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ADM-Aeolus vertical sampling scenarios
The Atmospheric Dynamics Mission ADM-Aeolus is
scheduled for launch in April 2011. ADM-Aeolus is ...
GJ Marseille, A Stoffelen, J de Kloe, K Houchi, H Kornich, H Schyberg, AG Straume, O LeRille | Conference: International Symposium on Tropospheric Profiling (ISTP) | Organisation: KNMI - TU Delft - RIVM | Place: Delft | Year: 2009 | First page: 0 | Last page: 0
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2Observation Representativeness Error
NWP models simulate the atmospheric state on a given model grid, thereby principally
limiting the...
GJ Marseille, A Stoffelen | Year: 2012
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The Contribution of Dutch GLOBE Schools to Validation of Aerosol Measurements from Space
In the past century, the mean surface temperature of the Earth has increased by 0.6˚ according to...
Joris de Vroom
| Year: 2003 | Pages: 47
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Atmospheric visibility inferred from continuous-wave Doppler wind lidar
Atmospheric visibility, or meteorological optical range (MOR), is governed by light extinction by...
Manuel Queißer, Michael Harris, and Steven Knoop | Journal: Atmos. Meas. Tech. | Volume: 15 | Year: 2022 | First page: 5527 | Last page: 5544 | doi: https://doi.org/10.5194/amt-15-5527-2022
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Horizontal and vertical background error correlations
Numerical Weather Prediction (NWP) model background error correlations play a decisive
role in da...
GJ Marseille, H Schyberg, A Stoffelen | Year: 2012
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