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Halogen chemistry reduces tropospheric O.sub.3 radiative forcing

Halogen chemistry reduces tropospheric O.sub.3 radiative forcing

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_gale_infotracacademiconefile_A479564562

Halogen chemistry reduces tropospheric O.sub.3 radiative forcing

About this item

Full title

Halogen chemistry reduces tropospheric O.sub.3 radiative forcing

Publisher

Copernicus GmbH

Journal title

Atmospheric chemistry and physics, 2017-01, Vol.17 (2), p.1557

Language

English

Formats

Publication information

Publisher

Copernicus GmbH

More information

Scope and Contents

Contents

Tropospheric ozone (O.sub.3) is a global warming gas, but the lack of a firm observational record since the preindustrial period means that estimates of its radiative forcing (RF.sub.TO.sub.3) rely on model calculations. Recent observational evidence shows that halogens are pervasive in the troposphere and need to be represented in chemistry-transp...

Alternative Titles

Full title

Halogen chemistry reduces tropospheric O.sub.3 radiative forcing

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_gale_infotracacademiconefile_A479564562

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_gale_infotracacademiconefile_A479564562

Other Identifiers

ISSN

1680-7316

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