CO2 seasonality indicates origins of post‐Pinatubo sink
- 5 June 2004
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 31 (11)
- https://doi.org/10.1029/2004gl019760
Abstract
No abstract availableThis publication has 38 references indexed in Scilit:
- Arctic Oscillation response to the 1991 Mount Pinatubo eruption: Effects of volcanic aerosols and ozone depletionJournal of Geophysical Research: Atmospheres, 2002
- Interannual growth rate variations of atmospheric CO2 and its δ13C, H2, CH4, and CO between 1992 and 1999 linked to biomass burningGlobal Biogeochemical Cycles, 2002
- A diagnostic study of temperature controls on global terrestrial carbon exchangeTellus B: Chemical and Physical Meteorology, 2001
- Interannual variability of the oceanic sink of CO2 from 1979 through 1997Global Biogeochemical Cycles, 2000
- Representations of transport, convection, and the hydrologic cycle in chemical transport models: Implications for the modeling of short‐lived and soluble speciesJournal of Geophysical Research: Atmospheres, 1997
- Sensitivity of the atmospheric CH4 growth rate to global temperature changes observed from 1980 to 1992Tellus B: Chemical and Physical Meteorology, 1997
- Changes in CH4 and CO growth rates after the eruption of Mt. Pinatubo and their link with changes in tropical tropospheric UV fluxGeophysical Research Letters, 1996
- A 1° × 1° distribution of carbon dioxide emissions from fossil fuel consumption and cement manufacture, 1950–1990Global Biogeochemical Cycles, 1996
- Extension and integration of atmospheric carbon dioxide data into a globally consistent measurement recordJournal of Geophysical Research: Atmospheres, 1995
- Calculation of surface and top of atmosphere radiative fluxes from physical quantities based on ISCCP data sets: 2. Validation and first resultsJournal of Geophysical Research: Atmospheres, 1995