Chapter 6: Weather & Climate. Midterm Exam 9:33 8: 22335778 7 : 5788 6:2335778 Average Score = 77 9:33 8: 22335778 7 : 5788 6:2335778 Average Score =

Slides:



Advertisements
Similar presentations
Michael B. McElroy ACS August 23rd, 2010.
Advertisements

The syllabus says: Atmosphere and change  Describe the functioning of the atmospheric system in terms of the energy balance between solar and long- wave.
Earth’s Global Energy Balance Overview
Climate change can be discussed in short, medium and long timescales. Short-term (recent) climate change is on a timescale of decades, an example would.
Outline Review of Ocean Stratification and Circulation Recent historical Climate Change External Climate Forcings Natural Climate Variability Paleoclimatology.
Climatic changes in the last 200 years (Ch. 17 & 18) 1. Is it warming? --climate proxy info (recap) -- info from historical & instrumental records 2. What.
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.
Atmosphere structure, Solar Inputs and the Transport of Heat.
Explaining the Evidence Activity 2: Clearing the Air.
Climate: What we know about it, How we know about it, and What we’re doing to it.]
Climate Chapter 14.
Essential Principles Challenge
1 THE CARBON CYCLE AND GLOBAL WARMING. 2 CARBON CYCLE Movement of carbon between the atmosphere, oceans, biosphere, and geosphere Movement of carbon between.
{ Natural Changes in Climate.  8.9 Long Term and Short Term Changes in Climate  8.10 Feedback Loops and Climate  8.11 Clues to Past Climates.
Climate Change UNIT 3 Chapter 7: Earth’s Climate System
UNIT FOUR: Matter and its Changes  Chapter 12 Atoms and the Periodic Table  Chapter 13 Compounds  Chapter 14 Changes in Matter  Chapter 15 Chemical.
Reviewing Climate Change Over Time Forcing Factors and Relevant Measurements.
Ozone Creation. Chapter 4 Atmosphere and Surface Energy Balances Geosystems 6e An Introduction to Physical Geography Robert W. Christopherson Charles.
Global Warming: Consequence of Fossil Fuel Use Do Now: Please copy the following definitions into your notes: Greenhouse Effect: The trapping of heat by.
CESD 1 SAGES Scottish Alliance for Geoscience, Environment & Society Observing and Modelling Climate Change Simon Tett, Chair of Earth System Dynamics.
Chapter 4 Atmosphere and Surface Energy Balances Robert W. Christopherson Charlie Thomsen.
Science, Society and Solutions
Samayaluca Dune Field, south of Juarez, Chihuahua Global Climate Change.
Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-
11.1 Natural Climate Change Science 10 p
What do you know about climate? What do you want to know to understand climate?
Global Warming Cause for Concern. Cause for Concern? What is the effect of increased levels of carbon dioxide in the Earth’s atmosphere? Nobody knows.
Handout 25-3 Climate Change.
Climate Change Factors that Affect Climate. Atmosphere –The atmosphere of Earth is a layer of gases surrounding the planet Earth that is retained by Earth's.
There are gases in our Earth’s atmosphere which can trap heat toward the Earth’s surface. This is called the greenhouse effect. The greenhouse effect.
Sustainability and Globalization Global Warming. A global issue with regards to sustainability A world-wide warming of the Earth’s lower atmosphere.
Samayaluca Dune Field, south of Juarez, Chihuahua Global Climate Change.
Questions for Today:  What is Weather and Climate?  What are four major factors that determine Global Air Circulation?  How do Ocean Currents affect.
2. Climate: “average” weather conditions, but the average doesn’t stay steady. I.e. Ice ages, El Niño, etc. 1. Weather: state of the atmosphere at a given.
Atmospheric and Climate Change
Climate Literacy Session: Causes Peter Coombe August 5, 2015.
Global Energy Balance and the Greenhouse Effect What determines Earth’s surface temperature? What is the history of CO 2 on Earth? ultravioletinfrared.
Lecture Outlines Physical Geology, 14/e Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Plummer, Carlson &
Conversations with the Earth Tom Burbine
Meteorology Lecture 1 Weather and Climate Review.
Global Climate Change The Evidence and Human Influence Principle Evidence CO 2 and Temperature.
UNIT 3 Climate Change 1.
 What is your view on climate change? Write down either: What you believe about climate change What you have heard someone say about climate change 
Climate and Climate Change Chapter 21
Kim M. Cobb Sustainable Atlanta Roundtable September 8, 2006 The science of global warming.
Climate Change November 4, Global Climate Change Global Warming – describes a rapid increase in the temperature of Earth’s surface, water, and atmosphere,
Chapter 13 Section 3 Global Warming Environmental Science Spring 2011.
Chapter 4 Atmosphere and Surface Energy Balances Geosystems 6e An Introduction to Physical Geography Robert W. Christopherson Charles E. Thomsen.
Climate Change. Need to have to memorize – no trick, just study Need to be able to explain/Answer questions about Example: In the Six Americas, some in.
HOW GLOBAL WARMING HAS AFFECTED GLACIERS By: Tunyasiri & Kankanit P.3.
© Yann Arthus-Bertrand / Altitude The Summary for PolicyMakers - final plenary The Summary for PolicyMakers - final plenary Michael Prather, LA, Chapter.
Climate Change. Causes Several factors affect global climate: 1.Changes in solar output 2.Changes in Earth's orbit 3.Changes in the distribution of continents.
Aim: How do increased carbon dioxide concentrations on our planet affect life?
Unit 4: Climate Change Earth’s Climate System. Introduction Atmosphere: layer of gases that surrounds a planet or moon Without the atmosphere, days would.
To recap Give 2 examples of research methods that show long term historical climate change? How reliable are these? Give 2 ways of measuring medium term.
Climatic Changes. Standards 4d: Students know the differing Greenhouse conditions on Earth, Mars and Venus; the origins of those conditions; and the climatic.
TEKS 8.10A recognize that the sun provides the energy that drives convection within the atmosphere and ocean, producing winds and ocean currents The Sun,
Ch 20 Global Warming Part one.
Radiation Balance and Feedbacks
Climate Changes.
DO NOW Pick up notes and Review #25..
3.3 Explaining & Predicting Climate Change
Climate Cycles & Recent Climate Change.
Thermal Response II Current News and Weather Surface Energy Balance
Patterns in environmental quality and sustainability
Climate Cycles & Recent Climate Change.
Good Morning! PREPARED: Climate Packet Pencil Highlighter
Chapter 5 Ecosystems and the Physical Environment
Natural Changes in Climate
Climate Change.
Presentation transcript:

Chapter 6: Weather & Climate

Midterm Exam 9:33 8: : : Average Score = 77 9:33 8: : : Average Score = 77

2 Topics before Chapter 6 Material 1.Keeling Curve 2.How scientists approach Climate Change 1.Keeling Curve 2.How scientists approach Climate Change

Keeling Curve +400 ppm

Keeling Curve

 Shows atm. CO2 rising at unprecedented rates  Driven by burning of fossil fuels past 200 yrs.  Pioneered in 1958 by scientist Charles Keeling.  Longest-running tally of carbon dioxide levels in atm.  Maintained by Scripps Institution of Oceanography.  Up 22 points from a decade ago.  Many scientists have warned that carbon dioxide readings must be brought down to 350 ppm to avoid severe climate impacts and stall "feedback loops" that will exacerbate the rise.  Shows atm. CO2 rising at unprecedented rates  Driven by burning of fossil fuels past 200 yrs.  Pioneered in 1958 by scientist Charles Keeling.  Longest-running tally of carbon dioxide levels in atm.  Maintained by Scripps Institution of Oceanography.  Up 22 points from a decade ago.  Many scientists have warned that carbon dioxide readings must be brought down to 350 ppm to avoid severe climate impacts and stall "feedback loops" that will exacerbate the rise.

Keeling Curve  Previous 800,000 years, CO 2 levels never exceeded 300 ppm  There is no known geologic period in which rates of increase have been so sharp.  Was about 280 ppm at the advent of Industrial Revolution  “I wish it weren't true, but it looks like the world is going to blow through the 400-ppm level without losing a beat," said Scripps geochemist Ralph Keeling, who has taken over the Keeling curve measurements from his late father. "At this pace we'll hit 450 ppm within a few decades."  Previous 800,000 years, CO 2 levels never exceeded 300 ppm  There is no known geologic period in which rates of increase have been so sharp.  Was about 280 ppm at the advent of Industrial Revolution  “I wish it weren't true, but it looks like the world is going to blow through the 400-ppm level without losing a beat," said Scripps geochemist Ralph Keeling, who has taken over the Keeling curve measurements from his late father. "At this pace we'll hit 450 ppm within a few decades."

Large body of evidence supports conclusion that human activity is primary driver of recent warming. 1.Our understanding of how gh gases trap heat, how climate system responds to increases, and how other human and natural factors influence climate. 2.Many indirect estimates of climate changes over the last 1,000 to 2,000 years. Ice cores, tree rings and corals - show recent T rise is unusual 1.Our understanding of how gh gases trap heat, how climate system responds to increases, and how other human and natural factors influence climate. 2.Many indirect estimates of climate changes over the last 1,000 to 2,000 years. Ice cores, tree rings and corals - show recent T rise is unusual

Large body of evidence… 3. Comparisons of actual climate with computer models. When models are run with historical inc. in gh gases show gradual warming of Earth, increases in ocean heat content, rise in sea level, retreat of sea ice and snow cover. In agreement with observations.

Climate Model Indications & the Observed Climate

 Global climate models clearly show effect of human-induced changes on global T.  blue band shows how global T would have changed due to natural forces only.  pink band shows model projections of effects of human and natural forces combined.  black line shows actual observed global average temperatures.  Global climate models clearly show effect of human-induced changes on global T.  blue band shows how global T would have changed due to natural forces only.  pink band shows model projections of effects of human and natural forces combined.  black line shows actual observed global average temperatures.

 Global climate models clearly show effect of human-induced changes on global T.  Close match between black line and the pink band indicates that observed warming over last half-century cannot be explained by natural factors alone, and is instead caused primarily by human factors.  Global climate models clearly show effect of human-induced changes on global T.  Close match between black line and the pink band indicates that observed warming over last half-century cannot be explained by natural factors alone, and is instead caused primarily by human factors.

800,000 Year Record of CO 2 Concentrations Measured from trapped air bubbles in Antarctic ice core

Energy from the Sun Has Not Increased Solar energy has been measured by satellites since 1978.

Now, Chapter 6

 Our layer model to date assumes that that surface temperature is the same everywhere on Earth!  But, we know this is not true.  So, we have to add yet more complexity to our climate change model!  Our layer model to date assumes that that surface temperature is the same everywhere on Earth!  But, we know this is not true.  So, we have to add yet more complexity to our climate change model!

1. Daily & Seasonal cycles - drive surface temperatures above and below average values. 2. Energy budgets DO NOT balance locally. – net heat input at low latitudes, transport to high latitudes.  turbulent flows of air and water.  requires complex computer climate models. 1. Daily & Seasonal cycles - drive surface temperatures above and below average values. 2. Energy budgets DO NOT balance locally. – net heat input at low latitudes, transport to high latitudes.  turbulent flows of air and water.  requires complex computer climate models.

Daily Variability: Simplified Surface Energy Balance  NET R =  +SW (insolation)  –SW (reflection)  +LW (infrared)  –LW (infrared)  NET R =  +SW (insolation)  –SW (reflection)  +LW (infrared)  –LW (infrared) Figure 6.2

Radiation Budgets El Mirage, CA Pitt Meadows, BC

Seasonal Variability Earth’s tilt is responsible for seasons.

Earth’s tilt determines how much heat the surface receives from the Sun each day as a function of latitude (y axis) and time of year (x axis).

net heat input at low latitudes, transport to high latitudes

Global Latent Heat Figure 4.19

Global Sensible Heat Figure 4.20

So we have to simulate the weather.  In order to forecast global warming we have to simulate the time and space variations and imbalances in the energy budget.  And the way the Earth’s climate responds by storing or transporting heat around.  Our original layer model can’t do this  Our original layer model can’t do this.  Physics that simulate flows of air/water is complex and difficult to simulate. So we have to simulate the weather.  In order to forecast global warming we have to simulate the time and space variations and imbalances in the energy budget.  And the way the Earth’s climate responds by storing or transporting heat around.  Our original layer model can’t do this  Our original layer model can’t do this.  Physics that simulate flows of air/water is complex and difficult to simulate.

Global Circulation without Rotation

Coriolis effectCoriolis effect - an inertial force described by 19th- century French engineer- mathematician Gustave- Gaspard Coriolis in Effect is an apparent deflection of the path of an object that moves within a rotating coordinate system. The object does not actually deviate from its path, but it appears to do so because of the motion of the coordinate system. Coriolis effectCoriolis effect - an inertial force described by 19th- century French engineer- mathematician Gustave- Gaspard Coriolis in Effect is an apparent deflection of the path of an object that moves within a rotating coordinate system. The object does not actually deviate from its path, but it appears to do so because of the motion of the coordinate system.

Global Circulation With Rotation With Coriolis Effect

1.Energy Budget of the Earth fluctuates on daily & seasonal timescales (in contrast to the layer model). 2.Annual Energy Budget doesn’t balance locally because excess heat is carried to higher latitudes by winds and ocean currents. 3.Global warming forecast requires simulation the weather – computational challenge. 1.Energy Budget of the Earth fluctuates on daily & seasonal timescales (in contrast to the layer model). 2.Annual Energy Budget doesn’t balance locally because excess heat is carried to higher latitudes by winds and ocean currents. 3.Global warming forecast requires simulation the weather – computational challenge.