| 1. | Hourly rainfall data are available from 1884 up to the present time
自一八八四年起记录每小时的雨量直至现在。 |
| 2. | Hourly rainfall data are available from 1884 up to the present time
自一八八四年起记录每小时的雨量直至现在。 |
| 3. | Figure 2 : rainfall data , location of station and corresponding country displayed on regional web page
图二:在区域版网页上显示大雨的数据、观测站位置及所属国家 |
| 4. | Subsequently , the co - kriging method may be used to fill in the gaps among rainfall data from the measurement sites
最后应用共克利金法推估观测漏失之测站，进行雨量补遣工作。 |
| 5. | The rainfall intensity - duration - frequency form is an experimental form based on a large number of rainfall data , but the theory base is unclear
暴雨公式是基于暴雨资料而建立起来的经验性公式，尚无合理的理论解释。 |
| 6. | This paper is concerned with the characteristics of dekad precipitation in china based on dekad rainfall data of 188 stations from 1955 to 1998
本文利用我国188个测站1955 - 1998年的逐旬降水资料，对我国的旬降水特征进行研究。 |
| 7. | The two versions are applied in modeling on the base of shijiazhang rainfall datas in flood period of many years , and are compared with traditional methods
这两种ga求解参数的策略被应用于据石家庄汛期降雨资料建立旱涝预测模型的研究中，并与传统的求参方法作了对比。 |
| 8. | According to the rainfall data analysis , equipment development , experimentation investigation , mathematical analysis and the calculation of examples , from which the product and conclusion are made as follow
本文根据降雨资料分析、设备研制、实验研究和数学分析以及实例的计算，主要得到了以下成果和结论。 |
| 9. | Rainfall data for cities in the mainland is provided by the national meteorological centre of the china meteorological administration , while rainfall data for macao is provided by the macao meteorological and geophysical bureau
中国内地各城市的雨量由中国气象局国家气象中心提供，澳门的雨量则由澳门地球物理暨气象局提供。 |
| 10. | Results show that a three - stepwise weight function correction method is effective and applicable and can be spread in other basins . it can eliminate the outlier of rainfall data and improve the accuracy of flood forecast
计算结果表明，采用雨量观测误差三步权函数修正法是有效的，能准确剔除雨量资料的粗差，改善雨量资料的合理性，提高洪水预报的精度。 |
