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Wind, precipitation, temperature, and barometric pressure changes affect only the surface and shallow subsurface of the Earth.

风、降水量、温度和大气压的改变只会影响地表和地表下的浅层部分。

Based on the data in 1996-2006 in Zhangjiakou region, the change trends of the temperature, precipitation, runoff depth and burying depth of the ground water were statistically analyzed.

利用统计分析方法,对张家口1960-2006年的气温、降水量、径流深和地下水埋深等变化趋势进行分析。

The results show as following: Caragana microphylla growth depended on soil water and precipitation in the earlier 10 years.

模拟柠条生长初期(1~10 a)9 m土层土壤有效含水量以101.0 mm/a的速度递减,此后长期在较低水平上随降水量变化而波动。

The correlation analysis between 30 morphological characters with significant difference and climatic factor, longitude and latitude can be summarized as:(1) the longitude, precipitation and air humidity have the same effects on the variability of G. uralensis;(2) the index number affected by light is the most, and the water is the most important factor affecting population variability of G. uralensis.(3) the variability shows that the height of plant, the number of small leaves of the compound leaf, the number of flower buds and the length of inflorescence increase with the increasing of climatic humidity, however, the number of lateral branch decreases.

对30项具有显著差异的指标与气候因素和地理经纬度进行的相关分析结果可概括为:(1)地理经度对变异的作用与降水量和大气湿度相一致;(2)光照因素影响到的指标最多,水分因素对变异的作用程度最大;(3)变异的主要表现为,随气候湿润程度增加,植株的高度、复叶小叶片的数量、花序的长度和花蕾数量等均呈增加趋势,而侧枝的分枝数量和长度呈减小趋势。

This paper proposes a new probability model-Multivariate compound extreme value distribution to predict 'typhoon-induced rainfall for the Wenzhou City in Zhejiang Province.

作者采用多维复合极值分布理论(Multivariate compound extreme value distribution),以受台风暴雨危害较严重的浙江温州地区为例,对台风诱发暴雨的降水量进行了概率预测。

Climate: Typical continental climate, average annual precipitation: 305 mm, average annual temperature: 5~10

气候:典型的温带大陆性气候,年均降水量305毫米,年均气温5~10℃。

The whole nation year fall is 200~1000mm, belong to continental climate.

全国年降水量为200~1000mm,属于大陆性气候。

In the last 20 years, a lot of geological data and climate simulation studies showed that continentality increased and water cycle between land and ocean became weaker at 21ka BP. Therefore, annual precipitation decreased significantly and climate became dry globally at 21ka BP.

近二十多年来大量地质资料和气候模拟研究表明,末次盛冰期大陆度增加、海陆水分循环减弱、年降水量减少,全球大陆普遍干燥。

During the PDO warm phase, however, there is a significant tropospheric biennial oscillation for the coupled interannual oscillations over these regions In addition , it seems to have a stronger correlation with the SST of the tropical eastern Pacific summer.

结果表明PDO冷暖位相中夏季江淮地区降水量与太平洋海温年际耦合振荡周期和强度均存在显著差异PDO冷位相中,夏季江淮地区降水与前期冬季西南太平洋和同期夏季黑潮区海温在7~8a时间尺度上的耦合最显著,而在PDO暖位相中,与这些地区海温呈现极显著的准2a耦合振荡,并且与同期夏季赤道东太平洋地区海温的准2a耦合振荡也迅速加强。

Response of tree-ring structure to the variance of average monthly temperature and precipitation on Populus simonii and P.×beijingensis collected from Mu Us Desert was studied using theories of dendrochronology.

摘 要:应用年轮气候学理论和方法对毛乌素沙地小叶杨和北京杨的年轮结构的变化特征及其与月平均气温和月降水量的响应关系进行了分析。

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