首页> 外文期刊>Meteorology and Atmospheric Physics >Easterly wave activity and associated heavy rainfall during the pre-monsoon season of 2005
【24h】

Easterly wave activity and associated heavy rainfall during the pre-monsoon season of 2005

机译:2005年前季风季节的东风波动和相关的大雨

获取原文
获取原文并翻译 | 示例
           

摘要

Waves in easterlies are a tropical disturbance, which are moving from east to west or west-northwest (WNW). Over the Indian region, easterly waves occur mainly in winter, pre-monsoon and post-monsoon seasons. These easterly waves have attracted the attention of many researchers due to the associated heavy rainfall, lightning and thunder squalls. Influence of easterly waves is less explored during pre-monsoon season. It is seen that during years 2001-2015, a total of 80 cases of trough in easterlies were witnessed by southern peninsular India in the pre-monsoon season. The maxima occurred in March (43 cases), followed by April (25 cases) and May (12 cases). It is observed that the year 2005 witnessed the longest spell of easterly waves for 18 days during 24 March to 10 April 2005, which is quite unusual. The event has claimed a death toll of 55 people in the two states of Tamil Nadu and Kerala, and heavy rains associated with this event damaged many houses and huts in Tamil Nadu. The unusual nature of the event has prompted us to undertake the study in details. In all, the event witnessed six systems as troughs in easterlies with their movement westwards from south Andaman Sea region to Lakshadweep and southeast Arabian Sea and Sri Lanka and adjoining Cape Comorin area. An attempt has been made to study the event of easterly waves during the year 2005 by exploring winds, temperature advection, vorticity, moisture convergence and potential instability. The causative reason is due to culmination of positive temperature advection, its multiple interactions with deep convective clouds and moisture incursion from anticyclonic flow close to eastern coast of south peninsular region of India. Observing the waves with the internal mechanism makes the study useful for operational forecasting and provides a better understanding of easterly waves.
机译:东方的波浪是一种热带障碍,从东到西部或西北(WNW)。在印度地区,东风海浪主要发生在冬季,季前翁和季风季节。由于相关的大雨,闪电和雷霆队,这些东风波浪引起了许多研究人员的注意力。在季风季节期间探讨了东风波的影响。人们看来,在2001 - 2015年期间,南半岛印度在季风季节南部的南部印度共有80例谷地宿舍。 Maxima发生在3月(43例),其次是4月(25例)和5月(12例)。据观察,2005年度,2005年3月24日至2005年4月10日,2005年度最长的浪潮咒语是最不寻常的。该活动在泰米尔纳德邦和喀拉拉邦的两个州声称55人的死亡人数,以及与此事件相关的大雨损坏了泰米尔纳德邦的许多房屋和小屋。事件的不寻常性质促使我们在详细中进行研究。总体而言,该活动目睹了六个系统,因为南安马海地区向西的东部飞往Lakshadweep和东南阿拉伯海和斯里兰卡和毗邻Cape Comorin地区。通过探索风力,温度平流,涡流,湿气收敛性和潜在不稳定,已经尝试研究2005年的东风浪潮事件。致病原因是由于阳性温度平流的高潮,其与印度南半岛地区东海岸的反周性流动与深层对流云和水分入侵的多重相互作用。使用内部机制观察波浪使研究可用于操作预测,并提供对东风的了解。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号