Strategies for combating ill effect of
climate change on soil and crop
productivity
Dr. K. Boomiraj
Assistant Professor (Environmental Science)
Climate change
 Climate change refers to a statistically significant variation in
either the mean stage of the climate or in its variability,
persisting for an extended period (typically decade or
longer).
 May be due to natural internal processes or external forcing,
or to persistent anthropogenic changes in the composition of
the atmosphere or in land use.
Natural and
anthropogenic
contributions to global
temperature change
(Meehl et al., 2004).
Observed values from
Jones and Moberg 2001.
Grey bands indicate 68%
and 95% range derived
from multiple simulations.
Natural cycles
Natural and
anthropogenic
contributions to global
temperature change
(Meehl et al., 2004).
Observed values from
Jones and Moberg 2001.
Grey bands indicate 68%
and 95% range derived
from multiple simulations.
Not Natural
GHG effect – Necessary Evil
 Green house Gas effect – to maintain the atmospheric
temperature to sustain the life on earth.
 Enhanced GHG effect has detrimental harmful effect on
human beings as well as all living organism
 Anthropogenic activity – Fossil fuel consumption,
deforestration land degradation etc..
Projected concentrations of CO2 during the 21st
century are two to four times the pre-industrial level
Year CO2, ppm
2000 369
2010-2015 388-398
2050/2060 463-623
2100 478-1099
Global mean temperatures have increased by 0.74oC during last
100 years. The rate has become faster in recent years
Warmest 12 years:
1998,2005,2003,2002,2004,2006,
2001,1997,1995,1999,1990,2000
IPCC, 2007
Future Climate is Likely to be Warmer
• Although there is considerable uncertainty about future, all climate
models indicate a rising trend in temperature. By 2100 a rise of 1.8 to
4oC is expected.
• Rise in sea level by 15 – 95cm
• Occurrence of extreme weather conditions
• Severe droughts and floods occur
• Adverse effects on ecological systems
• Effects on human health, economy and quality of life
Source: IPCC, 2007
In India, greater warming
is expected in the Indo-
Gangetic plains
Projected warming in 21st century
Warming is expected to be
greatest over land and at
most high northern latitudes
Future Climate Change -Temperature In Asia
 Temperature rise in Asia is likely to be:
1.6 +/- 0.20C in the 2020s
3.1 +/- 0.30 C in the 2050s
4.6 + /- 0.40C in the 2080s
 Indonesia, the Philippines and coastal south Asia and Indo-
China: least warming in the islands and coastal areas
 South Asia and Indo-China: greatest warming in inland
continental areas except from June to August in south Asia
Proportion of heavy rainfall has increased in most
places
Regions of disproportionate changes in heavy (95% fractile)
and very heavy (99% fractile) precipitation.
IPCC WG-I (2007)
Agriculture and climate change
Agriculture is highly integrated into the climate change challenge
Agriculture is one of the main emitters of greenhouse gases
Agriculture is highly impacted by climate change (temperature,
rainfall)
Issues
- GHG emissions (CO2, CH4, N2O)
- Climate change impacts
- Soil quality
- Water usage
- Resilience to climatic variability
- Adaptation to climate change
CROP PRODUCTION – WEATHER-DEPENDENT SECTOR
 80% of the world area rainfed and 20% irrigated
agriculture - A good rainy season means good crop
production, enhanced food security and a healthy
economy.
 Failure of rains and occurrence of natural disasters
such as floods and droughts could lead to crop
failures, food insecurity, famine, loss of property
and life, mass migration, and negative national
economic growth
Impacts of climate change
 Crop productivity is projected to decrease for even small local
temperature increases (1-20C) at lower latitude, especially
seasonal dry and tropical regions, which would increase the
risk of hunger.
 developing countries are expected to experience larger
percentage losses, global mean losses could be 1-5% GDP for
40C of warming
(IPCC, 2007)
 The rising temperatures and carbon dioxide, and uncertainties
in rainfall associated with global climate change may impact
food production in South Asia due to its large population,
predominance in agriculture, and its limited resource
endowments
( Aggarwal, 2003)
Impacts on Crop Productivity
Climate related drivers on crop productivity
1. Elevated carbon dioxide
2. Rainfall and associated water resource
availability
3. Temperature – both direct and indirect through
evaporation
4. Extreme weather events (wind, flood damage)
These interaction to affect crop productivity, quality,
pests and diseases.
Contd..
 Doubling of CO2, productivity of C3 crops particularly rice,
soybean, millets and tropical C3 grasses will likely to
increase.
 Rise in temperature as a result of doubling of CO2, C3 crops
like wheat, barley, potato, lentil, mustard and temperate
grasses will likely to be adversely affected.
 Productivity of C4 crops like maize, sugarcane, sorghum and
C4 tropical grasses will be little increased but temperature
will have more negative and rainfall will have variable
effects.
 Climate change will have impact on the extinction of
biodiversity species and shift in habitat is likely to occur.
 With the uniform rise of rainfall will have positive impact
on overall agriculture but skewed rise (extreme event) will
have negative impact on soil nutrient loss due to flood
damage and erosion, and will have negative impact on
overall agriculture.
Contd..
better winter
survival of pests
more root rots
with heavy rains
Insect, disease and weed
pressure is already changing
perennial
weeds
make
good use
of CO2
Some crops will be ‘winners’
Others will be ‘losers’
Impact of climate change on Indian Agriculture
 Cereal productivity to decrease by 10-40% by2100.
 1oC increase in temperature may reduce wheat production
by 4-5 mtons (1-2 mtons if adapted).
 Increased droughts and floods are likely to increase
production variability
 Reduced frequency of frost damage: less damage to potato,
peas, mustard
 Some improvement in chickpea, mustard, and rabi maize,
sorghum and millets; and coconut in west coast
Impact on Rainfed Sorghum
Sorghum CSH-16
-10.0
-5.0
0.0
5.0
10.0
15.0
20.0
25.0
30.0
35.0
M
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h
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n
%
loss
in
the
grain
yield
At2020
At2050
At2080
K. Boomraj and SP Wani, 2010
Climate change and soil
• Soil organic matter decrease
• N transformation process affected
• Nutrient imbalances
• Soil biodiversity affected
Climate change and desertification
– Increase in drought
– Increased soil salinisation and soil erosion
– Deserts become hotter
Climate change and Biomes
– Increased CO2 absorbed by the sea water forming
carbonic acid affecting corals and other marine
animals
– Habitat changes
– Increased occurrence of diseases
Climate change and coastal lowland
• Sea level rise by 2.5cm per decade
• Ingression of sea water – salinisation
• Accelerated coastal erosion
• India soil salinity affects 10 Mha
• In Sundarban, 600 families have migrated due to
sea water ingression
Conclusion
 Climate change is a reality and crop productivity is going to
reduce by 40% except some temperate regions.
 Positive effect CO2 enrichment on crop productivity will
be nullified by rise in temperature particularly in the
warmer environment.
 Present level of marginal surplus will continue to decline
and the country may face difficulties to attain agriculture
sufficiency.
Contd..
 Technological innovation will be required to bridge the
productivity gap between the actual and the potential.
 Use of adaptive crop varieties, improved seeds including
hybrids, Efficient use of fertilizer and irrigation and crop
diversification will reverse the likely impact of climate
change.
 Costs of adaptation and mitigation are unknown but likely to
be high; costs of inaction could be even higher
 Start with ‘no-regrets’ adaptation options

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  • 1.
    Strategies for combatingill effect of climate change on soil and crop productivity Dr. K. Boomiraj Assistant Professor (Environmental Science)
  • 2.
    Climate change  Climatechange refers to a statistically significant variation in either the mean stage of the climate or in its variability, persisting for an extended period (typically decade or longer).  May be due to natural internal processes or external forcing, or to persistent anthropogenic changes in the composition of the atmosphere or in land use.
  • 3.
    Natural and anthropogenic contributions toglobal temperature change (Meehl et al., 2004). Observed values from Jones and Moberg 2001. Grey bands indicate 68% and 95% range derived from multiple simulations. Natural cycles
  • 4.
    Natural and anthropogenic contributions toglobal temperature change (Meehl et al., 2004). Observed values from Jones and Moberg 2001. Grey bands indicate 68% and 95% range derived from multiple simulations. Not Natural
  • 5.
    GHG effect –Necessary Evil  Green house Gas effect – to maintain the atmospheric temperature to sustain the life on earth.  Enhanced GHG effect has detrimental harmful effect on human beings as well as all living organism  Anthropogenic activity – Fossil fuel consumption, deforestration land degradation etc..
  • 6.
    Projected concentrations ofCO2 during the 21st century are two to four times the pre-industrial level Year CO2, ppm 2000 369 2010-2015 388-398 2050/2060 463-623 2100 478-1099
  • 8.
    Global mean temperatureshave increased by 0.74oC during last 100 years. The rate has become faster in recent years Warmest 12 years: 1998,2005,2003,2002,2004,2006, 2001,1997,1995,1999,1990,2000 IPCC, 2007
  • 9.
    Future Climate isLikely to be Warmer • Although there is considerable uncertainty about future, all climate models indicate a rising trend in temperature. By 2100 a rise of 1.8 to 4oC is expected. • Rise in sea level by 15 – 95cm • Occurrence of extreme weather conditions • Severe droughts and floods occur • Adverse effects on ecological systems • Effects on human health, economy and quality of life
  • 10.
    Source: IPCC, 2007 InIndia, greater warming is expected in the Indo- Gangetic plains Projected warming in 21st century Warming is expected to be greatest over land and at most high northern latitudes
  • 11.
    Future Climate Change-Temperature In Asia  Temperature rise in Asia is likely to be: 1.6 +/- 0.20C in the 2020s 3.1 +/- 0.30 C in the 2050s 4.6 + /- 0.40C in the 2080s  Indonesia, the Philippines and coastal south Asia and Indo- China: least warming in the islands and coastal areas  South Asia and Indo-China: greatest warming in inland continental areas except from June to August in south Asia
  • 12.
    Proportion of heavyrainfall has increased in most places Regions of disproportionate changes in heavy (95% fractile) and very heavy (99% fractile) precipitation. IPCC WG-I (2007)
  • 13.
    Agriculture and climatechange Agriculture is highly integrated into the climate change challenge Agriculture is one of the main emitters of greenhouse gases Agriculture is highly impacted by climate change (temperature, rainfall) Issues - GHG emissions (CO2, CH4, N2O) - Climate change impacts - Soil quality - Water usage - Resilience to climatic variability - Adaptation to climate change
  • 14.
    CROP PRODUCTION –WEATHER-DEPENDENT SECTOR  80% of the world area rainfed and 20% irrigated agriculture - A good rainy season means good crop production, enhanced food security and a healthy economy.  Failure of rains and occurrence of natural disasters such as floods and droughts could lead to crop failures, food insecurity, famine, loss of property and life, mass migration, and negative national economic growth
  • 15.
    Impacts of climatechange  Crop productivity is projected to decrease for even small local temperature increases (1-20C) at lower latitude, especially seasonal dry and tropical regions, which would increase the risk of hunger.  developing countries are expected to experience larger percentage losses, global mean losses could be 1-5% GDP for 40C of warming (IPCC, 2007)  The rising temperatures and carbon dioxide, and uncertainties in rainfall associated with global climate change may impact food production in South Asia due to its large population, predominance in agriculture, and its limited resource endowments ( Aggarwal, 2003)
  • 16.
    Impacts on CropProductivity Climate related drivers on crop productivity 1. Elevated carbon dioxide 2. Rainfall and associated water resource availability 3. Temperature – both direct and indirect through evaporation 4. Extreme weather events (wind, flood damage) These interaction to affect crop productivity, quality, pests and diseases.
  • 17.
    Contd..  Doubling ofCO2, productivity of C3 crops particularly rice, soybean, millets and tropical C3 grasses will likely to increase.  Rise in temperature as a result of doubling of CO2, C3 crops like wheat, barley, potato, lentil, mustard and temperate grasses will likely to be adversely affected.  Productivity of C4 crops like maize, sugarcane, sorghum and C4 tropical grasses will be little increased but temperature will have more negative and rainfall will have variable effects.
  • 18.
     Climate changewill have impact on the extinction of biodiversity species and shift in habitat is likely to occur.  With the uniform rise of rainfall will have positive impact on overall agriculture but skewed rise (extreme event) will have negative impact on soil nutrient loss due to flood damage and erosion, and will have negative impact on overall agriculture. Contd..
  • 19.
    better winter survival ofpests more root rots with heavy rains Insect, disease and weed pressure is already changing perennial weeds make good use of CO2
  • 20.
    Some crops willbe ‘winners’ Others will be ‘losers’
  • 21.
    Impact of climatechange on Indian Agriculture  Cereal productivity to decrease by 10-40% by2100.  1oC increase in temperature may reduce wheat production by 4-5 mtons (1-2 mtons if adapted).  Increased droughts and floods are likely to increase production variability  Reduced frequency of frost damage: less damage to potato, peas, mustard  Some improvement in chickpea, mustard, and rabi maize, sorghum and millets; and coconut in west coast
  • 22.
    Impact on RainfedSorghum Sorghum CSH-16 -10.0 -5.0 0.0 5.0 10.0 15.0 20.0 25.0 30.0 35.0 M a h a r a t s r a A n d h r a P r a d e s h T a m i l n a d u M a d y a P r a d e s h K a r n a t a k a R a j a s t h a n % loss in the grain yield At2020 At2050 At2080 K. Boomraj and SP Wani, 2010
  • 23.
    Climate change andsoil • Soil organic matter decrease • N transformation process affected • Nutrient imbalances • Soil biodiversity affected
  • 24.
    Climate change anddesertification – Increase in drought – Increased soil salinisation and soil erosion – Deserts become hotter Climate change and Biomes – Increased CO2 absorbed by the sea water forming carbonic acid affecting corals and other marine animals – Habitat changes – Increased occurrence of diseases
  • 25.
    Climate change andcoastal lowland • Sea level rise by 2.5cm per decade • Ingression of sea water – salinisation • Accelerated coastal erosion • India soil salinity affects 10 Mha • In Sundarban, 600 families have migrated due to sea water ingression
  • 26.
    Conclusion  Climate changeis a reality and crop productivity is going to reduce by 40% except some temperate regions.  Positive effect CO2 enrichment on crop productivity will be nullified by rise in temperature particularly in the warmer environment.  Present level of marginal surplus will continue to decline and the country may face difficulties to attain agriculture sufficiency.
  • 27.
    Contd..  Technological innovationwill be required to bridge the productivity gap between the actual and the potential.  Use of adaptive crop varieties, improved seeds including hybrids, Efficient use of fertilizer and irrigation and crop diversification will reverse the likely impact of climate change.  Costs of adaptation and mitigation are unknown but likely to be high; costs of inaction could be even higher  Start with ‘no-regrets’ adaptation options