(Q58384749)

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Can the variability in tropospheric OH be deduced from measurements of 1,1,1-trichloroethane (methyl chloroform)?

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Can the variability in tropospheric OH be deduced from measurements of 1,1,1-trichloroethane (methyl chloroform)? (English)

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Maarten Krol

1

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Johannes Lelieveld

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2

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Jos Lelieveld

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language of work or name

English

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publication date

12 February 2003

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published in

Journal of Geophysical Research

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volume

108

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issue

D3

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Global OH trend inferred from methylchloroform measurements

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What controls tropospheric ozone?

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New observational constraints for atmospheric hydroxyl on global and hemispheric scales

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Identification of an El Niño-Southern Oscillation signal in a multiyear global simulation of tropospheric ozone

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Evidence for substantial variations of atmospheric hydroxyl radicals in the past two decades

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Estimating source regions of European emissions of trace gases from observations at Mace Head

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Three-dimensional climatological distribution of tropospheric OH: Update and evaluation

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Reply [to “Comment on “Global OH trend inferred from methylchloroform measurements” by Maarten Krol et al.”]

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7 January 2021

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Atmospheric Trends and Lifetime of CH3CCI3 and Global OH Concentrations

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Numerically stable algorithm for discrete-ordinate-method radiative transfer in multiple scattering and emitting layered media.

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Modeling modern methane emissions from natural wetlands: 1. Model description and results

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(Q58384749)

Can the variability in tropospheric OH be deduced from measurements of 1,1,1-trichloroethane (methyl chloroform)?

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