Sa. Saseendran et al., Effects of climate change on rice production in the tropical humid climateof Kerala, India, CLIM CHANGE, 44(4), 2000, pp. 495-514
The CERES-Rice v3. crop simulation model, calibrated and validated for its
suitability to simulate rice production in the tropical humid climate Keral
a State of India, is used for analysing the effect of climate change on ric
e productivity in the state. The plausible climate change scenario for the
Indian subcontinent as expected by the middle of the next century, taking i
nto account the projected emissions of greenhouse gases and sulphate aeroso
ls, in a coupled atmosphere-ocean model experiment performed at Deutsches K
limarechenzentrum, Germany, is adopted for the study. The adopted scenario
represented an increase in monsoon seasonal mean surface temperature of the
order of about 1.5 degrees C, and an increase in rainfall of the order of
2 mm per day, over the state of Kerala in the decade 2040-2049 with respect
to the 1980s. The IPCC Business-as-usual scenario projection of plant usab
le concentration of CO2 about 460 PPM by the middle of the next century are
also used in the crop model simulation.
On an average over the state with the climate change scenario studied, the
rice maturity period is projected to shorten by 8% and yield increase by 12
%. When temperature elevations only are taken into consideration, the crop
simulations show a decrease of 8% in crop maturity period and 6% in yield.
This shows that the increase in yield due to fertilisation effect of elevat
ed CO2 and increased rainfall over the state as projected in the climate ch
ange scenario nearly makes up for the negative impact on rice yield due to
temperature rise.
The sensitivity experiments of the rice model to CO2 concentration changes
indicated that over the state, an increase in CO2 concentration leads to yi
eld increase due to its fertilisation effect and also enhance the water use
efficiency of the paddy. The temperature sensitivity experiments have show
n that for a positive change in temperature up to 5 degrees C, there is a c
ontinuous decline in the yield. For every one degree increment the decline
in yield is about 6%. Also, in another experiment it is observed that the p
hysiological effect of ambient CO2 at 425 ppm concentration compensated for
the yield losses due to increase in temperature up to 2 degrees C. Rainfal
l sensitivity experiments have shown that increase in rice yield due to inc
rease in rainfall above the observed values is near exponential. But decrea
se in rainfall results in yield loss at a constant rate of about 8% per 2 m
m/day, up to about 16 mm/day.