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The importance of surface reflectance anisotropy for cloud and NO2 retrievals from GOME-2 and OMI
The angular distribution of the light reflected by the Earth's surface influences top-of-atmosphe...
A Lorente, KF Boersma, P Stammes, LG Tilstra, A Richter, H Yu, S Kharbouche, JP Muller | Status: published | Journal: Atmospheric Measurement Techniques | Volume: 11 | Year: 2018 | First page: 4509 | Last page: 4529 | doi: 10.5194/amt-11-4509-2018
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Sensitivity of winter North Atlantic-European climate to resolved atmosphere and ocean dynamics
Northern Hemisphere western boundary currents, like the Gulf Stream, are key regions for cyclogen...
R Haarsma, J Garcia-Serrano, C Prodhomme, O Bellprat, P Davini, S Drijfhout | Status: published | Journal: Scientific Reports | Year: 2019 | doi: 10.1038/s41598-019-49865-9
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S5P TROPOMI NO2 slant column retrieval: method, stability, uncertainties and comparisons with OMI
The Tropospheric Monitoring Instrument (TROPOMI), aboard the Sentinel-5 Precursor (S5P) satellite...
JHG van Geffen, KF Boersma, HJ Eskes, MC Sneep, M ter Linden, JP Veefkind | Status: published | Journal: Atmospheric Measurement Techniques | Volume: 13 | Year: 2020 | First page: 1315 | Last page: 1335 | doi: 10.5194/amt-13-1315-2020
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Satellite evidence for changes in the NO2 weekly cycle over large cities
Anthropogenic activities, by far the largest source of NOx into the atmosphere, induce a weekly c...
Stavrakou, T., Müller, J., Bauwens, M., Boersma, K.F. and van Geffen, J. | Journal: Sci. Rep. | Volume: 10 | Year: 2020 | First page: 10066 | doi: 10.1038/s41598-020-66891-0
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Impacts of horizontal resolution on global data assimilation of satellite measurements for tropospheric chemistry analysis
We present the results from a global 0.56°-resolution chemical data assimilation that integrates ...
Sekiya, T., Miyazaki, K., Ogochi, K., Sudo, K., Takigawa, M., Eskes, H., & Boersma, K. F. | Journal: Journal of Advances in Modeling Earth Systems | Volume: 13 | Year: 2021 | First page: e2020MS002180 | doi: 10.1029/2020MS002180
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