608
A dust concentration equation was built into the existing ETA/NMC regional forecast model
for the dynamics of the atmosphere. The model can give integrated dust concentration in the
atmosphere along with wet/dry depositional areas.
Arslan AN Cukurova University, Adana, Turkey
Diffraction problems in microwave remote sensing
Burford J York University, North York, Canada
Sublimation in Arctic environments
Chen C-T, Roeckner E, Soden BJ MPI fiir Meteorologie, Hamburg, Germany
A comparison of satellite observations and model simulations of column integrated moisture
and upper tropospheric humidity
Ivanova K, Jordanov 01, Michalev MA Institute of Electronics, BAS, Sofia, Bulgaria
Characterization and identification of fractal-like interfaces in the climate formations and the
environment
Karlsson KG SMHI, Norrkoping, Sweden
Comparison of modelled and satellite-observed cloudiness over northern Europe
Kubilay N, Nickovic S, Dobricic S Institute of Marine Sciences, Erdemli, Turkey
Climate processes related to Sahara dust in the Mediterranean
Li X, Morrison JM, Pietrafesa LJ North Carolina State University, Raleigh, USA
Dynamic analysis of oceanic internal waves from airborne synthetic aperture radar images
Mehrtens H Institut fiir Meereskunde, Kiel, Germany
Adjoint calculations of weighting functions
Oelke Ch Alfred-Wegener Inst. for Polar and Marine Research, Bremerhaven, Germany
Atmospheric signatures in passive microwave sea-ice algorithms
Pereira EB, Abreu SL, Stuhlmann R, Rieland M, Colle S University of Santa Catarina,
Santa Catarina, Brazil
Incident solar radiation in Brazil using the IGMK model (validation and first results)
Pierazzo E University of Arizona, Tucson, USA
Cretaceous climate simulation using NCAR general circulation model CCM2-BATS
Schroder C, Hense A Meteorologisches Institut der Universitat Bonn, Bonn, Germany
Statistical validation of simple energy balance model with satellite data
A dust concentration equation was built into the existing ETA/NMC regional forecast model
for the dynamics of the atmosphere. The model can give integrated dust concentration in the
atmosphere along with wet/dry depositional areas.
Arslan AN Cukurova University, Adana, Turkey
Diffraction problems in microwave remote sensing
Burford J York University, North York, Canada
Sublimation in Arctic environments
Chen C-T, Roeckner E, Soden BJ MPI fiir Meteorologie, Hamburg, Germany
A comparison of satellite observations and model simulations of column integrated moisture
and upper tropospheric humidity
Ivanova K, Jordanov 01, Michalev MA Institute of Electronics, BAS, Sofia, Bulgaria
Characterization and identification of fractal-like interfaces in the climate formations and the
environment
Karlsson KG SMHI, Norrkoping, Sweden
Comparison of modelled and satellite-observed cloudiness over northern Europe
Kubilay N, Nickovic S, Dobricic S Institute of Marine Sciences, Erdemli, Turkey
Climate processes related to Sahara dust in the Mediterranean
Li X, Morrison JM, Pietrafesa LJ North Carolina State University, Raleigh, USA
Dynamic analysis of oceanic internal waves from airborne synthetic aperture radar images
Mehrtens H Institut fiir Meereskunde, Kiel, Germany
Adjoint calculations of weighting functions
Oelke Ch Alfred-Wegener Inst. for Polar and Marine Research, Bremerhaven, Germany
Atmospheric signatures in passive microwave sea-ice algorithms
Pereira EB, Abreu SL, Stuhlmann R, Rieland M, Colle S University of Santa Catarina,
Santa Catarina, Brazil
Incident solar radiation in Brazil using the IGMK model (validation and first results)
Pierazzo E University of Arizona, Tucson, USA
Cretaceous climate simulation using NCAR general circulation model CCM2-BATS
Schroder C, Hense A Meteorologisches Institut der Universitat Bonn, Bonn, Germany
Statistical validation of simple energy balance model with satellite data
