Recovery of the one and two dimensional windfields from chemical constituent observations using the constituent transport equation and an extended Kalman filter
Author:
Publisher
Springer Science and Business Media LLC
Subject
Atmospheric Science
Link
http://link.springer.com/content/pdf/10.1007/BF01029789.pdf
Reference20 articles.
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2. Austin, J., 1992: Toward the four dimensional assimilation of stratospheric chemical constituents.J. Geophys. Res.,97 D18, 2569?2588.
3. Cohn, S. E., Dee, D. 1988: Observability of discretized partial differential equations.SIAM J. Numer. Anal.,25, 586?617.
4. Cohn, S. E., Sivakumaran, N., Todling, R., 1994: A fixed-lag Kalman smoother for retrospective atmospheric data assimilation.Mon. Wea. Rev.,122, 2838?2867.
5. Courtier, P., Talagrand, O., 1990: Variational assimilation of meteorological observations with the direct and adjoint shallow water equations.Tellus,42A, 531?549.
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