Global Warming and Florida; What you can do about it. UF, School of Building Construction August 29, 2002 Mark van Soestbergen International Carbon Bank.

Slides:



Advertisements
Similar presentations
What Are We Doing to Our Planet?
Advertisements

1.Why is the moist adiabatic lapse rate lower than the dry- adiabatic lapse rate? Heat is released during condensation. 2.When temperatures are below freezing,
Climate Change: A Primer on Carbon Offsets and Trading Cypress Swamp Cafe Dec 12, 2007 Mark van Soestbergen ICBE.
Climate Change (and You) UF, School of Building Construction Feb 3, 2004 Mark van Soestbergen ICBE.
Climate Change (and You) UF BCN 1582 August 29, 2006 Mark van Soestbergen ICBE.
February 2008 Green Infrastructure and Sustainable Communities 17-1 Global Climate Change & Carbon Footprinting resources and strategies Module 17 Mark.
Composition Earth Science / Mr. Bimber
Climate Change (and You) CBI Veterans April 12, 2006 Mark van Soestbergen ICBE.
GHG Management Approach - Layout - Practical Example - Local Context Gainesville Energy Advisory Committee (GEAC) May 21,2002.
© Oxford University Press 2009 Quit Part 7 Global warmingAre humans responsible? 7.2What is the normal global distribution global distribution pattern.
Continental Scale Rain Making A new tool to combat global warming or Drought Reduction as a Means of Carbon Sequestration By Mike Fallwell.
1 GLOBAL SCIENTIFIC RESEARCH TRENDS: Future Sustainable Livelihood Leading R&D & Innovation fields in the 21 st Century: Agricultural Technologies & Industries.
Human Impact on Air Resources
Introduction to global climate change and impacts in Ukraine National Ecological Centre of Ukraine Iryna.
Geoexchange at CMU Regional public higher education institution 3 campuses in Grand Junction, CO. Main campus 78 acres and 1.5 million s.f. under.
Carbon management in the supply chain Mike Bernon.
Geothermal Power Matthew Duarte Josh Ku-ha! Jerry Lu.
In this presentation you will:
GLOBAL CLIMATE CHANGE OCEAN IMPACT. Temperature Change Over Past 400,000 Years- Ice Core Data.
The Effect of Humans On Ecosystems and Biological Cycles On Ecosystems and Biological Cycles.
The Energy Challenge CONTEXT SCALE. Humanity’s Top 10 Problems for Next 50 Years 1.Energy 2.Water 3.Food 4.Environment 5.Poverty 6.Terrorism and War 7.Disease.
This is a journey which starts and ends in distances difficult for the human mind to capture.
Michael B. McElroy ACS August 23rd, 2010.
Mitigation Strategies What and Why?. What is mitigation? To decrease force or intensity. To lower risk. Earthquake mitigation Flood mitigation Climate.
What is CO2? Carbon Dioxide: two oxygen molecules bonded to a single carbon molecule.
DARGAN M. W. FRIERSON DEPARTMENT OF ATMOSPHERIC SCIENCES DAY 4: 04/08/2010 ATM S 111, Global Warming: Understanding the Forecast.
Aerosols and climate Rob Wood, Atmospheric Sciences.
Greenhouse Effect How we stay warm. The Sun’s energy reaches Earth through Radiation (heat traveling through Space)
CHAPTER 5. * Weather is daily changes in temp and precipitation. * CLIMATE is the average year to year conditions.
Air Quality and Climate Change. Coal and Oil Formation Both are Fossil Fuels: remains of plants and animals that died anywhere from 400 million to 1 million.
Global Warming What Is It?.
Green House Effect vs. Global Warming By; Shane Jones.
Global Warming Global warming is the increase in the average measured temperature of the Earth's near-surface air and oceans since the mid-20th century,
The Economic Perspective Economists are not concerned with whether it exists, but whether/what should be done about it. Even though climate change exists,
EARTH’S CLIMATE. Latitude – distance north or south of equator Elevation – height above sea level Topography – features on land Water Bodies – lakes and.
Ozone, Air Pollution, and Earth’s Energy Balance Presented by Stephen Schneider Deborah Carlisle June, 2012.
5-5. GLOBAL WARMING Introduction  Definition:  Rise in the average temperature of the Earth’s surface (mainly air T).  From the Environmental.
The Greenhouse Effect What is the greenhouse effect? Interaction between planet’s atmosphere, star’s light Results in heating of planet What causes the.
Climate Practice. True/False 1.______ The troposphere is the lower 10 km of the atmosphere. 2.______ Black clothing absorbs heat energy faster than white.
Our Carbon Footprints The primary footprint is a measure of our direct emissions of CO2 from the burning of fossil fuels including domestic energy consumption.
Chapter 5 frontispiece. A dust plume from an intense dust storm over the Sahara E.A. Mathez, 2009, Climate Change: The Science of Global Warming and Our.
Global Warming  Global warming is the increase in the average temperature of the Earth's near- surface air and oceans.
Global Warming and Florida; What we can do about it. Big Bend Group Sierra Club
Global Warming (and Florida) UF, School of Building Construction August 28, 2003 Mark van Soestbergen ICBE.
Climate Change. 2 Global carbon cycle (billion metric tons)
CarbonSolutions = Integrated GHG Management Approach - Layout - Practical Example - Local Context Miami-Dade Environmental Resource Management (DERM) August.
Energy,Carbon and Clean UF Greening UF March 18, 2004 Mark van Soestbergen ICBE.
Earth’s climate and how it changes
Session 2 Buildings and Measurements. Buildings Sector Accounts for About 40% of U.S. Energy, 72% of Electricity, 34% of Natural Gas, 38% of Carbon, 18%
Air Pollution By Ahmed Muztuba, 9-A. What is air pollution? Air pollution is a chemical, physical and biological agent which changes the natural characteristics.
Outline Earth from the perspective of Space Some basic science behind climate and global warming Effects of changing climate that we’re seeing now Effects.
LEARNING FROM GLOBAL DISASTER LABORATORIES PART 11A: FUNDAMENTALS OF GLOBAL CLIMATE CHANGE Walter Hays, Global Alliance for Disaster Reduction, Vienna,
C LIMATE Chapter 21. F ACTORS THAT A FFECT C LIMATE Latitude Less solar energy as you move away from the equator Tropical zones Rays from the sun hit.
Importance of the Atmosphere Earth's atmosphere is a mixture of gases that surrounds Maintains balance of heat Protects life forms from sun’s rays 1 1.
Balance of Energy on Earth Yumna Sarah Maria. The global energy balance is the balance between incoming energy from the sun and outgoing heat from the.
Greenhouse Effect How we stay warm.
Greenhouse Effect How we stay warm.
14.8 NOTES Greenhouse Gases
Climate Change (and You)
Composition of the Atmosphere
Greenhouse Effect How we stay warm.
Climate Change (and You)
Human Impact on Climate
Greenhouse Effect How we stay warm.
Greenhouse Effect How we stay warm.
Climate Change (and You)
Climate.
GLOBAL EFFECTS.
Atmosphere and Climate Change
Climate Change (and You)
Presentation transcript:

Global Warming and Florida; What you can do about it. UF, School of Building Construction August 29, 2002 Mark van Soestbergen International Carbon Bank and Exchange, Inc.

Carbon Dioxide Catches infrared waves going into space Distance between C and O; just right to catch infrared waves.

Gasoline is 85.5% carbon 1 gallon of conventional liquid gasoline turns into 172 cubic feet / 4.87 cubic meters of CO 2.

125 gallon make one ton CO 2 1 ton of CO 2 easily fills up a 19,866 cubic feet / 556 cubic meters container.

10 ton CO 2 fills Florida Field 3 foot high Every year, the average person in the United States produces 20 tons of CO 2.

About 3Gt C are added every year

The Asian brown haze, a cocktail of ash, acids, aerosols and dust that is 3 kilometers thick and now extends over 10 million square kilometres and covers large parts of South Asia, China and Indonesia. Researchers estimated that breathing New Delhi's air was the equivalent of smoking 20 packets of cigarettes every day. Copyright 2002 IPS-Inter Press Service

Notice the air over the Tibetan Plateau very clear. Most of this air pollution comes from human activities. The aerosol is notoriously rich in sulfates, nitrates, organic and black carbon, and fly ash. These particles represent a health hazard to those people living in the region, and have a significant impact on the region's hydrological cycle and climate. Jacques Descloitres, MODIS Land Rapid Response Team, NASA/GSFC

Image courtesy the SeaWiFS Project, NASA/Goddard Space Flight Center, and ORBIMAGE SeaWiFS Project,

Image courtesy the SeaWiFS Project, NASA/Goddard Space Flight Center, and ORBIMAGESeaWiFS Project,

Image courtesy the SeaWiFS Project, NASA/Goddard Space Flight Center, and ORBIMAGE SeaWiFS Project,

Provided by the SeaWiFS Project, NASA/Goddard Space Flight Center, and ORBIMAGE

Provided by the SeaWiFS Project, NASA/Goddard Space Flight Center, and ORBIMAGE

Climate Change changes everything More CO 2 changes plant behavior More CO 2 increases temperature of the atmosphere, the surface, the earths crust and the oceans Distribution of energy through currents on the planet Global hydro cycle; rain and moisture

The Coldest Areas Warm the Most

Summers will be real scorchers

Florida -Average temperature increase of 5 ~10°F -July temperature increase of ~ 15°F -Reversal of summer-wet, winter-dry -Change in soil / Fire risk -Vectors -Tropical diseases -Sea level rise -Intensive Storms -Will happen anyway

Impacts on: -Insurance -Agriculture -Health -Tourism -Tax Base -Economy

Florida +5meter, very likely unavoidable. Expected sea level increase 21 st Century: meter Courtesy: PBS

Much reduction is needed to reach stability Human emission rate in billion tC/yr t Equilibrium Latent atmospheric C is about 188 billion ton Emissions the earth absorbs in billion tC/yr

Climate Change: A hundred year problem Achieving carbon-neutrality (the switch to clean energy) = 30 years? Absorption of latent carbon (sequestration) 7% of planet surface = 150 years?

Possible Approaches The Big Picture The Big Picture Do nothing Strategic adaptation (we move!) Nuclear Renewable Energy Energy Efficiency Sequestration Price induced reductions International Carbon Trading

What can you do? Build Green Buildings! Lights vs Natural Light Solar Heating Solar Electricity Water and Rain Water Geo Cooling and Heating Air Delivery Energy Star Products

Buildings consume 1/3 of the energy in the U.S.

How much money and how many emissions since the delivery of Little Hall? What are the potential savings if it had been green? $2,458,539 24,716tCO 2

Little Hall used 967,700 gallons of water in How much water would it use over a hundred year period? 96,770,000 gallons If 10 tons CO2 fills Florida Field by 3 feet, how high would Little Halls stack of CO2 be? feet

Annual budget vs electrical - UM 470million/6million = 1.3% - UCF 578million/9million = 1.6% - UF 1,857million/26million = 1.4%

UF is planning to grow by 16% over the next 10 years.. What are the potential annual GHG and dollar savings if all new buildings are Green and operate at 50%? 2001 = 264,000tCO = 307,000tCO2 BAU 1tCO2 reduction also saves $83 in MWh 21,000 tCO2 and $1,743,000 per year How much over a hundred years? 2,100,000 tCO2 and $174,300,000

Conclusion: Green Buildings save MONEY Green Buildings save the environment Green Buildings make for happy campers & increase productivity What will you be doing over the next few years? Make Green Buildings!!

U.S. commitment under Kyoto Regardless, somebody has to initiate action.

Links and Resources

Contact ICBE - Nice meeting all of you! Mark van Soestbergen tel fax Toward Climate Stability