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Assimilation of conventional and satellite wind observations in a mesoscale atmospheric model for studying atmospheric dispersion
Authors:C.V. Srinivas  R. Venkatesan  V. Yesubabu  C. Nagaraju  K.M. Somayajai  P. Chellapandi  Baldev Raj
Affiliation:1. Institut Català de Cienciès del Clima (IC3), Barcelona, Spain;2. Institut de Tècniques Energètiques (INTE), Universitat Politècnica de Catalunya (UPC), Barcelona, Spain;3. European Commission, Joint Research Centre, Institute for Environment and Sustainability, Ispra, Italy;4. Departament d’Ecologia, Universitat de Barcelona (UB), Barcelona, Spain;5. Institució Catalana de Recerca i Estudis Avançats (ICREA), Barcelona, Spain;1. Institute of Environment and Sustainable Development, Banaras Hindu University, Varanasi, India;2. Atmospheric Research Laboratory, Department of Physics, Banaras Hindu University, Varanasi, India;1. Department of Soil Science, Faculty of Agriculture, University of Zagreb, Sveto?imunska 25, 10000 Zagreb, Croatia;2. Centro Nacional de Investigación sobre la Evolución Humana, Paseo Sierra de Atapuerca s/n, 09002 Burgos, Spain;3. School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, B15 2TT Birmingham, United Kingdom
Abstract:A mesoscale atmospheric model PSU/NCAR MM5 is used to provide operational weather forecasts for a nuclear emergency response decision support system on the southeast coast of India. In this study the performance of the MM5 model with assimilation of conventional surface and upper-air observations along with satellite derived 2-d surface wind data from QuickSCAT sources is examined. Two numerical experiments with MM5 are conducted: one with static initialization using NCEP FNL data and second with dynamic initialization by assimilation of observations using four dimensional data assimilation (FDDA) analysis nudging for a pre-forecast period of 12 h. Dispersion simulations are conducted for a hypothetical source at Kalpakkam location with the HYSPLIT Lagrangian particle model using simulated wind field from the above experiments. The present paper brings out the differences in the atmospheric model predictions and the differences in dispersion model results from control and assimilation runs. An improvement is noted in the atmospheric fields from the assimilation experiment which has led to significant alteration in the trajectory positions, plume orientation and its distribution pattern. Sensitivity tests using different PBL and surface parameterizations indicated the simple first order closure schemes (Blackadar, MRF) coupled with the simple soil model have given better results for various atmospheric fields. The study illustrates the impact of the assimilation of the scatterometer wind and automated weather stations (AWS) observations on the meteorological model predictions and the dispersion results.
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