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First 3125 results for ”M van den Berg”

1. Surface-Layer Wind Shear and Momentum Transport From Clear-Sky to Cloudy Weather Regimes Over Land

   This study investigates how wind shear and momentum fluxes in the surface- and boundary layer var...

   A. M. Koning, L. Nuijens, F. C. Bosveld, A. P. Siebesma, P. A. van Dorp, H. J. J. Jonker | Journal: Journal of Geophysical Research: Atmospheres | Volume: 126 | Year: 2021 | doi: https://doi.org/10.1029/2021JD035087

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2. Aeolus L2 Activities at KNMI

   KNMI has had a long involvement with the recently launched Aeolus mission. Aeolus is an ESA Earth...

   DP Donovan, Gert-Jan Marseille, Jos de Kloe, Ad Stoffelen | Journal: EPJ Web of Conferences | Volume: 237 | Year: 2020 | doi: https://doi.org/10.1051/epjconf/202023701002

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3. The Cloud_cci simulator v1.0 for the Cloud_cci climate data record and its application to a global and a regional climate model

   The Cloud Climate Change Initiative (Cloud_cci) satellite simulator has been developed to enable ...

   Eliasson, S., Karlsson, K. G., van Meijgaard, E., Meirink, J. F., Stengel, M., andWill´en, U | Journal: Geoscientific Model Development | Year: 2019 | doi: https://doi.org/10.5194/gmd-12-829-2019

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4. Evaluation of SCIAMACHY Level-1 data versions using nadir ozone profile retrievals in the period 2003–2011,

   Ozone profile retrieval from nadir-viewing satellite instruments operating in the ultraviolet–vis...

   S. Shah O.N.E. Tuinder J. van Peet P. Stammes A.T.J. de Laat | Journal: Atmospheric Measurement Techniques | Volume: 11 | Year: 2018 | First page: 2345 | Last page: 2360 | doi: 10.5194/amt-11-2345-2018

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5. On the improvement of ASCAT wind data assimilation in global NWP

   The assimilation of Advanced Scatterometer (ASCAT) winds has proven to be beneficial for the Euro...

   Wenming Lin, Marcos Portabella, Ad Stoffelen, Giovanna De Chiara, Justino Martínez | Journal: 2017 IEEE International Geoscience and Remote Sensing Symposium (IGARSS) | Year: 2017 | doi: https://doi.org/10.1109/IGARSS.2017.8126980

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