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Aerosol single-scattering albedo over the global oceans: Comparing PARASAL retrievals with AERONET, OMI and AeroCom models estimates
The aerosol single-scattering albedo (SSA) over the global ocean is evaluated based on polarimetr...
C Lacagnina, OP Hasekamp, H Bian, G Curci, G Myhre, T van Noije, M Schulz, RB Skeie, T Takemura, K Zhang | Status: published | Journal: J. Geophys. Res. | Volume: 120 | Year: 2015 | First page: 9814 | Last page: 9836 | doi: 10.1002/2015JD023501
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Reflectance comparison between SCIAMACHY and a radiative transfer code in the UV
SCIAMACHY, onboard Envisat, is an Earth-monitoring spectrometer over the wavelength range 240-240...
LG Tilstra, G van Soest, M de Graaf, JR Acarreta, P Stammes | Conference: Second Workshop on the Atmospheric Chemistry Validation of ENVISAT (ACVE-2) | Organisation: ESA-ESRIN | Place: Frascati, Italy | First page: 0 | Last page: 0
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Absorbing Aerosol Index: Sensitivity analysis, application to GOME and comparison with TOMS
The Absorbing Aerosol Index (AAI) was investigated and used to analyze GOME data and compare it t...
M de Graaf, P Stammes, O Torres, RBA Koelemeijer | Status: published | Journal: J. Geophys. Res. | Volume: 110 | Year: 2005 | doi: 10.1029/2004JD005178
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Stochastic Convection Parameterization with Markov Chains in an Intermediate-Complexity GCM
Conditional Markov chain (CMC) models have proven to be promising building blocks for stochastic ...
J Dorrestijn, DT Crommelin, AP Siebesma, HJJ Jonker, F Selten | Status: published | Journal: J. Atmos. Sci. | Volume: 73 | Year: 2016 | First page: 1367 | Last page: 1382 | doi: 10.1175/JAS-D-15-0244.1
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Stochastic Parameterization of Convective Area Fractions with a Multicloud Model Inferred from Observational Data
Observational data of rainfall from a rain radar in Darwin, Australia, are combined with data def...
J Dorrestijn, DT Crommelin, AP Siebesma, HJJ Jonker, C Jakob | Status: published | Journal: J. Atmos. Sci. | Year: 2015 | First page: 854 | Last page: 869 | doi: http://dx.doi.org/10.1175/JAS-D-14-0110.1
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