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Download Profile: CARBON FLUXES RESULTING FROM LAND-USE CHANGES IN THE STATE OF MORELOS, MEXICO


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This report presents information on land use changes and carbon stocks and fluxes resulting from land use-change in the subtropical dry forest of the State of Morelos, Mexico. Biomass components of standing vegetation were estimated from 40 quadrats (400 m2 each) distributed across this ecosystem. Regional land use changes using forest cover for two different periods (1976 and 1993) and present forest cover, as well as measurements of soil organic matter and soil organic carbon were used to predict carbon stocks and fluxes in this ecosystem. The results showed for the period of 1976-1993 that the annual deforestation rate is 0.87% indicating that approximately 20,000 ha of subtropical dry forest were lost during this period and that 57% of the original ecosystem has been lost since 1950. On the other side, intensive agriculture, including induced grasslands increased (22 000 ha) 15% of the total studied area largely at the expense of the tropical dry forest. Land use changes from the subtropical dry forest to agriculture contributed to carbon emissions of 6.49 Tg, of which standing biomass averaged 2.79 (± 0.28) Tg, root biomass averaged 1.75 (± 0.18) Tg, and soil organic carbon averaged 1.95 ( ± 0.2) Tg. Projected land-use changes will likely contribute to an additional carbon flux of 2.88 (± 0.14) Tg by the year 2050. Practices to conserve, sequester, and transfer carbon stocks in this ecosystem are discussed as a means to reduce carbon flux by deforestation practices.



Author: J. NĂ¡var and A.L. Estrada ( josedejesusnavar at yahoo dot com dot mx)
Filesize: 73.08 Kb


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     Talk History
Friday, September 30
· Discussion Panel
· Nitrogen Regulation of Carbon Sequestration in Terrestrial Ecosystems in Respons
· The Role of Water Relations in Driving Grassland Ecosystem Responses to Rising A
· Unraveling the Decline in High-latitude Surface Ocean Carbonate
Thursday, September 29
· Hazards of Temperature on Food Availability in Changing Environments (HOT-FACE)
· The Amazon and the Modern Carbon Cycle
· New Coupled Climate-carbon Simulations from the IPSL Model
· The Changing Carbon Cycle
· What are the Most Important Factors for Climate-carbon Cycle Coupling?
· CO2 Uptake of the Marine Biosphere
· European-wide Reduction in Primary Productivity Caused by the Heat and Drought i
· Persistence of Nitrogen Limitation over Terrestrial Carbon Uptake
· Atmospheric CO2, Carbon Isotopes, the Sun, and Climate Change over the Last Mill
· Proposing a Mechanistic Understanding of Atmospheric CO2 During the late Pleist
· Greenhouse Gas (CO2, CH4) and Climate Evolution since 650 kyrs Deduced from Anta
Wednesday, September 28
· (In and) Out of Africa: Estimating the Carbon Exchange of a Continent
· Recent Shifts in Soil Dynamics on Growing Season Length, Productivity, and...
· Interannual Variability in the Carbon Exchange Using an Ecosystem-fire Model
· Photosynthesis and Respiration in Forests in Response to Environmental Changes
· Seasonal and Interannual Variability in Net Ecosystem CO2 Exchange in Japan
· Estimating Landscape-level Carbon Fluxes from Tower CO2 Mixing Ratio Measurement
· Monitoring Effects in Climate and Fire Regime on Net Ecosystem Production
· Radiative Forcing from a Boreal Forest Fire
· The Influence of Soil and Water Management on Carbon Erosion and Burial
· Spatial and Temporal Patterns of CO2, CH4, and N2O Fluxes in Ecosystems
· Modeling the History of Terrestrial Carbon Sources and Sinks
· The Age of Carbon Respired from Terrestrial Ecosystems
· Discussion Panel
· The Underpinnings of Land Use History
Tuesday, September 27
· Regional CO2 Fluxes for North America Estimated from NOAA/CMDL Observatories

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The 7th International CO2 Conference

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September 25th - 30th
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