巴格达市日雨量的天气分析

D. Abd, Asraa K. Abdul kareem
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引用次数: 1

摘要

为了了解日降雨量变化的原因,通过指定研究期间(2007-2018年)每年雨季月份的最大日降雨量和最小日降雨量,对巴格达站进行了案例研究。雨季日降雨量的变化特征为最大值(89 mm)和最小值(0.1mm)。对压力等级(300,500,700,850和地表)的天气图进行了天气分析。卫星的可见图像被用来确定选定情况下的云的数量。结果表明,在所有情况下,天气分析都是由于高空急流的存在,伴随着300百帕斯卡水平的盆地的存在,700百帕斯卡水平的相对湿度增加超过70%,但锋面的存在使降雨量在没有锋面的情况下增加。在850百帕斯卡的高度和地面,影响伊拉克的低气压在其严重程度和湿度上也有所不同。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Synoptic Analysis for the Daily Rains of the City of Baghdad
To know the reasons for changing the daily rainfall amount, cases study were chosen for Baghdad station by specifying the maximum and minimum daily rain for the months of the rainy season for each year of the study period (2007-2018). The behavior of daily rainfall for the rainy season varying temporally with maximum (89 mm) and minimum (0.1mm). Synoptic analysis of weather chart for pressure levels (300, 500, 700, 850, and surface) was performed. Visible images of satellites were used to determine the quantities of the cloud for the selected cases. The results showed that synoptic analysis in all cases occurs due to the presence of a jet stream in the upper atmosphere, accompanied by the presence of a basin at the level of 300 hectopascals with an enhancement of relative humidity exceeding 70% at the level of 700 hectopascals, but the presence of the front makes the amount of rain greater in the absence of it. At the level of 850 hectopascals and the surface, the depressions that affect Iraq also differ in their severity and the amount of moisture loaded.
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