The carbon biogeochemical cycle in CLM4
calculates changes in vegetation and wildfire occurrences, both of which depend on hydrological conditions (Thonicke et al. 2001; Kloster et al. 2010).
Not exact matches
Houghton's method of reconstructing Land - Use Based Net Flux of Carbon appears arbitrary and susceptible to bias; i.e. «Rates of land - use
change, including clearing for agriculture and harvest of wood, were reconstructed from statistical and historic documents for 9 world regions and used, along with the per ha [hectare]
changes in vegetation and soil that result from land management, to
calculate the annual flux of carbon between land and atmosphere.»
Future global
vegetation carbon
change calculated by seven global
vegetation models using climate outputs and associated increasing CO2 from five GCMs run with four RCPs, expressed as the
change from the 1971 — 1999 mean relative to
change in global mean land temperature.
Albedo
change due to LGM — Holocene
vegetation change, much of which is inherent with ice sheet area
change, and albedo
change due to coastline movement are lumped together with ice sheet area
change in calculating the surface albedo climate forcing.