How Climatic Change Effects the Crop Growth and Development

1. Effects of enhanced CO2 on crop growthpractice of irrigation more expensive, particularly
Plants grow through the well-known process ofwhen with drier conditions more water will be
photosynthesis, utilizing the energy of sunlight torequired per acre. Peak irrigation demands are also
convert water from the soil and carbon dioxidepredicted to rise due to more severe heat
from the air into sugar, starches, andwaves. Additional investment for dams,
cellulose--the carbohydrates that are thereservoirs, canals, wells, pumps, and piping may
foundations of the entire food chain. CO2 enters abe needed to develop irrigation networks in new
plant through its leaves. Greater atmosphericlocations. Finally, intensified evaporation will increase
concentrations tend to increase the difference inthe hazard of salt accumulation in the soil.
partial pressure between the air outside and inside4. Climate variability
the plant leaves, and as a result more CO2 isExtreme meteorological events, such as spells of
absorbed and converted to carbohydrates. Crophigh temperature, heavy storms, or droughts,
species vary in their response to CO2. Wheat,disrupt crop production. Recent studies have
rice, and soybeans belong to a physiological classconsidered possible changes in the variability as
(called C3 plants) that responds readily towell as in the mean values of climatic variables.
increased CO2 levels. Corn, sorghum, sugarcane,Where certain varieties of crops are grown near
and millet are C4 plants that follow a differenttheir limits of maximum temperature tolerance,
pathway. The latter, though more efficientsuch as rice in Southern Asia, heat spells can be
photosynthetically than C3 crops at present levelsparticularly detrimental. Similarly, frequent droughts
of CO2, tend to be less responsive to enrichednot only reduce water supplies but also increase
concentrations. Thus far, these effects have beenthe amount of water needed for plant
demonstrated mainly in controlled environmentstranspiration.
such as growth chambers, greenhouses, and5. Soil fertility and erosion
plastic enclosures. Experimental studies of theHigher air temperatures will also be felt in the soil,
long-term effects of CO2 in more realistic fieldwhere warmer conditions are likely to speed the
settings have not yet been done on anatural decomposition of organic matter and to
comprehensive scale.increase the rates of other soil processes that
Higher levels of atmospheric CO2 also induceaffect fertility. Additional application of fertilizer
plants to close the small leaf openings known asmay be needed to counteract these processes
stomates through which CO2 is absorbed andand to take advantage of the potential for
water vapor is released. Thus, under CO2enhanced crop growth that can result from
enrichment crops may use less water even whileincreased atmospheric CO2. This can come at the
they produce more carbohydrates. This dualcost of environmental risk, for additional use of
effect will likely improve water-use efficiency,chemicals may impact water and air quality. The
which is the ratio between crop biomass and thecontinual cycling of plant nutrients--carbon,
amount of water consumed. At the same time,nitrogen, phosphorus, potassium, and sulfur--in the
associated climatic effects, such as highersoil-plant-atmosphere system is also likely to
temperatures, changes in rainfall and soil moisture,accelerate in warmer conditions, enhancing CO2
and increased frequencies of extremeand N2O greenhouse gas emissions. Nitrogen is
meteorological events, could either enhance ormade available to plants in a biologically usable
negate potentially beneficial effects of enhancedform through the action of bacteria in the soil.
atmospheric CO2 on crop physiology.This process of nitrogen fixation, associated with
2. Effects of higher temperaturegreater root development, is also predicted to
In middle and higher latitudes, global warming willincrease in warmer conditions and with higher
extend the length of the potential growing season,CO2, if soil moisture is not limiting. Where they
allowing earlier planting of crops in the spring,occur, drier soil conditions will suppress both root
earlier maturation and harvesting, and thegrowth and decomposition of organic matter, and
possibility of completing two or more croppingwill increase vulnerability to wind erosion, especially
cycles during the same season. Many crops haveif winds intensify. An expected increase in
become adapted to the growing-season dayconvective rainfall--caused by stronger gradients
lengths of the middle and lower latitudes and mayof temperature and pressure and more
not respond well to the much longer days of theatmospheric moisture--may result in heavier
high latitude summers. In warmer, lower latituderainfall when and where it does occur. Such
regions, increased temperatures may accelerate"extreme precipitation events" can cause
the rate at which plants release CO2 in theincreased soil erosion.
process of respiration, resulting in less than optimal6. Pests and diseases
conditions for net growth. When temperaturesConditions are more favorable for the proliferation
exceed the optimal for biological processes, cropsof insect pests in warmer climates. Longer
often respond negatively with a steep drop in netgrowing seasons will enable insects such as
growth and yield. If nighttime temperature minimagrasshoppers to complete a greater number of
rise more than do daytime maxima--as isreproductive cycles during the spring, summer,
expected from greenhouse warmingand autumn. Warmer winter temperatures may
projections--heat stress during the day may bealso allow larvae to winter-over in areas where
less severe than otherwise, but increasedthey are now limited by cold, thus causing greater
nighttime respiration may also reduce potentialinfestation during the following crop season.
yields. Another important effect of highAltered wind patterns may change the spread of
temperature is accelerated physiologicalboth wind-borne pests and of the bacteria and
development, resulting in hastened maturation andfungi that are the agents of crop disease.
reduced yield.Crop-pest interactions may shift as the timing of
3. Available waterdevelopment stages in both hosts and pests is
Agriculture of any kind is strongly influenced byaltered. Livestock diseases may be similarly
the availability of water. Climate change will modifyaffected. The possible increases in pest
rainfall, evaporation, runoff, and soil moistureinfestations may bring about greater use of
storage. Changes in total seasonal precipitation orchemical pesticides to control them, a situation
in its pattern of variability are both important. Thethat will require the further development and
occurrence of moisture stress during flowering,application of integrated pest management
pollination, and grain-filling is harmful to most cropstechniques.
and particularly so to corn, soybeans, and wheat.7. Sea-level rise
Increased evaporation from the soil andGlobal warming is predicted to lead to thermal
accelerated transpiration in the plants themselvesexpansion of sea water, along with partial melting
will cause moisture stress; as a result there will beof land-based glaciers and sea-ice, resulting in a
a need to develop crop varieties with greaterrise of sea level which may range from 0.1 to 0.5
drought tolerance.meters (4 to 20 inches) by the middle of the
The demand for water for irrigation is projectednext century, according to present estimates of
to rise in a warmer climate, bringing increasedthe Intergovernmental Panel on Climate Change
competition between agriculture--already the(IPCC). Such a rise could pose a threat to
largest consumer of water resources in semiaridagriculture in low- lying coastal areas, where
regions--and urban as well as industrial users. Fallingimpeded drainage of surface water and of
water tables and the resulting increase in thegroundwater, as well as intrusion of sea water
energy needed to pump water will make theinto estuaries and aquifers, might take place.