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Baseline Surface Radiation Network (BSRN): structure and data description (1992-2017)
Small changes in the radiation budget at the earth's surface can lead to large climatological res...
A Driemel and 38 others, WH Knap | Status: published | Journal: Earth System Science Data | Volume: 10 | Year: 2018 | First page: 1491 | Last page: 1501 | doi: https://doi.org/10.5194/essd-10-1491-2018
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Identifying the Origin of Anomalous High Tropospheric Ozone in the Ozonesonde Data at Uccle by Comparison with Nearby De Bilt
The ozonesonde stations at Uccle (Belgium) and De Bilt (Netherlands), separated by only 175 km, o...
R van Malderen, H de Backer, A Delcloo, M Allaart | Journal: Atmosphere-Ocean | Volume: 0 | Year: 2014 | First page: 1 | Last page: 15 | doi: 10.1080/07055900.2014.886552
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A mixed-layer model study of the stratocumulus response to changes in large-scale conditions
A mixed-layer model is used to study the response of stratocumulus equilibrium state solutions
to...
SRR de Roode, AP Siebesma, S Dal Gesso, HJJ Jonker, J Schalkwijk, J Sival | Status: published | Journal: J. of Advances in Modeling Earth Systems | Volume: 6 | Year: 2014 | First page: 1256 | Last page: 1270 | doi: http://dx.doi.org/10.1002/2014MS000347
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A first comparison of TROPOMI aerosol layer height (ALH) to CALIOP data
The TROPOspheric Monitoring Instrument (TROPOMI) level-2 aerosol layer height (ALH) product has n...
S Nanda, M de Graaf, JP Veefkind, MC Sneep, M ter Linden, J Sun, PF Levelt | Status: published | Journal: Atmospheric Measurement Techniques | Volume: 13 | Year: 2019 | First page: 3043 | Last page: 3059 | doi: 10.5194/amt-13-3043-2020
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The TROPOMI surface UV algorithm
The TROPOspheric Monitoring Instrument (TROPOMI) is the only payload of the Sentinel-5 Precursor ...
AV Lindfors, J Kujanpää, N Kalakoski, A Heikkilä, K Lakkala, T Mielonen, M Sneep, NA Krotkov, A Arola, J Tamminen1 | Status: published | Journal: Atmospheric Measurement Techniques | Volume: 11 | Year: 2018 | First page: 997 | Last page: 1008 | doi: 10.5194/amt-11-997-2018
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