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The rainfall is 762 to 1016 mm in the lowlands but higher in the Mourne Mountains.

这个地区的低地的年降水量为762毫米到1016毫米。但墨恩山脉一带的降水量更多一些。

Town, region-free ground water is River Irrigation District Maying.

全年平均降水量86mm,年均蒸发量2148mm,为降水量的25倍。

Precipitation analysis sub-system . Precipitation is the ultimate origin of water resource. According to the statistics of precipitation material in the past 50years, the spatial database of precipitation was founded, it included the location of precipitation observation stations, mensal precipitation, and so on.

1降水分析子系统降水是水资源最根本的来源,根据过去50年降水观测资料,建立降水量空间数据库,包括雨量观测站位置、按月统计的降水量等。

Dry spring weather, less rainfall, often 5,6-northerly winds or southerly wind, temperatures rise faster in April; summer, Temperature and Humidity airstream affected by the ocean, 6,7,8 three months of the year precipitation precipitation 63 to 70 percent; fall, the influence of high pressure Mongolia, sunny weather, the temperature moderate and pleasant weather, late autumn and more northeasterly winds, cold weather in winter, the Siberian cold high impact, the prevailing northwest wind, cold and dry climate, Shaoyang weather, less rainfall.

春季气候干燥,降水量少,常有5、6级偏北风或偏南风,4月份气温回升快;夏季,受海洋温湿气流影响,6、7、8三个月降水占全年降水量的63%-70%;秋季,受蒙古高压影响,晴朗少雨,温度适中,气候宜人,深秋多东北风,有寒潮天气发生;冬季,受西伯利亚冷高压的影响,盛行西北风,气候寒冷干燥,天气晴朗少云,降水少。

External regulator of positive feedback is variation of precipitation amount and frequency of extreme precipitation. It is shown that desertification is predetermined by the decreased precipitation as well as by the decrease in frequency of precipitation. In the second half of 20th century importance of man-induced degradation of dry lands as additional regulator of positive feedback has been increased.

正反馈的外部调节因子是降水量的变化和极端降水事件的出现频率,降水量减少以及降水频率的降低直接影响沙漠化的程度。20世纪下半叶,人类因素导致的干旱土地退化作为另外的正反馈调节因子,其重要性正在增加。

In order to verify the reliability of MODIS atmospheric precipitable water vapor, we used the NCEP atmospheric water vapor data.

为了验证MODIS大气可降水量资料的可靠程度,本文利用NCEP的大气可降水量资料对其进行了检验。

On the basis of the above analysis, the temporal and spatial distribution features of precipitable water vapor in GPS in North China are analyzed.

结果表明:可降水量在时间上先升后降,7、8月达到最大值;在空间上由北向南递增;可降水量的日变化特征不十分显著,仅表现为小幅度波动。

Utilizing the observed data of meteorological stations and the NCEP/NCAR monthly mean reanalysis gridded data, this...

祁连山地区的降水主要集中在5~9月,这5个月的降水量约占全年降水量的86.8%。

The wavelet variance verification also indicates that the first main period of the runoff of mountainous watershed in the Shiyang River Basin is 30years, and 22years and l5years are the second and third period respectively; 3 Then we also compared the total runoff of mountain watershed with climate factors of Wushaoling which station is in the mountain headstream area, such as precipitation and temperature, the data record that the correlation coefficient of annual runoff and precipitation variation over the upper reaches in the Shiyang River Basin is 0.61 ,which indicates precipitation is the main water recharge of the runoff.

石羊河流域出山口年径流的周期变化与乌鞘岭站年降水量和年均气温周期基本上都能在同一周期上下浮动,其中出山口年径流量与乌鞘岭山区年降水量相关系数为0.61,说明地表径流量主要是由山区降水补给;年径流量与山区年均气温变化呈0.28的反相关,说明该流域近50年来出山口径流与山区气温呈反比,即径流量随年均气温上升而减少,相关性暂时不十分明显。

The APW in summer is less than 25 mm which is the least limit value of monsoon areas.This means that Xinjiang is not affected by monsoon.The geographic distribution of APW is adverse with that of precipitation,videlicet,higherAPW values corresponding to lower precipitation values.With the effects of westerly winds,the APW mode presents as an uniform change within Xinjiang area and has a stable distribution.It is very different from Xinjiang rainfall mode which changes a lot spatially.As mentioned above,there is no obvious change during 1961~2000,this indicates that APW is not a dominant factor determining precipitation,it is the result of dynamic condition,water vapor convergence and other causes.

APW的地理分布与实际降水量分布相反,其最大区域却为降水量最小区,受西风带影响,新疆APW模态主要表现全疆一致变化,分布稳定,与降水模态分布差异性大有显著不同,且近40年来无显著变化趋势,表明决定新疆降水差异的根本原因不在于水汽的多少,而是由降水产生的动力条件、水汽辐合和其它因素差异决定的。

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