Please use this identifier to cite or link to this item:
Title: A theory for the scalar roughness and the scalar transfer coefficients over snow and sea ice
Authors: Andreas, Edgar L.
Keywords: Heat and moisture exchange
Surface processes
Roughness lengths
Sea ice
Issue Date: Sep-1986
Publisher: Cold Regions Research and Engineering Laboratory (U.S.)
Engineer Research and Development Center (U.S.)
Series/Report no.: CRREL report ; 86-9.
Description: CRREL Report
Abstract: The bulk aerodynamic transfer coefficients for sensible (๐˜พ๐—›) and latent (๐˜พ๐—˜) heat over snow and sea ice surfaces are necessary for accurately modeling the surface energy budget but are very difficult to measure. This report therefore presents a theory that predicts ๐˜พ๐—› and ๐˜พ๐—˜ as functions of the wind speed and a surface roughness parameter. The crux of the model is establishing the interfacial sublayer profiles of the scalars, temperature and water vapor, over aerodynamically smooth and rough surfaces. These interfacial sublayer profiles are derived from a surface-renewal model in which turbulent eddies continually sweep, down to the surface, transfer scalar contaminants across the interface by molecular diffusion, and then burst away. Matching the interfacial sublayer profiles with the usual semilogarithmic inertial sublayer profiles yields the roughness lengths for temperature and water vapor. With these and a model for the drag coefficient over snow and sea ice based on actual measurements, the transfer coefficients are predicted. ๐˜พ๐—˜ is always a few percent larger than ๐˜พ๐—›. Both decrease monotonically with increasing wind speed for speeds above 1 m/s, and both increase at all wind speeds as the surface gets rougher. Both, nevertheless, are almost always between 1.0x10^-3 and 1.5x10^-3.
Appears in Collections:CRREL Report

Files in This Item:
File Description SizeFormat 
CR-86-9.pdf1 MBAdobe PDFThumbnail