PUBLICATIONS Journal of Geophysical Research: Atmospheres RESEARCH ARTICLE Modeling atmospheric longwave radiation 10.1002/2014JD022310 at the surface during overcast skies: Key Points: The role of cloud base height • Comparison of several methods to estimate LW under cloudy skies A. Viúdez-Mora1, M. Costa-Surós2, J. Calbó2, and J. A. González2 is presented • fi Using synthetic pro les, estimated 1NASA Langley Research Center, Science Mission Directorate, Hampton, Virginia, USA, 2Group of Environmental Physics, CBH, LW is approached within À 7Wm 2 (1 SD) University of Girona, GIRONA, Spain • CRE at the surface decreases with CBH À at 4–5Wm 2/km in a midlatitude site Abstract The behavior of the atmospheric downward longwave radiation at the surface under overcast conditions is studied. For optically thick clouds, longwave radiation depends greatly on the cloud base height (CBH), besides temperature and water vapor profiles. The CBH determines the cloud emission Correspondence to: A. Viúdez-Mora, temperature and the air layers contributing to the longwave radiation that reaches the surface. Overcast
[email protected] situations observed at Girona (NE Iberian Peninsula) were studied by using a radiative transfer model. The data set includes different seasons, and a large range of CBH (0–5000 m). The atmosphere profiles were taken Citation: from the European Center for Medium-Range Weather Forecast analysis. The CBH was determined from Viúdez-Mora, A., M. Costa-Surós, J. Calbó, ceilometer measurements and also estimated by using a suitable method applied to the vertical profile of and J. A. González (2015), Modeling relative humidity. The agreement between calculations and pyrgeometer measurements is remarkably atmospheric longwave radiation at the À2 surface during overcast skies: The role good (1.6 ± 6.2 W m ) if the observed CBH is used; poorer results are obtained with the estimated CBH À of cloud base height, J.