climate change101 esip_2011

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Climate Change 101 Margaret Mooney Cooperative Institute for Meteorological Satellite Studies University of Wisconsin-Madison

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Climate Change 101, Margaret Mooney, at the ESIP Summer Meeting 2011, Santa Fe NM

TRANSCRIPT

Page 1: Climate change101 esip_2011

Climate Change 101

Margaret Mooney

Cooperative Institute for Meteorological Satellite Studies

University of Wisconsin-Madison

Page 2: Climate change101 esip_2011

Weather is the condition of the atmosphere at a particular location and moment. Each day current weather conditions are given in local weather reports.

Climate is the collective state of the atmosphere for a given place over a specified interval of time. There are three parts to this definition …

“Climate is what you expect, weather is what you get”

Differences between Weather & Climate

Page 3: Climate change101 esip_2011

Climate is the collective state of the atmosphere for a given place over a specified interval of time. There are three parts to this definition:

1. Location because climate can be defined for a globe, a continent, a region, or a city.

2. Time because climate must be defined over a specified interval. NOAA typically uses 30-year averages, whereas studying Earth’s history often involves averages of a century or longer.

3. Averages and extremes of variables such as temperature, precipitation, pressure & winds.

Page 4: Climate change101 esip_2011

1) What does the acronym IPCC stand for?

A - International Program on Climate and Culture

B - International Panel on Climate and Culture

C – Intergovernmental Panel on Climate Change

D - International Panel on Climate Change

E – Intergovernmental Program on Climate Change

First, a short test …

Page 5: Climate change101 esip_2011

2)  Which of the following best defines greenhouse gas?

A – Gas molecules that trap solar energy

B – Gas molecules that scatter green light

C – Heat-trapping gas molecules

D – Gases emitted by greenhouse plants

E – Gases emitted by greenhouse gardeners

Page 6: Climate change101 esip_2011

3) What is the most abundant greenhouse gas?

A – Water Vapor

B - Methane

C – Nitrous Oxide

D – Carbon Dioxide

E – Sulfur Dioxide

Page 7: Climate change101 esip_2011

4) Which greenhouse gas is of most concern to climate scientist studying warming?

A – Water Vapor

B - Methane

C – Nitrous Oxide

D – Carbon Dioxide

E – Sulfur Dioxide

Page 8: Climate change101 esip_2011

5) What element constitutes the bulk of the mass in any single tree ?

A - Chlorophyll

B - Carbon

C – Hydrogen

D - Oxygen

E – Carbon Dioxide

Page 9: Climate change101 esip_2011

6) What was the first creature added to the endangered species list because of human-induced global warming?

A – Carrier Pigeon

B – Polar Bear

C – Grizzly Bear

D – Red Wolf

E – White Sturgeon

Page 10: Climate change101 esip_2011

7) TRUE or FALSE The Ozone Hole contributes to global warming.

A - TRUE

B - FALSE

Page 11: Climate change101 esip_2011

A - TRUE

B - FALSE

8) TRUE or FALSE Global Warming is accelerated by the melting of snow and ice cover surfaces.

Page 12: Climate change101 esip_2011

9) Melting of Arctic snow & ice will likely result in rising sea levels.

A - TRUE

B - FALSE

Page 13: Climate change101 esip_2011

10) Melting of Antarctic snow and ice will likely result in rising sea levels.

A - TRUE

B - FALSE

Page 14: Climate change101 esip_2011

11) How long does it take for atmospheric C02 to disperse & quit trapping out-going thermal energy?

A – 5 years

B – 20 years

C – 50 years

D – 75 years

E – 100 years

Page 15: Climate change101 esip_2011

12) According to the 2007 IPCC report, how many inches could sea levels rise by 2100?

A – 1 to 4 inches

B – 4 to 7 inches

C – 7 to 24 inches

Page 16: Climate change101 esip_2011

Global Climate ChangeGlobal Temperature: Has increased by ~0.7°C over the last 100yr. The rate of increase is “accelerating”.

Global data & graphs in this presentation are from 2007 IPCC report

Page 17: Climate change101 esip_2011

Rising atmospheric temperature

Rising sea level

Reductions in NH snow cover

Warming is Unequivocal

Also, the Oceans are warming & becoming more acidic

Page 18: Climate change101 esip_2011
Page 19: Climate change101 esip_2011

Changes in sea ice don’t significantly affect sea level because this ice is already floating. Melting land ice (glaciers, ice caps, and ice sheets) increases sea level.

Significant decreases in Arctic sea ice extent.

A different world in the Arctic: present and future

Page 20: Climate change101 esip_2011

What drives the observed warming?

Page 21: Climate change101 esip_2011

Figure SPM.1

10,000 5,000 0

Years before 2005

Page 22: Climate change101 esip_2011

Industrial revolution and the atmosphere

The current concentrations of key greenhouse gases, and their rates of change, are unprecedented.

Carbon dioxide Methane Nitrous Oxide

Intergovernmental Panel on Climate Change 2007

Page 23: Climate change101 esip_2011

How do CO2

(and other gases) cause global

warming?

Page 24: Climate change101 esip_2011

Energy Gains

Energy Loses

System

Global Climate Change

Page 25: Climate change101 esip_2011

The climate system is more complex than just

CO2 and radiation

What about the feedbacks?

Page 26: Climate change101 esip_2011

In a warming climate, water vapor plays a major role in a positive feedback loop that amplifies global climate change. (H20 responds to changes in climate, but it doesn’t drive climate change)

One way to think about Climate Change is an intensification of the water cycle

As the temperature of the atmosphere rises, more water is evaporated from ground storage (rivers, oceans, reservoirs, soil). Because the air is warmer, the relative humidity can be higher, and the atmosphere can 'hold' more water vapor. As a greenhouse gas, the higher concentration of water vapor is then able to absorb more thermal IR energy radiated from the Earth, thus further warming the atmosphere. The warmer atmosphere can then hold more water vapor and so on and so on. This is referred to as a 'positive feedback loop'.

Page 27: Climate change101 esip_2011

"Extremes of precipitation are generally increasing because the planet is actually warming and more water is evaporating from the oceans, this extra water vapor in the atmosphere then enables rain and snow events to become more extensive and intense than they might otherwise be.“ Tom Karl, NOAA’s NCDC, June 2011.

Extreme weather events have grown more frequent in the United States since 1980, partly due to climate change.

Page 28: Climate change101 esip_2011

FEEDBACK SCENARIO:

Advancing sea ice in cold ocean waters resulting in more ice-covered ocean water with a higher albedo that reflects more sunshine and cools the ocean further

B – Negative Feedback Loop

A – Positive Feedback Loop

Page 29: Climate change101 esip_2011

FEEDBACK SCENARIO:

A person who starts to perspire experiences evaportative cooling and a reduction in body temperature.

B – Negative Feedback

A – Positive Feedback

Page 30: Climate change101 esip_2011

FEEDBACK SCENARIO:

Economic panic sends a large volume of shareholders to the bank to withdraw their assets. Massive withdrawals accelerates panic and leads to more economic disruption.

B – Negative Feedback

A – Positive Feedback

Page 31: Climate change101 esip_2011

FEEDBACK SCENARIO:

Increased CO2 allows plants to grow faster & remove more CO2 from the atmosphere tending toward a state of equilibrium.

B – Negative Feedback

A – Positive Feedback

Page 32: Climate change101 esip_2011

FEEDBACK SCENARIO:

A warmer atmosphere that results in warmer soil in the arctic allows more CO2 and CH4 to be released from the tundra which traps more IR and warms the atmosphere further.

B – Negative Feedback Loop

A – Positive Feedback Loop

Page 33: Climate change101 esip_2011

FEEDBACK SCENARIO:

Melting sea ice amidst warm(er) ocean waters resulting in more ice-free ocean water with a lower albedo that reflects less sunshine and warms the ocean further.

B – Negative Feedback Loop

A – Positive Feedback Loop

Page 34: Climate change101 esip_2011

Observed warming is consistent with observed changes:

The duration of ice cover on lakes decreased by about 2 weeks over the 20th century in mid- and high latitudes of the Northern Hemisphere.

There is a widespread retreat of nonpolar glaciers.

Arctic sea-ice has thinned by 40% in recent decades (summer & autumn)And decreased in extent by 15% since the 1950s in spring and summer.

Northern Hemisphere snow cover has decreased by 10% since the 1960s.

The growing season has lengthened by about 1 to 4 days per decade during the last 40 years in the Northern Hemisphere, especially at higher latitudes.

The global mean sea level has increased at an average annual rate of 1 to 2 mm during the 20th century.

Page 35: Climate change101 esip_2011

AgungChichon

Pinatubo

Observations

Are Humans Responsible?

IPCC (1995): “Balance of evidence suggests discernible human influence”

IPCC (2001): “Most of global warming of past 50 years likely (odds 2 out of 3) due to human activities”

IPCC (2007): “Most of global warming of past 50 years very likely (odds 9 out of 10) due to greenhouse gases”

Natural forcings only

Natural and human effects

IPCC WG1 - 2007(Intergovernmental Panel on Climate Change)

Page 36: Climate change101 esip_2011

Featuring information from the U.S. Global Change Research Program(USGCRP) 2009 report Global Climate Change Impacts in the United States

Regional Climate Change

Page 37: Climate change101 esip_2011

Increases in the average number of days with very heavy precipitation

1958 to 2007

From 1950 to 2006, Wisconsin as a whole became wetter, with a 10 percent increase in annual precipitation (3.1 inches)

2008 Lake Delton Dam failure due to heavy rains

FLOODING Observed

Page 38: Climate change101 esip_2011

www.climatewisconsin.org

STORIES & INTERACTIVESfrom

CLIMATE WISCONSIN

Page 39: Climate change101 esip_2011

Cities and agriculture face increasing risks from a changing climate.

Water supplies will become increasingly scarce, calling for trade-offs among competing uses, and potentially leading to conflict.

Increasing temperature, drought, wildfire, and invasive species will accelerate transformation of the landscape.

Increased frequency and altered timing of flooding will increase risks to people, ecosystems, and infrastructure.

Unique tourism and recreation opportunities are likely to suffer.

Southwest Key Issues

Page 40: Climate change101 esip_2011
Page 41: Climate change101 esip_2011

Mitigation: Necessary to avoid dangerous climate change

Adaptation:Climate change is happening; Adaptation needed to minimize impacts

Climate Knowledge for ActionSlowing and/or minimizing impacts

Mitigation: reduces amount of global warming

Adaptation: reduces the impact

Page 42: Climate change101 esip_2011

Humans can take actions to reduce climate change and its impacts

Guiding Principle:

Many actions have co-benefits

Page 43: Climate change101 esip_2011

Co-Benefits of Carbon Mitigation

1) By using less energy, you can reduce carbon emissions and save money

2) By walking or riding a bike to work a few days a week you can improve your health and save money

3) Did I mention saving money ???

Page 44: Climate change101 esip_2011

Co-Benefits of Driving Less: Clean Air Along with saving money on gas ….

Can you commit to car pooling, walking or riding to work one day a week? (or two or three?)

Page 45: Climate change101 esip_2011

Co-Benefits of Driving Less: Health Along with saving money on gas ….

Page 46: Climate change101 esip_2011

"The more mitigation we do, the less adaptation will be required & the less suffering there will be."

John Holdren, White House Director of Science & Technology

* Buy Local! Re-use stuffThe less distance food & other goods are transported the better.

* Identify personal options to save energy-Ceiling fans?-Rain garden?

* Use renewable energy

* VOTE! Get to know elected officials views and actionsaround reducing global warming

Page 47: Climate change101 esip_2011

Takes a village, or a planet - National Geographic video

http://video.nationalgeographic.com/video/player/specials/sitewide-redesign/ngm-7billion-typical.html