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GRADE Uncertainty Analysis
Summary
A main purpose in a frequency or extreme value analysis is to obtain an estimate for some...
HFP van den Boogaard, M Hegnauer, JJ Beersma | Year: 2014
Publication
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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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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
Publication
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Stratospheric ozone [in "State of the Climate in 2018"]
[section from the full abstract] Despite conducive conditions for its formation, the ozone hole a...
A.T.J. de Laat | Journal: Bulletin of the American Meteorological Society | Volume: Volume 99: Issue 8 | Year: 2018 | First page: S1 | Last page: S306 | doi: 10.1175/2019BAMSStateoftheClimate.1
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Daisyworld homeostasis and the earth system
This chapter examines the Daisymodel's steady state solution with emphasis on the mechanisms that...
SL Weber, JM Robinson | Year: 2004
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