首页> 外文期刊>Journal of earth system science >Simulation of Marine Boundary Layer characteristics using a 1-D PBL model over the Bay of Bengal during BOBMEX-99
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Simulation of Marine Boundary Layer characteristics using a 1-D PBL model over the Bay of Bengal during BOBMEX-99

机译:在BOBMEX-99期间使用1-D PBL模型在孟加拉湾上模拟海洋边界层特征

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摘要

The characteristic features of the marine boundary layer (MBL) over the Bay of Bengal during the southwest monsoon and the factors influencing it are investigated. The Bay of Bengal and Monsoon Experiment (BOBMEX) carried out during July-August 1999 is the first observational experiment under the Indian Climate Research Programme (ICRP). A very high-resolution data in the vertical was obtained during this experiment, which was used to study the MBL characteristics off the east coast of India in the north and south Bay of Bengal. Spells of active and suppressed convection over the Bay were observed, of which, three representative convective episodes were considered for the study. For this purpose a one-dimensional multi-level PBL model with a TKE-e??€ closure scheme was used. The soundings, viz., the vertical profiles of temperature, humidity, zonal and meridional component of wind, obtained onboard ORV Sagar Kanya and from coastal stations along the east coast are used for the study. The temporal evolution of turbulent kinetic energy, marine boundary layer height (MBLH), sensible and latent heat fluxes and drag coefficient of momentum are simulated for different epochs of monsoon and monsoon depressions during BOBMEX-99.The model also generates the vertical profiles of potential temperature, specific humidity, zonal and meridional wind. These simulated values compared reasonably well with the observations available from BOBMEX.
机译:研究了西南季风期间孟加拉湾海洋边界层(MBL)的特征及其影响因素。孟加拉湾和季风试验(BOBMEX)于1999年7月至8月进行,是印度气候研究计划(ICRP)的首次观测试验。在此实验期间,获得了垂直方向的高分辨率数据,该数据用于研究印度东部海岸孟加拉北部和南部海湾的MBL特征。观察到海湾上主动对流和抑制对流的法术,其中考虑了三个代表性对流事件。为此,使用了带有TKE-e ??€关闭方案的一维多层PBL模型。这项研究使用了在ORV Sagar Kanya上和从东海岸的沿海站点获得的测深,即温度,湿度,风向和子午线垂直分量。在BOBMEX-99期间,模拟了季风和季风凹陷不同时期的湍动能,海洋边界层高度(MBLH),显热和潜热通量以及动量阻力系数的时间演变,该模型还产生了势能的垂直剖面温度,比湿度,纬向和经向风。这些模拟值与BOBMEX提供的观察结果相当合理。

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