Regional and Global Atmospheric Changes

Slides:



Advertisements
Similar presentations
Atmosphere & Climate Change
Advertisements

© 2011 Pearson Education, Inc. CHAPTER 16 The Oceans and Climate Change.
Climatology Climatology is the study of Earth’s climate and the factors that affect past, present, and future climatic changes. Climate describes the long-term.
Future climate (Ch. 19) 1. Enhanced Greenhouse Effect 2. CO 2 sensitivity 3. Projected CO 2 emissions 4. Projected CO 2 atmosphere concentrations 5. What.
Class 14b: Global climate change Basics of global warming Potential effects Politics of global warming.
Class 14b: Global climate change Basics of global warming Potential effects Politics of global warming.
CHAPTER 16 The Oceans and Climate Change
© 2014 Pearson Education, Inc. Climate Change. © 2014 Pearson Education, Inc. Earth’s Climate System Climate – long-term atmospheric conditions in a region.
© Cengage Learning  World’s largest island – 80% covered by glaciers  10% of the world’s fresh water  Glacial melting and movement accelerating.
Unit 11 Notes: Climate Change
Global Warming Human-driven Climate Change Climate Change is Not New The Earth has historically gone through alternating periods of global warming and.
Climate Change.
Climate Change A Q and A Session Modified from
Climate Change Climate Change.
(events related to Earth science). Global Warming Global Warming – is the increase of Earth’s average surface temperature due to effect of greenhouse.
Chapter 4 Sections 3 and 4 Long Term Changes in Climate Global Changes in the Atmosphere.
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
Climate Change. Have you noticed any change in our summer weather? Our winter weather? The arrival of spring? Have you noticed any change in our summer.
Earth Science Chapter 11.2 Climate Change.
Chapter 21 Global Climate Change. Climate Change Terminology  Greenhouse Gas  Gas that absorbs infrared radiation  Positive Feedback  Change in some.
S6E2.c. relate the tilt of earth to the distribution of sunlight through the year and its effect on climate.
Samayaluca Dune Field, south of Juarez, Chihuahua Global Climate Change.
Environmental Problems Pollution Climate Change. Marine Pollution The introduction into the ocean by humans, substances that changes the physical, chemical.
What climate change means Climate consists of averages & extremes of –hot & cold –wet & dry –snowpack & snowmelt –winds & storm tracks –ocean currents.
GLOBAL CLIMATE CHANGE. WHAT IS THE GREENHOUSE EFFECT? LIGHT ENERGY IS CONVERTED TO HEAT ENERGY - INFRARED RADIATION HEAT IS TRAPPED BY GASES AROUND THE.
Unit 6.  Climate – the average weather conditions of an area over a long period of time  Weather is the day to day conditions *Climate you expect and.
S6E2.c. relate the tilt of earth to the distribution of sunlight through the year and its effect on climate.
Regional and Global Atmospheric Changes Chapter 20.
Chapter 20 Global Climate Change. Climate Change Terminology  Greenhouse Gas  Gas that absorbs infrared radiation  Positive Feedback  Change in some.
© 2011 Pearson Education, Inc. CHAPTER 16 The Oceans and Climate Change.
© 2014 Pearson Education, Inc. Chapter 16 Climate Change.
TOPIC 6: GLOBAL WARMING AND GREENHOUSE EFFECT. Temperature and Carbon Dioxide Concentration from 1880 to present.
Chapter 19 Global Change 1. o Global change- any chemical, biological or physical property change of the planet. o Global climate change- changes in the.
Earth’s climate and how it changes
Climate Change November 4, Global Climate Change Global Warming – describes a rapid increase in the temperature of Earth’s surface, water, and atmosphere,
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
GREENHOUSE EFFECT. What Is Greenhouse Effect??? an atmospheric heating phenomenon, caused by short-wave solar radiation being readily transmitted inward.
 You have time for test corrections today and we will complete the FRQ for this Quizzam.  Logistics:  We are going through a Chapter a week, so do your.
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
Chapter: Climate Section 3: Climatic Changes.
9.1Evidence of Changing Climate. Rising Temperatures  Records of Earth’s average temperatures over the past 100 years  Records show avg. temperatures.
Chapter 25 Climate Chapter 25 What are Climate Zones?
Years before present This graph shows climate change over the more recent 20,000 years. It shows temperature increase and atmospheric carbon dioxide. Is.
Climate Change Climate is what we expect, weather is what we get. ~Mark Twain.
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
Global Warming Environmental Science January 4, 2011.
Global Climate Change a.k.a. Global Warming. What is the green house effect?  A greenhouse is a house made of glass. It has glass walls and a glass roof.
Chapter 23 The Atmosphere, Climate, and Global Warming.
Evidence of Climate Change. CO 2 levels historically rose and fell below 300 ppm. Increase since Industrial Revolution: now reached 400 ppm.
Climate Factors of Climate El Nino Topography Greenhouse Effect
Chapter 19 Global Change.
Brett Weimer INTB-3000 July 20, 2011
Global Change.
Climate Change Climate – The average year after year pattern of temperature, precipitation, winds and clouds in an area. Climates are classified mainly.
Global Warming History & Geography
Chapter 19 Global Change.
Global Change.
Effects of the Doubling of Carbon Dioxide
Chapter 19 Global Change.
On a sheet of white paper
Climate Change CH 19.
Chapter 19 Global Change.
Chapter 19 Global Change 2 hour video from PBS called “Heat”
The Ocean and Climate Change
Greenhouse Gasses –in order of importance
Chapter 15 Global Change.
Chapter 19 Global Change.
Climate.
Chapter 19 Global Change.
Presentation transcript:

Regional and Global Atmospheric Changes Chapter 21 Regional and Global Atmospheric Changes

Proof Positive!

Non-Anthropogenic Reasons Sun Spots – solar energy Changes in Earth’s orbit Changes in axis tilt and wobble

Is Global Warming Anthropogenic? Svante Arrhenius A Swedish scientist first to claim in 1896 that fossil fuel combustion may eventually result in enhanced global warming. Charles Keeling Produce concentration curves for atmospheric CO2 starting in 1958 280ppm = preindustrial levels 392ppm levels in 2011 add 2ppm yearly 350ppm considered safe for life as we know it 450ppm or 20C change = serious weather change

Keeling Curve Winter High & Summer Low Scientists are pushing for CO2 caps that will stabilized us at 450 ppm in the next few decades. Many believe this goal isn't politically feasible, and prefer 550 ppm http://co2now.org/Current-CO2/CO2-Now/annual-co2.html Winter High & Summer Low

Temperature and Carbon Dioxide In the 1980's the global annual mean temperature curve started to rise

Greenhouse Gasses Water Vapor - absorbs and releases energy

Greenhouse Gases Water Vapor - absorbs and releases energy

Intergovernmental Panel on Climate Change http://www.ipcc.ch/

IPCC 4th report 2007 The IPCC predicts that by the end of the 21st century climate change will result in : A probable temperature rise between 1.1°C and 6.4°C (2.0-11.50F) by 2100. A sea level rise most likely to be 28-43cm (11-17inches) Arctic summer sea ice disappearing in second half of century An increase in heat waves very likely A likely increase in tropical storm intensity.

Effects of Temperature Changes Change wind and weather patterns Redistribute global moisture Shift Agricultural Areas Alter World’s Biomes Alter Some Ocean Currents Increase Sea Levels Flood Coastal Wetlands and Cities Increase Waterborne and Insect-transmitted diseases

Why Ocean’s Rise Thermal expansion Additions of water from melting ice

Antarctica

Major Ice Caps - Anarctica 1. Antarctica 90% of world’s ice, ocean’s rise 200Ft Landmass based Larsen B Ice Shelf, 650 feet thick about the size of Rhode Island The Ross Ice Shelf is roughly as big as Texas – attached to the ice sheets that cover almost 98% of the Antarctic continent.

Greenland Ice Cap

Major Ice Caps - Greenland Sea levels rise 23 feet if the entire ice sheet melted Landmass Based Florida and Sea Level Changes 550ppm ice free poles = 60-70 meters of sea rise http://geology.com/sea-level-rise/florida.shtml

Glacial Moulins

Major Ice Caps - The Arctic Temperature rise of 4-7C by 2100 All Ice Shelves

Arctic Ice Cap

Melting Glaciers

Albedo The fraction of radiation striking a surface that is reflected by that surface High Albedo - reflecting most of the energy Low Albedo - absorbing most of the energy

Proof of Global Warming 1. Global sea level rose about 17 centimeters (6.7 inches) in the last century. The rate in the last decade, however, is nearly double that of the last century. 2. Average Arctic temperatures increased at almost twice the global average rate in the past 100 years. Shrinking glaciers and ice caps. Most of this warming has occurred since the 1970s, with the 20 warmest years having occurred since 1981 and with all 10 of the warmest years occurring in the past 12 years. Despite an unusually deep solar minimum in 2007-2009 Seasonal events starting earlier and ending later The top 700 meters (about 2,300 feet) of ocean showing warming of 0.302 degrees Fahrenheit since 1969 The number of record high temperature events in the United States has been increasing, while the number of record low temperature events has been decreasing, since 1950. The U.S. has also witnessed increasing numbers of intense rainfall events.

Warmer Temperatures; Different Organisms Changes Occur In Distributions Population Sizes Population Density Wildlife Behavior

Periods of Climate Change Glacial (100,000 year average) Interglacial (12,000 year average)

Florida’s Glacial Shoreline

Extent of Last Glacial Period Little Ice Age 1550-1850

Analyzing atmospheric History 1. Air Bubbles in Ice Cores 2. Analyze sediments in lakes, ponds and swamps for pollen & fossils

Ice Core Sample

6 Geostrophic Gyres North Atlantic Gyre South Pacific Gyre South Atlantic Gyre North Pacific Gyre South Pacific Gyre The Indian Ocean Gyre Antarctic Circumpolar Current

Satellite Image of Ocean Gyres Based on Thermal Differences

Satellite Image of Gulf Stream and Major Eddies Gulf Stream – Warm Water Intersects with Cold Water Shelf Gyre Warm-Core Eddie Cold-Core Eddie

North Atlantic Current Cooling increases salinity and density

Where are we?

Positive Feedback - Clathrates Methane Clathrates In Siberian permafrost & ocean floor sediments are vast deposits of gas-filled ice (methane) called clathrates. Tundra - permafrost

Positive Feedback CO2 emissions, copious as they are, may just wind up pulling the trigger on the clathrate gun.

You Tubes http://www.youtube.com/watch?v=oa3M4ou3kvw&playnext=1&list=PLBE8E58A79407AB44&index=20 http://www.youtube.com/watch?v=YegdEOSQotE&feature=related

Cow Gas

Methane Emissions Landfills (35%) Domesticated Livestock (26%) Natural Gas and Oil Systems (20%) Coal Mining (10%) Rice Paddies

Resisting Change Other Pollutants Cool the Atmosphere known as the “aerosol” effect Sulfur emissions Volcanic Eruptions Jet Contrails Increased cloud cover from evaporation Increased absorption of CO2 in ocean’s

Mitigation Mitigation of Global Climate Change Alternatives to fossil fuels Sequestering Carbon in Trees Sequestering Carbon (technology) Fertilizing the Ocean with Iron Fertilizing the stratosphere with sulfur

Solutions? Iron in the oceans increases phytoplankton production - could seed the oceans?

Benefits of Global Warming Access to oceans for fishing and oil Increased plant production More livable climates such as twin cities