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Characterization of sea/land breeze circulation along the west coast of Indian sub-continent during pre-monsoon season

机译:季风前季节印度次大陆西海岸海陆风环流的特征

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摘要

High-resolution Regional Model is used to study the structure and dynamics of Sea/Land Breeze Circulation along west coast of Indian Sub-continent during pre-monsoon season. Both the observations from ocean and land are in agreement with the model simulations. From the model simulations, a time delay of 3 hours is observed in the onset of sea breeze over ocean and land (~28 km from the sea/land interface). The two main components of the sea breeze circulation cell, the sea breeze flow in the lower levels and the return current in the upper levels are clearly modeled. The vertical extent of sea breeze circulation cell is ~1 km and, the horizontal seaward and landward extensions are ~100 and ~75 km respectively from the sea/land interface. Within the sea breeze circulation cell, during daytime, a shallow mixed layer (600-800 m) over ocean and a convective mixed layer (1000-1200 m) over the land are observed. Observations and simulations verified the pre-assumption of the near neutral lapse rate existing over ocean and transferring to the onshore regions.
机译:高分辨率区域模型用于研究季风前季节印度次大陆西海岸海陆风环流的结构和动力学。海洋和陆地的观测都与模型模拟一致。从模型模拟中可以看出,海洋和陆地上的海风(距海陆界面约28 km)开始出现3个小时的延迟。海风循环池的两个主要组成部分,较低层的海风流动和较高层的回流电流均已清晰建模。从海陆界面来看,海风环流池的垂直范围为〜1 km,水平向海和向内延伸分别为〜100和〜75 km。在白天的海风循环室内,观察到海洋上空有浅层混合层(600-800 m),陆地上有对流混合层(1000-1200 m)。观测和模拟验证了对海洋上空存在的近中性流失率的预先假设,并转移到了陆上区域。

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