Rice paddies are a major source of atmospheric methane (CH4). However,
the strength of this source is highly uncertain. To improve estimates
of CH4 emission at the regional and global scales requires process-ba
sed models, integrating the environmental and biological factors that
determine the rate of CH4 emission. In this study, we used such a mode
l to calculate the spatial and seasonal variations in CH, emission fro
m rice paddies, with the support of an integrated GIS data set definin
g distribution of rice paddies, rice calendar, climate, and soil condi
tions. The calculated rates of CH4 emission in a rice-growing season v
aried greatly, from 5 to 90 g CH4 m(-2), for rice paddies across the g
lobe. In most rice paddies daily mean CH4 effluxes were from 50 to 400
mg CH4 m(-2). Annual total emission was estimated to be 53 Tg; two th
irds of this was emitted between 10 degrees N and 30 degrees N. Monthl
y CH4 emissions ranged from 1.4 Tg in January to 8.7 Tg in August, and
more than a half of the emission occurred between June and October. O
ur model suggests that, on average, 12% of the simple carbon substrate
from decomposition of soil organic matter and rice plants was transfo
rmed into CH4, and the emitted CH4 accounted for 6.5% of the rice net
primary production. Copyright (C) 1996 Elsevier Science Ltd