© Oxford University Press, 2008. All rights reserved. 1 Chapter 3 CHAPTER 3 THE GLOBAL ENERGY SYSTEM.

Slides:



Advertisements
Similar presentations
The Earth’s Global Energy Balance
Advertisements

The Greenhouse Effect and Earth-Atmosphere Energy Balance
Unit 3 Lesson 1 The Atmosphere
Radiative Forcing of Ozone
Earth Systems Science Chapter 3 I. Global Energy Balance and the Greenhouse Effect: The Physics of the Radiation Balance of the Earth 1.Electromagnetic.
MONITORING EARTH’S CLIMATE SYSTEM & PLANETARY ENERGY BUDGET.
Outline Further Reading: Chapter 04 of the text book - matter-energy interactions - shortwave radiation balance - longwave radiation balance Natural Environments:
Heat Energy Solar and gravitational energy are the fundamental sources of energy for the Earth's climate system. Air-sea exchanges of heat (& freshwater)
Handout (yellow) Solar Energy and the Atmosphere Standard 3 Objective 1 Indicators a, b, and c Standard 3 Objectives 1, 2, and 3 Workbook Pages 3,
Outline Further Reading: Chapter 05 of the text book - continental vs. marine regimes - temperature structure of the atmosphere - seasonal variations Natural.
1 BAESI - Global Warming: Food Climate Connections The Greenhouse Effect Dr. Eugene Cordero San Jose State University Outline  Greenhouse effect  Energy.
What is the Greenhouse Effect?. Review of last lecture – The two basic motions of the Earth – What causes the four seasons: the Earth’s tilt and the 3.
Module 1: Themes in Physical Geography Topic 3: Weather Unit A : Atmospheric heating, motion (winds) and moisture Unit B : Weather systems (air masses,
Solar Energy & the Atmosphere
Lecture 1: Introduction to the planetary energy balance Keith P Shine, Dept of Meteorology,The University of Reading
HEAT ENERGY TRANSFER AND AIR TEMPERATURE. As we have seen, Earth’s Weather and Climate are the results of the intricate interrelationships between the.
Atmospheric temperature
The Atmosphere Chapter 22. Atmosphere: A mixture of gasses that surrounds a planet, such as Earth.
Visualizing Physical Geography Copyright © 2008 John Wiley and Sons Publishers Inc. Chapter 2 The Earth’s Global Energy Balance.
ATMOSPHERE.
1 Met 10 Weather Processes Jeff Gawrych Temperature, Heat Transfer and Earth’s Energy Balance.
Ozone Creation. Chapter 4 Atmosphere and Surface Energy Balances Geosystems 6e An Introduction to Physical Geography Robert W. Christopherson Charles.
Chapter 4 Atmosphere and Surface Energy Balances Robert W. Christopherson Charlie Thomsen.
The Greenhouse Effect. What controls climate? Energy from the Sun – Radiation! Consider the 4 inner planets of the solar system: SUN 342 W m W.
Ch3: Energy Balance and Temperature. 1.About the first in-class assignment 2.About reading the textbook.
1 Global Changes in the Atmosphere Global Warming and Ozone Depletion msnbcmedia.msn.com/j/msnbc/Components/Photos/...
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.
Mid-term review 1 Chapter 1 1. Weather and Climate Climate: “average” weather conditions Weather: state of the atmosphere at a given time and place. It.
Energy: Warming the Earth & the Atmosphere
Ch Solar Energy and the Atmosphere
Chapter 3 Atmospheric Energy and Global Temperatures.
Sun Controls Earth’s Climate System Earth has a global climate system that includes air, land, liquid water, ice, and living things.climate system The.
Energy Balance Chapter 18.
AT622 Introduction Jan 23, Nearly all energy on earth ultimately comes from sun. There is an approximate equilibrium between absorbed solar radiation,
Topic 6. Without energy from the sun, conditions on Earth would be different. What is the energy that is radiated from the Sun? The energy that is radiated.
The Layered Atmosphere The Earth's atmosphere contains several different layers that can be defined according to air temperature temperature.
RADIATION. Insolation in tercepted sol ar radi ation.
Satellite Image Basics  Visible: Senses reflected solar (lunar) radiation Visible –Cloud thickness, texture; not useful at night  Infrared (IR): Senses.
CHAPTER 17 HEAT AND THE ATMOSPHERE HEATING THE ATMOSPHERE ENERGY FOR METEOROLOGY ORIGINATES IN THE SUN EARTH RECIEVES ONE 2 BILLIONTH OF SUNS ENERGY.
What is the Greenhouse Effect?. Review of last lecture – What is energy? 3 methods of energy transfer – The names of the 6 wavelength categories in the.
Lecture 3: Radiation and Earth’s Atmosphere EarthsClimate_Web_Chapter.pdfEarthsClimate_Web_Chapter.pdf, p. 1-5 For more advanced reading materials, please.
Section - 01 cont’d Lesson 2 Temperature and Heat.
AAAHHHHH!!!!. Climate Change Climate Physical properties of the troposphere of an area based on analysis of its weather records over a long period Two.
Chapter 11 Heating the Atmosphere. Weather versus Climate  Weather  Atmospheric conditions over a short period of time  Constantly changing  Climate.
Chapter 22 Section 2 Handout
Incoming & Outgoing of Energy of the Earth. The Earth’s Energy Balance The Earth's average temperature remains fairly constant from year to year. Therefore,
6061 Geoscience Systems ( Atmospheric Radiation Energy Budget How the atmosphere system is driven? Lecture.
Unit 10 Lesson 2 The Atmosphere Copyright © Houghton Mifflin Harcourt Publishing Company.
Copyright © 2011 by Oxford University Press, Inc. Energy and the Environment James A. Fay / Dan S. Golomb CHAPER 11 Global Warming and Climate Change.
ATMOSPHERE OBJECTIVE 1 1.What are the structural components of the
Chapter 4 Atmosphere and Surface Energy Balances Geosystems 6e An Introduction to Physical Geography Robert W. Christopherson Charles E. Thomsen.
Temperature Rainfall Wind WEATHER AND CLIMATE. Relevance of Weather.
Atmosphere-ocean interactions Exchange of energy between oceans & atmosphere affects character of each In oceans –Atmospheric processes alter salinity.
17 Chapter 17 The Atmosphere: Structure and Temperature.
Insolation and Temperature
Temperature Changes With Earth’s Atmosphere
Temperature Changes With Earth’s Atmosphere
Global energy balance SPACE
Natural Environments: The Atmosphere
Solar Energy and the Atmosphere
Energy Transfer in the Atmosphere
ATMOSPHERE.
GLOBAL ENERGY BUDGET - 3 Atmosphere Basics.
Composition, Structure, & Heat Budget
Quiz # 2 1. In which portion of the electromagnetic spectrum is the sun’s peak energy? 2. In which portion of the electromagnetic spectrum is the earth’s.
Journal #25 What is a greenhouse? What is the greenhouse effect?
Thermodynamics Atmosphere
Climate Earth’s Energy Budget.
Solar Energy and the Atmosphere
Presentation transcript:

© Oxford University Press, All rights reserved. 1 Chapter 3 CHAPTER 3 THE GLOBAL ENERGY SYSTEM

© Oxford University Press, All rights reserved. 1 Chapter 3 INTRODUCTION Scales of climate Atmospheric composition and structure –Troposphere –Stratosphere –Temperature profile Units used in climatology

© Oxford University Press, All rights reserved. 1 Chapter 3 BASIC PROPERTIES OF THE ATMOSPHERE Temperature Pressure Density Concentration Mixing ratio

© Oxford University Press, All rights reserved. 1 Chapter 3 THE SUN AS A SOURCE OF ENERGY The solar constant The solar spectrum –Ultraviolet –Visible –Infrared Spatial variations of solar energy at the top of the atmosphere How changes in solar energy lead to ice ages

© Oxford University Press, All rights reserved. 1 Chapter 3 THE RADIATION BUDGET OF THE EARTH–ATMOSPHERE SYSTEM – SHORTWAVE RADIATION Incoming shortwave radiation – Figures 3.6, 3.10 Atmospheric scattering –Air molecules –Particles Atmospheric absorption The impact of clouds

© Oxford University Press, All rights reserved. 1 Chapter 3 SHORTWAVE ENERGY AT THE EARTH’S SURFACE Absorption at the Earth’s surface Albedo How efficient is solar energy as a power source?

© Oxford University Press, All rights reserved. 1 Chapter 3 IS THERE REALLY A HOLE OVER ANTARCTICA? Chemical players in ozone depletion The circumpolar vortex Polar stratospheric clouds Very low temperatures

© Oxford University Press, All rights reserved. 1 Chapter 3 THE RADIATION BUDGET OF THE EARTH–ATMOSPHERE SYSTEM – LONGWAVE RADIATION Longwave radiation from the Earth’s surface Atmospheric absorption and re-radiation Assessing the Earth’s environment through infrared photography What’s all this fuss about greenhouse warming?

© Oxford University Press, All rights reserved. 1 Chapter 3 THE RADIATION BUDGET OF THE EARTH-ATMOSPHERE SYSTEM – NET RADIATION AND ENERGY BUDGET Net radiation and its global distribution Latent heat of evaporation (Chapter 5) Sensible heat and temperature –Vertical profiles during the day –Isotherms The global temperature distribution –Australian distribution

© Oxford University Press, All rights reserved. 1 Chapter 3 SUB-SURFACE HEAT FLUX Land compared to water Differences by surface characteristics Impacts on seasonal and diurnal temperatures Global examples Australian example Controlling sub-surface heat flux in your garden