Radiative forcing of the Earth's climate system due to tropical tropospheric ozone production
- 27 April 1997
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 102 (D8) , 9409-9417
- https://doi.org/10.1029/96jd04007
Abstract
No abstract availableKeywords
This publication has 32 references indexed in Scilit:
- Origin of ozone and NOx in the tropical troposphere: A photochemical analysis of aircraft observations over the South Atlantic basinJournal of Geophysical Research: Atmospheres, 1996
- Analysis of the distribution of ozone over the southern Atlantic regionJournal of Geophysical Research: Atmospheres, 1996
- Where did tropospheric ozone over southern Africa and the tropical Atlantic come from in October 1992? Insights from TOMS, GTE TRACE A, and SAFARI 1992Journal of Geophysical Research: Atmospheres, 1996
- Radiative forcing due to increased tropospheric ozone concentrationsAtmospheric Environment, 1996
- Concentrations of Tropospheric Ozone from 1979 to 1992 over Tropical Pacific South America from TOMS DataScience, 1996
- On the derivation of tropospheric column ozone from radiances measured by the total ozone mapping spectrometerJournal of Geophysical Research: Atmospheres, 1995
- Evidence of a long‐term increase in tropospheric ozone from Pic du Midi data series: Consequences: Positive radiative forcingJournal of Geophysical Research: Atmospheres, 1994
- Effects of Aerosol from Biomass Burning on the Global Radiation BudgetScience, 1992
- Climate Forcing by Anthropogenic AerosolsScience, 1992
- Tropospheric ozone and climateNature, 1979