The CARL project is a joint effort involving research teams from Germany, France, Greece and the Netherlands. It is a three years project, started in December 1997, in the European Commision's RTD programme " Enviroment and Climate". New methodologies will be tested in order to derive microphysical parameters of warm and cold clouds during several campaigns involving groud-based and airborne radar and lidar systems. The most interesting cases of the experimental campaigns will be simulated with an advanced limited area model. A significant effort has been devoted in the intercomparison between the collected data from the observational systems and the model outputs. The model used for the simulations is the Regional Atmospheric Modeling System, RAMS.
GKSS Research Center Geesthacht, Institute of Atmospheric Physics, Max Planck Strasse D-21502 Geestacht, Germany
M.Quante (Quante@gkss.de), tel: 494152871501, fax:494152872020
O.Danne (Danne@gkss.de), tel: 494152871520, fax:494152872020
F.Albers (Albers@gkss.de), D.Milferstadt, fax:494152872020
Institut Pierre Simon Laplace, 10-12 avenue de l'Europe, 78140 Velizy, France
J.Testud ( Testud@cetp.ipsl.fr), tel:33139254476, fax: 33139254922
F.Baudin (Baudin@cept.ipsl.fr), tel:33139254850, fax: 33139254872
P.H.Flamant (Flamant@lmd.polytechnique.fr), Ecole Polytechnique, 91128, Palaiseau, France, tel: 33169334550, fax:33169333005
J.Pelon(Jacques.Pelon@aero.jussieu.fr), Universite Pierre et Marie Curie,T14,E5,B102,4,Place Jussieu,75252, Paris cedex 05, France; tel: 33144273779, fax: 33144273776
National and Kapodistrian University of Athens (NKUA), Department of Physics, Division of Applied Physics, Atmospheric Modeling and Weather Forecasting Group, Panepistimioupolis, Bldg PHYS-V, 15784, Athens, Greece.
G. Kallos (email@example.com), tel: 30 1 7276923, fax: 30 1 72 95 281
E. Mavromatidis (firstname.lastname@example.org), tel: 30 1 7276832, fax: 30 1 72 95 281
KNMI, Koninklijk Nederlands Meteorologisch Institut, Postbus 201, 3730 AE De Bilt, Wilhelminalaan 10.
Hannelore Bloemink (email@example.com)
The main objectives of the project are:
During the project, a cloud Radar (with polarization diversity to discriminate water and ice phases and Doppler capabilities) and two backscattering Lidar ( with polarization diversity) will be operated from the same site and airborne platform. The target of the measurements is high, middle and low level clouds. The main objective is to retrieve the effective radius and the water content of such clouds. To do so, it is aimed at deriving the second and third moment of the cloud droplet distribution from lidar and radar signal analysis, and to correct for diffraction and multiple scattering. Model calculations will be performed to analyze the impact of the retrieval and related errors, and check the quality of retrieved cloud parameters and their representativeness, with reference to radiation budget parameters measured at the same time. The atmospheric model will be used to perform multi-scale simulations with a state of the art cloud microphysical parameterization module activated. Two-way interactive nesting capabilities of the model will be used in order to cover a regional scale area and simultaneously to obtain very high resolution over the experimental location.
Two experimental campaigns have been organized so far and a third is under way. The main task of the Atmospheric Modeling and Weather Forecasting Group of the University of Athens (NKUA/AM&WFG) is to perform the appropriate model development and simulations with RAMS and inter-compare the results with the observations from the experimental radar and lidar platforms.
1st experimental campaign
Date: 6 December 1995
Period of observations: 8 minutes, from 16:06 UTC to 16:14 UTC.
Instruments: The GKSS 95 GHz cloud Radar.
2nd experimental campaign
Location: Palaiseau ( near Paris)
Period of observations: 26 April to 15 May 1999
For ground-based measurements: 5.5 GHz Radar (IPSL), 95 GHz Radar (GKSS), Lidar 0.53 and 10.6 mm (IPSL), Lidar ceilometer 0.9 mm (KNMI), visible and infrared radiometers ( KNMI, IPSL)
For airborne measurements: FSSP, 2DC, 2DP sondes(GKSS), Visible and infrared broadband radiometer, narrow band narrow beam infrared radiometer( Meteo-France)
Flights : Five flights were performed during the campaign with the Merlin aircraft ( Meteo-France, subcontractor of IPSL) to get the observed cloud microphysics, for comparison and validation.
Additional model simulations for the 2nd experimental period
In order to investigate the model sensitivity to various settings, a number of additional simulations were performed. The new version of RAMS (4.2.9) was used. A number of figures have been prepared, especially in the form of time-versus-height form for better inter-comparison with the experimental observations (Radar, Lidar, ceilometer) and conventional measurements (soundings)
A quick description of RAMS
RAMS is a highly versatile numerical code developed by scientists at Colorado State University and Aster Division of Mission Research Inc. (http://www.aster.com) for simulating and forecasting meteorological phenomena (Walko and Tremback, 1996; Pielke et al., 1992). It is considered as one of the most advanced modeling systems available today. It is a merger of a non-hydrostatic cloud model (Tripoli and Cotton, 1982) and a hydrostatic mesoscale model (Mahrer and Pielke, 1977). It has been developed in order to simulate atmospheric phenomena with resolution ranging from tens of kilometers to a few meters. There is no lower limit to the domain size or to the mesh cell size of the model finite difference grid. A general description of the model and its capabilities is given in Pielke et al (1992). However some RAMS features are summarized in the following: