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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).
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. , Pal, P. K. & Joshi, P. C. (2007). , Pure and Applied Geophysics 164: 1617 – 1637. Ramachandran, R. (2008). DWR Data Assimilation in Numerical Weather Prediction for Forecasts of Thunderstorms at Sriharikota, Technology Development for Atmospheric Research and Applications pp.
Similar to total cloud fraction, HRM could simulate rainfall pattern also to a good extent. During PSLV-C12 launch campaign, the Bay of Bengal (BoB) underwent severe cyclonic storm named - BIJLI between 14 - 16 April 2009 and it was one of the prime concerns for launch related activities. In this regard, HRM simulated meteorological fields were found to be quite useful in inference of wind circulation prevailing over the launch site 34 10 Atmospheric Model Applications ATMOSPHERIC MODELS (a) HRM-simulated total cloud cover +6 Hrs in (b) HRM-simulated total cloud cover +30 Hrs in advance; advance; (c) Kalpana satellite imagery of cloud coverage in the visible range over the Indian sub-continent for 17th October 2008: 0700 GMT during Chandrayaan campaign; Fig.
