Evidence for Milankovitch theory (wikipedia!). Px272 Lect 3: Forcing and feedback.

Slides:



Advertisements
Similar presentations
Earths Climate System Dr. R. M. MacKay. Natural and Anthropogenic Climate Forcing.
Advertisements

Michael B. McElroy ACS August 23rd, 2010.
Climate Change and the Oceans
1 Climate Change Science Kathryn Parker U.S. Environmental Protection Agency Rocky Mountain National Park March 21, 2007 July 1932July 1988 Glacier National.
A discussion of “The Science of Climate Change” From Richard Tol’s 2014 book: Climate economics: economic analysis of climate, climate change and climate.
Global Warming and Climate Sensitivity Professor Dennis L. Hartmann Department of Atmospheric Sciences University of Washington Seattle, Washington.
Climate Change.
IPCC Climate Change Report Moving Towards Consensus Based on real world data.
Outline Review of Ocean Stratification and Circulation Recent historical Climate Change External Climate Forcings Natural Climate Variability Paleoclimatology.
IPCC Climate Change Report Moving Towards Consensus Based on real world data.
Air Pollutant Climate Forcings within the Big Climate Picture * Jim Hansen March 11, 2009 Climate Change Congress Global Risks, Challenges & Decisions.
PX272 revision summary Main topics: Evidence of Warming Atmospheric Greenhouse effect Forcing and Feedbacks Scenarios and Modelling Consequences of Warming.
Evidence for Milankovitch theory (wikipedia!). Px272 Lect 3: Forcing and feedback Balance of solar incoming, and earth emitted outgoing radiation Increments.
Forcing the Climate. Climate Forcing Radiative Forcing Non-Radiative Forcing Change in the Earth’s energy balance.
Global temp 140 years IPCC Summary for Policymakers 2001.
Many past ice ages were caused by… 1.Volcanic activity 2.Photosynthesis 3.Prehistoric humans 4.Changes in the earth’s orbit 5.Sun spots.
Global Energy Balance Te/KTm/KTsurf/K Venus Earth Mars [Jupiter ]
Many past ice ages were caused by… 1.Volcanic activity 2.Photosynthesis 3.Prehistoric humans 4.Changes in the earth’s orbit 5.Sun spots.
Coupled Ocean- Atmosphere General/Global Circulation Models ~100km horizontal res’n; Finer (~2) for ocean than atmosphere. ~20 layers atmosphere; ~20 layers.
Coupled Ocean- Atmosphere General/Global Circulation Models ~100km horizontal res’n; Finer (~2) for ocean than atmosphere. ~20 layers atmosphere; ~20 layers.
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.
The challenges of climate change
Humans are the Primary Cause of Global Warming The science indicates humans are the primary cause of global warming at the >95% probability (In science.
Class #11: Wednesday July 21 Earth’s changing climate Chapter 16 1Class #11 Wednesday, July 21.
Global Warming Thony Castellanos. Global Warming What is Global Warming? Global Warming is defined as the increase of the average temperature on Earth.
Rising Temperatures. Various Temperature Reconstructions from
4. Models of the climate system. Earth’s Climate System Sun IceOceanLand Sub-surface Earth Atmosphere Climate model components.
Climate Change – 1: Background
Lecture 14 Climate Sensitivity, thermal inertia. Climate Sensitivity The change in equilibrium temperature per unit of radiative forcing.
I. I.Climate Change – Greenhouse Gases A. A.Background Greenhouse Effect Gases absorb heat Natural Greenhouse Effect Mean planetary temperature = 15 o.
1 Observed physical and bio-geochemical changes in the ocean Nathan Bindoff ACECRC, IASOS, CSIRO MAR University of Tasmania TPAC.
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.
Heating of the Atmosphere
Why is the global temperature not increasing more rapidly? Lennart Bengtsson ISSI ESSC.
Human Induced Climate Change: The IPCC Fourth Assessment AKE-Programme Annual Conference the German Physical Society (DPG) Regensberg, March
Alan Robock Department of Environmental Sciences Rutgers University, New Brunswick, New Jersey USA
Projecting changes in climate and sea level Thomas Stocker Climate and Environmental Physics, Physics Institute, University of Bern Jonathan Gregory Walker.
Climate Literacy Session: Causes Peter Coombe August 5, 2015.
Earth’s Energy Balance Complexity, climate change and human systems HCOL 185.
Lecture Outlines Physical Geology, 14/e Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Plummer, Carlson &
1 Observed physical and bio-geochemical changes in the ocean Nathan Bindoff ACECRC, IASOS, CSIRO MAR University of Tasmania TPAC.
Understanding the Science of Climate Change Susquehanna University January 9, 2015
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.
INTERGOVERNMENTAL PANEL ON CLIMATE CHANGE (IPCC) Working Group I Working Group I Contribution to the IPCC Fourth Assessment Report Climate Change 2007:
Temperature Anomaly (  C) Annual Solar Radiation (W m -2 )
International Environment Forum Conference Ottawa October 12 th, 2007 John M R Stone Carleton University.
Human fingerprints on our changing climate Neil Leary Changing Planet Study Group June 28 – July 1, 2011 Cooling the Liberal Arts Curriculum A NASA-GCCE.
CHAPTER 15 THE EARTH’S CHANGING CLIMATE CHAPTER 15 THE EARTH’S CHANGING CLIMATE.
Anthropocene physical basis of climate spring 2011 Introduction and UNEP reports Observations –Emissions and other natural forcingsEmissions and other.
TOPIC III THE GREENHOUSE EFFECT. SOLAR IRRADIANCE SPECTRA 1  m = 1000 nm = m Note: 1 W = 1 J s -1.
Climate Change: Causes and Evidence Part 1.. Climate Change What is the cause? How do we know? What is the Keeling Curve? How much CO 2 is in the atmosphere.
Climate Change. Any long-term significant change in the average weather of a region or the Earth as a whole Includes changes in average temperature, precipitation.
1.Abrupt climate change 2.Greenhouse gases in the past 3.Climate change simulation Atlas Week 2008 Climate Change: How Physics Lays the Basis.
Modelling the climate system and climate change PRECIS Workshop Tanzania Meteorological Agency, 29 th June – 3 rd July 2015.
AOS 101 March 4/6 Climate Change: Introduction.
Chapter 13: The Earth’s Changing Climate Climate change Climate change Possible causes of climatic change Possible causes of climatic change Global warming.
CHAPTER 15 THE EARTH’S CHANGING CLIMATE CHAPTER 15 THE EARTH’S CHANGING CLIMATE.
03/02 Please, turn in your homework! “The World We Create” NATS 101 Section 6.
© Yann Arthus-Bertrand / Altitude The Summary for PolicyMakers - final plenary The Summary for PolicyMakers - final plenary Michael Prather, LA, Chapter.
Ch16: Global Warming-part 1 What is it? What causes it? Focus on Carbon Dioxide.
Cloud formation and Atmospheric CO2. Cloud Formation There are a few ways clouds form 1.Rising Hot Air 2.Warm air over a cold body of water 3.On Mountainsides.
Climate change: the IPCC 5 th assessment and beyond… Prof. Martin Todd Dept. Geography University of Sussex
Global energy balance SPACE
Chapter 14: Climate Change
IPCC Climate Change 2013: The Physical Science Basis
IPCC Climate Change Report
Global Warming Effects of increase CO2
Chapter 13: The Earth’s Changing Climate
Points for discussion Have human activities changed the composition of Earth’s atmosphere? Has Earth’s temperature changed in the past 150 years? In the.
Global Change Welcome Meeting, Edinburgh, October 15th 2010
Presentation transcript:

Evidence for Milankovitch theory (wikipedia!)

Px272 Lect 3: Forcing and feedback

Figure TS.5 Anthropogenic Radiative Forcings IPCC AR4 2007

Aerosol direct forcing Nature 438, 1138 (Dec 2005)

Aerosol indirect forcing effect

Figure TS.5 Radiative Forcings IPCC AR4 2007

G/house gas and aerosol buildup Rise of global Greenhouse gases with industrial era ( IPCC S/PM 2001) CO2 emissions continue to accelerate (IPCC 2007)

IPCC 2007

(b) Sulphate aerosols deposited in Greenland ice Industrial sulphate aerosols appear to have peaked for Greenland record.

Response and Feedback

Water vapour feedback Water saturation (mid troposphere) <-Simulation Observed->

Cloud Radiation Feedback Potentially quite large Altitude dependent Net highly uncertain

Ocean Circulation Feedback Huge heat capacity - delays warming Circulation driven by: temperature difference salinity difference rotation of earth - redistributes regionally: more winter heat to NW Europe from ocean transport than from sun - global heat redistribution still dominated by atmosphere

Ice Albedo Feedback

Arctic sea ice decrease

(ca 2002)

Changes in atmospheric composition IPCC fig 3.4