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Cited by 204

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Indirect long‐term global radiative cooling from NOx Emissions

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Wild, Oliver, Prather, Michael J., Akimoto, Hajime·2001·Geophysical Research Letters

Abstract

Anthropogenic emissions of short‐lived, chemically reactive gases, such as NOx and CO, are known to influence climate by altering the chemistry of the global troposphere and thereby the abundance of the greenhouse gases O 3, CH 4 and the HFCs. This study uses the characteristics of the natural modes of the tropospheric chemical system to decompose the greenhouse effect of NOx and CO emissions into (i) short‐lived modes involving predominantly tropospheric O 3 and (ii) the long‐lived mode involving a global coupled CH 4‐CO‐O 3 perturbation. Combining these two classes of greenhouse perturbations—large, short‐lived, regional O 3 increases and smaller, long‐lived, global decreases in CH 4 and O 3—we find that most types of anthropogenic NOx emissions lead to a negative radiative forcing and an overall cooling of the earth.

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Metadata

Authors
Wild, O., Prather, M. J., & Akimoto, H.
Venue
Geophysical Research Letters
Published
2001-05
Volume
28
Issue
9
Pages
1719-1722
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W1990831891
Cited by
204
References
2
FWCI
3.53
Type
journal article
Language
en
Open access
green

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CoChat. (2026). Citation check: Indirect long‐term global radiative cooling from NOx Emissions. https://app.cochat.ai/papers/10.1029/2000gl012573
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Wild, O., Prather, M. J., & Akimoto, H. (2001). Indirect long‐term global radiative cooling from NOx Emissions. Geophysical Research Letters. https://doi.org/10.1029/2000gl012573

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