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First 4224 results for ” and Schmeits”

1. Spectra en gradienten van hoge windsnelheden te Cabauw tot 200 meter

   Spectra en gradienten van hoge windsnelheden te Cabauw tot 200 meter 

   R.W.M. Meijer | Year: 1989 | Pages: 172

   Publication

2. Pole-to-pole validation of Envisat GOMOS ozone profiles using data from ground-based and balloon sonde measurements
   YJ Meijer, DPJ Swart, MAF Allaart, SB Andersen, G Bodeker, I Boyd, G Braathen, Y Calisesi, H Claude, V Dorokhov, P von der Gathen, M Gil, S Godin-Beekman, F Goutail, .............................. | Status: published | Journal: J. Geophys. Res. | Volume: 109 | Year: 2004 | doi: 10.1029/2004JD004834

   Publication

3. What is the surface mass balance of Antarctica? An intercomparison of regional climate model estimates

   We compare the performance of five different regional climate models (RCMs) (COSMO-CLM2, HIRHAM5,...

   Mottram, R., Hansen, N., Kittel, C., van Wessem, J. M., Agosta, C., Amory, C., Boberg, F., van de Berg, W. J., Fettweis, X., Gossart, A., van Lipzig, N. P. M., van Meijgaard, E., Orr, A., Phillips, T., Webster, S., Simonsen, S. B., and Souverijns, N | Journal: The Cryosphere | Volume: 15 | Year: 2021 | First page: 3751 | Last page: 3784 | doi: 10.5194/tc-15-3751-2021

   Publication

4. Spatial and Temporal Propagation of Scatterometer Winds

   Ocean models are generally forced by synthetic (global) NWP model wind fields. It has however bee...

   D Harutyunyan, ACM Stoffelen | Year: 2012

   Publication

5. Spatial and Temporal Propagation of Scatterometer Winds

   Ocean models are generally forced by synthetic (global) NWP model wind fields. It has however bee...

   D Harutyunyan, A Stoffelen | Year: 2011

   Publication