Climate Change: Use of Climate Science in Decisionmaking - PowerPoint PPT Presentation

About This Presentation
Title:

Climate Change: Use of Climate Science in Decisionmaking

Description:

PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS. Climate Change: ... the Swiss Alpine Museum in Bern documents the gradual disappearance of ... – PowerPoint PPT presentation

Number of Views:68
Avg rating:3.0/5.0
Slides: 66
Provided by: IIT5
Category:

less

Transcript and Presenter's Notes

Title: Climate Change: Use of Climate Science in Decisionmaking


1
Climate Change Use of Climate Science in
Decision-making
  • Eugene S. Takle, PhD, CCM
  • Professor of Atmospheric Science
  • Department of Geological and Atmospheric Sciences
  • Professor of Agricultural Meteorology
  • Department of Agronomy
  • Faculty Director, University Honors Program
  • Iowa State University
  • Ames, Iowa 50011
  • gstakle_at_iastate.edu

Annual Conference Iowa State Extension
Service Ames 10 October 2007
2
Image courtesy of NASA/GSFC
3
Outline
  • Changes in atmospheric carbon dioxide
  • Radiative forcing
  • Simulations of global climate and future climate
    change
  • Four components for addressing climate change
  • Climate change for Iowa and the Midwest
    adaptation strategy
  • Climate information and forecasts for
    use in extension

Except where noted as personal views or from the
ISU Global Change course or the Iowa
Environmental Mesonet, all materials presented
herein are from peer-reviewed scientific reports
4
(No Transcript)
5
Pattern repeats about every 100,000 years
Natural cycles
6
IPCC Third Assessment Report
7
Carbon Dioxide and Temperature
2007 380 ppm
8
Carbon Dioxide and Temperature
2050 550 ppm
9
Carbon Dioxide and Temperature
Business as Usual 950 ppm
10
Carbon Dioxide and Temperature
Business as Usual 950 ppm
?
11
http//www.ncdc.noaa.gov/img/climate/research/2006
/ann/glob_jan-dec-error-bar_pg.gif
12
Mann, M. E., R. S. Bailey, and M. K. Hughes,
1999 Geophysical Research Letters 26, 759.
13
Source IPCC, 2001 Climate Change 2001 The
Scientific Basis
14
Source IPCC, 2001 Climate Change 2001 The
Scientific Basis
15
(No Transcript)
16
IPCC Fourth Assessment Report Summary for Policy
Makers
17
El Chichon (1982)
Agung, 1963
Mt. Pinatubo (1991)
At present trends the imbalance 1 Watt/m2 in
2018
Hansen, Scientific American, March 2004
18
http//www.nytimes.com/interactive/2007/10/01/scie
nce/20071002_ARCTIC_GRAPHIC.html?ex1191902400en
c94928ddecd5ba57ei5070emceta3
19
http//www.nytimes.com/interactive/2007/10/01/scie
nce/20071002_ARCTIC_GRAPHIC.html?ex1191902400en
c94928ddecd5ba57ei5070emceta3
20
http//www.nytimes.com/interactive/2007/10/01/scie
nce/20071002_ARCTIC_GRAPHIC.html?ex1191902400en
c94928ddecd5ba57ei5070emceta3
21
http//www.nytimes.com/interactive/2007/10/01/scie
nce/20071002_ARCTIC_GRAPHIC.html?ex1191902400en
c94928ddecd5ba57ei5070emceta3
22
http//www.nytimes.com/interactive/2007/10/01/scie
nce/20071002_ARCTIC_GRAPHIC.html?ex1191902400en
c94928ddecd5ba57ei5070emceta3
23
http//www.nytimes.com/interactive/2007/10/01/scie
nce/20071002_ARCTIC_GRAPHIC.html?ex1191902400en
c94928ddecd5ba57ei5070emceta3
24
http//www.nytimes.com/interactive/2007/10/01/scie
nce/20071002_ARCTIC_GRAPHIC.html?ex1191902400en
c94928ddecd5ba57ei5070emceta3
25
Source Corell, R. W., 2004 Impacts of a
warming Arctic. Arctic Climate Impact Assessment
(www.acia.uaf.edu) Cambridge University Press
(www.cambridge.org).
26
Kennedy Space Center
Impact of a 1-m rise in sea level on low-lying
areas
Projected sea-level rise In 21st century 0.5 to
1.0 m
Areas subjected to Inundation with a 1 m (3 ft)
rise in sea level
Miami
Source Corell, R. W., 2004 Impacts of a
warming Arctic. Arctic Climate Impact Assessment
(www.acia.uaf.edu) Cambridge University Press
(www.cambridge.org).
27
(No Transcript)
28
(No Transcript)
29
Hansen, Scientific American, March 2004
30
Antarctica
Greenland
Ice Volume
0
Warm
Cold
Climate
31
An exhibition of old and new photographs at the
Swiss Alpine Museum in Bern documents the gradual
disappearance of Switzerland's glaciers.?The
Rhone glacier with the Hotel Belvedere in the
foreground and the Furka pass, Canton Valais
circa 1906 and 2003?(Pictures Gesellschaft fur
okologische Forschung, Munich)
32
http//www.ncdc.noaa.gov/img/climate/research/2006
/ann/glob_jan-dec-error-bar_pg.gif
33
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.
34
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
35
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
36
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.
Highly Likely Not Natural
Not Natural
37
Source Jerry Meehl, National Center for
Atmospheric Research
38
IPCC Fourth Assessment Report Summary for Policy
Makers
39
Energy intensive
Reduced Consumption
Energy conserving
IPCC Fourth Assessment Report Summary for Policy
Makers
40
Energy intensive
Reduced Consumption
Energy conserving
The planet is committed to a warming over the
next 50 years regardless of political decisions
IPCC Fourth Assessment Report Summary for Policy
Makers
41
Energy intensive
Reduced Consumption
Energy conserving
Mitigation Possible
Adaptation Necessary
IPCC Fourth Assessment Report Summary for Policy
Makers
42
IPCC Fourth Assessment Report Summary for Policy
Makers
43
IPCC Fourth Assessment Report Summary for Policy
Makers
44
Four-Component Approach for Addressing Climate
Change
  • Mitigation policies 2050-2100
  • Example reduction in GHG emissions
  • Adaptation (long-term) 2015-2050
  • Example Developing Iowas competitive economic
    advantage
  • Adaptation (short-term) 2008-2015
  • Example redefining climate normals
    when needed and scientifically justified
  • Scenario planning for Iowas Katrina 2007-2100
  • Example Multi-year drought, recurrent floods,
    combination of both drought and wildfire

EST personal view
45
Climate Adaptation(Short-Term)
If a meteorological variable began departing from
its long-term background near or after 1970 it
may be related to the radiation imbalance and
thereby has a better chance than not of
continuing its new trend over the next 5-10 years.
EST personal view
46
Projected Changes for the Climate of Iowa/Midwest
(My tentative assessment)
  • Longer frost-free period (high)
  • Higher average winter temperatures (high)
  • Fewer extreme cold temperatures in winter (high)
  • More extreme high temperatures in summer (medium)
  • Higher nighttime temperatures both summer and
    winter (high)
  • More (10) precipitation (medium)
  • More variability of summer precipitation (high)
  • More intense rain events and hence more runoff
    (high)
  • Higher episodic streamflow (medium)
  • Longer periods without rain (medium)
  • Higher absolute humidity (high)
  • Stronger storm systems (medium)
  • Reduced annual mean wind speeds (medium)

Follows trend of last 25 years and projected by
models No current trend but
model suggestion or current trend but models
inconclusive
47
Reasons Crop Yields Might Increase in the Midwest
  • Longer growing season
  • Warmer spring soil temperatures
  • Modest or no increase in summer daily maximum
    temperatures
  • Increase in nighttime temperatures
  • Reduced risk of late frost in spring or early
    frost in fall
  • More freeze-thaw cycles that will recharge
    soil moisture in winter

48
Reasons Crop Yields Might Increase in the Midwest
  • More precipitation
  • More soil moisture
  • Higher dew-point temperatures reduces moisture
    stress
  • Higher CO2 increased carbon uptake by crops
  • Higher CO2 increases the water-use
    efficiency of crops

49
Reasons Crop Yields Might Decrease in the Midwest
  • More precipitation extremes
  • More rain events bring heavy rain
  • More droughts
  • More floods
  • More over-wintering pests
  • More pathogens due to higher humidity
  • More vigorous weed growth

50
D. Herzmann, Iowa Environmental Mesonet
51
D. Herzmann, Iowa Environmental Mesonet
52
D. Herzmann, Iowa Environmental Mesonet
53
D. Herzmann, Iowa Environmental Mesonet
54
D. Herzmann, Iowa Environmental Mesonet
55
D. Herzmann, Iowa Environmental Mesonet
56
D. Herzmann, Iowa Environmental Mesonet
57
North America Regional Climate Change Assessment
Program
Linda O. Mearns, National Center for Atmospheric
Research Principal Investigator
  • Raymond Arritt, William Gutowski, Gene Takle,
    Iowa State University
  • Erasmo Buono, Richard Jones, Hadley Centre, UK
  • Daniel Caya, OURANOS, Canada
  • Phil Duffy, Lawrence Livermore National
    Laboratories, USA
  • Filippo Giorgi, Jeremy Pal, Abdus Salam ICTP,
    Italy
  • Isaac Held, Ron Stouffer, NOAA Geophysical Fluid
    Dynamics Laboratory, USA
  • René Laprise, Univ. de Québec à Montréal, Canada
  • Ruby Leung, Pacific Northwest National
    Laboratories, USA
  • Linda O. Mearns, Doug Nychka, Phil Rasch, Tom
    Wigley, National Center for Atmospheric Research,
    USA
  • Ana Nunes, John Roads, Scripps Institution of
    Oceanography, USA
  • Steve Sain, Univ. of Colorado at Denver, USA
  • Lisa Sloan, Mark Snyder, Univ. of California at
    Santa Cruz, USA

http//www.narccap.ucar.edu/
58
NOAAs currently funded Regional Integrated
Sciences and Assessments
teams
59
Proposed new Midwest
Consortium for Climate Assessment (MiCCA)
60
(No Transcript)
61
(No Transcript)
62
Tin and Seager
63
Midwest Consortium for Climate Change (MiCCA)
  • Mission
  • To translate NOAA seasonal to inter-annual
    climate forecasts into decision-making tools for
    agriculture and to disseminate these products
    through the state extension services

64
Summary
  • Climate change of the past 35 years is not
    consistent with natural variations over the last
    400,000 years
  • Evidence clearly shows that radiative forcing due
    to anthropogenic greenhouse gases has contributed
    over half of the warming of the last 35 years
  • Mitigation efforts, although urgently needed,
    will have little effect on global warming until
    the latter half of the 21st century
  • Adaptation strategies should be developed
    for the next 50 years
  • Recent trends and model projections
    should be used to develop adaptation
    strategies for the next 10 years

EST personal view
65
For More Information
  • For peer-reviewed evidence supporting everything
    you have seen in this presentation, see my online
    Global Change course
  • http//www.meteor.iastate.edu/gccourse
  • Contact me directly
  • gstakle_at_iastate.edu
  • Current research on regional climate and climate
    change is being conducted at Iowa State Unversity
    under the Regional Climate Modeling Laboratory
  • http//rcmlab.agron.iastate.edu/
  • North American Regional Climate Change Assessment
    Program
  • http//www.narccap.ucar.edu/
  • For this and other climate change presentations
    see my personal website
  • http//www.meteor.iastate.edu/faculty/takle/

Or just Google Eugene Takle
Write a Comment
User Comments (0)
About PowerShow.com