The science of global warming: Often confused but actually clear

Similar documents
Climate Change. April 21, 2009

Extremes of Weather and the Latest Climate Change Science. Prof. Richard Allan, Department of Meteorology University of Reading

Topic 6: Insolation and the Seasons

Shepard Glacier-2005 Glacier National Park, Montana

Weather Forecasts and Climate AOSC 200 Tim Canty. Class Web Site: Lecture 27 Dec

2. Fargo, North Dakota receives more snow than Charleston, South Carolina.

Prof. Dr. Anders Levermann Junior Professor for climate modelling on long timescales, Potsdam Institute for Climate Impact Research, Potsdam, Germany

Chapter Introduction. Earth. Change. Chapter Wrap-Up

What is the IPCC? Intergovernmental Panel on Climate Change

Surface Temperature Reconstructions for the Last 2,000 Years. Statement of

Climate change: How do we know?

Science of Global Warming and Climate Change

Climate Change 2007: The Physical Science Basis

Climate Change: Global Warming Claims

Northern New England Climate: Past, Present, and Future. Basic Concepts

Climate Changes due to Natural Processes

Introduction to Climate ~ Part I ~

Global warming and Extremes of Weather. Prof. Richard Allan, Department of Meteorology University of Reading

Lecture 8. The Holocene and Recent Climate Change

Climate Modeling Dr. Jehangir Ashraf Awan Pakistan Meteorological Department

What is Climate? Understanding and predicting climatic changes are the basic goals of climatology.

Global Climate Change and the Implications for Oklahoma. Gary McManus Associate State Climatologist Oklahoma Climatological Survey

MAR110 LECTURE #28 Climate Change I

Lecture 3: Global Energy Cycle

Short-Term Climate Variability (Ch.15) Volcanos and Climate Other Causes of Holocene Climate Change

Torben Königk Rossby Centre/ SMHI

Climate Change: Past and Future ERTH 303, 3 December, 2009

Recent Climate History - The Instrumental Era.

Global temperature record reaches one-third century

ATM S 111, Global Warming Climate Models

MAR110 LECTURE #22 Climate Change

THE GREENHOUSE EFFECT

GLOBAL WARMING AND THE GREENHOUSE EFFECT

Introduction to Climate Change

GEOL 437 Global Climate Change 2/1/18: Solar radiation and the annual cycle

Today s Climate in Perspective: Hendrick Avercamp ( ) ~1608; Rijksmuseum, Amsterdam

COURSE CLIMATE SCIENCE A SHORT COURSE AT THE ROYAL INSTITUTION

Course Outline CLIMATE SCIENCE A SHORT COURSE AT THE ROYAL INSTITUTION. 1. Current climate. 2. Changing climate. 3. Future climate change

What is Climate? Climate Change Evidence & Causes. Is the Climate Changing? Is the Climate Changing? Is the Climate Changing? Is the Climate Changing?

Greenhouse Effect & Global Warming

Original (2010) Revised (2018)

XV. Understanding recent climate variability

TOPIC #12 NATURAL CLIMATIC FORCING

The ocean s overall role in climate

Earth s Heat Budget. What causes the seasons? Seasons

Hypothesis: an informal idea that has not been thoroughly tested by the scientific community. Most are discarded.

Welcome to ATMS 111 Global Warming.

Energy Systems, Structures and Processes Essential Standard: Analyze patterns of global climate change over time Learning Objective: Differentiate

ESS15 Lecture 16. Past climates, Part 1

Name Date Class. growth rings of trees, fossilized pollen, and ocean. in the northern hemisphere.

Climate Feedbacks from ERBE Data

Overview of Climate Change and Impacts

XVI. Warming and the cryosphere

Climate changes in Finland, but how? Jouni Räisänen Department of Physics, University of Helsinki

FORCING ANTHROPOGENIC

Atmospheric CO2 and mass extinctions: implications for global warming

Intergovernmental Panel on Climate Change Founded Provides science assessments. Policy-relevant, not policy-prescriptive. Major reports: 1990,

Climate. What is climate? STUDY GUIDE FOR CONTENT MASTERY. Name Class Date

Chapter 14: The Changing Climate

Global Warming: The known, the unknown, and the unknowable

Global Climate Change

Update on Climate Science. Professor Richard Betts, Met Office

lecture 12 Paleoclimate

Observed and Projected Climate Change. David R. Easterling, Ph.D. NOAA/National Climatic Data Center. Asheville, NC

Climate Variability Natural and Anthropogenic

Today. Events. Terrestrial Planet Atmospheres (continued) Homework DUE

Course Outline. About Me. Today s Outline CLIMATE SCIENCE A SHORT COURSE AT THE ROYAL INSTITUTION. 1. Current climate. 2.

NATS 101 Section 13: Lecture 32. Paleoclimate

Planetary Atmospheres (Chapter 10)

Fundamentals of Climate Change (PCC 587): Introduction

Global climate change

1990 Intergovernmental Panel on Climate Change Impacts Assessment

SOME LIKE IT HOT! An Alternative View to Climate Change. Larry Vardiman, PhD

Components of the Climate System. Lecture 2: Earth s Climate System. Pop Quiz. Sub-components Global cycles What comes in What goes out

Climate Dynamics (PCC 587): Clouds and Feedbacks

2/18/2013 Estimating Climate Sensitivity From Past Climates Outline

CLIMATE. SECTION 14.1 Defining Climate

Today we will discuss global climate: how it has changed in the past, and how the current status and possible future look.

Lecture 2: Earth s Climate System

The Oceans in a Warming World

7.5-year global trends in GOME cloud cover and humidity - a signal of climate change? Institut für Umweltphysik, Uni-Heidelberg, Germany

The science and impact of climate change.

Title: Greenhouse Gases & Climate Change 2/19. You should take notes for today s lecture & put the notes into your notebook

Climate Variability and Change Past, Present and Future An Overview

Sea level change recent past, present, future

Global Climate Change and the Implications for Oklahoma. Gary McManus Associate State Climatologist Oklahoma Climatological Survey

Lecture Impacts of rising sea-level. 2. Global warming deniers or so-called skeptics

Lecture 33. Ice shelves continued. Sea-level rise: Past and Future. 1. Impacts of rising sea-level. 2. Global warming deniers or so-called skeptics

Ocean s Influence on Weather and Climate

Earth is tilted (oblique) on its Axis!

Climate Modeling Research & Applications in Wales. John Houghton. C 3 W conference, Aberystwyth

Weather & Climate. Sanjay S. Limaye Space Science & Engineering Center University of Wisconsin-Madison

The Distribution of Cold Environments

( 1 d 2 ) (Inverse Square law);

6. What has been the most effective erosive agent in the climate system? a. Water b. Ice c. Wind

Australian Meteorological and Oceanographic Society (AMOS) Statement on Climate Change

Climate Variability and Change: Basic Concepts. Jeffrey A. Andresen Dept. of Geography Michigan State University

Satellite Observations and Climate Modeling: What They Can and Cannot Reveal About Future Climate

Earth s Heat Budget. What causes the seasons? Seasons

Transcription:

The science of global warming: Often confused but actually clear 2011 MinnTS Lecture Katsumi Matsumoto Geology and Geophysics, University of Minnesota 24 March, 2011

The science of global warming: Often confused but actually clear 2011 MinnTS Lecture Do you believe that global warming is occurring? Do you believe that global warming is caused by human activities? Do you believe that scientists are divided over global warming? Katsumi Matsumoto Geology and Geophysics, University of Minnesota 24 March, 2011

Outline The big picture: Energy in vs. energy out Detection of global warming Attribution of global warming Paleoclimate perspective Scientists on climate change

Sun What determines the temperatures of the terrestrial planets? (relative sizes are to scale) 179 ºC 477 ºC 15 ºC -47 ºC Mercury Venus Earth Mars Hot House Just Right Ice House

What determines the surface temperature? (energy in versus energy out ) Analogy: bank account balance is determined by income and expense Houghton (2009)

Infrared radiation from a building (depends on temperature) Charles (2009)

Infrared radiation from Earth (again depends on temperature) Northern hemisphere winter (Sverdrup, 2006)

CO2 in atmosphere will absorb thermal radiation In > Out, so warms, but when will it stop? Human emissions of CO 2 increases the greenhouse effect and reduces energy out Houghton (2009)

Earth will stop warming when it is warm enough to radiate out as much energy as before Earth s surface Houghton (2009) Global warming is a natural response of the planet to restore radiative balance...something we ve known for a long time

A long history 1681 : greenhouse effect of glass (Mariotte) 1824 : greenhouse effect of atmosphere (Fourier) 1861 : laboratory confirmation of the greenhouse properties of CO 2 and H 2 O (Tyndall) 1895 : prediction of CO 2 -induced warming (Arrhenius)

All this history lead to the Keeling Curve

Today s radiative imbalance: 2 X-mas light bulbs/m 2 Physics predicts that there must be global warming! 2 W/m2 Hansen (2004)

Detection of global warming

Annually averaged, global surface temperature Instrumental records 1653 - First meteorological network in Italy 1873 - IMO (later WMO) to standardize temperature data 550 million temp readings! Figure 1.3, IPCC AR4

Satellite data 2005-1979 Historical data (Fig. TS6, IPCC AR4) IPCC TAR

Shrinking arctic sea ice NSIDC Northwest Passage

Greenland is melting Jakobshavn Ice Stream Hansen (2004)

Satellite altimetry data net loss of ice mass (NASA)

Glacial earthquakes (Ekström, Tsai, Nettles, 2006)

Global ocean heat content The smoking gun of GW 10 22 J 2003-1961 2003-1993 About 90% of heat from GW into the ocean...but small temp change Reason for delay in climate response (Fig 5.4, IPCC AR4)

~1 mm/yr globally Wikipedia data from Douglas (1997)

Detection winter in Lake Superior Period of ice cover in Bayfield, WI First boat Last boat Howk (2009)

Other organisms noticing the change: (Analysis of ~1500 species on migration, flowering, reproduction...) Root et al., 2003

Attribution of global warming

Attribution of global warming What do we need to show? (1) Anthropogenic forcings are doing it (2) Natural forcings are insufficient Orbital variations Tectonic activity Solar variability Internal variability How to show this? Earth science no control experiment Use global climate models

Forcings IPCC TAR

How reliable are the global climate models? (show movies) 1) Models based on established physical laws 2) Ability to model key aspects of current climate large scale temperature, precipitation, radiation, wind, ocean temperatures, currents, ice cover, seasonality of monsoons and storm tracks 3) Examine model predictions of: past climate, larger warming of nighttime temperatures, larger NH warming, short-term cooling following volcanic eruptions Uncertainties in tropical precipitation, El Nino, representation of clouds, small scale projections IPCC AR4 FAQ8.1

(Ed Wolfe, USGS, 1991) 1991 Mt Pinatubo In 1988 Hansen predicted the radiative effect of a volcanic eruption later proved correct (-1 W m -2 )

Models correctly predict impacts of volcanic eruptions Height of lower atmosphere obs obs Temperature model mean (Fig. 9.5 & 9.14, IPCC AR4)

More NH warming 2005-1979 Other fingerprinting of anthropogenic warming: faster night time warming etc. Acceleration of warming (Fig. TS6, IPCC AR4) IPCC TAR

Paleoclimate perspective

(Pictures from www.winona.edu) Glaciation and Moraines in Minnesota

Interglacial (today) G-I cycles Glacial (20,000 yrs ago) CLIMAP (1981)

18,000 YEARS AGO Note the ice, lakes and coasts

14,000 YEARS AGO

13,000 YEARS AGO

12,000 YEARS AGO

11,000 YEARS AGO

10,000 YEARS AGO

9,000 YEARS AGO

8,000 YEARS AGO

7,000 YEARS AGO

We can reconstruct past ice by examining isostatic rebound 6,000 YEARS AGO

Ice age viewed from ice and ocean sediment cores (climate and CO2 are highly correlated) Houghton (2009)

The last glacial cycle Houghton (2009)

Past sea level vs. global temperature Archer (2007)

Climate change deniers

Scientists on the problem Jim Hansen in 1988 testified to US Senate that he was certain that record warmth was not natural Got the ball rolling (UNFCCC in 92) An almost complete unanimity among climate scientists on the reality of global warming Complete disconnect from public perception...

Scientific consensus What is consensus? And how do we know it exists? Experts read peer-reviewed publications, have informal discussions in the hallways and conferences...usually hard for the public to assess What is peer-review? Careful, highly critical examination of the work being proposed for publication; very toug Anyone can say anything, but not everyone can get research results published in peer-reviewed journals Climate science consensus unusually public IPCC assessment of the state of climate science on the basis of peer-reviewed publications

Oreskes survey of peer-reviewed publications Searched 8500 journal publications between 1993 and 2003 w/ global climate change. Is global warming occurring and are humans partly responsible?

Who s arguing that global warming is here? Intergovernmental Panel on Climate Change 1990 qualitative persuasion of human interference 1995 discernable human influence on global climate 2001 most of the warming over the last 50 yrs is likely attributable to human activities 2007 very likely (>90% probability) National science academies Professional societies whose membership expertise bears on global climate change Reports and statements by IPCC, academies, and societies drafted through a careful process involving many opportunities to comment, criticize, and revise won t deviate much from membership opinions

Who are the deniers? Fred Singer, electrical engineer Works with Exxon, American Petroleum Institute: proposed a $5 million campaign to convince the public that the science of global warming is riddled with controversy and uncertainty Newsweek 2007 Patrick Michaels fellow of the Cato Institute Paid at least $100,000 by companies involved in coal-fired power production to make the public case against climate change Richard Lindzen, MIT professor in meteorology gets funding from OPEC, $2500/day consulting fee Michael Crichton! (invited by Congress to testify)

Myths and skepticisms look these up yourself 1. Scientists can t even predict next week s weather 2. Climate model predictions have never been tested 3. Hansen has been wrong before 5. Global warming + global dimming -> Southern warming 6. GCMs don t have clouds 7. Climate models can t explain the past 8. Climate is chaotic and thus not predictable 9. Regional and local climate predictions are bogus

Summary Physics predicts global warming when incoming solar radiation is greater than outgoing terrestrial radiation Detection by observations - warming of atmosphere, ocean, Arctic sea ice, Greenland melting, sea level rise Attribution to humans - use of global climate models, fingerprinting predictions validated, observed changes cannot be explained with natural causes alone Paleoclimate perspective CO 2 and climate are highly correlated; so are sea level and global temperature Complete unanimity among active climate scientists