Prediction of Heatwave 2013 over Andhra Pradesh and Telangana, India using WRF Model

IF 1.1 Q4 METEOROLOGY & ATMOSPHERIC SCIENCES Asian Journal of Atmospheric Environment Pub Date : 2021-09-01 DOI:10.5572/ajae.2020.117
N. Naveena, G. Ch. Satyanarayana, A. Dharma Raju, N. Umakanth, D. Srinivas, K. Sivasankar Rao, M. Suman
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Abstract

Heatwaves are acknowledged to be the major meteorological disaster, causing a noticeable impact on humans and animals’ lives during the last few decades. The number, frequency, duration, intensity, and areal extent of the heatwaves are on the rise during recent years. The Maximum temperature data of 2013 is analyzed to assess the synoptic nature, intensity, frequency, and various significant facets of the heatwave over the south peninsular states of Andhra Pradesh and Telangana. Indian subcontinent experienced a major heatwave during 2013, which claimed 1216 human lives. Even though the highest intensity of maximum temperatures is observed in May over major areas of India, the increasing (incidence, duration, number of spells, and the sweltering temperatures) number of heatwaves are observed over many parts of the country. The northwest and southeast coastal regions are the two heat wave prone regions. The advection of heat from the northwest with the aid of north-westerly winds causes heatwaves over northwest India to sweep or move towards India’s southeast and east coast. The heatwave record over south-eastern India, i.e, Andhra Pradesh and the adjoining Telangana state during May 22–24, 2013 were described in this study. Maximum temperatures above 40°C are observed with a sudden rise by 6 to 7°C over the study region. An attempt is made to predict the maximum temperatures 72 hours before the existence of a heatwave at 3 km horizontal resolution using the Advanced core of the Weather Research and Forecasting (WRF) model. Model predicted temperature values match with observations and the statistical metrics show a high index of the agreement, lower values for root-mean-square error and mean absolute error. Atmospheric circulation patterns associated with this heatwave are also presented. The arrest of sea breeze, the hovering of diabatic heat because of subsidence is the factor that abetted the heatwave blockade over the south-eastern part of the country. The WRF model forecasts could present the occurance of the heat wave over AP and Telangana region with 72 hour lead time with high accuracy.

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利用 WRF 模型预测 2013 年印度安得拉邦和特伦甘纳邦热浪
热浪是公认的主要气象灾害,在过去几十年中对人类和动物的生活造成了明显的影响。近年来,热浪的数量、频率、持续时间、强度和区域范围都呈上升趋势。本文对 2013 年的最高气温数据进行了分析,以评估南半岛安得拉邦和特兰加那邦热浪的同步性质、强度、频率和各种重要方面。印度次大陆在 2013 年经历了一场大热浪,夺去了 1216 人的生命。尽管印度主要地区 5 月份的最高气温强度最高,但印度许多地区的热浪次数(发生率、持续时间、阵雨次数和闷热气温)都在不断增加。西北和东南沿海地区是两个热浪多发区。在西北风的帮助下,来自西北部的热量平流导致印度西北部的热浪席卷或移向印度的东南部和东部沿海地区。本研究描述了 2013 年 5 月 22-24 日期间印度东南部(即安得拉邦和毗邻的特兰干纳邦)的热浪记录。在研究区域观测到的最高气温超过 40°C,气温骤然升高 6 至 7°C。本研究尝试使用天气研究和预报(WRF)模型的高级核心,以 3 千米的水平分辨率预测热浪出现前 72 小时的最高气温。模型预测的气温值与观测值相吻合,统计指标显示吻合指数较高,均方根误差和平均绝对误差值较低。此外,还介绍了与此次热浪相关的大气环流模式。海风的停滞、下沉导致的二重热量徘徊是导致热浪封锁我国东南部地区的因素。WRF 模式的预报可以在 72 小时内高精度地预测到热浪将出现在亚太地区和特兰加那地区。
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来源期刊
Asian Journal of Atmospheric Environment
Asian Journal of Atmospheric Environment METEOROLOGY & ATMOSPHERIC SCIENCES-
CiteScore
2.80
自引率
6.70%
发文量
22
审稿时长
21 weeks
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