Abstract
The presence of fog and low clouds in the lower atmosphere can have a critical impact on both airborne and ground
transports and is often connected with serious accidents. An improvement of localisation, duration and variations
in visibility therefore holds an immense operational value for the field of transportation in conditions of low visibility.
However, fog is generally a small scale phenomenon which is mostly affected by local advective transport,
radiation, turbulent mixing at the surface as well as its microphysical structure. Therefore, a detailed description
of the microphysical processes within the three-dimensional dynamical core of the forecast model is necessary.
For this purpose, three-dimensional fog forecast models with a high vertical resolution with different microphysical
complexity have been developed. COSMO-FOG and NMMFOG include a new microphysical
parameterisation based on the one-dimensional fog forecast model. The implementation of the cloud water
droplets as a new prognostic variable allows a detailed definition of the sedimentation processes and the variations
in visibility. Also, we compare WRF mesoscale model results using different boundary-layer schemes that ignore
or account for specific fog microphysics.
In some realistic fog situations (radiative fog) the potential of these three-dimensional fog models will be
presented. The fog spatial extension will be compared with MSG satellite products for fog and low cloud. It will
be shown that the initialisation and the interaction between the earth’s surface and the atmosphere is one of the
most important issues for reliable fog forecasts.
Original language | English |
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Publication status | Published - 2010 |
Event | 5th International Conference on Fog, Fog Collection and Dew, 25-30 July 2010, Münster, Germany - Duration: 25 Jul 2010 → 30 Jul 2010 |
Conference/symposium
Conference/symposium | 5th International Conference on Fog, Fog Collection and Dew, 25-30 July 2010, Münster, Germany |
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Period | 25/07/10 → 30/07/10 |