| 1. | The main contents and results are as follows . the distributive feature of global land rainfall for jja during 1948 - 2001 is analyzed
主要研究内容和结论如下：分析了全球陆地6 - 8月降水量的分布特点。 |
| 2. | Meanwhile , the january precipitation of the mid - lower yangtze tends to increase , and the el - nino events have occurred more frequently since late l970s
此外，长江中下游1月降水量增多；厄尔尼诺事件从20世纪70年代末开始也明显增多。 |
| 3. | In the most of areas in global land , the average precipitation in einino years is decreasing , the average precipitation in lanina years is increasing
Elnino年全球大部分区域3 - 5月降水量偏少， lanina年全球大部分区域3 - 5月降水量偏多。 |
| 4. | With the model and the gis technology , the high - resolution dimensional grid - layer chart of monthly temperature and precipitation in viet nam is built . 3
利用该模型和地理信息系统技术，建立了越南各月气温、各月降水量高分辨率空间分布栅格图层。 |
| 5. | 3 . there exists distinct statistical relationship between precipitation of each summer month and prophase atmosphere general circulation in troposphere and low stratosphere
青藏高原东北侧地区夏季各月降水量同对流层、平流层前期环流特征之间存在明显的统计相关。 |
| 6. | Although the annual rainfall in counties of ningnan mountainous area fluctuates in time scales ( year , month , and 10 - days ) , the rainfall is on the trend of decreasing in forty years
以40年为尺度比较年降水量变化都呈降低趋势；各月降水量随时序的变化趋势与年降水量随时间变化的趋势有不一致性。 |
| 7. | The results indicate that the precipitation of global , nh and sh experienced decadal change : a minus - trend from 1974s global precipitation for djf , regression coefficient is - 0 . 017mm / a
结果表明：全球、南、北半球的12 - 2月的陆面降水有明显的年代际变化，全球12 - 2月降水量从1975年开始的明显的下降趋势，回归系数约为- 0 . 017mm a 。 |
| 8. | The study on the distribution feature of global land rainfall for march - may during 1948 - 2001 points out that the maximum precipitation occurs in the monsoon areas , and their standard deviation is bigger in monsoon areas than the others
分析了全球陆地3 - 5月降水量的分布特点。指出降水量最大区域主要在季风区，而且季风区降水均方差较大，降水在纬带分布上有着较大的连贯性。 |
| 9. | The paper in the context of the statistic - dynamic analyses the heterogeneity of spatial distribution of the precipitation . the generality of the spatial probability distribution model of the precipitation was explored
本文从陆面过程的物理机制出发，利用统计? ?动力学方法，阐述了中国区域的月降水量和日降水量的空间分布非均匀性，并寻求适宜的空间分布概率密度函数进行描述。 |
| 10. | Reof analysis was carried out for summer and autumn rainfall field over zhejiang province . the results indicate that the rainfall fields spatially are classified 3 subregions in summer and autumn , but they include some different place in each subregion
就夏季降水量而言，浙江北部区降水最少，浙江东南沿海降水最多，无论从季节还是月降水量看，浙江北部区夏季降水都表现出非常明显的正趋势。 |
