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ASCAT NWP Ocean Calibration
The objective of Ocean Calibration (OC) is to find corrections of the normalized radar cross sect...
J Verspeek, A Verhoef, A Stoffelen | Year: 2011
Publication
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Water mass transformation and subduction in the South Atlantic
The transformation of water masses induced by air-sea
fluxes in the South Atlantic is calculated...
J Donners, S Drijfhout, W Hazeleger | Status: published | Journal: J. Phys. Oceanogr. | Volume: 35 | Year: 2005 | First page: 1841 | Last page: 1860 | doi: 10.1175/JPO2782.1
Publication
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Evaluation of a regional atmospheric model using measurements of surface heat exchange processes from a site in Antarctica
A regional atmospheric climate model with a horizontal grid spacing of 55 km has been used to sim...
NPM van Lipzig, E van Meijgaard, J Oerlemans | Status: published | Journal: Mon. Wea. Rev. | Volume: 127 | Year: 1999 | First page: 1994 | Last page: 2011
Publication
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Tropospheric mercury vertical profiles between 500 and 10 000 m in central Europe
The knowledge of the vertical distribution of atmospheric mercury (Hg) plays an important role in...
A Weigelt, R Ebinghaus, N Pirrone, J Bieser, J Bodewadt, G Esposito, F Slemr, PFJ van Velthoven, A Zahn, H Ziereis | Status: published | Journal: Atm. Chem. Phys. | Year: 2016 | First page: 4135 | Last page: 4146 | doi: 10.5194/acp-16-4135-2016
Publication
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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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