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Can we explain the observed methane variability after the Mount Pinatubo eruption?
The CH4 growth rate in the atmosphere showed large variations after the Pinatubo eruption in June...
N Bândă, M Krol, M van Weele, T van Noije, P Le Sager, T Röckmann | Status: published | Journal: Atmos. Chem. Phys. | Volume: 16 | Year: 2016 | First page: 195 | Last page: 214 | doi: 10.5194/acp-16-195-2016
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From ship smokestack to global air pollution: bridging the scales to better constrain ship NOx emissions from space
Seagoing ships combust massive amounts of
marine heavy fuel, which leads to significant
emissions...
GCM Vinken, KF Boersma | Journal: SOLAS Newsletter | Year: 2011 | First page: 8 | Last page: 0
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Supermodels: Dynamically Coupled Ensembles of Imperfect Models
At a dozen or so institutes around the world, comprehensive climate models are being developed an...
W Wiegerinck, FM Selten | Conference: Conference on Artificial Intelligence (AAAI-12) | Organisation: AAAI | Year: 2012 | First page: 0 | Last page: 0
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Clouds, Circulation and Climate Sensitivity
Fundamental puzzles of climate science remain unsolved because of our limited understanding of ho...
S Bony, B Stevens, DMW Frierson, C Jakob, M Kageyama, R Pincus, TG Shepherd, SC Sherwood, AP Siebesma, AH Sobel, M Watanabe, MJ Webb | Status: published | Journal: Nature Geoscience | Volume: 8 | Year: 2015 | First page: 261 | Last page: 268 | doi: doi:10.1038/ngeo2398
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ADM-Aeolus, VAMP, Vertical Aeolus Measurement Positioning, TN3, v0.3
This document describes the work done and the results obtained for Work Package (WP) 4 of the Ver...
J de Kloe, GJ Marseille, A Stoffelen | Year: 2009
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