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The impact of reflectivity correction and accounting for raindrop size distribution variability to improve precipitation estimation by weather radar for an extreme low-land mesoscale convective system
Between 25 and 27 August 2010 a long-duration mesoscale convective system was observed above the ...
P Hazenberg, H Leijnse, R Uijlenhoet | Status: published | Journal: J. Hydrol. | Volume: 519 | Year: 2014 | First page: 3410 | Last page: 3425 | doi: 10.1016/j.jhydrol.2014.09.057
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Representativeness errors in comparing chemistry transport and chemistry climate models with satellite UV–Vis tropospheric column retrievals
Ultraviolet–visible (UV–Vis) satellite retrievals of trace gas columns of nitrogen dioxide (NO2),...
KF Boersma, GCM Vinken, HJ Eskes | Status: published | Journal: Geoscientific Model Development | Year: 2016 | First page: 875 | Last page: 898 | doi: 10.5194/gmd-9-875-2016
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A global hybrid coupled model based on Atmosphere-SST feedbacks
A global hybrid coupled model is developed, with the aim of studying the effects of ocean--atmosp...
AA Cimatoribus, SS Drijfhout, HA Dijkstra | Status: published | Journal: Clim. Dyn. | Volume: 38 | Year: 2012 | First page: 745 | Last page: 760 | doi: 10.1007/s00382-011-1094-1
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Transport of biomass burning smoke to the upper troposphere by deep convection in the equatorial region
During LBA-CLAIRE-98, we found atmospheric layers with aged biomass smoke at altitudes >10 km ...
MO Andreae, P. Artaxo, H. Fischer, SR Freitas, J.-M. Gregoire, A Hansel, P. Hoor, R Kormann, R. Krjeci, L Lange, J. Lelieveld | Status: published | Journal: Geophys. Res. Lett. | Volume: 28 | Year: 2006 | First page: 951 | Last page: 954
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Rarity of upper-tropospheric low O3 mixing ration events during MOZAIC flights
Only a few previous observations of very low O3 mixing ratios in the upper troposphere are availa...
WAH Asman, MG Lawrence, CAM Brenninkmeijer, PJ Crutzen, JWM Cuijpers, P Nedelec | Status: published | Journal: Atm. Chem. Phys. | Volume: 3 | Year: 2003 | First page: 1541 | Last page: 1549
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