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Water mass transformation and subduction in the South Atlantic
The transformation of water masses induced by air-sea
fluxes in the South Atlantic is calculated...
J Donners, S Drijfhout, W Hazeleger | Status: published | Journal: J. Phys. Oceanogr. | Volume: 35 | Year: 2005 | First page: 1841 | Last page: 1860 | doi: 10.1175/JPO2782.1
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The GeoStationary Scanning Imaging absorption Spectrometer (GeoSCIA) as part of the Geo Stationary Tropospheric Pollution Explorer (GeoTROPE) Mission: Objectives and Requirements
One of the major challenges facing atmospheric sciences is to assess, understand and quantify the...
H Bovensmann, KU Eichmann, S Noel, JM Flaud, J Orphal, ..........................., APH Goede | Status: published | Journal: Adv.Space Res. | Volume: 34 | Year: 2004 | First page: 694 | Last page: 699 | doi: doi:10.1016/j.asr.2003.08.068
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High Resolution Model Intercomparison Project (HighResMIP v1.0) for CMIP6
Robust projections and predictions of climate vari-
ability and change, particularly at regional ...
RJ Haarsma, et al. | Status: published | Journal: Geoscientific Model Development | Year: 2016 | doi: 10.5194/gmd-9-4185-2016
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A 3D cloud-construction algorithm for the EarthCARE satellite mission
This article presents and assesses an algorithm that constructs 3D distributions of cloud from pa...
HW Barker, MP Jerg, T Wehr, S Kato, DP Donovan, RJ Hogan | Status: published | Journal: Quart. J. Royal Meteor. Soc. | Volume: 137 | Year: 2011 | First page: 1042 | Last page: 1058 | doi: DOI: 10.1002/qj.824
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The 2018 fire season in North America as seen by TROPOMI: aerosol layer height validation and evaluation of model-derived plume heights
Before the launch of the TROPOspheric Moni- toring Instrument (TROPOMI), only two other satellite...
G Griffin, C Sioris, J Chen, N Dickson, A Kovachik, M de Graaf, S Nanda, JP Veefkind, E Dammers, CA McLinden, P Makar | Status: published | Journal: Atmospheric Measurement Techniques | Volume: 13 | Year: 2020 | First page: 1427 | Last page: 1445 | doi: 10.5194/amt-13-1427-2020
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