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An AeroCom–AeroSat study: intercomparison of satellite AOD datasets for aerosol model evaluation
To better understand and characterize current uncertainties
in the important observational constr...
N Schutgens, AM Sayer, A Heckel, C Hsu, H Jethva, G de Leeuw, Et al. | Status: published | Journal: Atm. Chem. Phys. | Volume: 20 | Year: 2020 | First page: 12431 | Last page: 12457 | doi: https://doi.org/10.5194/acp-20-12431-2020
Publication
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Recurrence intervals for the closure of the Dutch Maeslant surge barrier
The Dutch Maeslant Barrier, a movable surge barrier in the mouth of the river Rhine, closes when ...
HW van den Brink, S de Goederen | Status: published | Journal: Ocean Science | Volume: 13 | Year: 2017 | First page: 691 | Last page: 701 | doi: 10.5194/os-13-691-2017
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The role of aerosol layer height in quantifying aerosol absorption from ultraviolet satellite observations
The purpose of this study is to demonstrate the role of aerosol layer height (ALH) in quantifying...
J Sun, JP Veefkind, S Nanda, PFJ van Velthoven, PF Levelt | Status: published | Journal: Atmospheric Measurement Techniques | Volume: 12 | Year: 2019 | First page: 6319 | Last page: 6340 | doi: 10.5194/amt-12-6319-2019
Publication
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Inconsistencies in scatterometer wind products based on ASCAT and OSCAT-2 collocations
Sea surface vector winds from multiple satellite scatterometers are especially useful for oceanic...
Z Wang, ACM Stoffelen, B Zhang, Y He, W Lin, X Li | Status: published | Journal: Remote Sens. Environ. | Volume: 225 | Year: 2019 | First page: 207 | Last page: 216 | doi: 10.1016/j.rse.2019.03.005
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Analysis of properties of the 19 February 2018 volcanic eruption of Mount Sinabung in S5P/TROPOMI and HIMAWARI satellite data,
This study presents an analysis of TROPOMI cloud heights as a proxy for volcanic plume heights in...
ATJ de, M Vazquez-Navarro, N Theys, P Stammes | Status: published | Journal: Natural Hazards and Earth System Sciences | Volume: 20 | Year: 2020 | First page: 1203 | Last page: 1217 | doi: 10.5194/nhess-20-1203-2020
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