A Study on the Heat Wave Conditions over Bangladesh During 1990 - 2019

G. Rashid, M. M. T. Hossain, M. A. E. Akhter, M. A. K. Mallik
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Abstract

When temperature exceed 36 degrees with a large area and linger for minimum three or more days can be considered as heat wave (HW). In the Pre-monsoon, the sun ray drops down on the ‘Thar’ desert (India) and the foothill of the Himalayas vertically, the area makes a hot-tempered zone. That is why, these regions produce a trough of low and there is a possibility to advect temperature towards Bangladesh. The south/south westerly wind carries a high amount of moisture over Bangladesh. The heat capacity of moisture is higher than that of dry air. Solar insulation, temperature advection and moisture incursion are three main phenomena that are responsible for HW condition. Veering is also responsible for especially severe and very severe HW conditions. The present study is accompanying with all category’s frequency of heat wave days (HWD) and HW for the Pre-monsoon (March to May) over most of the stations (34) of Bangladesh for the period 1990-2019. Microsoft excel, Surfer and Arc GIS software have been used for data calculation, however, linear trend analysis and Mann-Kendall test have been used to draw the trend of HW frequency. The highest numbers of HWD are found in Jashore (30.9 days) of all types of events whereas the highest frequencies of HW are found in Rajshahi (4.2333) during pre-monsoon season. The lowest numbers of frequency of HWD and HW, both are found at Chattogram. April is the hottest month in Bangladesh. On the basis of frequency of HWD, the obtained highest hot places are Jashore, Chuadanga, Rajshahi, Ishurdi and Satkhira. while in Kutubdia and Teknaf, no HW is found at all. Among 30 years, 2014 is found the hottest year and 2018 is the recorded lowest hot year. By Mann-Kendall test, the HW trend of M. Court, Mongla, Patuakhali and Chandpur have indicated positive significant value, and Mymensing station has given only negative significant value. From spatial distribution, it shows the hottest areas which are south western and middle-western parts of Bangladesh. Journal of Engineering Science 14(2), 2023, 59-67
关于 1990 - 2019 年孟加拉国热浪情况的研究
当大面积地区的气温超过 36 度并持续至少三天或更长时间时,可被视为热浪(HW)。在季风前期,太阳光线垂直洒落在 "塔尔 "沙漠(印度)和喜马拉雅山山脚下,使该地区成为高温区。这就是为什么这些地区会产生低槽,并有可能将气温推向孟加拉国。南/西南风在孟加拉国上空携带大量水汽。水汽的热容量高于干燥空气。太阳隔热、温度平流和湿气侵入是造成 HW 条件的三种主要现象。转向也是造成特别严重和非常严重的湿热状况的原因。本研究对 1990 年至 2019 年期间孟加拉国大部分站点(34 个)季风前期(3 月至 5 月)的热浪日(HWD)和热浪频率进行了分析。计算数据时使用了 Microsoft excel、Surfer 和 Arc GIS 软件,但在绘制热浪频率趋势图时使用了线性趋势分析和 Mann-Kendall 检验。在所有类型的事件中,贾肖尔(30.9 天)的 HWD 数量最高,而在季风前季节,拉杰沙希(4.2333)的 HW 频率最高。夏特洛格的 HWD 和 HW 频率最低。四月是孟加拉国最热的月份。根据 HWD 频率,热度最高的地方是 Jashore、Chuadanga、Rajshahi、Ishurdi 和 Satkhira。在 30 年中,2014 年是最热的一年,2018 年是热度最低的一年。通过 Mann-Kendall 检验,M. Court、Mongla、Patuakhali 和 Chandpur 的热量趋势显示为正显著值,而 Mymensing 站仅显示为负显著值。从空间分布来看,最热的地区是孟加拉国的西南部和中西部地区。
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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16 weeks
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