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Comparison of particle number size distribution trends in ground measurements and climate models
Despite a large number of studies, out of all drivers of radiative forcing, the effect of aerosol...
V Leinonen, H Kokkola, T Yli-Juuti, T Mielonen, T. Kühn, T Nieminen, S Heikkinen, T Miinalainen, T Bergman, K Carslaw, S Decesari, M Fiebig, T Hussein, N Kivekäs, R Krejci, M Kulmala, A Leskinen, A Massling, N Mihalopoulos, JP Mulcahy, SM Noe, T van Noije, FM O'Connor, C O'Dowd, D Olivie, JB Pernov, T Petäjä, Ø Seland, M Schulz, CE Scott, H Skov, E Swietlicki, T Tuch, A Wiedensohler, A Virtanen, S Mikkonen | Journal: Geosci. Mod. Dev. | Volume: 22 | Year: 2022 | First page: 12873 | Last page: 12905 | doi: 10.5194/acp-22-12873-2022
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Integration of Surface Reflectance and Aerosol Retrieval Algorithms for Multi‐Resolution Aerosol Optical Depth Retrievals over Urban Areas.
The SEMARA approach, an integration of the Simplified and Robust Surface Reflectance
Estimation ...
Bilal, M.; Mhawish, A.; Ali, A.; Nichol, J.E.; de Leeuw, G.; Mazhar, U.; Qiu, Z.; Bleiweiss, M.P.; Nazeer, M. | Journal: Remote Sensing | Volume: 14 | Year: 2022 | First page: 373 | doi: https://doi.org/10.3390/rs14020373
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Winschoten events, 19-11-2017
A succession of at least 4 events was measured on November 19, 2017, close to the city of Winscho...
E. Ruigrok, J. Spetzler, B. Dost and L. Evers | Year: 2018 | Pages: 27
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Aerosol Optical Depth and Cloud Parameters from Ascension Island retrieved with a UV-depolarisation Lidar : An outlook on the validation
Aerosol-Cloud Interactions (ACIs) are one of the least understood climate feedbacks. Ground-based...
M. Schenkels | Year: 2018 | Pages: 81
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Introduction to the Special Section on Seismoacoustics and Seismoacoustic Data Fusion
A variety of geophysical hazards (e.g., volcanic activity, earthquakes, mass movements, marine st...
FK Dannemann Dugick, JW Bishop, L Martire, AM Iezzi, JD Assink, Q Brissaud, S Arrowsmith | Journal: Bulletin of the Seismological Society of America | Year: 2023 | doi: https://doi.org/10.1785/0120230049
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