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PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
Agriculture and Climate
Change
Eugene S. Takle
Agronomy Department
Geological and Atmospheric Science
Department
Iowa State University
Ames, Iowa 50011
gstakle@iastate.edu
Underwriting/Marketing Seminar, 30 March 2005
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
Outline
 Evidence for global climate change
 Future atmospheric carbon dioxide concentrations
 Simulations of global climate and future climate
change
 Impacts of climate change for the US Midwest
 “Climate surprises”
 Social inequities and ethical issues
surrounding climate change
 Summary
Carbon Dioxide
and Temperature
Carbon Dioxide
and Temperature
2005
Carbon Dioxide
and Temperature
2005
2040
(375 ppm)
(440 ppm)
Carbon Dioxide
and Temperature
Stabilization at 550 ppm
Carbon Dioxide
and Temperature
“Business as Usual”
(fossil intensive)
2100
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
Associated Climate Changes
 Global sea-level has increased 1-2 mm/yr
 Duration of ice cover of rivers and lakes decreased by 2 weeks in N.
Hemisphere
 Arctic ice has thinned substantially, decreased in extent by 10-15%
 Reduced permafrost in polar, sub-polar, mountainous regions
 Growing season lengthened by 1-4 days in N. Hemisphere
 Retreat of continental glaciers on all continents
 Poleward shift of animal and plant ranges
 Snow cover decreased by 10%
 Earlier flowering dates
 Coral reef bleaching
Source: Intergovernmental Panel on Climate Change, 2001 Report
Mann, M. E., R. S. Bailey, and M. K. Hughes, 1999: Geophysical Research Letters 26, 759.
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
Hansen, Scientific American, March 2004
Mt. Pinatubo (1991)
El Chichon (1982)
Agung, 1963
Source: Jerry Meehl, National Center for Atmospheric Research
Source: National Center for Atmospheric Research
Source: National Center for Atmospheric Research
The planet is committed to
a warming over the next
50 years regardless of
political decisions
Source: Intergovernmental Panel on Climate Change, 2001 Report
40% Probability
5% Probability
Source: Intergovernmental Panel on Climate Change, 2001 Report
Climate Change
Projected for 2100
Rapid Economic
Growth
Slower Economic
Growth
Source: IPCC, 2001: Climate Change 2001: The Scientific Basis
Source: IPCC, 2001: Climate Change 2001: The Scientific Basis
IPCC Summary for
Policy Makers
 An increasing body of observations gives a
collective picture of a warming world and
other changes in the climate system
IPCC Summary for
Policy Makers
 An increasing body of observations gives a
collective picture of a warming world and
other changes in the climate system
 Emissions of greenhouse gases and aerosols
due to human activities continue to
alter the atmosphere in ways that
are expected to affect the climate
IPCC Summary for
Policy Makers, cont’d
 Confidence in the ability of models to
project future climate has increased
IPCC Summary for
Policy Makers, cont’d
 Confidence in the ability of models to
project future climate has increased
 There is new and stronger evidence that
most of the warming observed over
the last 50 years is attributable
to human activities
IPCC Summary for
Policy Makers, cont’d
 Anthropogenic climate change will persist
for many centuries
IPCC Summary for
Policy Makers, cont’d
 Anthropogenic climate change will persist
for many centuries
 Further action is required to address
remaining gaps in information and
understanding
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
Climate Surprises:
Low Probability but High-Impact Events
 Breakdown of the ocean thermohaline
circulation (Greenland melt water)
 Breakoff of the West Antarctic Ice Sheet
Climate
Cold Warm
0
Antarctica
Greenland
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
Meltwater flows into
a large moulin on
Greenland and down to
the bedrock to "lubricate"
the sheet
BBC News: World Edition
http://news.bbc.co.uk/2/hi/science/nature/2558319.stm
For the Midwest
 Warming will be greater for winter than summer
 Warming will be greater at night than during the
day
 A 3oF rise in summer daytime temperature triples
the probability of a heat wave
 Growing season will be longer (8-9 days longer
now than in 1950)
 More precipitation
 Likely more soil moisture in summer
 More rain will come in intense rainfall events
 Higher stream flow, more flooding
Sub-Basins of the
Upper Mississippi
River Basin
119 sub-basins
Outflow measured
at Grafton, IL
Approximately one
observing station
per sub-basin
Approximately one
model grid point
per sub-basin
RegCM2 Simulation Domain
Red = global model grid point Green/blue = regional model grid points
Ten-Year Mean Monthly Stream Flow Generated by the
RegCM2 Regional Climate Model Driven
with HadCM2 Global Model Results for the
Contemporary and Future Scenario (2040s) Climate
Relation of Runoff to Precipitation
for Various Climates
More precip
goes to
streamflow in a
future climate
“Warming Hole”
DTmax (JJA)
˚C
Source: IPCC, 2001: Climate Change 2001: The Scientific Basis
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
Social Inequities due to Climate
Change
 Agricultural production
 Freshwater availability
 Sea-water innundation
 Intergenerational equities
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
Social Inequities due to Climate
Change
 Agricultural production
 Freshwater availability
 Sea-water innundation
 Intergenerational equities
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
Impact on US Agriculture
(my speculations)
 The US is a large enough country at a high enough latitude that it will have
regional winners and losers
 Areas now marginal for agriculture may become less suitable
 Some areas now having abundant water but limited growing seasons may be
winners
 Areas with good soils and robust climate, like Iowa, may be impacted less
 The US Midwest may experience more variability from
year to year, which would make agricultural yields
more variable (flooding, water-logging, drought)
 Changes in consumption and agricultural production
in other nations may affect US agriculture more
than changes to US climate
 Environmental refugees?
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
Social Inequities due to Climate
Change
 Agricultural production
 Freshwater availability
 Sea-water innundation
 Intergenerational equities
http://www.grida.no/climate/vital/37.htm
http://www.grida.no/climate/vital/38.htm
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
Social Inequities due to Climate
Change
 Agricultural production
 Freshwater availability
 Sea-water innundation
 Intergenerational equities
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
Sea-Water Innundation
Example: The Maldives
 Area: 115 square miles
 Population: 143,000
 Highest point: 20 ft above sea level
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
Social Inequities due to Climate
Change
 Agricultural production
 Freshwater availability
 Sea-water innundation
 Intergenerational inequities
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
Intergenerational Inequities
 Sustainable Development: “To meet the needs of
the present without compromising the ability of
future generations to meet their needs.”
 Energy sources?
 Non-renewable earth resources?
 Agricultural productivity?
 Fresh water supplies?
 Heavy metal contamination of soil
and water?
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
Summary
 Climate change is real and we need to be doing
something about it
 The longer we wait, the fewer our options
 Regional patterns of warming will be complicated
 Climate surprises can’t be discounted
 Climate change will create regional
agricultural winners and losers
 Climate change carries ethical
implications
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
For More Information
 See my online Global Change course:
http://www.meteor.iastate.edu/gccourse
 Contact me directly:
gstakle@iastate.edu
http://www.meteor.iastate.edu/faculty/takle/

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Underwriting-Mktng.ppt

  • 1. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS Agriculture and Climate Change Eugene S. Takle Agronomy Department Geological and Atmospheric Science Department Iowa State University Ames, Iowa 50011 gstakle@iastate.edu Underwriting/Marketing Seminar, 30 March 2005
  • 2. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS Outline  Evidence for global climate change  Future atmospheric carbon dioxide concentrations  Simulations of global climate and future climate change  Impacts of climate change for the US Midwest  “Climate surprises”  Social inequities and ethical issues surrounding climate change  Summary
  • 7. Carbon Dioxide and Temperature “Business as Usual” (fossil intensive) 2100
  • 8.
  • 9. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS Associated Climate Changes  Global sea-level has increased 1-2 mm/yr  Duration of ice cover of rivers and lakes decreased by 2 weeks in N. Hemisphere  Arctic ice has thinned substantially, decreased in extent by 10-15%  Reduced permafrost in polar, sub-polar, mountainous regions  Growing season lengthened by 1-4 days in N. Hemisphere  Retreat of continental glaciers on all continents  Poleward shift of animal and plant ranges  Snow cover decreased by 10%  Earlier flowering dates  Coral reef bleaching Source: Intergovernmental Panel on Climate Change, 2001 Report
  • 10. Mann, M. E., R. S. Bailey, and M. K. Hughes, 1999: Geophysical Research Letters 26, 759.
  • 11. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
  • 12. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
  • 13. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
  • 14. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
  • 15. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
  • 16. Hansen, Scientific American, March 2004 Mt. Pinatubo (1991) El Chichon (1982) Agung, 1963
  • 17. Source: Jerry Meehl, National Center for Atmospheric Research
  • 18. Source: National Center for Atmospheric Research
  • 19. Source: National Center for Atmospheric Research The planet is committed to a warming over the next 50 years regardless of political decisions
  • 20. Source: Intergovernmental Panel on Climate Change, 2001 Report
  • 21. 40% Probability 5% Probability Source: Intergovernmental Panel on Climate Change, 2001 Report
  • 22. Climate Change Projected for 2100 Rapid Economic Growth Slower Economic Growth
  • 23. Source: IPCC, 2001: Climate Change 2001: The Scientific Basis
  • 24. Source: IPCC, 2001: Climate Change 2001: The Scientific Basis
  • 25. IPCC Summary for Policy Makers  An increasing body of observations gives a collective picture of a warming world and other changes in the climate system
  • 26. IPCC Summary for Policy Makers  An increasing body of observations gives a collective picture of a warming world and other changes in the climate system  Emissions of greenhouse gases and aerosols due to human activities continue to alter the atmosphere in ways that are expected to affect the climate
  • 27. IPCC Summary for Policy Makers, cont’d  Confidence in the ability of models to project future climate has increased
  • 28. IPCC Summary for Policy Makers, cont’d  Confidence in the ability of models to project future climate has increased  There is new and stronger evidence that most of the warming observed over the last 50 years is attributable to human activities
  • 29. IPCC Summary for Policy Makers, cont’d  Anthropogenic climate change will persist for many centuries
  • 30. IPCC Summary for Policy Makers, cont’d  Anthropogenic climate change will persist for many centuries  Further action is required to address remaining gaps in information and understanding
  • 31. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS Climate Surprises: Low Probability but High-Impact Events  Breakdown of the ocean thermohaline circulation (Greenland melt water)  Breakoff of the West Antarctic Ice Sheet
  • 33. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
  • 34. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS Meltwater flows into a large moulin on Greenland and down to the bedrock to "lubricate" the sheet BBC News: World Edition http://news.bbc.co.uk/2/hi/science/nature/2558319.stm
  • 35.
  • 36.
  • 37. For the Midwest  Warming will be greater for winter than summer  Warming will be greater at night than during the day  A 3oF rise in summer daytime temperature triples the probability of a heat wave  Growing season will be longer (8-9 days longer now than in 1950)  More precipitation  Likely more soil moisture in summer  More rain will come in intense rainfall events  Higher stream flow, more flooding
  • 38. Sub-Basins of the Upper Mississippi River Basin 119 sub-basins Outflow measured at Grafton, IL Approximately one observing station per sub-basin Approximately one model grid point per sub-basin
  • 39.
  • 40.
  • 41. RegCM2 Simulation Domain Red = global model grid point Green/blue = regional model grid points
  • 42. Ten-Year Mean Monthly Stream Flow Generated by the RegCM2 Regional Climate Model Driven with HadCM2 Global Model Results for the Contemporary and Future Scenario (2040s) Climate
  • 43. Relation of Runoff to Precipitation for Various Climates More precip goes to streamflow in a future climate
  • 45. Source: IPCC, 2001: Climate Change 2001: The Scientific Basis
  • 46. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS Social Inequities due to Climate Change  Agricultural production  Freshwater availability  Sea-water innundation  Intergenerational equities
  • 47. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS Social Inequities due to Climate Change  Agricultural production  Freshwater availability  Sea-water innundation  Intergenerational equities
  • 48.
  • 49.
  • 50. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS Impact on US Agriculture (my speculations)  The US is a large enough country at a high enough latitude that it will have regional winners and losers  Areas now marginal for agriculture may become less suitable  Some areas now having abundant water but limited growing seasons may be winners  Areas with good soils and robust climate, like Iowa, may be impacted less  The US Midwest may experience more variability from year to year, which would make agricultural yields more variable (flooding, water-logging, drought)  Changes in consumption and agricultural production in other nations may affect US agriculture more than changes to US climate  Environmental refugees?
  • 51. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS Social Inequities due to Climate Change  Agricultural production  Freshwater availability  Sea-water innundation  Intergenerational equities
  • 54. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS Social Inequities due to Climate Change  Agricultural production  Freshwater availability  Sea-water innundation  Intergenerational equities
  • 55. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS
  • 56. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS Sea-Water Innundation Example: The Maldives  Area: 115 square miles  Population: 143,000  Highest point: 20 ft above sea level
  • 57. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS Social Inequities due to Climate Change  Agricultural production  Freshwater availability  Sea-water innundation  Intergenerational inequities
  • 58. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS Intergenerational Inequities  Sustainable Development: “To meet the needs of the present without compromising the ability of future generations to meet their needs.”  Energy sources?  Non-renewable earth resources?  Agricultural productivity?  Fresh water supplies?  Heavy metal contamination of soil and water?
  • 59. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS Summary  Climate change is real and we need to be doing something about it  The longer we wait, the fewer our options  Regional patterns of warming will be complicated  Climate surprises can’t be discounted  Climate change will create regional agricultural winners and losers  Climate change carries ethical implications
  • 60. PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS For More Information  See my online Global Change course: http://www.meteor.iastate.edu/gccourse  Contact me directly: gstakle@iastate.edu http://www.meteor.iastate.edu/faculty/takle/

Hinweis der Redaktion

  1. From Jerry Meehl This slide shows the time evolution of globally averaged surface air temperature from multiple ensemble simulations of 20th century climate from the NCAR Parallel Climate Model (PCM) compared to observations. The simulations start in the late 19th century, and continue to the year 2000. The temperature scale at left is in degrees Centigrade, and temperature anomalies are calculated relative to a reference period averaged from 1890 to 1919. The black line shows the observed data, or the actual, recorded globally averaged surface air temperatures from the past century. The blue and red lines are the average of four simulations each from the computer model. The pink and light blue shaded areas depict the range of the four simulations for each experiment, giving an idea of the uncertainty of a given realization of 20th century climate from the climate model. The blue line shows the average from the four member ensemble of the simulated time evolution of globally average surface air temperature when only "natural" influences (solar variability and volcanic eruptions) are included in the model. Therefore, the blue line represents what the model says global average temperatures would have been if there had been no human influences. The red line shows the average of the four member ensemble experiment when natural forcings AND anthropogenic influences (greenhouse gases including carbon dioxide, sulfate aerosols from air pollution, and ozone changes) are included in the model. Note that this model can reproduce the actual, observed data very well only if the combined effects of natural and anthropogenic factors are included. The conclusion that can be drawn is that naturally occuring influences on climate contributed to most of the warming that occurred before WWII, but that the large observed temperature increases since the 1970s can only be simulated in the model if anthropogenic factors are included. This confirms the conclusion of the IPCC Third Assessment Report that most of the warming we have observed in the latter part of the 20th century has been due to human influences.
  2. A feature that corresponds to later 20th century trends. Not seen in GCMs. Linked to mesoscale circulation.