Editorial Type:
Article
Article Type:
Research Article

Jet Alignment in a Two-Layer Quasigeostrophic Channel Using One-Dimensional Grid Warping

Brad E. Beechler Department of Atmospheric and Oceanic Sciences, University of Colorado, Cooperative Institute for Research in Environmental Sciences, and NOAA/Earth System Research Laboratory, Boulder, Colorado

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Jeffrey B. Weiss Department of Atmospheric and Oceanic Sciences, University of Colorado, Boulder, Colorado

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Gregory S. Duane National Center for Atmospheric Research,* Boulder, Colorado

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Joseph Tribbia National Center for Atmospheric Research,* Boulder, Colorado

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Print Publication:
01 Jul 2010
DOI:
https://doi.org/10.1175/2009JAS3263.1
Page(s):
2296–2306
Restricted access

Abstract

Because of position errors traditional methods of data assimilation can broaden and weaken jets or other flow structures leading to reduced forecast skill. Here a technique to assimilate properties of coherent structures is developed and tested. Focusing on jets, the technique identifies jets in both the modeled and observed fields and warps the model grid so that the jet positions are better aligned prior to further assimilation of observations. The technique is tested using optimal interpolation on the flow in a two-layer quasigeostrophic channel. The results show that a simple and fast jet position correction algorithm can significantly improve the skill of a 12-h forecast. Furthermore, the results indicate that this method of position correction maintains its utility when observations become sparse.

Corresponding author address: Brad Beechler, NOAA/GSD, Earth Systems Research Lab, Boulder, CO 80305. Email: brad.e.beechler@noaa.gov

Abstract

Because of position errors traditional methods of data assimilation can broaden and weaken jets or other flow structures leading to reduced forecast skill. Here a technique to assimilate properties of coherent structures is developed and tested. Focusing on jets, the technique identifies jets in both the modeled and observed fields and warps the model grid so that the jet positions are better aligned prior to further assimilation of observations. The technique is tested using optimal interpolation on the flow in a two-layer quasigeostrophic channel. The results show that a simple and fast jet position correction algorithm can significantly improve the skill of a 12-h forecast. Furthermore, the results indicate that this method of position correction maintains its utility when observations become sparse.

Corresponding author address: Brad Beechler, NOAA/GSD, Earth Systems Research Lab, Boulder, CO 80305. Email: brad.e.beechler@noaa.gov

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