The retrieval of asymmetric tropical cyclone structures using doppler radar simulations and observations with the extended GBVTD technique

AMS Citation:
Liou, Y. -C., T. -C. C. Wang, W. -chau Lee, and Y. -J. Chang, 2006: The retrieval of asymmetric tropical cyclone structures using doppler radar simulations and observations with the extended GBVTD technique. Monthly Weather Review, 134, 1140-1160, doi:10.1175/MWR3107.1.
Date:2006-04-01
Resource Type:article
Title:The retrieval of asymmetric tropical cyclone structures using doppler radar simulations and observations with the extended GBVTD technique
Abstract: The ground-based velocity track display (GBVTD) technique is extended to two Doppler radars to retrieve the structure of a tropical cyclone's (TC’s) circulation. With this extension, it is found that the asymmetric part of the TC radial wind component can be derived up to its angular wavenumber-1 structure, and the accuracy of the retrieved TC tangential wind component can be further improved. Although two radar systems are used, a comparison with the traditional dual-Doppler synthesis indicates that this extended GBVTD (EGBVTD) approach is able to estimate more of the TC circulation when there are missing data. Previous research along with this study reveals that the existence of strong asymmetric radial flows can degrade the quality of the GBVTD-derived wind fields. When a TC is observed by one radar, it is suggested that the GBVTD method be applied to TCs over a flat surface (e.g., the ocean) where the assumption of relatively smaller asymmetric radial winds than asymmetric tangential winds is more likely to be true. However, when a TC is observed by two radar systems, especially when the topographic effects are expected to be significant, the EGBVTD rather than the traditional dual-Doppler synthesis should be used. The feasibility of the proposed EGBVTD method is demonstrated by applying it to an idealized TC circulation model as well as a real case study. Finally, the possibility of combining EGBVTD with other observational instruments, such as dropsonde or wind profilers, to recover the asymmetric TC radial flow structures with even higher wavenumbers is discussed.
Peer Review:Refereed
Copyright Information:Copyright 2006 American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be "fair use" under Section 107 or that satisfies the conditions specified in Section 108 of the U.S. Copyright Law (17 USC, as revised by P.L. 94-553) does not require the Society's permission. Republication, systematic reproduction, posting in electronic form on servers, or other uses of this material, except as exempted by the above statements, requires written permission or license from the AMS. Additional details are provided in the AMS Copyright Policies, available from the AMS at 617-227-2425 or amspubs@ametsoc.org. Permission to place a copy of this work on this server has been provided by the AMS. The AMS does not guarantee that the copy provided here is an accurate copy of the published work.
OpenSky citable URL: ark:/85065/d7057gkx
Publisher's Version: 10.1175/MWR3107.1
Author(s):
  • Yu-Chieng Liou
  • Tai-Chi Chen Wang
  • Wen-chau Lee - NCAR/UCAR
  • Ya-Ju Chang
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