Impact of Doppler Radar Wind in Simulating the Intensity and Propagation of Rainbands Associated with Mesoscale Convective Complexes Using MM5-3DVAR System

Author:

Abhilash S.,Das Someshwar,Kalsi S. R.,Das Gupta M.,Mohankumar K.,George John P.,Banerjee S. K.,Thampi S. B.,Pradhan D.

Publisher

Birkhäuser Basel

Reference23 articles.

1. Anderson, T. (1998), VAD winds from C band Ericsson Doppler Weather Radars, Meteor. Zeitschrift 7, 309–319.

2. Banerjee, S. K., Kundu, S. K., and Singh, H. A. K. (2004), A study of 12th November 2002 Cyclonic storm in the Bay of Bengal using Doppler Weather Radar, Mausam, 55,4, 671–680.

3. Barker, D.M., Huang, W., Guo, -Y. R., and Xio, Q. N. (2004), A three dimensional Variational (3DVAR) Data Assimilation System with MM5: Implementation and Initial results, Mon. Wea. Rev., 132, 897–914.

4. Barker, D. M., Huang, W., Guo,-Y. R., and Bourgeois, Al (2003), A Three-Dimensional Variational (3DVAR) Data Assimilation System for Use With MM5, NACR Technical Note, NCAR/TN-453+STR, February 2003, 68

5. Browning, K. A. and Wexler, R. (1968), The determination of kinematic properties of a wind field using Doppler radar, J. Appl. Meteor. 7, 105–113.

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