Role of Four-Dimensional Data Assimilation on Track and Intensity of Severe Cyclonic Storms. (27th February 2013)

• Record Type: Journal Article
• Authors: Kanase, Radhika D.; Salvekar, P. S.
• Other Names: Georgiadis T. Academic Editor.; Saha A. Academic Editor.; Wang D.-Y. Academic Editor.
• Is Part Of: ISRN meteorology. Volume 2013(2013)
• Publication Date: 2013-02-27
• Subjects: Meteorology -- Periodicals; Meteorology; Periodicals; Electronic journals; 551.5
• DOI: 10.1155/2013/972713
• Languages: English
• ISSNs: 2090-7516

Abstract

Abstract : To examine the role of four dimensional data assimilation (FDDA) on prediction of two Severe Cyclonic Storm (Aila (May 23–26, 2009) andJal (Nov 4–8, 2010)), four numerical experiments are performed using WRF-ARW model with three nested domains having two-way interaction and physical parameterization schemes as CPS-BMJ, MP-WSM6, and PBL-YSU. In each experiment, the model integration is started prior to the formation of depression and continued till the observed landfall. For the experiment without FDDA, NCEP-FNL data alone is used as initial and boundary conditions and for the experiments with FDDA, additional observations are used. In all the experiments, FDDA is considered only in the outer domain upto 24 hrs of integration and then the inner domain is introduced. The results are examined in terms of surface circulation, vorticity, CSLP, MSW, and surface track error. FDDA-produced surface circulation and vorticity showed well-organized structure. For the case of Aila, the surface track (maximum track error: 281 km) and landfall position (88°E/21.73°N) in FDDA experiment are predicted better than experiment without FDDA (track error: 445 km and landfall position 87.13°E/20.37°N) whereas the landfall time experiment without FDDA is closer to observations (between 09 and 12 UTC of May 25) than that of experiment with FDDA(06 UTC of May 25). When CSLP and MSW are examined, the overall intensity is well predicted with FDDA experiment except near to the landfall time. For Jal cyclone, FDDA played significant role to improve the landfall position (80.16°E/13.67°N) with a time lead of ~ 10 hrs but other parameters remain more or less unchanged.