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CMOD5
A new geophysical model function, CMOD5, for the retrieval of surface winds from ERS scatteromete...
S de Haan, A Stoffelen | Year: 2001
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NWP Ocean Calibration for the CFOSAT Wind Scatterometer
The unique rotating fan-beam feature of SCAT onboard CFOSA T leads to varying geometries across t...
Zhen Li, Ad Stoffelen, Anton Verhoef, Jeroen Verspeek
| Journal: 2021 IEEE International Geoscience and Remote Sensing Symposium IGARSS | Year: 2021 | doi: https://doi.org/10.1109/IGARSS47720.2021.9554965
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Strong universality in forced and decaying turbulence in a shell model
The weak version of universality in turbulence refers to the independence of the scaling exponent...
VS L\'vov, RA Pasmanter, A Pomyalov, I Procaccia | Status: published | Journal: Phys. Rev. E. | Volume: 67 | Year: 2003 | First page: 066310-1 | Last page: 066310-9
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How big is an OMI pixel?
The Ozone Monitoring Instrument (OMI) is a
push-broom imaging spectrometer, observing solar...
M de Graaf, H Sihler, LG Tilstra, P Stammes | Status: published | Journal: Atmospheric Measurement Techniques | Volume: 9 | Year: 2016 | First page: 3607 | Last page: 3618 | doi: 10.5194/amt-9-3607-2016
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Parametric representation of the cloud droplet spectra for LES warm bulk microphysical schemes
Parametric functions are currently used to represent droplet spectra in clouds and to develop bul...
O Geoffroy, JL Brenguier, F Burnet | Status: published | Journal: Atm. Chem. Phys. | Volume: 10 | Year: 2010 | First page: 4835 | Last page: 4848 | doi: doi:10.5194/acp-10-4835-2010
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