ACP Atmospheric Chemistry and Physics ACP 1680-7324 Copernicus GmbH Göttingen, Germany 10.5194/acp-11-421-2011 A regional real-time forecast of marine boundary layers during VOCALS-REx Wang S. 1 O'Neill L. W. 2 Jiang Q. 1 de Szoeke S. P. 3 Hong X. 1 Jin H. 1 Thompson W. T. 1 Zheng X. 4 Naval Research Laboratory, Monterey, CA, USA National Research Council, Naval Research Laboratory, Monterey, CA, USA Oregon State University, College of Ocean and Atmospheric Sciences, Corvallis, Oregon, USA RSMA, University of Miami, Miami, FL, USA 17 01 2011 11 2 421 437 This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. This article is available from http://www.atmos-chem-phys.net/11/421/2011/acp-11-421-2011.html The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/421/2011/acp-11-421-2011.pdf

This paper presents an evaluation and validation of the Naval Research Laboratory's COAMPS<sup>®</sup> real-time forecasts during the VOCALS-REx over the area off the west coast of Chile/Peru in the Southeast Pacific during October and November 2008. The analyses focus on the marine boundary layer (MBL) structure. These forecasts are compared with lower troposphere soundings, in situ surface measurements, and satellite observations. The predicted mean MBL cloud and surface wind spatial distributions are in good agreement with the satellite observations. The large-scale longitudinal variation of the MBL structure along 20° S is captured by the forecasts. That is, the MBL height increases westward toward the open ocean, the moisture just above the inversion decreases, and the MBL structure becomes more decoupled offshore. The observed strong wind shear across the cloud-top inversion near 20° S was correctly predicted by the model. The model's cloud spatial and temporal distribution in the 15 km grid mesh is sporadic compared to satellite observations. Our results suggest that this is caused by grid-scale convection likely due to a lack of a shallow cumulus convection parameterization in the model. Both observations and model forecasts show wind speed maxima near the top of MBL along 20° S, which is consistent with the westward upslope of the MBL heights based on the thermal wind relationship. The forecasts produced well-defined diurnal variations in the spatially-averaged MBL structure, although the overall signal is weaker than those derived from the in situ measurements and satellite data. The MBL heights are generally underpredicted in the nearshore area. An analysis of the sensitivity of the MBL height to horizontal and vertical grid resolution suggests that the underprediction is likely associated with overprediction of the mesoscale downward motion and cold advection near the coast.

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