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A Case-Study of Sea Breeze Circulation at Thumba Coast through Observations and Modelling

机译:拇指海岸沿岸海风环流的观测与模拟研究

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摘要

A case study of sea breeze circulation at a coastal region Thumba (8.5°N, 76.9°E) was carried out using Doppler Sodar, surface wind, temperature, humidity measurements and radiosonde ascents. The analysis of surface meteorological data showed that the onset of sea breeze on 12th April 2006 was at 0945 hrs. GPS sonde observation over sea at 1425 hrs and Radiosonde observation over land at 1730 showed a well developed sea breeze circulation over Thumba coast by afternoon hours. The vertical extent of sea breeze circulation was ~1000m over sea as well as on land. The Thermal Internal Boundary Layer (TIBL) depth associated with sea breeze circulation was about 400m at 8 km away from coast. The marine mixed layer height was ~500m about 12 km away from the coast. Numerical simulation of sea breeze was made using HRM (High Resolution Model) and compared the results with the observations.
机译:利用多普勒声雷达,表面风,温度,湿度测量和探空仪上升,对拇指地区沿海海风环流(8.5°N,76.9°E)进行了案例研究。对地表气象数据的分析表明,2006年4月12日海风开始于0945小时。 GPS探空仪在1425时对海上的观测和无线电探空仪在1730年对陆地的观测表明,下午时分,Thumba海岸的海风环流发育良好。海面和陆地上海风环流的垂直范围均为〜1000m。与海风循环相关的热内边界层(TIBL)深度在距海岸8公里处约为400m。海洋混合层高度为〜500m,距海岸约12 km。使用HRM(高分辨率模型)对海风进行了数值模拟,并将结果与​​观测值进行了比较。

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