首页> 外文期刊>Journal of atmospheric and solar-terrestrial physics >Numerical simulation of mesoscale surface pressure features with trailing stratiform squall lines using WRF -ARW model over Gangetic West Bengal region
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Numerical simulation of mesoscale surface pressure features with trailing stratiform squall lines using WRF -ARW model over Gangetic West Bengal region

机译:Messcale表面压力特征的数值模拟,使用WRF -ARW模型在Gancet西孟加拉邦地区使用WRF -ARW模型

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AbstractIn the present study, an attempt has been made to investigate the simulation of mesoscale surface pressure patterns like pre-squall mesolow, mesohigh and wake low associated with leading convective line-trailing stratiform (TS) squall lines over Gangetic West Bengal (GWB). For this purpose, a two way interactive triple nested domain with high resolution WRF model having2 km grid length in the innermost domain is used. The model simulated results are compared with the availablein-situobservations obtained as a part of Severe Thunderstorm: Observations and Regional Modeling (STORM) programme, reflectivity products of Doppler Weather Radar (DWR) Kolkata and TRMM rainfall. Three TS squall lines (15 May 2009, 5 May 2010 and 7 May 2010) are chosen during pre-monsoon thunderstorm season for this study. The model simulated results of diurnal variation of temperature, relative humidity, wind speed and direction at the station Kharagpur in GWB region reveal a sudden fall in temperature, increase in the amount of relative humidity and sudden rise in wind speed during the arrival of the storms. Such results are well comparable with the observations though there are some leading or lagging of time in respect of actual occurrences of such events. The study indicates that the model is able to predict the occurrences of three typical surface pressure features namely: pre-squall mesolow, meso high and wake low. The predicted surface parameters like accumulated rainfall, maximum reflectivity and vertical profiles (temperature, relative humidity and winds) are well accorded with the observations. The convective and stratiform precipitation region of
机译:<![CDATA [ 抽象 在本研究中,已经尝试调查Mesoscale表面压力图案的模拟,如预先打火Mesolow,间隙和唤醒与难以置的对流线尾拖纹状(TS)难以达到难以置的难潮西孟加拉邦(GWB)。为此目的,使用了一种具有高分辨率WRF模型的两种交互式三重嵌套域,使用了在最内域中的2km网格长度。将模型模拟结果与可用的原位进行比较,以雷暴的一部分获得的Italic> Italic>观察结果:观察和区域建模(风暴)计划,多普勒天气雷达的反射率产品(DWR)加尔各答和TRMM降雨。三个TS Squall系列(2009年5月15日,2010年5月5日和2010年5月7日)在这项研究的季风雷暴季节期间被选中。在GWB区域的kharagpur驻地喀古斯的温度,相对湿度,风速和方向上的日本变化的模型结果突然下降,在风暴到来期间,风速突然增加的湿度和风速突然上升的突然下降。 。这种结果与观察结果相比,虽然关于这些事件的实际发生的时间存在一些领先或滞后。该研究表明,该模型能够预测三种典型表面压力的发生,即:预先打褶的模态,中间高,唤醒低。预测的表面参数,如累积的降雨,最大反射率和垂直轮廓(温度,相对湿度和风)很好地符合观察结果。对流和层状沉淀区

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