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An Objective Approach for Prediction of Daily Summer Monsoon Rainfall over Orissa (India) due to Interaction of Mesoscale and Large-scale Synoptic Systems

机译:中尺度和大尺度天气系统相互作用的印度奥里萨邦夏季夏季季风降水的客观预测方法

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Orissa State, a meteorological subdivision of India, lies on the east coast of India close to north Bay of Bengal and to the south of the normal position of the monsoon trough. The monsoon disturbances such as depressions and cyclonic storms mostly develop to the north of 15° N over the Bay of Bengal and move along the monsoon trough. As Orissa lies in the southwest sector of such disturbances, it experiences very heavy rainfall due to the interaction of these systems with mesoscale convection sometimes leading to flood. The orography due to the Eastern Ghat and other hill peaks in Orissa and environs play a significant role in this interaction. The objective of this study is to develop an objective statistical model to predict the occurrence and quantity of precipitation during the next 24 hours over specific locations of Orissa, due to monsoon disturbances over north Bay and adjoining west central Bay of Bengal based on observations to up 0300 UTC of the day. A probability of precipitation (PoP) model has been developed by applying forward stepwise regression with available surface and upper air meteorological parameters observed in and around Orissa in association with monsoon disturbances during the summer monsoon season (June-September). The PoP forecast has been converted into the deterministic occurrenceon-occurrence of precipitation forecast using the critical value of PoP. The parameters selected through stepwise regression have been considered to develop quantitative precipitation forecast (QPF) model using multiple discriminant analysis (MDA) for categorical prediction of precipitation in different ranges such as 0.1–10, 11–25, 26–50, 51–100 and >100 mm if the occurrence of precipitation is predicted by PoP model. All the above models have been developed based on data of summer monsoon seasons of 1980–1994, and data during 1995–1998 have been used for testing the skill of the models. Considering six representative stations for six homogeneous regions in Orissa, the PoP model performs very well with percentages of correct forecast for occurrenceon-occurrence of precipitation being about 96% and 88%, respectively for developmental and independent data. The skill of the QPF model, though relatively less, is reasonable for lower ranges of precipitation. The skill of the model is limited for higher ranges of precipitation.
机译:奥里萨邦(Orissa State)是印度的一个气象部门,位于印度的东海岸,靠近孟加拉北部湾,位于季风槽正常位置的南部。诸如凹陷和气旋风暴之类的季风扰动大多发展到孟加拉湾北部15°N以北,并沿着季风槽移动。由于奥里萨邦(Orissa)处于此类扰动的西南部,由于这些系统与中尺度对流的相互作用有时会导致洪水,因此降雨非常多。由东高止山脉和奥里萨邦及周边地区的其他山峰造成的地形在这种相互作用中起着重要作用。这项研究的目的是建立一个客观的统计模型,以预测北部奥里萨邦特定位置未来24小时内由于北部海湾和毗邻的孟加拉中西部海湾的季风扰动引起的降水的发生和数量。当天的0300 UTC。通过在夏季风季(6月至9月)与季风扰动相关的奥里萨邦及其周围地区观测到的可用地面和高空气象参数,通过进行逐步逐步回归,建立了降水概率(PoP)模型。使用PoP的临界值,将PoP预报转换为确定的降水预测发生/不发生。通过逐步回归选择的参数已被认为可以使用多重判别分析(MDA)建立定量降水预报(QPF)模型,以便对0.1-10、11-25、26-50、51-100等不同范围的降水进行分类预测如果通过PoP模型预测降水的发生,则> 100 mm。以上所有模型都是根据1980-1994年夏季风季节的数据开发的,而1995-1998年的数据已用于检验模型的技巧。考虑到奥里萨邦六个均质地区的六个代表站,PoP模型的效果非常好,对于发展和独立数据,降水发生/不发生的正确预测百分比分别约为96%和88%。 QPF模型的技能虽然相对较少,但对于较低的降水范围是合理的。该模型的技能仅限于更高的降水范围。

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