Fire emissions from C3 and C4 vegetation and their influence on interannual variability of atmospheric CO2 and δ13CO2
- 7 May 2005
- journal article
- Published by American Geophysical Union (AGU) in Global Biogeochemical Cycles
- Vol. 19 (2)
- https://doi.org/10.1029/2004gb002366
Abstract
No abstract availableKeywords
This publication has 69 references indexed in Scilit:
- Influences of boreal fire emissions on Northern Hemisphere atmospheric carbon and carbon monoxideGlobal Biogeochemical Cycles, 2005
- Improved estimates of net carbon emissions from land cover change in the tropics for the 1990sGlobal Biogeochemical Cycles, 2004
- Measurements of biomass burning influences in the troposphere over southeast Australia during the SAFARI 2000 dry season campaignJournal of Geophysical Research: Atmospheres, 2003
- Global distribution of C3and C4vegetation: Carbon cycle implicationsGlobal Biogeochemical Cycles, 2003
- Isotopic composition of carbon dioxide from a boreal forest fire: Inferring carbon loss from measurements and modelingGlobal Biogeochemical Cycles, 2003
- 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
- 13C content of ecosystem respiration is linked to precipitation and vapor pressure deficitOecologia, 2002
- Effects of fire protection on savanna structure in Central BrazilJournal of Biogeography, 2000
- An assessment of vegetation fire in Africa (1981–1991): Burned areas, burned biomass, and atmospheric emissionsGlobal Biogeochemical Cycles, 1999
- A global 1° by 1° NDVI data set for climate studies derived from the GIMMS continental NDVI dataInternational Journal of Remote Sensing, 1994