Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

The Performance of RAMS in Representing the Convective Boundary Layer Structure in a Very Steep Valley

Journal Article · · Environmental Fluid Mechanics

Data from a comprehensive field study in the Riviera Valley of Southern Switzerland are used to investigate convective boundary layer structure in a steep valley and to evaluate wind and temperature fields, convective boundary layer height, and surface sensible heat fluxes as predicted by the mesoscale model RAMS. Current parameterizations of surface and boundary layer processes in RAMS, as well as in other mesoscale models, are based on scaling laws strictly valid only for flat topography and uniform land cover. Model evaluation is required to investigate whether this limits the applicability of RAMS in steep, inhomogeneous terrain. One clear-sky day with light synoptic winds is selected from the field study. Observed temperature structure across and along the valley is nearly homogeneous while wind structure is complex with a wind speed maximum on one side of the valley. Upvalley flows are not purely thermally driven and mechanical effects near the valley entrance also affect the wind structure. RAMS captured many of the observed boundary layer characteristics within the steep valley. The wind field, temperature structure, and convective boundary layer height in the valley are qualitatively simulated by RAMS, but the horizontal temperature structure across and along the valley is less homogeneous in the model than in the observations. The model reproduced the observed net radiation, except around sunset and sunrise when RAMS does not take into account the shadows cast by the surrounding topography. The observed sensible heat fluxes fall within the range of simulated values at grid points surrounding the measurement sites. Some of the scatter between observed and simulated turbulent sensible heat fluxes are due to sub-grid scale effects related to local topography.

Research Organization:
Pacific Northwest National Laboratory (PNNL), Richland, WA (US)
Sponsoring Organization:
USDOE
DOE Contract Number:
AC05-76RL01830
OSTI ID:
15020533
Report Number(s):
PNNL-SA-40460; KP1202010
Journal Information:
Environmental Fluid Mechanics, Journal Name: Environmental Fluid Mechanics Journal Issue: 1-2 Vol. 5
Country of Publication:
United States
Language:
English

Similar Records

Breakup of a nocturnal temperature inversion in the Dischma Valley during DISKUS
Journal Article · Sun Jan 31 23:00:00 EST 1988 · J. Appl. Meteorol.; (United States) · OSTI ID:5091980

Bridging the gap between microscale land-surface processes and land-atmosphere interactions at the scale of GCM`s
Journal Article · Sat Jun 20 00:00:00 EDT 1992 · AIP Conference Proceedings · OSTI ID:142574

The T-REX valley wind intercomparison project
Conference · Thu Aug 07 00:00:00 EDT 2008 · OSTI ID:945606