The current major expansion in observational capability of the National Weather Service is principally in the volume of asynchronous data rather than synchronous observations at the standard synoptic times. Hence, the National Meteorological Center is considering a continuous data assimilation system to replace at some time the intermittent system now used by its regional and global operational models. We describe this system, based on the Newtonian relaxation technique, as developed for the eta model. Experiments are performed for the first intensive observing period of the Genesis of Atlantic Lows Experiment (GALE) in January 1986, when strong upper-level cyclogenesis occurred, with a pronounced tropopause fold but only modest surface development. The GALE level IIIb dataset was used for initializing and updating the model. -from Authors
CITATION STYLE
Ramamurthy, M. K., & Tai-Yi Xu. (1993). Continuous data assimilation experiments with the NMC eta model: a GALE IOP 1 case study. Monthly Weather Review, 121(11), 3082–3105. https://doi.org/10.1175/1520-0493(1993)121<3082:CDAEWT>2.0.CO;2
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