global warming briefing for ksl television lis cohen university of utah [email protected]

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Global Warming Briefing for KSL Television Lis Cohen University of Utah [email protected] www.WeatherOutreach.or

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Page 1: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

Global Warming Briefing for KSL Television

Lis CohenUniversity of [email protected]

Page 2: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

Today’s Topics

• Temperature Trends

• What is Global Warming?– Causes– Uncertainties

• Consequences of Global Warming

• What can people do about this problem?

Page 3: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

Data Sources

• The 2007 IPCC (Intergovernmental Panel on Climate Change) report – Includes

• 2,500 + scientific expert reviewers• 800+ contributing authors• 450+ lead authors from • 130+ different countries• 6 years of work • 4 volumes • 1 report

• Scientific Literature• Presentations from experts at the University of Utah –

Dr. Dave Chapman, Dr. Tim Garrett, Dr. Gerald Mace, Dr. Thomas Reichler

Page 4: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

Temperature Analysis

• “Warming of the climate system is unequivocal, as is now evident from observations of increases in global average air and ocean temperatures, widespread melting of snow and ice, and rising global average sea level” (IPCC report 2007).

Page 5: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu
Page 6: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu
Page 7: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

Contributions to Sea Level Rise

Page 8: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

Long-term Changes in Climate• Long-term changes are observed at:

– Continental Scales– Regional Scales– Ocean basin Scales

• These changes include:– Changes in Arctic temperatures and ice– Widespread changes in precipitation amounts– Ocean salinity– Wind patterns – Aspects of extreme weather

• including droughts• heavy precipitation• heat waves• intensity of tropical cyclones

- 2007 IPCC report

Page 9: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

What can influence the climate?

• Changes in these factors alter the energy balance of the climate system:– The atmospheric abundance of greenhouse

gases and aerosols– Solar radiation– In land surface properties

-2007 IPCC Report

Page 10: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

The Greenhouse Effect

Page 11: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu
Page 12: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

Effects of changing the amounts of Greenhouse Gases

• These changes are expressed in terms of radiative forcing, which is used to compare how a range of human and natural factors drive warming or cooling influences on global climate.

Page 13: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

LOSU = level of understandingRF = Radiative Forcing

Error bars

Additional forcing factors not included here are considered to have a very low level of scientific understand.

Page 14: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

How is the sun affecting climate change?

The effect of the sun’s variations accounts for +.12 W/m2.

There is very high confidence that the globally averaged net effect of human activities since 1750 has been one of warming, with a radiative forcing of +1.6 [+0.6 to +2.4] W/m2.

Natural Climate Variability because of the sun has been not very significant.

Page 15: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

How do we know that this is not a normal cycle?

We use past climate data and compare influencing factors.

Page 16: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

How do we know about past climates?

• Tree Rings – Growth is controlled by temperature, precipitation and sunlight

• Pollens – give a good indication of what was living at the time indicating a temperature range

• Ice and sea bed cores – Gasses in bubbles, dust, isotopes, accumulation rate

• The fossil record • Coral beds

Note: Uncertainties generally increase with time into the past due to increasingly limited spatial coverage.

Page 17: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

Paleoclimate Information

“Paleoclimate information supports the interpretation that the warmth of the last half century is unusual in at least the previous 1300 years.”

“The last time the polar regions were significantly warmer than present for an extended period (about 125,000 years ago), reductions in polar ice volume led to 4 to 6 meters (13-20 feet) of sea level rise.”

-2007 IPCC Report

Page 18: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

What has Changed and what has Not Changed?

Page 19: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

Aspects of climate that have NOT changed

• Day night temperature differences have remained constant. Both the maximum and minimum temperatures have increased at the same rate. The trends are highly variable from one region to another.

• Antarctic sea ice extent continues to show inter-annual variability and localized changes but no statistically significant average trends, consistent with the lack of warming reflected in atmospheric temperatures averaged across the region.

• There is insufficient evidence to determine whether trends exist in– Meridional overturning circulation of the global ocean– Small scale phenomena

• Tornadoes• Hail• Lightning • Dust-storms

Page 20: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

Ward Hunt Ice Shelf, 2002

Consequences of Global Warming

Page 21: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu
Page 22: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

Trend of Less Ice• Many ice bodies

from the poles to the tropics are in retreat.

• Polar warming in 2100 may reach levels of 130,000 years ago, when sea levels were several meters above today.

Larsen B ice shelf, AntarcticaLarsen B ice shelf, Antarcticaca. 100 x 80 milesca. 100 x 80 miles

Mar. 5, 2002Mar. 5, 2002Feb. 17, 2002Feb. 17, 2002

Page 23: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

Muir Inlet, Alaska

National Snow and Ice data centerhttp://nsidc.org/cgi-bin/gpd_run_pairs.pl

20042004

19411941 Glacier Bay National Park and Preserve

Page 24: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

Arctic Polar Ice Cap

• Since 1979, the size of the summer polar ice cap has shrunk more than 20 percent.

• On Sept. 21, 2005, sea ice extent dropped to 2.05 million sq. miles, the lowest extent yet recorded in the satellite record.

• This loss is twice the size of Texas.

1979

http://www.nasa.gov/centers/goddard/news/topstory/2003/1023esuice.html

2003

Page 25: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

NAS

A

Page 26: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

Global Warming

1. Warming is real.

2. Humans are contributing to the warming.

3. Feedback system is complex.

4. Greenhouse gas emissions are growing; residence times are long.

5. Consequences of warming will not be easy for human life.

Page 27: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

How can everyone help?

Vote for politicians that strongly support the environment!

Other ideas…

Page 28: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

Carpool When You CanReduce GarbagePlant a TreeInsulate Your Water HeaterReplace Old AppliancesWeatherize Your HomeUse a Push MowerUnplug Un-Used ElectronicsPut on a SweaterInsulate Your HomeAir Dry Your ClothesSwitch to a Tankless Water HeaterSwitch to Double Pane WindowsBuy Organic FoodBring Cloth Bags to the Market

Use Compact Fluorescent BulbsInflate Your TiresChange Your Air FilterFill the DishwasherUse Recycled Paper Adjust Your ThermostatCheck Your Water heaterChange the AC FilterTake Shorter ShowersInstall a Low-Flow ShowerheadBuy Products LocallyBuy Energy CertificatesBuy Minimally Packaged GoodsBuy a Hybrid Car

Page 29: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

What you at KSL can do!

• Talk to your viewers about climate change and let them know what they can do to help!– There are many events in Salt Lake about climate change (you

can cover them). – Talk with politicians who have worked on the issue. – Interview scientists at the University of Utah (I can help you with

this).

• Get the ball rolling and see what questions and concerns your viewers have and answer them.

• Try to get rid of their misconceptions about climate change.

• Talk to your viewers about climate change (Repeated for emphasis )!

Page 30: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

References

• Climate Change 2007: The Physical Science Basis. Intergovernmental Panel on Climate Change.

• Garrett, T. “Rapid Arctic Climate ChangeForcing the Feedbacks.” 2007.

• Chapman, D. “Global Warming – Just Hot Air?” 2006.

Page 31: Global Warming Briefing for KSL Television Lis Cohen University of Utah liscohen@met.utah.edu

Thank you!

Questions?

Lis Cohen: [email protected]