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山地降水
相关语句
  mountain precipitation
    THE THREE-PARAMETER GAUSS FORMULA AND ITS APPLICATION IN MOUNTAIN PRECIPITATION VERTICAL DISTRIBUTION STUDIES
    山地降水垂直分布三参数高斯模式及其应用
短句来源
    A DISCUSSION ON THE MATHEMATICAL MODEL OF MOUNTAIN PRECIPITATION WITH VERTICAL DISTRIBUTION
    山地降水垂直分布模式讨论
短句来源
    THE IMPROVEMENT AND APPLICATION OF MOUNTAIN PRECIPITATION VERTICAL DISTRIBUTION FORMULAS
    山地降水垂直分布模式计算方法的改进
短句来源
  mountain precipitation
    THE THREE-PARAMETER GAUSS FORMULA AND ITS APPLICATION IN MOUNTAIN PRECIPITATION VERTICAL DISTRIBUTION STUDIES
    山地降水垂直分布三参数高斯模式及其应用
短句来源
    A DISCUSSION ON THE MATHEMATICAL MODEL OF MOUNTAIN PRECIPITATION WITH VERTICAL DISTRIBUTION
    山地降水垂直分布模式讨论
短句来源
    THE IMPROVEMENT AND APPLICATION OF MOUNTAIN PRECIPITATION VERTICAL DISTRIBUTION FORMULAS
    山地降水垂直分布模式计算方法的改进
短句来源
  “山地降水”译为未确定词的双语例句
    THE MICROSTRUCTURE FEATURES OF PRECIPITATION OVER MOUNTAIN AREA ALONG PLATEAU BORDER
    高原山地降水的微结构特征
短句来源
    Based on the raindrop spectrum data of different type precipitation over plateau border, this paper analysed the frequency, the duration of rainfall and the structure of the precipitations cell.
    本文根据高原边缘山地各种类型降水的雨滴谱资料,分析了山地降水出现的频数、降水持续时间和降水云的单体结构。
短句来源
    The analysis of Joss spectrum parameter indicated that most of the instant raindrop spectra for this region were convex.
    用Joss谱型因子分析得知高原山地降水的大部分瞬时雨滴谱呈上凸形状。
短句来源
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  mountain precipitation
Because mountains are generally wetter and cooler than adjacent basins, groundwater in the West is derived mainly from mountain precipitation.
      
In the West, because moun tains are generally wetter and cooler than adjacent basins, most ground water is derived from mountain precipitation.
      
The area belongs to dry regions of the country with about 400 mm of precipitations per year due to the Erzgebirge Mountain precipitation shadow.
      
  mountain precipitation
Because mountains are generally wetter and cooler than adjacent basins, groundwater in the West is derived mainly from mountain precipitation.
      
In the West, because moun tains are generally wetter and cooler than adjacent basins, most ground water is derived from mountain precipitation.
      
The area belongs to dry regions of the country with about 400 mm of precipitations per year due to the Erzgebirge Mountain precipitation shadow.
      


This paper discusses by using two examples the calculating question of professor Fu Baopu's experimental formula for Mountain precipitation and points out that the improvement of the calculating method for this formula suggested by yan Yuhua and Lai Hongnian which was published on Geographical research 6(1) has a lot of questions. Between the calculating result of Fu's formula and the practical material of the two examples, there appear more dif f erentiations. According to the analysis of the practical material,...

This paper discusses by using two examples the calculating question of professor Fu Baopu's experimental formula for Mountain precipitation and points out that the improvement of the calculating method for this formula suggested by yan Yuhua and Lai Hongnian which was published on Geographical research 6(1) has a lot of questions. Between the calculating result of Fu's formula and the practical material of the two examples, there appear more dif f erentiations. According to the analysis of the practical material, we suggest a model of normal frequency distribution function for Mountain pre-cipitaton p7 with vertical distribution:where z the altitude.H-the height with the maximun precipitation, This model and its characteristic values the inflection point z and c) can de dbtter idenical with the practical material. Thus this model is possible better.

本文通过两个实例,讨论傅抱璞山地降水公式的优化计算问题,并提出另一种可能的高斯曲线型分布模式

Based on the raindrop spectrum data of different type precipitation over plateau border, this paper analysed the frequency, the duration of rainfall and the structure of the precipitations cell. The mean spectra for this region are basically the exponential distribution, though there are some deviation with concave or convex shape for individual events.The raininess mainly depends on the concentration of raindrop, and bears no relation to the maximal diameter. The analysis of Joss spectrum parameter indicated...

Based on the raindrop spectrum data of different type precipitation over plateau border, this paper analysed the frequency, the duration of rainfall and the structure of the precipitations cell. The mean spectra for this region are basically the exponential distribution, though there are some deviation with concave or convex shape for individual events.The raininess mainly depends on the concentration of raindrop, and bears no relation to the maximal diameter. The analysis of Joss spectrum parameter indicated that most of the instant raindrop spectra for this region were convex. This provids a base for determining the Z-R relation of radar precipitation detection.

本文根据高原边缘山地各种类型降水的雨滴谱资料,分析了山地降水出现的频数、降水持续时间和降水云的单体结构。分析指出:不同类型降水的雨滴谱呈上凸和下凹形状偏离。雨强的大小主要取决于滴浓的变化,而与雨滴最大直径关系不大。用Joss谱型因子分析得知高原山地降水的大部分瞬时雨滴谱呈上凸形状。这为雷达测雨的Z-R关系提供了依据。

In this paper, after changing Alpert' s method estimating mountain precipitation rate into the method estimating the mountain yearly mean rainfall, the method was utilized to estimate the yearly rainfall variation with height along 87 ° and 95 ° longitudes over Himalayas . The results show that the calculated precipitation have good agreement with the observed values along 87 ° E over the Himalayas.There are two maximums of preciptation along the longitude on the southern slope of the mountain: one situating...

In this paper, after changing Alpert' s method estimating mountain precipitation rate into the method estimating the mountain yearly mean rainfall, the method was utilized to estimate the yearly rainfall variation with height along 87 ° and 95 ° longitudes over Himalayas . The results show that the calculated precipitation have good agreement with the observed values along 87 ° E over the Himalayas.There are two maximums of preciptation along the longitude on the southern slope of the mountain: one situating at the heights between 1 000 to 1 500 m above sea level, with yearly rainfall of about 2 800 mm; The another , at the heights between 3 000 to 3 500 m, with yearly rainfall of about 2 000 mm. While there are three maximums of precipitation along the 95 ° E meridian on the southern slope of the Himalayas. They are located at heights of about 1 000, 2 000 and 3 500 m, respectively. The corresponding rainfall are about 4 100, 2 700 and 2 100 mm, respectively.

本文对Alpert提出的计算山地降水率方法加以改进成为估算山脉气候平均的年降水量的方法;并对沿87°E和95°E喜马拉雅山的经向降水分布进行了估算.结果表明:沿87E处估算的降水分布与实测值相当吻合,并存在两个最大降水量高度,一个位于1000—1500 m之间,年降水量为2800 mm;另一最大降水高度在3000—3500 m之间,年降水量为2000 mm。在沿95°E处的降水分布中有三个极大降水高度,分别为1000,2000和3500 m左右,其年降水量分别为4100,2700和2100 mm。

 
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