Global & Regional Climate Change Science a presentation from the CIMSS Climate Literacy Ambassadors community A low-carbon climate education project.

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Presentation transcript:

Global & Regional Climate Change Science a presentation from the CIMSS Climate Literacy Ambassadors community A low-carbon climate education project

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

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.

Global Climate Change Global 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

Rising atmospheric temperature Rising sea level Reductions in NH snow cover Warming is Unequivocal Also, the Oceans are warming & becoming more acidic

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

What drives the observed warming?

Figure SPM.1 10,0005,0000 Years before 2005

Industrial revolution and the atmosphere The current concentrations of key greenhouse gases, and their rates of change, are unprecedented. Carbon dioxideMethane Nitrous Oxide Intergovernmental Panel on Climate Change 2007

How do CO 2 (and other gases) cause global warming?

Global Climate Change

The climate system is more complex than just CO 2 and radiation What about the feedbacks?

In a warming climate, water vapor plays a major role in a positive feedback loop that amplifies global climate change. ( H 2 0 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'.

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.

Agung Chichon 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 WG (Intergovernmental Panel on Climate Change)

Featuring information from two recent reports: Global Climate Change Impacts in the United States – U.S. Global Change Research Program Midwest Region Wisconsin’s Changing Climate: Impacts and Adaptation Wisconsin Initiative on Climate Change Impacts (WICCI) Regional Climate Change /

While the longer growing season provides the potential for increased crop yields, increases in heat waves, floods, droughts, insects, and weeds will present increasing challenges to managing crops, livestock, and forests. Great Lakes Key Issues During the summer, public health & quality of life, especially in cities, will be negatively affected by increasing heat waves, reduced air quality, and increasing insect and waterborne diseases. The likely increase in precipitation in winter and spring, more heavy downpours, and greater evaporation in summer would lead to more periods of both floods and water deficits. Reductions in Great Lakes water levels will have impacts on shipping, infrastructure, beaches, & ecosystems. Native species are very likely to face increasing threats from rapidly changing climate conditions, pests, diseases, and invasive species.

Observed Changes

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

Climate Change in Wisconsin What does the historical record tell us? Climate change in Wisconsin: Wisconsin isn’t necessarily getting hotter, but rather less cold.

Winter T max Spring T max Summer T max Fall T max Kucharik and Serbin, in prep The Greatest Amount of Warming is Occurring in Winter and Spring Climate Change in Wisconsin What does the historical record tell us? Changes in Daily Maximum Temperature:

Winter T min Spring T min Summer T min Fall T min Kucharik and Serbin, in prep Nighttime low temperatures are warming faster than daytime highs Climate Change in Wisconsin What does the historical record tell us? Changes in Daily Minimum Temperature:

Climate Change in Wisconsin

Learn more from CLIMATE WISCONSIN

UW-Madison researchers used “down-scaled” climate models to project that Wisconsin’s warming trend will continue and increase considerably in the decades ahead. By the middle of the century, statewide annual average temperatures are likely to warm by 6-7 degrees Fahrenheit. Models Project Continued Warming

Mitigation: Necessary to avoid dangerous climate change Adaptation: Climate change is happening; Adaptation needed to minimize impacts Slowing Change & Minimizing Impacts Mitigation: reduces amount of global warming Adaptation: reduces the impact

Humans can take actions to reduce climate change and its impacts Guiding Principle: Many actions have co-benefits

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 we mention saving money ???

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?)

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

Learn More On-Line Developed collaboratively by four UW departments (CIMSS, AOS, Geology, CCR) Consistent with Climate Literacy Framework Clarifies IPCC report Beta version debuted 2008 NASA 2010 GCCE support for updates, revisions & stipends for G6-12 teachers Credit OR Certificate

Humans can take actions to reduce climate change and its impacts The Climate Literacy Ambassadors program was developed to raise awareness of climate science and lay the foundation for the guiding principle of the Climate Literacy: