INSIGHTS and INNOVATIONS Parameterization of the Atmospheric Boundary Layer A View from Just Above the Inversion BY J . TEIXEIRA, B. STEVENS, C . S. BRETHERTON, R . CEDERWALL, J . D . DOYLE, J . C . GOLAZ, A . A . M. HOLTSLAG, S. A . KLEIN, J . K . LUNDQUIST, D . A . RANDALL, A . P. SIEBESMA, AND P. M. M. SOARES ne of th e mai n components of th e climate system layer processes are known to have a profoun d in- fluenc e on the climate system. Relevant examples is th e atmospheric boundar y layer, whic h medi- Oates the interactions between the ocean/land include the feedbacks betwee n boundar y layer clouds an d climate. However, in weather and climate predic- surface and the free atmosphere. Several boundary FIG. I. Changes in low (below 700 hPa) cloud cover and low liquid + ice path (TWP ) for different perturbation experiment s and for thre e U.S . climate models (CAM , GFDL , and GMAO) . Note the opposite signs, in term s of the low cloud and low TW P sensitivities, between the different models. Thre e
Bulletin of the American Meteorological Society – American Meteorological Society
Published: Apr 1, 2008
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