降水和气温 meaning in Chinese
precipitaion & temperature
Examples
- The precipitation and temperature both existed 5year periodic variation in the pre - flood period in the south of china
华南前汛期降水和气温都有5a的主周期。 - The precipitation and temperature in the pre - flood period in the south of china is the same to that of the neimeng and the southeast of china
华南前汛期降水和气温都与东北以及内蒙古部分地区4 - 6月的降水和气温呈同位相分布。 - The precipitation in recent 40 years decreased slightly , mainly in spring and autumn for each period and each region , the changes of precipitation and air temperature showed a kind of reverse tendency . for example , in the coldest 1980 ' s , precipitation was the richest
近40a来重庆岩溶地区的降水略有减少，贡献最大的是春季和秋季，对于各个年代，各个地区来说，降水和气温的变化呈相反的变化，在最冷的80年代，是降水最丰富时期。 - Then by using of statistics and numerical simulation analysis , research abnormality of the main circulation system at following summer in east asia , and the influence of the abnormality on the rainfall and temperature in summer in china , when sst over the kuroshio area during winter show cold or warm anomaly
再分别通过统计和数值模拟的方法，系统的分析了冬季黑潮海温冷暖异常时，后期夏季东亚地区高低空的主要环流系统的异常，以及这些异常又如何进一步影响了我国夏季的降水和气温。 - With reof analyze technique , the mainly anomalous spatial features of soil humidity in the 0 - 50cm layer of huai river basin and their relations to different periods of precipitation and air temperature are specially analyzed by using the observed data including dekad averaged soil moisture , precipitation and air temperature data over the east of china from 1990 to 2000 . the results indicate that in the springtime the 30cm layer soil can be treated as a boundary
本文首先利用中国东部1990 - 2000年旬平均土壤湿度、降水和气温观测资料，通过对0 - 50cm层次土壤湿度进行旋转主分量分析( reof ) ，重点分析了淮河流域土壤湿度的时空分布特征，并初步研究了与前期、同期和后期不同时段降水与气温的关系。