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daily precipitation meaning in Chinese

日降水量
日降雨量

Examples

  1. The pearson distribution and the logarithmic normal distribution are used respectively to fit the asymptotic distributions of yearly maximum of the daily precipitation in chengdu during the period between 1951 and 1999
    摘要利用1951 ~ 1999年成都日降水量年极大值的记录,通过统计推断,找出了成都日降水量年极大值遵循的渐近分布。
  2. In this paper , we selected 82 hydrologic stations and 8 weather stations in wenzhou that had 11 years daily precipitation data from 1991 to 2000 , used daily runoff data from 1999 to 2000 of feiyunjiang catchment basin in wenzhou and a wenzhou dem map with a scale of 1 : 25000
    本文用温州地区82个水文站和8个常规气象站1991 - 2000年的日降水观测资料、温州地区飞云江流域觉口站1999 - 2000年的日流量资料,以及温州地区1 : 25万的100m 100mdem数据。
  3. The analysis of persistent heavy rain in south china is performed using the daily precipitation data of 45 stations in south china and the ncep / ncar reanalysis daily data from 1958 to 2004 . 157 persistent heavy rains in south china are divided into three categories according to water vapor transfer , unstable energy and lifting condition , and their formation mechanism are discussed
    摘要利用1958 - 2004年ncep / ncar全球逐日再分析格点资料和同期我国华南地区45站的逐日降水资料,从水汽条件、不稳定能量及抬升条件对发生在华南地区的157个连续性暴雨进行分析,并结合各自的爆发时间,对暴雨进行分类,讨论了不同类型华南持续性暴雨的形成原因。
  4. Based on the daily surface air temperature data from 200 stations and daily precipitation data th from 739 stations during the second half of the 20 century , schemes for analyzing climate extremes were designed mainly according to percentiles of a non - parametric distribution and the gross errors in the daily data were removed based on a newly designed quality control procedure . the spatial and temporal characteristics of change of climate extremes over china were studied , the major conclusions are summarized as : th 1 . slight decrease trends were found for the 95 percentiles of daily maximum temperatures during summer , but larger increase trends were revealed for the 5th percentiles of daily minimum temperatures during winter , especially in northern china
    本文利用中国20世纪后半叶较为完整的逐日温度和降水观测资料,设计了严格的资料质量控制方法,以统计上的边缘分布的客观定义为主要依据,确定了极端温度和降水事件,研究揭示了近50年中国极端气候事件变化的规律,得到以下主要结果: 1 .全国最高温度的极端高值略趋下降;最低温度的极端低值升温趋势显著,这种增温在冬季、在北方最显著。
  5. Based on the daily precipitation data accumulated in forty years from 1961 - 2000 in typical dryland areas of jingyuan , longde , xiji , guyuan , haiyuan , tongxin and yanchi counties in ningnan section of ningxia autonomous region , on the recognition of the precipitation character and rule in this areas , this paper has scientifically estimated the precipitation in drought stressed areas and explored the restrictive factors to rainfall resources
    本研究以宁南旱区泾源县、隆德县、西吉县、固原县、海原县、同心县和盐池县等典型地区40年( 1961 - 2000年)日降水资料为基础,在深入认识宁南旱区降水特征及规律的基础上,对旱区降水进行科学分析,揭示了降水资源化的制约因素。
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