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Atmospheric Composition Change: Climate-Chemistry interactions
Chemically active climate compounds are either primary compounds like methane (CH4), removed by o...
ISA Isaksen, C Granier, G Myhre, TK Berntsen, SB Dalsoren, M Gauss, Z Klimont, M van Weele, co-authors | Status: published | Journal: Atmos. Environm. | Volume: 43 | Year: 2009 | First page: 5138 | Last page: 5192 | doi: 10.1016/j.atmosenv.2009.08.003
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Drag of the sea surface
It is shown how the drag of the sea surface can be computed from
the wind speed and the sea state...
VK Makin, VN Kudryavtsev, C Mastenbroek | Status: published | Journal: Bound.-Layer Meteorol. | Volume: 73 | Year: 1995 | First page: 159 | Last page: 182
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The importance of surface reflectance anisotropy for cloud and NO2 retrievals from GOME-2 and OMI
The angular distribution of the light reflected by the Earth's surface influences top-of-atmosphe...
A Lorente, KF Boersma, P Stammes, LG Tilstra, A Richter, H Yu, S Kharbouche, JP Muller | Status: published | Journal: Atmospheric Measurement Techniques | Volume: 11 | Year: 2018 | First page: 4509 | Last page: 4529 | doi: 10.5194/amt-11-4509-2018
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Comparison of modelled ozone distributions with ozonesonde observations in the Tropics
Modelling as a tool for supporting research on major scientific questions in atmospheric chemistr...
Rob Puts | Year: 2001 | Pages: 44
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Atmospheric visibility inferred from continuous-wave Doppler wind lidar
Atmospheric visibility, or meteorological optical range (MOR), is governed by light extinction by...
Manuel Queißer, Michael Harris, and Steven Knoop | Journal: Atmos. Meas. Tech. | Volume: 15 | Year: 2022 | First page: 5527 | Last page: 5544 | doi: https://doi.org/10.5194/amt-15-5527-2022
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