Atmospheric Model Applications by I. Yucel

By I. Yucel

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Results and discussion With reference to the LCC conditions summarized in Section 5, the basic requirements for satellite launch missions from SHAR (India) can be summarized under the following classes: • Low Pressure Systems: Since SHAR is a coastal station located on the eastern coastline of the Indian subcontinent, the local weather is severely affected by low pressure systems formed in the Bay of Bengal. Thus an adequate information on the probability of formation Applications of Mesoscale Atmospheric Models in Short-Range Predictions Satellite Launch Campaigns in India Applications of Mesoscale Weather Atmospheric Models in Short-RangeDuring Weather Predictions during Satellite Launch Campaigns in India 339 of any low pressure system over Bay of Bengal with sufficient lead time remain one of the basic requirements from the mission team.

In a broad sense, atmospheric models can be classified into two categories: (1) Hydrostatic; and (2) Non-hydrostatic. The first class of models assume hydrostatic equilibrium of atmosphere, while the second class are useful in dealing non-hydrostatic processes and their effects become more useful when the length of the feature is approximately equivalent to its height (Anthes & Warner, 1974; Bannoon, 1995; Pielke, 1984). Thus, non-hydrostatic models can be quite sensitive to small differences in atmospheric structure in vertical.

A typical comparison of ARPS model-simulated zonal and meridional winds in vertical with balloon-borne GPS Sonde measurements. 4. By choosing HRM and ARPS, we take care of the possible differences in forecasting due to hydrostatic and non-hydrostatic approach. Thus, we make use of both the models simultaneously to provide short-range weather predictions over SHAR. 8. Scope for future work In the present chapter, we described the potential of two atmospheric models, namely HRM and ARPS in providing valuable information with respect to launch commit criteria for satellite launch missions.

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