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Spatiotemporal variation and provincial scale differences of the AOD across China during 2000–2021.
The spatiotemporal variation of the aerosol optical depth (AOD) over China was studied using MODI...
de Leeuw, G., Fan, C, Li, Z., Dong, J., Li, Y., Ou, Y., and Zhu, S. | Journal: Atmospheric Pollution Research | Volume: 13 | Year: 2022 | First page: 101359 | doi: https://doi.org/10.1016/j.apr.2022.101359
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Improved SIFTER v2 algorithm for long-term GOME-2A satellite retrievals of fluorescence with a correction for instrument degradation
Solar-induced fluorescence (SIF) data from satellites are increasingly used as a proxy for photos...
E. van Schaik, M.L. Kooreman, P. Stammes, L.G. Tilstra, O.N.E. Tuinder, A.F.J. Sanders, W.W. Verstraeten, R. Lang, A. Cacciari, J. Joiner, W. Peters, K.F. Boersma | Journal: Atmospheric Measurement Techniques | Volume: 13 | Year: 2020 | doi: https://doi.org/10.5194/amt-13-4295-2020
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Rainfall generator for the Meuse basin: Extension of the base period with the years 1999-2008
In KNMI publication 196-III a multi-site weather generator for the French and Belgian parts of th...
TA Buishand, R Leander | Year: 2011 | Pages: 36
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How well do the regional atmospheric and oceanic models describe the Antarctic sea ice albedo?
We assessed how well regional climate models (HCLIM, MAR, RACMO), ocean models (MetROMSUHel, NEMO...
Kristiina Verro, Cecilia Äijälä, Roberta Pirazzini, Ruzica Dadic, Damien Maure, Willem Jan van de Berg, Giacomo Traversa, Christiaan T. van Dalum, Petteri Uotila, Xavier Fettweis, Biagio Di Mauro, Milla Johansson | Journal: The Cryosphere | Volume: 19 | Year: 2025 | First page: 4409 | Last page: 4436 | doi: 10.5194/tc-19-4409-2025
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Constraining local ocean dynamic sea-level projections using observations
The redistribution of ocean water volume under ocean–atmosphere dynamical processes results in se...
Dewi Le Bars, Sybren Drijfhout, Iris Keizer | Journal: Ocean Science | Volume: 21 | Year: 2025 | First page: 1303 | Last page: 1314 | doi: https://doi.org/10.5194/os-21-1303-2025
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