Atmospheric Model Applications by I. Yucel

By I. Yucel

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121. , Wergen, G. P. D. , & Baumgardner, J. (2002). The Operational Global Icosahedral-Hexagonal Gridpoint Model GME: Description and High-Resolution Tests, Monthly Weather Review 130. , Zack, W. & Taylor, G. E. (1996). Work station based real-time mesoscale modeling designed for weather support to operations at the Kennedy Space Center and Cape Canaveral Air Station, Bullen of American Meteorological Society 77: 653 – 672. Pielke, R. A. (1984). Mesoscale Meteorological Modeling, Academic Press Inc,Orlando, Florida.

3 depicts wind vector field at 850 hPa seen through NCEP reanalysis during formation of BIJLI cyclonic storm in the month of April 2009. HRM simulated wind vector field for the same time +18 hours in advance shown in Fig. 3 is well in tune with the NCEP reanalysis. A cyclonic circulation with low pressure over the BoB at 850 hPa levels are clearly captured in simulations almost 18 hours in advance; however there is a mismatch in the exact location of low pressure of the system and it can be attributed to lack of observational data in HRM model runs.

DWR products are also being assimilated in ARPS model simulations. • Visibility: Periodical observations on the visibility are required for range safety operations. Ideally, direct visual observation of the launch vehicle is required through the lower troposphere (≈ 5000 m). In the case of overcast sky conditions, range safety measures depend on other remote sensing techniques. • Surface and Upper Winds: During the movement of launch vehicle from assembly building to the launch pad, the surface wind speeds should not exceed a pre-designated threshold (≈ 20m/s).

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