Climate Change What Does the Science Really Tell Us? Craig Cogger WSU Puyallup.

Slides:



Advertisements
Similar presentations
Andy Bose Shame Dishberg Aaron Rostsberg Jonathon McPeterson Harry Eudora.
Advertisements

Atmosphere & Climate Change
Explaining the Evidence Activity 2: Clearing the Air.
The Greenhouse Effect. The problem of global warming We can’t say that we do not notice it or know nothing about it. The melting of ice, earthquakes and.
Greenhouse Effect: The heating of the surface of the earth due to the presence of an atmosphere containing gases that absorb and emit infrared radiation.
Essential Principles Challenge
Global Warming Causes and Mechanics. What is Global Warming? “The recent increase in the world's temperature that is believed to be caused by the increase.
Radiation’s Role in Anthropogenic Climate Change AOS 340.
CHAPTER 5. * Weather is daily changes in temp and precipitation. * CLIMATE is the average year to year conditions.
Air Quality and Climate Change. Coal and Oil Formation Both are Fossil Fuels: remains of plants and animals that died anywhere from 400 million to 1 million.
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
Earth Science Chapter 11.2 Climate Change.
20 Global Climate Change. Overview of Chapter 20  Introduction to Climate Change  Causes of Global Climate Change  Effects of Climate Change  Melting.
Chapter 21 Global Climate Change. Climate Change Terminology  Greenhouse Gas  Gas that absorbs infrared radiation  Positive Feedback  Change in some.
Global Warming Global warming is the increase in the average measured temperature of the Earth's near-surface air and oceans since the mid-20th century,
Heating of the Atmosphere
24 Global Ecology. Figure 24.2 A Record of Coral Reef Decline.
GLOBAL WARMING BY JULIANA MORENO 11°2 English work 04/09/15 I.E LUCRECIO JARAMILLO VELEZ 04/09/15 I.E LUCRECIO JARAMILLO VELEZ.
The Greenhouse Effect A large majority of the insolation that is radiated back into the atmosphere gets absorbed by greenhouse gases. A large majority.
What climate change means Climate consists of averages & extremes of –hot & cold –wet & dry –snowpack & snowmelt –winds & storm tracks –ocean currents.
Understanding the Greenhouse Effect Sara Kalinowski and Ellen Cercena.
The Greenhouse Effect Too much of a good thing?. Light from the sun is composed of many frequencies.
GLOBAL CLIMATE CHANGE. WHAT IS THE GREENHOUSE EFFECT? LIGHT ENERGY IS CONVERTED TO HEAT ENERGY - INFRARED RADIATION HEAT IS TRAPPED BY GASES AROUND THE.
Return to Home Page Return to Home Page January 23, 2014 Introduction to GEOG 495: The Geographies of Climate Change.
Lecture Outlines Physical Geology, 14/e Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Plummer, Carlson &
Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial.
Chapter 20 Global Climate Change. Climate Change Terminology  Greenhouse Gas  Gas that absorbs infrared radiation  Positive Feedback  Change in some.
Topic 6 Insolation and the Seasons. Insolation (INcoming SOLar radiATION) Intensity of Insolation depends on the angle of the Sun’s rays, which are due.
Global Warming and Green House effect. By. Maci, Jessica.
Global Warming Chapter 13 Section 3. Learning Targets Students will understand the importance of the greenhouse effect. Students will understand why the.
By: Cody Pineau Global warming. Natural Causes Natural causes are causes created by nature. One natural cause is a release of methane gas from arctic.
Chapter 20 Global Climate Change. Climate Change Terminology  Greenhouse Gas  Gas that absorbs infrared radiation  Positive Feedback  Change in some.
Modelling the climate system and climate change PRECIS Workshop Tanzania Meteorological Agency, 29 th June – 3 rd July 2015.
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
 Journal: Compare and contrast the carbon cycle and the nitrogen cycle.
KEY CONCEPT Fossil fuel emissions affect the biosphere.
Chapter 21 Global Climate Change. Overview of Chapter 21  Introduction to Climate Change  Causes of Global Climate Change  Effects of Climate Change.
 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.
The Green House Effect ISCI (1). The fate of solar radiation – 26% reflected back into space 20% clouds; 6% by atmosphere – 19% absorbed by clouds,
HOW GLOBAL WARMING HAS AFFECTED GLACIERS By: Tunyasiri & Kankanit P.3.
How does variability in the earth’s physical structure affect the transformations of energy? - albedo of different “spheres”; clouds What is the physical.
Climate Change. Natural Processes That Change Climates  Volcanic Eruptions  The presence of volcanic aerosols (ash, dust, and sulfur-based aerosols),CO.
Atmospheric Heating Radiation Conduction Convection.
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
Climate Change Overview: Key Concepts. Climate vs. Weather What is weather? – Conditions of the atmosphere over a short period of time (e.g. day- to-day).
The Greenhouse Effect. Natural heating of earth’s surface caused by greenhouse gases –CO 2 (Carbon Dioxide) –CH 3 (Methane) –N 2 O (Nitrous Oxide) –H.
Chapter 23 The Atmosphere, Climate, and Global Warming.
Aim: How do increased carbon dioxide concentrations on our planet affect life?
Do Now: 1.What is scale in regards to maps? 2.Which map has a larger scale? a. map of the U.S. b. Robinson projection of the world 3. Which map has a larger.
Chapter 19 Global Change.
Chapter 19 Global Change.
Global Change.
Global Atmospheric Changes
Climate Change All facts and images are from NASA and NOAA unless otherwise indicated.
Global Climate Change
DO NOW Pick up notes and Review #25..
Climate Change CH 19.
Global Climate Change.
Chapter 19 Global Change.
Climate Change: Fitting the pieces together
Energy Drives the Earth System
Chapter 6 Climate.
Chapter 15 Global Change.
Chapter 19 Global Change.
Human Impacts on Climate Change
Climate.
The Art of Mind Mapping!.
Chapter 19 Global Change.
Recent Climate Change Chapter 14 Lesson 3.
Presentation transcript:

Climate Change What Does the Science Really Tell Us? Craig Cogger WSU Puyallup

Simplified Greenhouse Effect Solar energy passes through atmosphere and is absorbed by the earth Energy radiates back toward space as lower-energy infrared waves Greenhouse gases absorb and re-radiate some of the infrared energy, trapping heat in the atmosphere

Greenhouse Gases CO 2, H 2 O, N 2 O, CH 4 : Absorb infrared energy Act like a blanket Without the greenhouse effect, earth’s mean temperature would be 0 o F, nearly 60 o lower than it is now Carbon Dioxide Water

The Problem: We are increasing atmospheric CO 2, adding to the greenhouse effect, and warming the planet

NASA G. Holloway, Institute of Ocean Sciences, Sidney, BC UCAR USDOE PNNL Ocean Circulation moves and stores heat and CO 2 Atmospheric Circulation moves heat Carbon Cycle moves, transforms, and stores CO 2 Aerosols interact with solar energy Some of the Complicating Details

Definitions: Weather and Climate Weather: The current state of the atmosphere (hours, days, weeks, months) Climate: Average weather over time (30 years or more) Climate is what you expect, weather is what you get San Antonio Daily

Weather: Climate:

Climate Forcing Climate forcing: Affects global energy balance, forcing a change in climate Examples: o Changes in solar energy (sunspot cycles, orbital changes – small over short time scales) o Changes in greenhouse gas concentrations (CO 2, CH 4, N 2 O, others) o Aerosols NOAA Minnesota public radio USGS

Climate Feedback Amplifies or dampens climate forcing H 2 O in atmosphere: Positive feedback, increases warming Snow and ice melting: Positive feedback – more melting, less reflection of heat, more warming Melting permafrost and thawing soil releasing greenhouse gases: Positive feedback Changes in cloud cover: Both positive and negative NASA UNEP Katey Walter, UAF Jon Sullivan

Evidence for Current Climate Change: Temperature Anomalies

Evidence for Current Climate Change: Temperature Extremes – US 48 states

Evidence for Current Climate Change: Sea Ice Extent

USGS Evidence for Current Climate Change: Accelerating Glacier Loss

Evidence for Current Climate Change: Ecosystem Changes Bleached coral reef o Coral death and decline appear linked to increased water temperatures Pine bark beetle damage o Extreme cold keeps beetle populations in check. Recent severe infestations appear related to moderating winter temperatures US Forest Service NOAA

Evidence for Current Climate Change: Sea Level Rise

Evidence for Current Climate Change:

IPCC 4 th Assessment IPCC Regional Temperature Projections Change compared with baseline

IPCC 4 th Assessment IPCC Regional Precipitation Projections for Compared with baseline

Saiful Huq Omi/Polaris, for The New York Times Land at risk from 1m sea level rise

Watts Up With That? Commentary on puzzling things in life, nature, science, weather, climate change, technology, and recent news by Anthony Watts Isn’t there another point of view? Not one with a credible scientific basis.

The Global Challenge 86% of world’s energy comes from fossil fuel Deforestation is #2 human source of CO 2 Target 80% reduction in CO 2 emissions by 2050 to avoid worst outcomes of climate change Individual and government action needed

Responding to the climate change challenge We basically have three choices: mitigation, adaptation and suffering. We’re going to do some of each. The question is what the mix is going to be. The more mitigation we do, the less adaptation will be required and the less suffering there will be. John Holdren

The “Wedge Strategy” for Mitigation Each wedge plays a role in reducing greenhouse gas emissions Think of how our industry can contribute to these wedges. NRDC

Getting Involved Reduce emissions at home and work Learn more about climate science Talk to your friends, neighbors, and co-workers Write to decision makers Support organizations who work for those in greatest need

Take-home message Greenhouse effect – Science is unassailable: Added greenhouse gases warm the earth Multiple lines of evidence show effects of warming across the globe We need to act now to avoid the most severe harm to people and the environment.

Looking to the future: Many of the youngest among us will still be alive in the closing decades of this century. How can we shape the world will they be living in?

Recommended Reading IPCC synthesis of the best science, 2007 (already a little out-of-date) Well written by a physicist/historian, 2008 Readable, robust science, 2009 Trustworthy climate science blogs