Climatic Characteristics of Dust Storms in Jordan

Pub Date : 2020-04-20 DOI:10.4236/ajcc.2020.92010
A. Ghanem
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引用次数: 2

Abstract

This study is devoted to examine the climate characteristics of the Dust Storms (DS) with visibility 0 - 1 km that occurred in Jordan for the period 1988 to 2018. It is found that the DS varies temporally and spatially, as the largest number of DS occurred in 2003 (36 DS) and the lowest occurred in 1999 (one DS). The average was 17.22 DS with the coefficient of variation of 45%, the DS durations ranged from 1 - 4 days, most of them occurred in spring (54.1%) especially in April (22.2%). The DS increased southward and eastward directions, they increased from 13 DS in Irbid in the north to 182 DS in Al-Jafr in the south and to 102 DS in Safawi in the east. The results showed positive relationships between wind speeds. There were negative relationships with relative humidity, pressure and rainfall, and there was no relationship between DS and the maximum temperature.
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约旦沙尘暴的气候特征
本研究致力于研究1988年至2018年约旦能见度为0-1公里的沙尘暴的气候特征。研究发现,DS在时间和空间上都有变化,2003年DS数量最多(36个),1999年DS数量最低(1个)。平均值为17.22 DS,变异系数为45%,DS持续时间为1-4天,大部分发生在春季(54.1%),尤其是4月(22.2%)。DS向南和向东增加,从北部Irbid的13 DS增加到南部Al Jafr的182 DS,再到东部Safawi的102 DS。结果显示风速之间存在正相关关系。与相对湿度、气压和降雨量呈负相关,DS与最高气温无相关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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