江南北降水年代际变化的可能机制是热带西太平洋海表温度正（负）异常减弱（加强）东亚夏季风环流，从而使江南降水增加（减少） ，江北降水减少（增加） ；夏季中部北太平洋ssta年代际变化影响中国长江中下游地区夏季降水年代际变化的可能机制是中部北太平洋海表温度负异常，将导致热带地区高度场普遍增高，副高加强西伸，副高北界南退，致使高空槽北缩东移，梅雨锋西移北进，中国长江游中游、中卜游降水增多，反之亦反；夏季中高纬西北太平洋一低纬中东太平洋反向距平分布结构影响中国东北降水的可能机制是低纬中东太平洋海表温为负异常。 - The annual precipitation has a fluctuation change trend , the precipitation increases obviously in winter , the summer precipitation and the annual precipitation increase slowly , in each age the maximum precipitation in winter , summer , autumn and the maximum annual precipitation all appear at the beginning of 21st century in which the air temperature is warmer , the climate has a change trend from dry and warm to wet and warm
年降水呈波动式变化趋势，冬季降水增加明显，夏季和年降水增加缓慢，各年代中冬季、夏季、秋季和年最多降水均出现在气温偏暖的21世纪初，气候有从暖干向暖湿转变的趋势。