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Characteristics and Origin of Lowermost Stratospheric Aerosol at Northern Midlatitudes under Volcanic Quiescent Conditions Based on CARIBIC Observations
Characteristics and origin of the aerosol in the lowermost stratosphere at northern midlatitudes ...
BG Martinsson, NN Hung, CAM Brenninkmeijer, A Zahn, J Heintzenberg, M Hermann, PFJ van Velthoven | Status: published | Journal: J. Geophys. Res. | Volume: 110 | Year: 2005 | doi: 10.1029/2004JD005644
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Tropospheric ozone over a tropical Atlantic station in the Northern Hemisphere: Paramaribo, Surinam (6°N, 55°W)
We present an analysis of 2.5 yr of weekly ozone soundings conducted at a new monitoring station ...
W Peters, P Fortuin, H Kelder, CR Becker, J Lelieveld, PJ Crutzen, AM Thompson | Status: published | Journal: Tellus | Volume: 56 | Year: 2004 | First page: 21 | doi: doi:10.1111/j.1600-0889.2004.00083.x
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Chemical depletion of arctic ozone in winter 1999/2000
During Arctic winters with a cold, stable stratospheric circulation, reactions on the surface of ...
M Rex, RJ Salawitch, NRP Harris, P von der Gathen, GO Braathen, A Schulz, H Deckerlmann, MAF Allaart | Status: published | Journal: J. Geophys. Res. | Volume: 107 | Year: 2002 | First page: 8276 | doi: doi:10.1029/2001JD000533
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Arctic winter: comparison of nudged GCM runs with observations
We have compared satellite and balloon observations of methane (CH4) and hydrogen fluoride (HF) d...
M Aalst, A Bregman, C Brühl, B Steil, G Toon, S Garcelon, G Hansford, R Jones, T Gardiner, G Roelofs, J Lelieveld, P Crutzen | Status: published | Journal: Atm. Chem. Phys. | Volume: 4 | Year: 2004 | First page: 81 | Last page: 93 | doi: http://www.cosis.net/members/journals/df/abstract.php?a_id=498
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A comparison of KNMI Quality Control and JPL Rain Flag for SeaWinds
In the past few years, scatterometer winds have been successfully assimilated in weather analysis...
M Portabella, A Stoffelen | Status: published | Journal: Canadian Journal of Remote Sensing | Volume: 28 | Year: 2002 | First page: 424 | Last page: 430 | doi: 10.5589/m02-040
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