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首页> 外文期刊>Mausam: Journal of the Meteorological Department of India >Synoptic study of extremely heavy rainfall events over lower Yamuna catchment : Some cases
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Synoptic study of extremely heavy rainfall events over lower Yamuna catchment : Some cases

机译:亚穆纳河下游流域特大降雨事件的天气学研究:一些案例

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摘要

Extreme rainfall results in landslides, flash flood and crop damage that have major impact on society, the economy and the environment. During southwest monsoon season, flood mostly occurs in India due to extremely or very heavy rain that originates from environmental and synoptic conditions. An attempt has been made to identify the main synoptic reasons, which are responsible for extremely heavy rainfall events over Lower Yamuna catchment (LYC) through the analysis of the relationship between this rainfall and atmospheric systems for the period 1998-2010 based on modern observational technology and developed forecasting technique in the field of short range prediction. The finding of this study show that the major factor have is the arrival of Bay of Bengal low pressure systems in this region, of course if the ascent local conditions such as heat occur, causing the heaviest rains there. The low pressure systems (LPS like, Cyclone, depression, low pressure area etc.) developed generally over Bay of Bengal moved in west to north-westwards direction and reached over the LYC region. Also LPS may be formed in situ under the influence of upper air cyclonic circulation (cycir) responsible for such events. Such system yield extremely heavy rainfall events (generally in the south-west sector of the system) at isolated places and heavy to very heavy rainfall at a few places and there by caused flood situation. The possibility of occurrence of such type of rainfall would be higher if the LPS is either stagnate or slow over LYC region. The NWP products of RSMC (IMD) New Delhi forecast contours / wind charts for 72, 48 & 24 hrs were found good tool for accurate forecast position of the movement of the LPS. Such information certainly facilitate to forecaster in prediction of extreme rainfall events more accurately so that district authorities may set up necessary infrastructures for disaster preparedness in time.
机译:极端降雨导致滑坡,山洪暴发和农作物受损,对社会,经济和环境产生重大影响。在西南季风季节,洪水主要发生在印度,这是由于来自环境和天气条件的降雨过大或过大。通过基于现代观测技术的分析,分析了1998-2010年该降雨与大气系统之间的关系,试图找出造成下亚木那流域(LYC)特大降雨事件的主要原因。在近距离预测领域开发了预测技术。这项研究的发现表明,主要因素是孟加拉湾低压系统到达该区域,当然,如果发生局部局部条件(如高温),从而导致那里的降雨最多。低压系统(LPS,如旋风,低压,低压区等)总体上在孟加拉湾上空发展,从西向西北方向移动并到达了LYC地区。此外,LPS可能在造成此类事件的高空旋风循环(cycir)的影响下原位形成。这样的系统在偏远地区产生极强的降雨事件(通常在系统的西南部),在少数地区产生强降雨至极强降雨,并由此引发洪水。如果LPS在LYC区域停滞或缓慢,则发生此类降雨的可能性会更高。已发现RSMC(IMD)新德里NWP产品在72、48和24小时内的预测等高线/风向图是准确预测LPS运动位置的良好工具。这样的信息无疑有助于预报员更准确地预测极端降雨事件,以便地区当局可以及时建立必要的基础设施以备灾。

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