Current Climate Change Ch. 17, Bush. Outline  Evidence for recent climate change  Are humans the cause?  Potential ecological effects of climate change.

Slides:



Advertisements
Similar presentations
In our October 11, 2010, cover story, “A Message From Mother Nature?” you’ll read about the increase in the number of extreme weather events. Many scientists.
Advertisements

Name: Liang Wei Major: Electric Machinery and Electric Equipment
Arctic summers ice-free by 2013 predict scientists European heat waves kill 35, – the UK’s warmest year on record Rising sea levels threaten Pacific.
Your Name Your Title Your Organization (Line #1) Your Organization (Line #2) Global warming.: Matthieu BERCHER, Master M.I.G.S., University of Burgundy,
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.
Climate Change Assess current knowledge on climate change.
Teacher: Samarripa GLOBAL WARMING. The Global Warming & The Greenhouse Effect.
Objective: Understand Causes, Effects and Solutions of Global Warming
The Greenhouse Effect Presenters: Jaime Pinto & Nathalie Mokuba
+ YEAR 10 EARTH AND SPACE SCIENCE (ESS). + EARTH & SPACE SCIENCE 2 parts to the unit: EARTH – Global systems & SPACE – Origins of the universe We’re going.
(events related to Earth science). Global Warming Global Warming – is the increase of Earth’s average surface temperature due to effect of greenhouse.
How it happens and how it affects us.
Chapter 4 Sections 3 and 4 Long Term Changes in Climate Global Changes in the Atmosphere.
I. Background A. global warming: the gradual increase in planet-wide temperatures B. temperature of Earth depends on amount of sunlight received, amount.
Greenhouse Effect - Natural Heating of Earth’s surface by certain atmospheric gases.
CLIMATE CHANGE THE GREAT DEBATE Session 10. CLIMATE CHANGE? If we have learnt anything from this course, it is that climate is not constant It is, and.
Earth Science Chapter 11.2 Climate Change.
Greenhouse effect Sources, Causes & Impacts. Interpretation of global warming Global warming is a long-term climate change which raises the temperature.
Global warming is caused by green house gases, which trap in the sun’s infrared rays in the earth’s atmosphere, which in turn heat up the earth’s atmosphere.
Climate Change. Weather vs. Climate The earth’s climate is dependent on the weather over a long period of time.
Causes Effects Solutions
Global Warming oJAbATJCugs.
Unit 9G Lesson 4: Global Warming Objective: to learn about the causes and effects of global warming. 4, 11.
Climate Change and Ozone Loss Climate Change Review session Climate Change Review session Brian Kaestner and Dr. Richard Clements.
 Greenhouse gases are gases in the atmosphere that absorbs and emits radiation. Greenhouse gases help to allow Earth to continue to remain warm. Without.
Instructions: 1.Click on a box under the category you want. 2.Read the question and try to answer to yourself. 3.Click one time for the answer to appear.
S6E2.c. relate the tilt of earth to the distribution of sunlight through the year and its effect on climate.
Climate Review. Climate Long term average conditions of a region (occurs over many years) –Usually described in terms of average temperatures, precipitation,
Earth’s Changing Environment Lecture 13 Global Warming.
Environmental Chemistry Greenhouse effect, global warming,
Global Warming Vs Climate Change
GLOBAL WARMING By Nicole.
Handout 25-3 Climate Change.
What climate change means Climate consists of averages & extremes of –hot & cold –wet & dry –snowpack & snowmelt –winds & storm tracks –ocean currents.
The Greenhouse Effect and Global Warming GHB 2005.
Greenhouse Effect Mechanisms Affecting the Greenhouse Evidence for Climate Change.
Global Warming Definition: an increase in the earth's atmospheric and oceanic temperatures widely predicted to occur due to an increase in the greenhouse.
S6E2.c. relate the tilt of earth to the distribution of sunlight through the year and its effect on climate.
Science Starter At night the moon is -387  F, and during the day it is 253  F. Why do you think temperatures are so much more extreme on the moon than.
Carbon cycle and Human activity. Carbon cycle Carbon cycles though the atmosphere, living things, soils, and the ocean.Carbon cycles though the atmosphere,
AIM: What is Global Warming?
Evidence of Global Warming and Consequences
Greenhouse Effect Intro
Global Warming.
Global Warming Chapter 13 Section 3. Learning Targets Students will understand the importance of the greenhouse effect. Students will understand why the.
AIM: What is Global Warming? DN: Fill in the following chart: ProblemDefinitionCauseEffect Acid Rain Ozone Depletion.
Your “Do Now”5/25 Take ½ sheet of paper Write down 5 things you remember from the visit by the GVSU scientists yesterday.
 Journal: Compare and contrast the carbon cycle and the nitrogen cycle.
Chapter 13 Section 3 Global Warming Environmental Science Spring 2011.
GREENHOUSE EFFECT. What Is Greenhouse Effect??? an atmospheric heating phenomenon, caused by short-wave solar radiation being readily transmitted inward.
Global Warming “The Era of Procrastination, of Half-Measures, of Soothing and Baffling Expedients, of Delays, is Coming to its Close. In its Place We are.
HUMAN IMPACT ON THE ENVIRONMENT Global Warming and Acid Rain.
Greenhouse Effect (E 3 ) Pages ) Definitions 2) Description 3) Greenhouse Gases 4) Greenhouse Gases Effect on Atmosphere.
Assumption College Mathayom 1, Foundation Science Miss Anna.
Section Climate Change According to NASA’s Goddard Institute for Space Studies, 2009 tied for second warmest year on record, just behind The.
Climate Change: Should We Be Worried? Chapter 17: Climate.
H Graham BSc PGCE1 What is Global Warming?. H Graham BSc PGCE2.
Guided Notes on the Human Factor Chapter 14, Section 4.
Unit 4 Lesson 7 Climate Change Copyright © Houghton Mifflin Harcourt Publishing Company.
Chapter 23 The Atmosphere, Climate, and Global Warming.
The Greenhouse Effect. Like a greenhouse, our planet traps heat – How does it work? Greenhouse gases trap heat radiating from earth – Water vapor – Carbon.
Climate Change. History of the E arth  4,56 billion years old  ‘snowball earth’  Glacial periods  Interglacial periods  The peak of the last ice.
What is Climate Change? Long term changes in the Earth’s heat budget resulting from radiative inbalance can result in a colder or warmer climate.
Climate Change Climate – The average year after year pattern of temperature, precipitation, winds and clouds in an area. Climates are classified mainly.
Indicators and Effects of Climate Change
5.1 What is Climate? 5.2 Climate Zones
Climate and Change.
Climate.
Climate.
Presentation transcript:

Current Climate Change Ch. 17, Bush

Outline  Evidence for recent climate change  Are humans the cause?  Potential ecological effects of climate change

Outline  Evidence for recent climate change  Are humans the cause?  Potential effects of climate change

Evidence of Temperature Changes  Three main sources of data: –Direct measurements of temperature –Location of ice caps and tropical glaciers –Thickness of ice caps

Temperature records  We have accurate records only for the past 120 years  Most temperature readings taken at cities which are “heat islands”

Whaling and Polar Ice caps

Changes in extent of sea ice

Thickness of Ice Caps  Submarines make careful measurements of the distance between the ice and the bottom of the sea  Have estimated that the thickness of the ice caps have decreased from 3.1m to 1.8m

Tropical Glaciers are melting  All tropical glaciers are above 4800 m  At the current rate of temperature change, it is estimated that all will be gone in 50 years Kilimanjaro

The effect of melting ice caps  There is not enough water trapped in the ice caps to create “Waterworld”  The biggest effect of ice caps melting comes from the decrease in ALBEDO

Albedo = brightness

Ice caps have high albedo

Outline  Evidence for recent climate change  Are humans the cause?  Potential effects of climate change

Last glacial period ended 11,000 years ago  90% of last 2 million years has been glacial  For the last 10,000 years, plants and animals have been living in an unusually warm environment

Temperature changes over the years  The rate of climate change we are currently experiencing is only matched by the rapid warming at the end of the last ice age

Temperature changes in history  Between the earth was a few degrees colder  Called “The Little Ice Age”  Influenced history: –Outcome of battles –Crops failing causing famine

Greenhouse effect  Light energy enters the atmosphere  Changes to heat energy  Light energy exits atmosphere but heat energy is trapped

The Greenhouse effect  The greenhouse effect is not all bad  Without the greenhouse effect, the earth would be, on average, -18  C

Creation of greenhouse gases  The burning of fossil fuels is increasing the greenhouse effect  Important greenhouse gases: –HCF’s, CFC’s –Methane –CO 2 –Water vapour

Relative contribution of greenhouse gases to predicted warming  Other chemicals are actually better at trapping heat but CO 2 contributes more to the greenhouse effect due to the fact that it is way more abundant

CO 2 and water vapour  CO 2 causes minor increase in temperature  Increase in temperature causes more water vapour via evaporation  Water vapour leads to further greenhouse effect and higher temperature

Carbon cycle  In the natural carbon cycle, respiration and decomposition increase CO 2  Photosynthesis decreases CO 2  Burning fossil fuels now contributes to CO 2 gain

Fossil fuels Fossil fuels are ancient organisms that did not decompose

The major culprits…

Carbon sinks  Each year humanity dumps roughly 8 billion metric tons of carbon into the atmosphere – 6.5 billion tons from fossil fuels and 1.5 billion from deforestation  But less than half that total, 3.2 billion tons, remains in the atmosphere to warm the planet  Forests, grasslands, and the waters of the oceans are acting as carbon sinks

Outline  Evidence for recent climate change  Are humans the cause?  Potential effects of climate change

Potential effects of CO 2 increase  Predicted changes in temperature  Changes to the natural world  Changes to human life

Recent increases in CO 2  Jagged line is caused by seasonal changes in photosynthesis; in summer N. Hemisphere plants use up more CO 2

Pollution can mitigate increases in temperature  Pollutants such as those from car exhaust are causing increases in cloud cover  Cloud cover increases albedo

Air pollution increases albedo

CO 2 and temperature changes  Simulations of temperature changes are becoming increasingly accurate

Predicted temperature change  Five principal research groups all produce climate models  Differences arise in the predictions made about social and political change  Medium estimate is that the average temperature on Earth will rise ~3.5  C

Increased photosynthesis

Planting trees to decrease temp  Deforestation causes decreases in CO 2 absorption  Planting trees will have the opposite effect ->decreases CO 2

C4 evolution changing atmospheres  C4 photosynthesis appears to have evolved at a time when O 2 was high and CO 2 was low and temperatures were high

The global distribution of C4 plants in today's world  C4 grasslands (orange) have evolved in the tropics and warm temperate regions where C3 forests (green) are excluded by seasonal drought and fire.  C3 grasses (yellow) remain dominant in cool temperate grasslands because C4 grasses are less productive at low temperatures.

Temperature and precipitation

Climate affects ecology

Deserts will spread

N. Hemi. plants will migrate north Predicted migration of beech and maple trees

Migration of species  Industrialization may impede the migration of many species  Temperate species (and island species) may have nowhere to migrate to  If migration can not occur then extinction will likely take place

Cold-adapted species

Implications to Conservation

Extinction and global warming  One study indicated that, by 2050, current warming trends could bring about extinction of 15 to 37 percent of the 1,103 species they studied  A mere 6 degrees of global warming was enough to wipe out up to 95 per cent of the species which were alive on earth at the end of the Permian period, 250 million years ago

Arable land will have new locations  Best conditions for farming will move towards poles  Will be at the latitude of the Canadian Shield  More irrigation needed as crop land will be drier  Expected 20% decrease in cultivatable land

Other reasons why global warming a threat to life on Earth?  Incidences of heat attacks, respiratory disease and stroke will increase  Disease and pests are more likely to spread  Tropical storms, tornadoes, landslides, heatwaves and droughts will both increase in number and intensity  Air quality will become poorer  coastal cities like Miami, New Orleans, Los Angeles and Bangkok will be flooded as ocean level rises due to melting glaciers  ocean levels rise, some inland drinking water sources will become contaminated by saltwater

Summary  The Earth is becoming increasingly warm  Recently, humans have contributed to this phenomenon  Temperature increases will have severe effects to the natural world