Separating the shortwave and longwave components of greenhouse gas radiative forcing

Shine, K. P. ORCID: https://orcid.org/0000-0003-2672-9978, Byrom, R. E. ORCID: https://orcid.org/0000-0002-5992-6962 and Checa‐Garcia, R. ORCID: https://orcid.org/0000-0001-7653-3653 (2022) Separating the shortwave and longwave components of greenhouse gas radiative forcing. Atmospheric Science Letters, 23 (10). e1116. ISSN 1530-261X doi: 10.1002/asl.1116

Abstract/Summary

Many important greenhouse gases (including water vapour, carbon dioxide, methane and ozone) absorb solar radiation. When gas concentrations change, this absorption exerts a radiative forcing that modifies the thermal infrared (‘longwave’) radiative forcing which is predominant for most gases (ozone being a major exception). The nature of the solar forcing differs from the longwave forcing in several ways. For example, the sign of the instantaneous solar forcing can differ between the tropopause and top-of-atmosphere, and the sign can differ between gases. In addition, a significant part of the solar forcing can be manifested in the longwave, following stratospheric temperature adjustment, which can counteract or enhance the instantaneous solar forcing. Here the nature of solar forcing is examined via a mixture of idealised and more realistic calculations, which consider the effect of perturbations in carbon dioxide, methane and ozone. An apparent contradiction in the sign of the solar forcing of carbon dioxide is resolved; it is shown to be negative, reducing the net carbon dioxide forcing by about 2.3%. The relevance of this work to the effective radiative forcing concept is also discussed.

Item Type	Article
URI	https://reading-clone.eprints-hosting.org/id/eprint/105665
Identification Number/DOI	10.1002/asl.1116
Refereed	Yes
Divisions	Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
Publisher	Royal Meteorological Society
Download/View statistics	View download statistics for this item