Not exact matches
Tropical forests convert more carbon
from the atmosphere into
biomass than any other
terrestrial ecosystem on Earth.
Recent estimates
from satellite imagery indicate that humans now appropriate 38 percent of all
terrestrial biomass generated annually.
Carozza et al (2011) find that natural global warming occurred in 2 stages: First, global warming of 3 ° to 9 ° C accompanied by a large bolus of organic carbon released to the atmosphere through the burning of
terrestrial biomass (Kurtz et al, 2003) over approximately a 50 - year period; second, a catastrophic release of methane hydrate
from sediment, followed by the oxidation of a part of this methane gas in the water column and the escape of the remaining CH4 to the atmosphere over a 50 - year period.
«For 20 million years,
from the early Neogene approximately 23 million years ago until the Pleistocene started around 2 million years ago, this rule applied: The larger the amount of
biomass produced by plants, the higher the diversity of
terrestrial mammals that evolved.
Such connections would be much harder to detect
from space for
terrestrial plant
biomass.»
Carozza et al (2011) find that natural global warming occurred in 2 stages: First, global warming of 3 ° to 9 ° C accompanied by a large bolus of organic carbon released to the atmosphere through the burning of
terrestrial biomass (Kurtz et al, 2003) over approximately a 50 - year period; second, a catastrophic release of methane hydrate
from sediment, followed by the oxidation of a part of this methane gas in the water column and the escape of the remaining CH4 to the atmosphere over a 50 - year period.
This means that the equivalent of half our annual emissions of CO2 is removed
from the atmosphere by the oceans and
terrestrial biomass.
This is because any net additions of CO2 to the atmosphere resulting
from biomass combustion should be captured by analyzing land - use, land - use change activities and their associated effects on
terrestrial biomass carbon stocks.
We attribute this increase to the response
from the
terrestrial component of the carbon cycle — a combination of reduction in biospheric uptake of CO2 over pan-tropical regions and an enhancement in
biomass burning emissions over Southeast Asia and Indonesia.