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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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Connecting the dots: NOx emissions along a West Siberian natural gas pipeline
New high quality satellite measurements of nitrogen dioxide (NO2) of the TROPOspheric Monitoring ...
van der A, R.J., de Laat, A.T.J., Ding, J., Eskes, H.J. | Journal: npj Climate and Atmospheric Science | Volume: 3 | Year: 2020 | doi: 10.1038/s41612-020-0119-z
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Glacier contribution to streamflow in two headwaters of the Huasco River, Dry Andes of Chile
Quantitative assessment of glacier contribution to present-day streamflow is a prerequisite to th...
S Gascoin, C Kinnard, R Ponce, S Lhermitte, S MacDonell, A Rabatel | Status: published | Journal: The Cryosphere | Volume: 5 | Year: 2011 | First page: 1099 | Last page: 1113 | doi: doi:10.5194/tc-5-1099-2011
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100-yr Lower-Mississippi floods in a global climate model: characteristics and future changes
Floods in the Mississippi basin can have large negative societal, natural, and economic impacts. ...
K van der Wiel, SB Kapnick, GA Vecchi, JA Smith, PCD Milly, L Jia | Status: published | Journal: J. Hydrometeor. | Volume: 19 | Year: 2018 | First page: 1547 | Last page: 1563 | doi: 10.1175/JHM-D-18-0018.1
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High sensitivity of Aeolus UV surface returns to surface reflectivity
Global ultraviolet (UV) surface reflectivity climatologies are all composed from daylight passive...
L. D. Labzovskii, G. J. van Zadelhoff, L. G. Tilstra, J. de Kloe, D. P. Donovan & A. Stoffelen | Journal: Nature scientific reports | Volume: 13 | Year: 2023 | First page: 17552 | doi: 10.1038/s41598-023-44525-5
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