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A Precipitation Prediction Method for the Qinghai-Tibet Plateau

机译:青藏高原的降水预测方法

摘要

#$%^&*AU2020101241A420200806.pdf#####Abstract of Description A precipitation prediction method for the Qinghai-Tibet Plateau comprises the following steps: S100, collecting and processing data; S200, obtaining the data of the area to be predicted; S300, predicting the possibility of precipitation; S400, predicting the actual precipitation. By collecting and analyzing the precipitation data of the Qinghai-Tibet Plateau over the years, the method for predicting precipitation on the Qinghai-Tibet Plateau creatively puts forward water vapor content of the entire atmosphere, water vapor density and dew-point temperature of each isobaric surface as the main factors affecting the actual precipitation on the Qinghai-Tibet Plateau. Through the establishment of a database, the Qinghai-Tibet Plateau is gridded to achieve a more practical regional division, and at the same time, it is divided at the preset time to achieve a more practical time division. Based on precipitation data of the Qinghai-Tibet Plateau over the years, the accuracy of the regression equation established has been greatly improved.Drawing of Description S100 Collect and processing data S200 Obtain the data of the area to be predicted S300 Predictthei-possbiofprciitafion S400 Predict the actual precipitation FIG. 1 1/1
机译:#$%^&* AU2020101241A420200806.pdf #####描述摘要青藏高原的降水预报方法包括以下内容步骤:S100,收集并处理数据; S200,获取待预测区域的数据;S300,预测降水的可能性; S400,预测实际降水。通过收集并分析了青藏高原多年来的降水数据,青藏高原降水预报方法创新提出水整个大气的蒸汽含量,每种气体的水蒸汽密度和露点温度等压面是影响青藏高原实际降水的主要因素。通过建立数据库,对青藏高原进行网格化处理,以实现更多目标。实用的区域划分,并同时在预设时间进行划分,以实现更多实用的时间划分。根据多年来青藏高原的降水资料,建立的回归方程的准确性得到了极大的提高。说明图S100收集和处理数据S200获取该区域的数据以被预测S300预测生物功能S400预测实际降水图。 1个1/1

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