Demistify: a large-eddy simulation (LES) and single-column model (SCM) intercomparison of radiation fog

被引:27
|
作者
Boutle, Ian [1 ]
Angevine, Wayne [2 ,3 ]
Bao, Jian-Wen [4 ]
Bergot, Thierry [5 ]
Bhattacharya, Ritthik [6 ]
Bott, Andreas [7 ]
Duconge, Leo [5 ]
Forbes, Richard [8 ]
Goecke, Tobias [9 ]
Grell, Evelyn [2 ,4 ]
Hill, Adrian [1 ]
Igel, Adele L. [10 ]
Kudzotsa, Innocent [11 ]
Lac, Christine [5 ]
Maronga, Bjorn [12 ]
Romakkaniemi, Sami [11 ]
Schmidli, Juerg [6 ]
Schwenkel, Johannes [12 ]
Steeneveld, Gert-Jan [13 ]
Vie, Benoit [5 ]
机构
[1] Met Off, Exeter, Devon, England
[2] Univ Colorado, CIRES, Boulder, CO USA
[3] NOAA, Chem Sci Lab, Boulder, CO USA
[4] NOAA, Phys Sci Lab, Boulder, CO USA
[5] Univ Toulouse, CNRS, Meteo France, CNRM, Toulouse, France
[6] Goethe Univ Frankfurt, Inst Atmospher & Environm Sci, Frankfurt, Germany
[7] Univ Bonn, Inst Geosci, Bonn, Germany
[8] European Ctr Medium Range Weather Forecasts, Reading, Berks, England
[9] Deutsch Wetterdienst, Offenbach, Germany
[10] Univ Calif Davis, Dept Land Air & Water Resources, Davis, CA USA
[11] Finnish Meteorol Inst, Kuopio, Finland
[12] Leibniz Univ Hannover, Inst Meteorol & Climatol, Hannover, Germany
[13] Wageningen Univ, Meteorol & Air Qual Sect, Wageningen, Netherlands
基金
欧盟地平线“2020”;
关键词
NUMERICAL WEATHER PREDICTION; PARAMETERIZATION; AEROSOL; CLOUDS; VISIBILITY; SYSTEM; IMPACT;
D O I
10.5194/acp-22-319-2022
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
An intercomparison between 10 single-column (SCM) and 5 large-eddy simulation (LES) models is presented for a radiation fog case study inspired by the Local and Non-local Fog Experiment (LANFEX) field campaign. Seven of the SCMs represent single-column equivalents of operational numerical weather prediction (NWP) models, whilst three are research-grade SCMs designed for fog simulation, and the LESs are designed to reproduce in the best manner currently possible the underlying physical processes governing fog formation. The LES model results are of variable quality and do not provide a consistent baseline against which to compare the NWP models, particularly under high aerosol or cloud droplet number concentration (CDNC) conditions. The main SCM bias appears to be toward the overdevelopment of fog, i.e. fog which is too thick, although the inter-model variability is large. In reality there is a subtle balance between water lost to the surface and water condensed into fog, and the ability of a model to accurately simulate this process strongly determines the quality of its forecast. Some NWP SCMs do not represent fundamental components of this process (e.g. cloud droplet sedimentation) and therefore are naturally hampered in their ability to deliver accurate simulations. Finally, we show that modelled fog development is as sensitive to the shape of the cloud droplet size distribution, a rarely studied or modified part of the microphysical parameterisation, as it is to the underlying aerosol or CDNC.
引用
收藏
页码:319 / 333
页数:15
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