Three-Dimensional Wind Field Retrieved from Dual-Doppler Radar Based on a Variational Method: Refinement of Vertical Velocity Estimates-Reference-Cited by-同舟云学术

Three-Dimensional Wind Field Retrieved from Dual-Doppler Radar Based on a Variational Method: Refinement of Vertical Velocity Estimates

Published:2022-01 Issue:1 Volume:39 Page:145-160
ISSN:0256-1530
Container-title:Advances in Atmospheric Sciences
language:en
Short-container-title:Adv. Atmos. Sci.

Author:

Xue Chenbin,Ding Zhiying,Shen Xinyong,Chen Xian

Publisher

Springer Science and Business Media LLC

Subject

Atmospheric Science

Link

https://link.springer.com/content/pdf/10.1007/s00376-021-1035-9.pdf

Reference48 articles.

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2. Boucher, R. J., R. Wexler, D. Atlas, and R. M. Lhermitte, 1965: Mesoscale wind structure revealed by doppler radar. J. Appl. Meteor., 4, 590–597, https://doi.org/10.1175/1520-0450(1965)004<0590:MWSRBD>2.0.CO;2.

3. Bousquet, O., and M. Chong, 1998: A multiple-doppler synthesis and continuity adjustment technique (MUSCAT) to recover wind components from doppler radar measurements. J. Atmos. Oceanic Technol., 15, 343–359, https://doi.org/10.1175/1520-0426(1998)015<0343:AMDSAC>2.0.CO;2.

4. Caton, P. G., 1963: The measurement of wind and convergence by doppler radar. Proc. 10th Weather Radar Conf., Washington DC, Amer. Meteor. Soc., 290–296.

5. Chong, M., and C. Campos, 1996: Extended overdetermined dual-doppler formalism in synthesizing airborne doppler radar data. J. Atmos. Oceanic Technol., 13, 581–597, https://doi.org/10.1175/1520-0426(1996)013<0581:EODDFI>2.0.CO;2.

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