Journal
MONTHLY WEATHER REVIEW
Volume 139, Issue 6, Pages 1952-1959Publisher
AMER METEOROLOGICAL SOC
DOI: 10.1175/2010MWR3513.1
Keywords
-
Categories
Funding
- National Science Foundation
- Department of Energy through DOE-ARM [DE-FG02-08ER64575]
Ask authors/readers for more resources
An upper-level cold bias in potential temperature tendencies of 10 K day(-1), strongest at the top of the model, is observed in Weather Research and Forecasting (WRF) model forecasts. The bias originates from the Rapid Radiative Transfer Model longwave radiation physics scheme and can be reduced substantially by 1) modifying the treatment within the scheme by adding a multilayer buffer between the model top and top of the atmosphere and 2) constraining stratospheric water vapor to remain within the estimated climatology in the stratosphere. These changes reduce the longwave heating rate bias at the model top to +/- 0.5 K day(-1). Corresponding bias reductions are also seen, particularly near the tropopause.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available