Climate Change and Climate Modeling Kristina Fitzhugh November 17, 2009.

Slides:



Advertisements
Similar presentations
Draft Essential Principles with Fundamental Concepts By Marlene Kaplan & David Herring NOAA & NASA.
Advertisements

Earth’s Climate System. Factors Affecting Climate Change  Earth is surrounded by a layer of gases called the atmosphere.  The characteristic pattern.
Determining the Local Implications of Global Warming Clifford Mass University of Washington.
Your Name Your Title Your Organization (Line #1) Your Organization (Line #2) Global warming.: Matthieu BERCHER, Master M.I.G.S., University of Burgundy,
Determining the Local Implications of Global Warming Clifford Mass University of Washington.
Explaining the Evidence Activity 2: Clearing the Air.
Essential Principles Challenge
The Greenhouse effect By: Lucas Carr, Mason Hoffman and Cole Ament.
Climate and Climate Change
Climate Change UNIT 3 Chapter 7: Earth’s Climate System
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
Atmosphere and Climate Change
Greenhouse Effect - Natural Heating of Earth’s surface by certain atmospheric gases.
(c) McGraw Hill Ryerson Human Activity and Climate Change Climate change is the change in long-term weather patterns in certain regions.  These.
Miss Nelson SCIENCE ~ CHAPTER 9 CLIMATE. Climate Change SECTION 4.
Earth Science Chapter 11.2 Climate Change.
WWK How interactions between the hydrosphere and atmosphere cause weather changes!
Climate Review. Climate Long term average conditions of a region (occurs over many years) –Usually described in terms of average temperatures, precipitation,
Global Warming Vs Climate Change
Chapter 19 Global Change. Global change-Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures.
PROSPERIDAD J. ABONETE JULY 3, 2003 Understanding Climate Change.
The Atmosphere and the Water Cycle. Earth’s system’s have two sources of energy Internal External.
Climate Change and Greenhouse Effect Notes. What we want to know? What is climate change? What is the greenhouse effect? How will climate change affect.
Sustainability and Globalization Global Warming. A global issue with regards to sustainability A world-wide warming of the Earth’s lower atmosphere.
Greenhouse Gases & the Greenhouse Effect. General Information Greenhouse gases (GHG) were naturally found in the environment before the industrial revolution.
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.
13-3 Climate Change Page 339. Picture it…….. Have you ever sat in a car…….. ……….on a hot day……. ……..like todaaaaayyyyy….. 8{ Windows are up, heat is trapped….
S6E2.c. relate the tilt of earth to the distribution of sunlight through the year and its effect on climate.
Global Warming (Climate Change) The Greenhouse Effect Sunlight streams through the atmosphere and heats the Earth. Some of the heat radiates back out into.
Lecture Outlines Physical Geology, 14/e Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Plummer, Carlson &
The Atmosphere Atmosphere- A thin layer of gases that surrounds the Earth –78% nitrogen –21% oxygen –1% water vapor, argon, carbon dioxide, neon, helium.
THE GREENHOUSE EFFECT Greenhouse Gases:  chemical compounds in the atmosphere that trap heat  they retain a proportion of the sun’s heat through the.
Global Warming By: Melissa Jurado What is the problem? The sun heats the earths surface. The earth radiates energy back into space. Greenhouse gases.
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 
TOPIC 6: GLOBAL WARMING AND GREENHOUSE EFFECT. Temperature and Carbon Dioxide Concentration from 1880 to present.
Climate: The average, year-after-year conditions of temperature, precipitation, winds and clouds in an area.
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
Heat in the Atmosphere The sun’s energy is transferred to earth and the atmosphere three ways Radiation, Convection and Conduction.
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
 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.
Bailey, Christine, Epiphany, and Justina What is Global Warming? Global Warming is a natural increase in temperature each year caused by gases and also.
How does variability in the earth’s physical structure affect the transformations of energy? - albedo of different “spheres”; clouds What is the physical.
Chapter 16 Global Climate Change. 1. Weather = state of the atmosphere at a particular place at a particular moment. 2. Climate is the long-term weather.
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
Climate. Weather vs. Climate Weather – the condition of Earth’s atmosphere at a particular time and place. – Short-term: Hours and days – Localized: Town,
Atmosphere. Earth’s Radiation Budget Earth maintains an energy balance and a temperature balance by radiating as much energy into space as it absorbs.
THE DYNAMIC EARTH Chapter 3 CP ENVL SCI. The Earth as “a System”
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.
Climate Factors of Climate El Nino Topography Greenhouse Effect
Chapter 19 Global Change.
Chapter 19 Global Change.
Climate Change.
Chapter 19 Global Change.
Global Change.
Chapter 19 Global Change.
Chapter 19 Global Change.
Climate Changes.
DO NOW Pick up notes and Review #25..
Climate Change CH 19.
Atmosphere and Climate Change
Chapter 19 Global Change.
Chapter: Climate Section 3: Climatic Changes.
Chapter 15 Global Change.
Chapter 19 Global Change.
Climate.
Chapter 19 Global Change.
Presentation transcript:

Climate Change and Climate Modeling Kristina Fitzhugh November 17, 2009

Earthrise “The picture became known as ‘Earthrise’ and the image of the world from the perspective of a desolate lunar surface became an iconic reminder of our need to protect the Earth’s fragile resources. Earthrise and images like it are widely credited with inspiring the environmental movement and indirectly the start of the Environmental Protection Agency in 1970.” (5)

What is Climate Change? “A long-term change in the Earth’s climate, or of a region on Earth” Can be the change in average weather or change in weather distributions (ex: fewer or greater extreme weather events) Can occur locally, regionally, or globally (1,2,4)

Misconception 1 Temperatures in some areas aren’t increasing, so global warming is a myth. “It is certainly true that the temperature is not rising at every point on the planet...global warming refers to the rise in average temperature...the impacts of climate change will not be the same everywhere”

Climate Change vs. Global Warming Terms sometimes used interchangeably Global warming refers to the average surface temperature increase caused by rising levels of greenhouse gases (ghg’s) Originally introduced in a 1975 Science article by geochemist Wallace Broecker of Columbia University Previously referred to as “inadvertent climate modification” (4)

Climate Change vs. Global Warming Scientist knew human activity would affect the climate, but they didn’t know how In 1979 the National Academy of Science conducted a study on the effects of carbon dioxide on climate Adopted Broecker’s term when referring to rising surface temperatures Used “climate change” when referring to other changes to the climate (4)

Misconception 2 Scientists disagree about whether humans are causing the Earth’s climate to change “Scientists overwhelmingly agree that the Earth is getting warmer, that this trend is caused by people, and that if we continue to pump greenhouse gases into the atmosphere, the warming will be increasingly harmful”

Causes of Climate Change Plate tectonics Ocean currents Volcanoes Earth’s orbit and tilt Greenhouse gases

Plate Tectonics & Ocean Currents Earth’s lithosphere is broken into tectonic plates Plates sit on the asthenosphere Plates move in relation with one another at plate boundaries Moved by convection currents beneath the plates Position of continents affect ocean currents (4)

Plate Tectonics & Ocean Currents The ocean is important in controlling heat and moisture transfer Location of land masses affects the distribution of temperature Affects climate around the world (4)

Volcanoes Emit aerosols and carbon dioxide into the atmosphere Aerosols block sunlight and causes short term cooling, though no long term affects CO2 causes warming, but relatively small amount released compared to humans (6)

Earth’s Orbit & Tilt Majority of Earth’s land mass is above the equator Spring/Summer – Northern Hemisphere is pointed toward the Sun Fall/Winter – Northern Hemisphere is pointed away from the Sun (7)

Greenhouse Effect

1.Water vapor – the most abundant ghg, increases clouds and precipitation so important feedback to the climate 2.Methane – produced naturally and through human processes, much less abundant than other ghg’s decomposition of waste, rice cultivation, livestock 3.Nitrous oxide – produced naturally and through human processes microbials in soil, agriculture soil management, sewage treatment (8) Greenhouse Gases

4.Chlorofluorocarbons – completely of industrial origin, severe depletion of ozone layer 1987 Montreal Protocol: complete elimination of CFC’s by 2000, gone from developing countries by Carbon dioxide – produced naturally and through human processes, most important ghg (8)

Carbon Dioxide Emissions (9)

Misconception 3 Climate naturally varies over time, so any change we’re seeing now is just a part of a natural cycle “Climate does naturally change....but these changes all took place with natural variations in carbon dioxide levels that were smaller than the one we are now causing...carbon dioxide levels are higher now than they have been at any time in the last 650,000 years, which means we are outside the realm of natural climate variation. ”

Misconception 4 Antarctica’s ice sheets are growing, so it must not be true that global warming is causing glaciers and sea ice to melt. “Some ice on Antarctica may be growing...study shows that overall the ice is shrinking in Antarctica...Globally more than 85% of glaciers are shrinking.”

Hurricane Katrina Less than a month before Hurricane Katrina hit New Orleans and the South with it’s huge forces, MIT had released a study that said... “Major storms spinning in both the Atlantic and the Pacific since the 1970’s have increased in duration and intensity by about 50 percent” (7)

Climate Models Study dynamic climate system Predict relation of ghg emissions and future climate Predict regional environments, such as future stream flow or vegetation changes 2007 International Panel on Climate Change Report – models show predicted ranges for average worldwide temperature increase of: Low range: (1.1 – 2.9) 1.8 C High range: (2.4 – 6.4) 4.0 C (11)

Simple Climate Model Want to find Earth’s temperature from an energy model in equilibrium solar radiation (S) = 1370/4 % of albedo (a) = 0.3 Stefan Boltzmann constant (q) = 5.67 x Temperature (T) (13)

Stefan Boltzmann Constant All bodies radiate energy as electromagnetic radiation SB Law is the total energy, I, emitted by a black body at any temperature, T, by: I(T) = q(T 4 ) I = energy per unit area emitted per second T = absolute temperature (K) q = Stefan Boltzmann constant (13)

Simple Climate Model Looking for the Earth’s temperature T = (S/q) (1/4) Plugging in values from previous slides we get... T = [(1370/4)/(5.67 x )] (1/4) = 279 K = 6 C Too cold! (13)

Slightly More Complicated Model Looking for the Earth’s temperature T= [(S(1-a)(1+T vis ))/(q(1+T ir )] (1/4) S, a, and q are previously defined T vis =proportion of incoming energy absorbed by the atmosphere T ir =proportion of infrared energy not absorbed by the atmosphere Plugging in we get... T = K ~ 15.5 C Average surface temperature of Earth currently 16 C (12,13)

Climate Models More accurate model The model gets very complicated very fast Add seasonal cycle Cover whole Earth (sphere) Plants, clouds, etc. Derived from fundamental physical laws, empirical data, observations Ex: Newton’s Law of Motion, Conservation of Energy, etc. Altered to fit large-scale climate system by adding details about Earth’s geography Ex: topography and vegetation (12,14,15)

Climate Models

Earth Simulator Was the fastest supercomputer in the world from Used to run “global climate models to evaluate the effects of global warming and problems in solid earth geophysics” trillion floating point calculations per second (2)

Earth Simulator

Do They Really Work? IPCC says they have “considerable confidence” Have ability to reproduce features of past and current climate Cannot reproduce the weather of a specific day, but can calculate the average weather conditions Confidence higher for predictions of some weather circumstances than others Higher for temperature than precipitation (14)

Implications of Climate Change Decrease in biodiversity Sea level rise Higher population concentration Spread of disease And the list goes on... “The Himalayas contain 100 times as much ice as the Alps and provide more than half of the drinking water for 40% of the world’s population...that 40% of the world’s people may well face a very serious drinking water shortage” (7)

Misconception 5 There is nothing we can do about climate change. It’s already too late. “There are lots of things we can do – but we need to start now...We need to reduce our use of fossil fuels, through a combination of government initiatives, industry innovation, and individual action.”

What Can We Do? U.S. Mayors Climate Protection Agreement Over 500 cities Save energy at home Lighting, appliances, heating and cooling Reduce miles driven Public transportation, walk, bike Consume less, conserve more

Sources 1) 2) 3) 4) 5) 6) 7)An Inconvenient Truth by Al Gore 8) 9) 10) Work.ppt#273,18,Greenhouse gases 11) 12) Work.ppt#273,18,Greenhouse gases 13) 14) 15)