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CLIMATE CHANGE
FAQs
Chris Swanston, cswanston@fs.fed.us
Director, Northern Institute of Applied Climate Science
Director, USDA Northern Forests Climate Hub
Isn’t there still a scientific
debate about climate change?
(So you believe…; Who am I supposed to believe...)
2
Debate?
Intergovernmental Panel on Climate Change (2007, 2010, 2013)
 Evidence for climate change is “unequivocal”
 It is “extremely likely” that humans are main cause since 1950
• “Human influence on the climate system is clear.”
 Future changes depend partly on human actions
18 National Academies have endorsed the consensus position of
the IPCC on climate change
 National Academy of Sciences (USA)
 Royal Society of Canada
3
Debate?
Doran et al. 2009, Anderegg et al. 2010, Cook et al. 2013
4
Doran et al. 2009, Anderegg et al. 2010, Cook et al. 2013
Debate? 5
Is there still a debate?
 No scientific debate on “if”.
 Current scientific debate revolves around how
much, how fast, and feedback mechanisms.
 Virtually all climate scientists agree humans are a
driver.
A practical risk assessment may be a better strategy
than belief.
6
Is it climate change or
global warming?
7
Climate change or global warming?
The average global surface temperature has risen 1.53°F over
the past 100 years
IPCC 2007, 2013
8
NCA 2014
Climate change or global warming?
Contiguous US: 1991-2012 departure from 1901-1960 average
9
Climate change or global warming?
NCA 2014
Contiguous US: 1991-2011 departure from 1901-1960 average
10
Climate change or global warming?
NCA 2014
11
Is it climate change or global warming?
• About 1.5F warming globally.
• US warming similar, with regional variation.
• General increases in US annual precipitation,
except in the southwest.
• More big rain events, more of annual precip within
those events.
Both. The earth has warmed and the climate is
changing as a result, with regional variations.
12
Didn’t climate change stop
about 15 years ago?
(What about the pause?)
13
Are we done yet?
Recent years - La Niña, lower solar activity, volcanic cooling,
and sulfate aerosols have reduced the rate of warming in
surface air…
NASA Goddard Institute for Space Studies: http://data.giss.nasa.gov/gistemp/graphs_v3/; see also , Schmidt et al. 2014; Saffioti et al. 2015;
Lewandowsky et al. 2015
14
Are we done yet?
…but not in oceans – which account for ~93% of earth system
warming since 1955.
Levitus et al. 2012, Balmeseda et al. 2013; see also Guemas et al. 2013
15
Courtesy of www.skepticalscience.com (calculated from IPCC AR4 5.2.2.3)
Are we done yet?
16
Figures courtesy of NOAA.
Has El Niño increased global warming?
Nope. Heat was transferred from ocean to surface air.
BONUS: EL NIÑO! 17
Didn’t climate change stop?
• The rate of surface air warming slowed recently.
• Oceans continued to absorb heat rapidly.
• The oceans have absorbed >90% of warming since
1955.
No – the earth is still warming.
18
The atmosphere is
massive – how can we
actually change it?
19
Anthropogenic change?
Net sources
and sinks
20
Anthropogenic change?
21
The atmosphere is massive, how can we
change it?
• We move massive amounts of carbon into the
atmosphere.
• Fossil carbon is an addition – it has been isolated
from the carbon cycle for millions of years.
• GHGs have different atmospheric lifetimes – CO2
may last decades to centuries.
• Land cover change transfers carbon to the
atmosphere.
The measurement record clearly shows our
additions to the atmosphere.
22
Hasn’t climate always
changed? Why worry now?
23
graph data from the NOAA NCDC and Mauna Loa Observatory
Milankovitch Cycles
Eccentricity – more or less oval orbit, every ~100,000 years
Tilt – earth shifts its tilt every ~41,000 years
Precession – earth wobbles on its axis, every ~23,000 years
Change happens.
24
Courtesy of K. Marcinkowski, NIACS;
see also: Hansen et al. 1990, Petit et al. 1999, Shackleton 2000, Ruddiman 2006, Shakun et al. 2012
Change happens.
25
IPCC 2007
Change happens.
26
http://www.globalwarmingart.com
• The sun and earth emit energy in different wavelengths.
• Shorter wavelengths (sun) move through the atmosphere more
easily.
BONUS: GREENHOUSE EFFECT! 27
http://www.globalwarmingart.comHarries et al. 2001
• More absorption
and scattering for
outgoing energy
• Water vapor is
important
• CO2 absorbs only
outgoing energy
• Impact of CO2
greatest in situations
with less water
vapor (dry, cold)
• Less heat escaping
overall.
BONUS: GREENHOUSE EFFECT! 28
-0.4 °F
Average
Surface
Temperature
Temperature
without
greenhouse
effect
+57 °F
Others ~15%
CO2 9-26%
H2O 36-66%
Kiehl and Trenberth 1997,
realclimate.org (G. Schmidt, NASA)
Change happens.
29
Hasn’t the climate always changed? Why
worry now?
• Milankovitch cycles have previously driven climate
changes.
• Humans are driving the current change.
• The change is very rapid.
The rapidity and potential severity of climate change
will affect forestry, agriculture, infrastructure,
demographics, economies, …virtually everything.
30
Isn’t future climate
change uncertain?
(I don’t trust climate models!)
31
Uncertainty?
IPCC 2007
32
Uncertainty?
Emissions Model sensitivity
IPCC 2007
33
Tamino, 2010 (blog: http://tamino.wordpress.com/ )
From IPCC AR4: 22 models, 106 runs
*Omits Canadian CCCMA
Uncertainty?
34
NCA 2014
Uncertainty?
35
A2A1BB1
Change in Mean Monthly Temperature (°C)
2070-2099 vs 1961-1990
Future Emissions Higher
CSIRO
MIROC
HAD
Higher
ModelSensitivity
Uncertainty?
36
Simple representation of uncertainty:
Least
Projected
Change
Most
Projected
Change
Insensitive model
Low emissions (B1)
Uncertainty?
Sensitive model
High emissions (A2)
37
Simple representation of uncertainty:
Least
Projected
Change
Most
Projected
Change
Uncertainty?
38
Isn’t future climate change uncertain?
• Models have acknowledged shortcomings.
• They do well globally with air temps, much less well
with precip, and will likely never be “good enough”
at a management scale.
• Great at multi-decadal trends, poor at multi-year.
• Emissions uncertainties are inherent.
All models are wrong, some are useful – best to use
multiple models, think long term, and consider a range
of futures.
39
Summary
Climate
• overwhelming evidence for change, from thousands
of sources
Uncertainty
• it’s inherent in climate projections, and this will not
change
• we’ll always have a range of plausible futures
Questions
• Questions are good. Keep asking.
Chris Swanston
cswanston@fs.fed.us
40

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Swanston - Climate change Frequently Asked Questions

  • 1. CLIMATE CHANGE FAQs Chris Swanston, cswanston@fs.fed.us Director, Northern Institute of Applied Climate Science Director, USDA Northern Forests Climate Hub
  • 2. Isn’t there still a scientific debate about climate change? (So you believe…; Who am I supposed to believe...) 2
  • 3. Debate? Intergovernmental Panel on Climate Change (2007, 2010, 2013)  Evidence for climate change is “unequivocal”  It is “extremely likely” that humans are main cause since 1950 • “Human influence on the climate system is clear.”  Future changes depend partly on human actions 18 National Academies have endorsed the consensus position of the IPCC on climate change  National Academy of Sciences (USA)  Royal Society of Canada 3
  • 4. Debate? Doran et al. 2009, Anderegg et al. 2010, Cook et al. 2013 4
  • 5. Doran et al. 2009, Anderegg et al. 2010, Cook et al. 2013 Debate? 5
  • 6. Is there still a debate?  No scientific debate on “if”.  Current scientific debate revolves around how much, how fast, and feedback mechanisms.  Virtually all climate scientists agree humans are a driver. A practical risk assessment may be a better strategy than belief. 6
  • 7. Is it climate change or global warming? 7
  • 8. Climate change or global warming? The average global surface temperature has risen 1.53°F over the past 100 years IPCC 2007, 2013 8
  • 9. NCA 2014 Climate change or global warming? Contiguous US: 1991-2012 departure from 1901-1960 average 9
  • 10. Climate change or global warming? NCA 2014 Contiguous US: 1991-2011 departure from 1901-1960 average 10
  • 11. Climate change or global warming? NCA 2014 11
  • 12. Is it climate change or global warming? • About 1.5F warming globally. • US warming similar, with regional variation. • General increases in US annual precipitation, except in the southwest. • More big rain events, more of annual precip within those events. Both. The earth has warmed and the climate is changing as a result, with regional variations. 12
  • 13. Didn’t climate change stop about 15 years ago? (What about the pause?) 13
  • 14. Are we done yet? Recent years - La Niña, lower solar activity, volcanic cooling, and sulfate aerosols have reduced the rate of warming in surface air… NASA Goddard Institute for Space Studies: http://data.giss.nasa.gov/gistemp/graphs_v3/; see also , Schmidt et al. 2014; Saffioti et al. 2015; Lewandowsky et al. 2015 14
  • 15. Are we done yet? …but not in oceans – which account for ~93% of earth system warming since 1955. Levitus et al. 2012, Balmeseda et al. 2013; see also Guemas et al. 2013 15
  • 16. Courtesy of www.skepticalscience.com (calculated from IPCC AR4 5.2.2.3) Are we done yet? 16
  • 17. Figures courtesy of NOAA. Has El Niño increased global warming? Nope. Heat was transferred from ocean to surface air. BONUS: EL NIÑO! 17
  • 18. Didn’t climate change stop? • The rate of surface air warming slowed recently. • Oceans continued to absorb heat rapidly. • The oceans have absorbed >90% of warming since 1955. No – the earth is still warming. 18
  • 19. The atmosphere is massive – how can we actually change it? 19
  • 22. The atmosphere is massive, how can we change it? • We move massive amounts of carbon into the atmosphere. • Fossil carbon is an addition – it has been isolated from the carbon cycle for millions of years. • GHGs have different atmospheric lifetimes – CO2 may last decades to centuries. • Land cover change transfers carbon to the atmosphere. The measurement record clearly shows our additions to the atmosphere. 22
  • 23. Hasn’t climate always changed? Why worry now? 23
  • 24. graph data from the NOAA NCDC and Mauna Loa Observatory Milankovitch Cycles Eccentricity – more or less oval orbit, every ~100,000 years Tilt – earth shifts its tilt every ~41,000 years Precession – earth wobbles on its axis, every ~23,000 years Change happens. 24
  • 25. Courtesy of K. Marcinkowski, NIACS; see also: Hansen et al. 1990, Petit et al. 1999, Shackleton 2000, Ruddiman 2006, Shakun et al. 2012 Change happens. 25
  • 27. http://www.globalwarmingart.com • The sun and earth emit energy in different wavelengths. • Shorter wavelengths (sun) move through the atmosphere more easily. BONUS: GREENHOUSE EFFECT! 27
  • 28. http://www.globalwarmingart.comHarries et al. 2001 • More absorption and scattering for outgoing energy • Water vapor is important • CO2 absorbs only outgoing energy • Impact of CO2 greatest in situations with less water vapor (dry, cold) • Less heat escaping overall. BONUS: GREENHOUSE EFFECT! 28
  • 29. -0.4 °F Average Surface Temperature Temperature without greenhouse effect +57 °F Others ~15% CO2 9-26% H2O 36-66% Kiehl and Trenberth 1997, realclimate.org (G. Schmidt, NASA) Change happens. 29
  • 30. Hasn’t the climate always changed? Why worry now? • Milankovitch cycles have previously driven climate changes. • Humans are driving the current change. • The change is very rapid. The rapidity and potential severity of climate change will affect forestry, agriculture, infrastructure, demographics, economies, …virtually everything. 30
  • 31. Isn’t future climate change uncertain? (I don’t trust climate models!) 31
  • 34. Tamino, 2010 (blog: http://tamino.wordpress.com/ ) From IPCC AR4: 22 models, 106 runs *Omits Canadian CCCMA Uncertainty? 34
  • 36. A2A1BB1 Change in Mean Monthly Temperature (°C) 2070-2099 vs 1961-1990 Future Emissions Higher CSIRO MIROC HAD Higher ModelSensitivity Uncertainty? 36
  • 37. Simple representation of uncertainty: Least Projected Change Most Projected Change Insensitive model Low emissions (B1) Uncertainty? Sensitive model High emissions (A2) 37
  • 38. Simple representation of uncertainty: Least Projected Change Most Projected Change Uncertainty? 38
  • 39. Isn’t future climate change uncertain? • Models have acknowledged shortcomings. • They do well globally with air temps, much less well with precip, and will likely never be “good enough” at a management scale. • Great at multi-decadal trends, poor at multi-year. • Emissions uncertainties are inherent. All models are wrong, some are useful – best to use multiple models, think long term, and consider a range of futures. 39
  • 40. Summary Climate • overwhelming evidence for change, from thousands of sources Uncertainty • it’s inherent in climate projections, and this will not change • we’ll always have a range of plausible futures Questions • Questions are good. Keep asking. Chris Swanston cswanston@fs.fed.us 40