Abstract
The parameterization of the stably stratified atmospheric boundary layer is a difficult issue, having a significant impact on medium-range weather forecasts and climate integrations. To pursue this further, a moderately stratified Arctic case is simulated by nineteen single-column turbulence schemes. Statistics from a large-eddy simulation intercomparison made for the same case by eleven different models are used as a guiding reference. The single-column parameterizations include research and operational schemes from major forecast and climate research centres. Results from first-order schemes, a large number of turbulence kinetic energy closures, and other models were used. There is a large spread in the results; in general, the operational schemes mix over a deeper layer than the research schemes, and the turbulence kinetic energy and other higher-order closures give results closer to the statistics obtained from the large-eddy simulations. The sensitivities of the schemes to the parameters of their turbulence closures are partially explored
Original language | English |
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Pages (from-to) | 273-303 |
Number of pages | 31 |
Journal | Boundary-Layer Meteorology |
Volume | 118 |
Issue number | 2 |
DOIs | |
Publication status | Published - 2006 |
Keywords
- turbulence closure-model
- large-eddy simulation
- part i
- scheme
- parameterization
- formulation
- diffusion
- dynamics
- surfaces
- system