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In-flight performance of the Ozone Monitoring Instrument
The Dutch–Finnish Ozone Monitoring Instrument (OMI) is an imaging spectrograph flying on NASA's E...
Schenkeveld, V. M. E.; Jaross, G.; Marchenko, S.; Haffner, D.; Kleipool, Q. L.; Rozemeijer, N. C.; Veefkind, J. P.; Levelt, P. F. | Journal: Atmospheric Measurement Techniques | Year: 2017 | doi: https://doi.org/10.5194/amt-10-1957-2017
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On the temperature dependence of the cloud ice particle effective radius - a satellite perspective
Cloud ice particle effective radius in atmospheric models is usually parametrized. A widelyused
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M. Stengel, J.F. Meirink, S. Eliasson | Journal: Geophysical Research Letters | Volume: 50 | Year: 2023 | doi: 10.1029/2022GL102521
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ERA15 seen from the ocean
The air-sea fluxes of ERA15 have been used to drive wave and ocean models. The results of the wav...
A Sterl, H Bonekamp, GJ Komen | Journal: Change | Volume: 58 | Year: 2001 | First page: 14 | Last page: 16
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On Bayesian scatterometer wind inversion
For ERS scatterometer inversion, several studies reveal that the shape of the measurement space w...
M Portabella, A Stoffelen | Conference: Fourth WMO International Symposium on Assimilation of Observations in Meteorology and Oceanography | Organisation: WMO | Place: Prague, Czech Republic | Year: 2005 | First page: 0 | Last page: 0
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Upper Air Climatology of Amsterdam FIR, using ERA-Interim 1989-2008 Part 2
This report presents upper-air climatology for the lower troposphere (below 850 hPa
or 1.5 km) f...
G Groen, D Wolters | Year: 2011 | Pages: 106
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