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TRANSCRIPT
Five Things Everyone Should Know About Climate Change
David KaroweDepartment of Biological Sciences
Western Michigan University
The source of information on a slide is indicated by a superscripted number, which refers to a specific citation
in the three slides at the end of the presentation
Tem
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(o C)
13 warmest years in history: 2002-2013, 1998*
Warming is 10-20 times faster than in at least the last 800,000 years
Since 1900, Earth has warmed ~ 0.8o C
1. Climate change is real, and humans are causing it.
http://data.giss.nasa.gov/gistemp/graphs/
Temperature difference relative to 1950-1980
http://data.giss.nasa.gov/gistemp/animations/
- severe rainstorms have become more common
43% increase in Ohio since 19481
Precipitation is a very important component of climate
1950-1959
At the same time, much of the world has been experiencing more frequent and stronger droughts2
Palmer Drought Severity Index (PDSI)
mild
dro
ught
extr
eme
seve
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mod
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exce
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2000-2009
At the same time, much of the world has been experiencing more frequent and stronger droughts2
Palmer Drought Severity Index (PDSI)
mild
dro
ught
extr
eme
seve
re
mod
erat
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exce
ptio
nal
Climate predictions are coming true in the U.S.
In 2011, Ohio had its wettest spring on record
http://www.ncdc.noaa.gov/temp-and-precip/maps
As a result, much of Ohio experienced extensive flooding
2012 was the warmest year on record for the U.S.
http://www.ncdc.noaa.gov/cag/
September 2, 201447% Drought (4% Exceptional)
Since 2011, much of the U.S. has been in severe drought
http://droughtmonitor.unl.edu/MapsAndData/MapArchive.aspx
January 2014 Temperatures
This winter, most of the world was not like the Midwest
http://www.ncdc.noaa.gov/sotc/global/2014/1
Three lines of evidence against a meaningful contribution of “natural variation” to current warming
Since 1900, most of the heat added to Earth’s climate is from greenhouse gasses (GHG)3
GHG added ~ 2.98 W/m2
the sun added ~ 0.12 W/m2
Temperature
Solar Irradiance
Temperature data: http://data.giss.nasa.gov/gistemp/tabledata_v3/GLB.Ts+dSST.txtSolar irradiance data: http://www.mps.mpg.de/projects/sun‐climate/data/tsi_1611.txt,
http://www.pmodwrc.ch/pmod.php?topic=tsi/composite/SolarConstantGraph: http://www.skepticalscience.com/solar‐activity‐sunspots‐global‐warming.htm
Recently, while Earth has been warming fastest, solar irradiance has been decreasing4
natural factors only
Models do a good job of replicating past climate change only if they include anthropogenic factors5
- natural factors (the sun and volcanoes) would have caused a slight cooling since 1900
anthropogenic and natural factors
observedmodeledobserved
modeled
Best estimate: ≥ 95% of current warming is due to human activities
In two major ways, current warming is very different than any warming period
in at least the last 800,000 years
1. It’s at least 10 times faster
2. It’s happening while solar input is decreasing
Are Americans aware of the cause?6
“We’re causing it”
“It’s natural”
Is there any debate among scientists about whether humans are the primary cause of global warming?
“Most of the global warming in recent decades can be attributed to human activities."
Scientific organizations endorsing this statement7: United States:National Academy of SciencesAmerican Medical AssociationAmerican Association for the Advancement of ScienceAmerican Meteorological SocietyAmerican Institute of Biological SciencesAmerican Chemical SocietyAmerican Geophysical UnionAmerican Institute of Physics
Geological Society of AmericaAmerican Academy of PaediatricsAmerican College of Preventive MedicineAmerican Public Health AssociationNational Oceanic and Atmospheric Administration National Aeronautics and Space Administration Environmental Protection Agency National Center for Atmospheric ResearchUniversity Corporation for Atmospheric ResearchEcological Society of AmericaAmerican Society of AgronomyAmerican Society of Plant BiologistsAssociation of Ecosystem Research CentersBotanical Society of AmericaCrop Science Society of AmericaNatural Science Collections Alliance
American Statistical AssociationOrganization of Biological Field StationsAmerican Physical SocietySociety for Industrial and Applied MathematicsSociety of Systematic BiologistsSoil Science Society of AmericaFederation of American ScientistsNational Research CouncilNational Association of Geoscience TeachersAmerican Quaternary AssociationAmerican Association of Wildlife VeterinariansAmerican Society for MicrobiologySociety of American ForestersAmerican Astronomical Society
Europe:European Academy of Sciences and ArtsEuropean Science FoundationEuropean Geosciences UnionEuropean Physical SocietyEuropean Federation of GeologistsRoyal Society of the United KingdomAcademie des Sciences (France)Deutsche Akademie der Naturforscher (Germany)Accademia dei Lincei (Italy)Royal Irish AcademyRoyal Swedish Academy of SciencesRoyal Academy of Belgium for Sciences and the ArtsRoyal Meteorological SocietyBritish Antarctic SurveyUnited Kingdom Institute of Biology
Other countries (≥ 35):Chinese Academy of SciencesScience Council of JapanRussian Academy of SciencesIndian National Science AcademyRoyal Society of New ZealandAustralian Academy of SciencesAustralian Medical AssociationPolish Academy of SciencesAcademia Brasiliera de Ciencias (Brazil)Royal Society of CanadaAfrican Academy of SciencesCaribbean Academy of SciencesAcademy of Sciences of MalaysiaIndonesian Academy of SciencesAcademy of Science of South Africa
Scientific organizations holding a dissenting opinion:
American Institute of Petroleum Geologists
Until 2007:
Since 2008:none
Are Americans aware of the strength of the scientific consensus6?
“Scientists agree”
“Scientists don’t agree”
In fact, 97.5% of climate scientists agree
What does the future hold?
It depends on our choices
“No fate but what we make”
2o
4o
Depending on choices we make, Earth is likely to warm by
2-5o Cby 21008
“Business as usual”
Alternate energy sources
Actual
2. If we remain on our current course, future climate change will be severe.
5o
Will a 5o temperature rise matter?When Earth was 5o cooler:
http://www.scotese.com/lastice.htm
Warming is likely to cause sea level rise of 1-2 meters by 2100
- up to 300 million people could be flooded each year9
Much of U.S. would be affected by 1 meter rise10
Much of Florida would also be under water
So would much of the east coast
Climate change will also include altered precipitation patterns11
Summer Precipitation
Summer rainfall is predicted to decrease throughout U.S.12
Most summers are likely to be hotter than any experienced thus far13
2060-2069
Palmer Drought Severity Index (PDSI)
mild
dro
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extr
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Much of the world is likely to experience much more frequent and stronger droughts by the 2060s2
What will this mean for Earth’s species?It depends on the choices we make
3. If we remain on our current course, there will be serious adverse consequences for most species.
With 2o warming: 2,100 of 5,200 African plant species (40%) are predicted to go extinct14
3. If we remain on our current course, there will be serious adverse consequences for most species.
With 2o warming: 2,100 of 5,200 African plant species (40%) are predicted to go extinct
African mammals are likely to be adversely affected
With 3.5o warming: 55 of 275 species (20%) are predicted to go extinct15
Even if suitable future habitat exists, species may not be able to get there in time to avoid extinction
This is the worst time in Earth’s history for climate change
Which species are particularly vulnerable?
1. Species that have nowhere to go2. Species that live in coral reefs 3. Species that live on land in the tropics
High latitude species have nowhere to go
Most, but not all, polar bear populationsare predicted to decline dramatically by 205016
All decline or disappearby 2100
Alaska
Red = decliningBlue = increasing
All ice-obligate species are highly vulnerable
In Antarctica, Emperor and Adelie penguins need ice
but Chinstrap and Gentoo penguins nest on land
High altitude species may also have nowhere to go
All of Earth’s 1,009 montane bird species are predicted to be “climate losers”17
Coral reef species are also particularly vulnerable
because both warming and ocean acidification can cause bleaching
Even 2o warming is likely to cause a massive increase in bleaching events18,19
Acidification alone may make most or all of the ocean unsuitable for corals20
- 650 ppm CO2 may cause near total loss of coral reefs
Low Moderate High
Probability of disappearing climate
Tropical species have narrow temperature ranges, so are very likely to experience “disappearing climates”21
Therefore, tropical species are particularly vulnerable
Where do most species live?
What will happen to plants and animals in Ohio?
American beechWhite ash
10 of the 20 most abundant Ohio tree species are predicted to decline by at least 50%22-24
Sugar mapleBigtooth aspen
Black cherry
-91%
-89% -79% -78%
-100%White pine-100%
Three of the 20 most abundant Ohio tree species are predicted to increase22-24
+150-fold+112%Post oakBlack oakBlack gum
+14%
Several rare tree species are predicted to increase dramatically in Ohio22-24
Sweetgum+43-fold
- and many southern species are predicted to arrive
Shortleaf pine+104-fold
Winged elm+6-fold
Today
2o warming
Ohio forests are predicted to change fairly dramatically22-24
4o warming
But forests are more than just trees
36 Ohio bird species are predicted to decline by >90%25-26
Cedar Waxwing
-96%
Bobolink
-99%
Bank Swallow
-99%
Veery
-99%
House Wren
-99%
Savannah Sparrow
-100%
Willow Flycatcher
-98%Tree Swallow
-98%
Another 19 species are predicted to decline by 50-90%25-26
Rose-breasted Grosbeak
-69%
song sparrow
-89%
Yellow Warbler
-88%
American Redstart
-81%
Cerulean Warbler
-74%
Ovenbird
-56%
American Goldfinch
-53%
Blue-winged Warbler
-82%
32 species are predicted to increase by >50%
Loggerhead Shrike*
Pine Warbler*
Yellow-billed Cuckoo
+77%
+660-fold
+58%Summer Tanager
+5-fold
Chuck-will’s Widow*
Black Vulture*
Carolina Wren
+113-fold +104-fold +7-fold
Northern Bobwhite
+103%
10 new species are predicted to occur in Ohio25-26
Brown-headed Nuthatch
Snowy EgretLittle Blue Heron
Cattle Egret
Scissor-tailed Flycatcher
Bachman’s Sparrow
Mississippi Kite
Painted Bunting
4. If we remain on our current course, there will beserious adverse consequences for human health.
1. Increased heat stress
2. Increased disease
3. Increased malnutrition
4. Change in air quality
5. Change in frequency and/or severity of conflict
Major ways in which climate change is likely to affect human health:
and decreased cold stress
Record hot summers are likely to result in dramatic increases in heat stress13
Chicago 1995-like heat waves per decade
2o C 4o C
For many cities, the number of Chicago 1995-like heat waves (~700 deaths) will increase dramatically28,29
Climate change is likely to increase vector-borne diseases
Malaria: World Health Organization estimates 250,000,000 cases and 1,000,000 deaths annually
- every 30 seconds a child dies from malaria30
+ 2o C
Malaria is generally predicted to increase, but change depends on climate scenario31
+ 4o C
With 2-4o warming:
200-400 million more people at risk worldwide by 208032
About 450 million of the world’s poorest people depend entirely on agriculture
- grains provide ~ 2/3 of the total human protein intake
1950-19592000-20092060-2069
Palmer Drought Severity Index (PDSI)
Much more frequent and stronger droughts will decrease crop yields substantially
Future U.S. corn and soybean yields are likely to decrease dramatically33
20-25% decrease by 2050
55-60% decrease by 2100
Coal-fired power plants kill people34
Climate change is predicted to increase civil wars in sub-Saharan Africa by 50% in the next 20 years35
Most worrisome scenario: India and Pakistan start a “water war”36
- Indus supplies83% of Pakistan’sirrigationwater
Climate change is a major U.S. national security threat
“The effects of climate change in the world’s most vulnerable regions present a serious threat toAmerican national security interests. Washingtonmust lead on this issue now.”37
Partnership for a Secure America, February 2013
Developed countries are causing the problem, but developing countries suffer most of the effects38
Countries proportional to CO2 emissions through 2002:
Countries proportional to climate-related health effects:
What can I do to minimize climate change?
5. We don’t have to remain on our current course. We can change the future by implementing
multiple solutions that already are available.
Stop deforestation: great idea, but not a solution
Unfortunately, energy conservation is not a solution
- really just delays the outcome
This can only happen through aggressive expansion of alternate energy sources
Solar Wind
To limit warming to 2o C, we need to reduce greenhouse gas emissions by 80% by 2050
Globally, we generate only 0.2% of our energy from wind,and only 0.1% from solar39
23x
183x
18x3x8x
8x3x
30x183x
Global wind potential is >40 times worldwide use40
All 9 highest CO2-emitting countries could use wind alone
e.g. Luddington pumped storage plant
The “intermittency problem” can be solved easily
Solar energy has even greater potential Three main technologies:
photovoltaicssolar thermal parabolic trough
Global potential estimated at up to 100 times total current use41,42
A small portion of the Sahara desert could supply all of the world’s electricity43
A solar array 100 x 100 miles could provide all of US energy needs today44
Again, “intermittency problem” can be solved easily
- store excess heat during day, generate electricity at night
solar thermal parabolic trough
Educate others
Encourage policymakers to make smarter choices
What would we gain by switching to green energy?
Higher Emissions Lower Emissions
3.5o Warming
Low Moderate High
Probability of disappearing climate
Switching to green energy sources would improve the fate of most species on Earth
2o Warming
Bottom Line:
1. We’re causing climate to change at an alarming rate.
2. If we continue on our current path, the future is very likely to include unprecedented hardships for all of Earth’s species, includinghumans.
3. We can change our path by using smarter choices we have available today.
Sources of information used in this talk1. Madsen, T. and E. Figdor. 2007. When it rains, it pours: Global warming and the rising frequency of extreme
precipitation in the United States. Environment Rhode Island Research and Policy Center. www.environmentrhodeisland.org.
2. Dai, A. 2011. Drought under global warming: a review. Wiley Interdisciplinary Reviews: Climate Change 2: 45-65. 3. IPCC (Intergovernmental Panel on Climate Change). 2007. Fourth Assessment Report, Chapter 2, Changes in
Atmospheric Constituents and Radiative Forcing, Section 2.9.2. http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch2s2-9-2.html
4. Lockwood, M. and C. Froehlich. 2008. Recent oppositely directed trends in solar climate forcings and the global mean surface air temperature. II. Different reconstructions of the total solar irradiance variation and dependence on response time scale. Proc. Roy. Soc. A 464: 1367-1385.
5. IPCC. 2007. Fourth Assessment Report, Working Group I, Chapter 9, Understanding and Attributing Climate Change, Section 9.4.1.2. http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch9s9-4-1-2.html
6. Leiserowitz, A., Maibach, E., Roser-Renouf, C., Feinberg, G., & Howe, P. (2014) Climate change in the American mind: Americans’ global warming beliefs and attitudes in April, 2014. Yale University and George Mason University. New Haven, CT: Yale Project on Climate Change Communication.
7. http://climate.nasa.gov/scientific-consensus; Cook et al. 2013. Quantifying the consensus on anthropogenic global warming in the scientific literature. Environmental Research Letters 8 024024 doi:10.1088/1748-9326/8/2/024024
8. IPCC AR4 WG1. 2007. Chapter 10: Global Climate Projections, G. A. Meehl and T. F. Stocker, Co-ordinating Lead Authors.
9. Stern, Nicholas. 2006. Stern Review: The Economics of Climate Change. Chapter 3: How Climate Change Will Affect People Around The World. Cambridge University Press, Cambridge.
10. Weiss, A. and J. Overpeck. 2003. Climate Change and Sea Level. Environmental Studies Laboratory, Department of Geosciences, The University of Arizona. www.geo.arizona.edu/dgesl/research/other/climate_change_and_sea_level/sea_level_rise/sea_level_rise.htm
11. IPCC. 2007. Fourth Assessment Report, Working Group I, Chapter 10, Global Climate Projections, Section 10.3. http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch10s10-3.html
12. Walsh, J. and D. Wuebbles (Convening Lead Authors). 2013. National Climate Assessment Draft Report. Chapter 2: Our Changing Climate. http://ncadac.globalchange.gov/download/NCAJan11-2013-publicreviewdraft-chap2-climate.pdf
13. Battisti, D. and R. Naylor. 2009. Historical warnings of future food insecurity with unprecedented seasonal heat. Science 323: 240-244
14. McClean, C.J., J. Lovett, W. Kuper, L. Hannah, J. Sommer, W. Barthlott, M. Termansen,G. Smith, S. Tokumine, and J. Taplin. 2005. African plant diversity and climate change. Ann. Missouri Bot. Gard. 92:139-152.
15. Thuiller, W. et al. 2006. Vulnerability of African mammals to anthropogenic climate change under conservative land transformation assumptions. Global Climate Biology 12: 424-440.
Sources of information cited in this talk (cont.)16. Durner, G. et al. 2009. Predicting 21st-century polar bear habitat distribution from global climate models. Ecological
Monographs 79: 25-58.17. LaSorte, F. and W. Jetz. 2010. Projected range contractions of montane biodiversity under global warming. Proc.
R. Soc. B 277: 3401-3410.18. Donner, S.D. 2009. Coping with commitment: Projected thermal stress on coral reefs under different future
scenarios. PLoS ONE 4(6): e5712.19. Burke, L., K. Raytar, M. Spalding, and A. Perry. 2011. Reefs at Risk Revisited. World Resources Institute,
Washington D.C.20. Hoegh-Guldberg, O. et al. 2007. Coral reefs under rapid climate change and ocean acidification.” Science 318: 1737–
1742. 21. Williams, J., S. Jackson, and J. Kutzbach. 2007. Projected distributions of novel and disappearing climates by 2100
AD. Procedings of the National Academy of Sciences 104: 5738-5742. 22. Prasad, A. M., L. R. Iverson., S. Matthews., M. Peters. 2007-ongoing. A Climate Change Atlas for 134 Forest Tree
Species of the Eastern United States [database]. Northern Research Station, USDA Forest Service, Delaware, Ohio. http://www.nrs.fs.fed.us/atlas/tree/tree_atlas.html
23. Prasad, A. M., L. R. Iverson., S. Matthews., M. Peters. 2007-ongoing. http://www.nrs.fs.fed.us/atlas/tree/ft_summary.html
24. Iverson, L. R., A. M. Prasad, S. N. Matthews, and M. Peters. 2008. Estimating potential habitat for 134 eastern US tree species under six climate scenarios. Forest Ecology and Management. 254:390-406. http://www.treesearch.fs.fed.us/pubs/13412
25. Matthews, S.N., L. R. Iverson, A.M. Prasad, A. M., and M.P. Peters. 2007-ongoing. A Climate Change Atlas for 147 Bird Species of the Eastern United States [database]. http://www.nrs.fs.fed.us/atlas/bird, Northern Research Station, USDA Forest Service, Delaware, Ohio.
26. Matthews, S. N., Iverson, L. R., Prasad, A. M. and Peters, M. P. 2011. Changes in potential habitat of 147 North American breeding bird species in response to redistribution of trees and climate following predicted climate change. Ecography, 34: no. doi: 10.1111/j.1600-0587.2010.06803.x Published online: http://onlinelibrary.wiley.com/doi/10.1111/j.1600-0587.2010.06803.x/full
27. Patz, J., D. Campbell-Lendrum, T. Holloway and J. Foley. 2005. Impact of regional climate change on human health. Nature 438: 310-317.
28. Hayhoe, K., S. Sheridan, L. Kalkstein, and J. S. Greene. Climate change, heat waves, and mortality projections for Chicago. Journal of Great Lakes Research 36, no. Supplement 2 (2010): 65-73.
29. Hayhoe, K., J. VanDorn, N. Vaishali, and K. Wuebbles. Midwest: Projections of future temperature and precipitation.Cambridge, MA. Union of Concerned Scientists. http://www.ucsusa.org/assets/documents/global_warming/midwest-climate-impacts.pdf
Sources of information cited in this talk (cont.)
30. World Health Organization. 2012. World Malaria Report 2012. http://www.who.int/malaria/publications/world_malaria_report_2012/report/en/index.html
31. Tonnang, H., R. Kangalawe, and P. Yanda. 2010. Predicting and mapping malaria under climate change scenarios: the potential redistribution of malaria vectors in Africa. Malaria Journal 9:111.
32. van Lieshout, M., R.S. Kovats, M.T. Livermore, and P. Martens. 2004. Climate change and malaria: analysis of the SRES climate and socio-economic scenarios. Global Environmental Change 14: 87–99.
33. Schlenker, W. and M. Roberts. 2009. Nonlinear temperature effects indicate severe damages to U.S. crop yields under climate change. Proceedings of the National Academy of Sciences 106: 15594-15598.
34. Schneider, C. and J. Banks. 2010. The Toll From Coal. Clean Air Task Force, Boston, MA.35. Burke, M., E. Miguelc, S. Satyanathd, J. Dykemae, and D. Lobell. 2009. Warming increases the risk of civil war in
Africa. Proceedings of the National Academy of Sciences 106: 20670–20674. 36. Center for Naval Analysis. 2007. National Security and the Threat of Climate Change. 37. Partnership for a Secure America. 2013. The Cost of Inaction.
http://www.psaonline.org/downloads/PSAClimateChange_NationalSecurity%20Handout.pdf38. Costello, A. et al. 2009. Managing the health effects of climate change. The Lancet 373 (9676): 1693-1733.39. IPCC. 2011. Summary for Policymakers. In: IPCC Special Report on Renewable Energy Sources and Climate Change
Mitigation. O. Edenhofer, R. Pichs-Madruga, Y. Sokona, K. Seyboth, P. Matschoss, S. Kadner, T. Zwickel, P. Eickemeier, G. Hansen, S. Schlomer, and C. von Stechow (eds), Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA.
40. Lu, X., M. McElroy and J. Kiviluoma. 2009. Global potential for wind-generated electricity. Proceedings of the National Academy of Sciences 106: 10933-10938.
41. Arvizu, D., P. Balaya, L. Cabeza, T. Hollands, A. Jager-Waldau, M. Kondo, C. Konseibo, V. Meleshko, W. Stein, Y. Tamaura, H. Xu, and R. Zilles. 2011. Direct Solar Energy. Chapter 3 in IPCC Special Report on Renewable EnergySources and Climate Change Mitigation [O. Edenhofer, R. Pichs-Madruga, Y. Sokona, K. Seyboth, P. Matschoss, S.Kadner, T. Zwickel, P. Eickemeier, G. Hansen, S. Schlomer, C. von Stechow (eds)], Cambridge University Press,Cambridge, United Kingdom and New York, NY, USA.
42. National Academy of Sciences of the United States. 2010. Climate Stabilization Targets: Emissions, Concentrations, and Impacts over Decades to Millenia. http://dels.nas.edu/resources/static-assets/materials-based-on-reports/reports-in-brief/Stabilization-Targets-Final.pdf
43. Trans-Mediterranean Interconnection for Concentrating Solar Power Final Report. German Aerospace Center (DLR), Institute of Technical Thermodynamics, Section Systems Analysis and Technology Assessment.
44. America's Solar Energy Potential. http://www.americanenergyindependence.com/solarenergy.aspx.
The next few slides were not part of the lecture, but have information about personal behaviors that
can help you reduce your carbon footprint.
1. Next time, buy a more fuel-efficient car
20 mpg 30 mpg
50 mpg34 mpg
How can I conserve energy?
Increasing by 10 mpg saves $585 and 1.6 tons of CO2 per year
2. Weatherize your home
weather-strip
insulate attic
single-pane windows → triple-pane windows
Would reduce U.S. CO2 emissions by 23 million tons/year
3. Next time, buy energy star appliances
Would reduce U.S. CO2 emissions by 15 million tons/year
4. When necessary, replace older furnace and central air conditioning unit with Energy Star model
Would reduce U.S. CO2 emissions by 14 million tons/year
5. Change to compact fluorescent light bulbs
One per household would have the same effect as taking 6 million cars off the road
- can save 7 tons of CO2 per year for a family of four
6. Turn the thermostat down (winter) or up (summer)
One GreenBlock costs $1.50/month and is equal
to driving 3,300 fewer miles
7. Offset what you can’t (or don’t want to) reduce
To offset all of my driving costs me $22/year
Can visit www.care2.com/click-to-donate/ daily to offset computer use