Ra. Houghton et al., CURRENT LAND-COVER IN THE TROPICS AND ITS POTENTIAL FOR SEQUESTERING CARBON, Global biogeochemical cycles, 7(2), 1993, pp. 305-320
Emissions of carbon dioxide and other greenhouse gases from human acti
vity are increasing the concentrations of these gases in the atmospher
e. The Earth is expected to warm as a result, with consequences that a
re potentially highly disruptive to human societies. Reductions in the
use of fossil fuels and in rates of deforestation worldwide will redu
ce emissions of CO2, but atmospheric concentrations will continue to i
ncrease unless emissions are reduced by more than 60% (about 4.5 billi
on tons of carbon annually). Reforestation seems to offer one of the f
ew means for reducing the atmospheric concentration of CO2 over period
s as short as human generations. We report here an approach for evalua
ting the potential for reforestation to help stabilize or even reduce
the concentration of CO2 in the atmosphere. Reforestation is defined b
roadly to include tree plantations, natural regrowth of secondary fore
sts, and the practice of agroforestry. Our premise is that human use o
f the land has generally reduced woody biomass and that such lands hav
e a potential for reaccumulating carbon if appropriately managed. We u
sed published ground studies together with global vegetation index dat
a from the NOAA 7 satellite to estimate current land cover in tropical
regions. Then, superimposing this map of current land cover over maps
depicting the distribution of vegetation cover prior to human disturb
ance, we obtained an estimate of about 3200 X 10(6) ha in the tropics
(almost 60% of the total land area considered) where woody biomass had
been decreased, and where carbon might again be sequestered. We calcu
lated the amount of carbon that could be withdrawn from the atmosphere
and stored in woody biomass if several management options were implem
ented. Biomass accumulations were determined from forestry statistics.
Application of the data on biomass to the areas suitable for accumula
tion of carbon yielded an estimate of potential accumulation of 160-17
0 Pg carbon, an amount equivalent to the accumulation of carbon in the
atmosphere since the start of the industrial revolution, or to about
25 years of fossil fuel emissions at current rates. Estimates of both
area and potential accumulation of carbon were crude, probably not bet
ter than +/-50%. They are useful for suggesting the role that tropical
lands might play in stabilizing atmospheric concentrations of CO2, bu
t they should not be used to suggest specific management options in in
dividual countries. As maps with higher spatial resolution become avai
lable, however, the method should provide more precise estimates overa
ll and in specific locations.