Global Warming Status 1. Knowledge Gap Between - What is Understood (science) - What is Known (public/policymakers) 2. Planetary Emergency - Climate Inertia.

Slides:



Advertisements
Similar presentations
Shrinking Ice: The Global Impact of Polar Warming World Meteorological Day Presentation Geneva 23 rd March 2007 Chris Rapley Director British Antarctic.
Advertisements

Global Warming Status 1. Knowledge Gap Between - What is Understood (science) - What is Known (public/policymakers) 2. Planetary Emergency - Climate Inertia.
Royal Society Coral Crisis Working Group 6 July 2009.
Uncertainty, Lags, and Nonlinearity: Challenges to Governance in a Turbulent World Thomas Homer-Dixon CIGI Chair of Global Systems Balsillie School of.
Global Warming: we’re on thin ice! Evidence of global warming Denial of global warming Convergence of evidence Compton Tucker NASA/Goddard Space Flight.
MET 12 Global Warming: Lecture 10
Climate Change: Science, Impacts, Risks and Response Scientific Basis for Human Induced Climate Change Jagadish Shukla Department of Atmospheric, Oceanic.
Greenland Ice Sheet melting and MOC Aixue Hu, Gerald A. Meehl, Weiqing Han and Jianjun Yin.
1 Changing Earth’s Climate. `The balance of evidence suggests that there is a discernible human influence on global climate ' Intergovernmental Panel.
Global Warming Status 1. Knowledge Gap Between - What is Understood (science) - What is Known (public/policymakers) 2. Planetary Emergency - Climate Inertia.
Status of the Matter 1. A Knowledge Gap - What is Understood (scientists) - What is Known (public/policymakers) 2. The Climate Crisis - Positive Feedbacks.
IPCC 4 th Assessment Report: WG1: Physical Science Basis Chapter 2.
Air Pollutant Climate Forcings within the Big Climate Picture * Jim Hansen March 11, 2009 Climate Change Congress Global Risks, Challenges & Decisions.
1988 Testimony: Conclusions 1. Earth is warmer in 1988 than at any time in the history of instrumental measurements 2. Global warming is now large enough.
1 Uncertainty, Lags, Nonlinearity and Feedbacks: New Terms for a New Millennium We must transition out of our 19 th century view of Technology as basic.
Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics.
NASA. Global Warming 101 Roy W. Spencer, Ph.D Principal Research Scientist The University of Alabama In Huntsville 19 March 2007.
CO 2, CH 4 and temperature records from Antarctic ice core data Source: Vimeux, F., K.M. Cuffey, and Jouzel, J., 2002, "New insights into Southern.
Global Climate Change Overview Michael D. Mastrandrea, Ph.D. Deputy Director, Science, IPCC Working Group II and Assistant Consulting Professor Woods Institute.
Recent results from GRACE in Greenland and Antarctica Isabella Velicogna* and John Wahr** * ESS, University of California Irvine, Irvine CA ** Dept Of.
Ocean Response to Global Warming William Curry Woods Hole Oceanographic Institution Wallace Stegner Center March 3, 2006.
Brief Climate Discussion William F. Ryan Department of Meteorology The Pennsylvania State University.
Global Sea Level Rise Laury Miller NOAA Lab for Satellite Altimetry.
Rising Temperatures. Various Temperature Reconstructions from
Part 4 Temperature Rise. Global Average Temperature Change for the Past 11,300 Years (Holocene) (Science, 8 March 2013: Vol. 339 no. 6124, pp )
Part 3 Climate Change Basics and Past Climates. The Greenhouse Effect.
The Basic Science of Climate Change Janina Moretti September 6, 2012.
New Core Curriculum Foundations of Scientific Process Current Environmental Problems.
Areas of Focus within The Weather and Climate Unit: What is weather?, Climate, Importance of the Atmosphere, Components of the Atmosphere, Layers of the.
Arctic Climate Change John C. Fyfe Canadian Centre for Climate Modelling and Analysis.
Climate Science Context Brian Hoskins Director Grantham Institute for Climate Change, Imperial College Professor of Meteorology, University of Reading.
Global Warming: Consequence of Fossil Fuel Use Do Now: Please copy the following definitions into your notes: Greenhouse Effect: The trapping of heat by.
Human-Made Climate Change: A Scientific, Moral and Legal Issue * James Hansen 4 December 2010 Circolo dei Lettori Rome, Italy * Statements relating to.
Oluwakemi Izomo Hans-Peter Plag October 6, 2014 Trends or Transitions What does this mean for Sea Level The Challenge: Leaving the Holocene Anticipating.
The Changing Environment and the Next Decade of Environmental Prediction Models by Michel Béland Incheon, November 17th 2009, Pre-CAS Technical Conference.
Earth’s Changing Environment Lecture 13 Global Warming.
There are gases in our Earth’s atmosphere which can trap heat toward the Earth’s surface. This is called the greenhouse effect. The greenhouse effect.
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.
1 Geologic Perspective on Climate  El Nino  The last 1,000 Years: Natural Variability?  The Ice Ages and their cause  The world the Dinosaurs inhabited.
The realities of climate change S. Mulkey June 2006 Stephen Mulkey, PhD Director, Research & Outreach/Extension School of Natural Resources and Environment.
1 What causes global warming? You do,silly! Kevin Cummins Sierra Club Volunteer.
Preventing Dangerous Climate Change Session 10 Neil Leary Changing Planet Study Group July 19-22, 2010 Cooling the Liberal Arts Curriculum A NASA-GCCE.
Climate and Change 7. Is this enough evidence that global warming is happening …. if so how bad do people think the situation is?
Global Warming And the Planetary Water Cycle Ruth Curry Woods Hole Oceanographic Institution Ruth Curry Woods Hole Oceanographic Institution Global Warming.
The realities of climate change The balance of evidence suggests that there is a discernible human influence on global climate. IPCC 2nd Assessment Report,
There are gases in our Earth’s atmosphere which can trap heat toward the Earth’s surface. This is called the greenhouse effect. The greenhouse effect.
Citizen’s Climate Lobby 2015 Great North Wind Country Regional Conference Nov 6-8, 2015 November, 2015 #CCLWind2015.
Ocean Response to Global Warming/Global Change William Curry Woods Hole Oceanographic Institution Environmental Defense May 12, 2005 Possible changes in.
Evidence of global warming Global Warming have been occurring for the last 30-50yrs Here is a example of how global warming is affecting…
Are Humans Causing Global Warming? How do we know? What is the Evidence?
Status of the Matter 1. A Knowledge Gap - What is Understood (scientists) - What is Known (public/policymakers) 2. The Climate Crisis - Climate Inertia.
Impacts of Climate Change on Physical Systems Lesson Plan 4 – Day 2 PPT
Global Climate Change and my career Your Name. Global climate change … is unequivocal, is almost certainly caused mostly by us, is already causing significant.
Presenters: S.SUAT ALKIS & A. SEFA CALISKAN. I BET YOU THE HOTTEST TOPIC OF THIS CLASS IS CLIMATE CHANGE.
IPY/NSTA Web Seminar: Arctic and Antarctic Living Systems LIVE INTERACTIVE YOUR DESKTOP Thursday, December 20, 2007.
1 Since 1850:Ref: IPCC- AR4 Temperature is up 1°C (1.8°F) and climbing steeply Sea Level is up 2 cm (5”) and climbing fast (due to melting ice & snow)
Climate Change Mark C. Serreze Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO.
James Hansen, Goddard Institute for Space Studies, NASA Long-term feedback systems more powerful than thought previously Amplification – albedo, methane,
How Convection Currents Affect Weather and Climate.
Prompt 1Prompt 1  Addressing Question 1 in the GCC Guide: Discuss how global climate change has affected the abiotic factors of earth. This includes.
Climate Threat to the Planet:* Implications for Energy Policy and Intergenerational Justice Jim Hansen December 17, 2008 Bjerknes Lecture, American Geophysical.
Chapter 23 The Atmosphere, Climate, and Global Warming.
IPCC First Assessment Report 1990 IPCC Second Assessment Report: Climate Change 1995 IPCC Third Assessment Report: Climate Change 2001 IPCC Fourth Assessment.
Global Warming Status 1. Knowledge Gap Between - What is Understood (science) - What is Known (public/policymakers) 2. Planetary Emergency - Climate Inertia.
Ice sheets and their relation to sea level
Global Warming Status 1. Knowledge Gap Between 2. Planetary Emergency
Change in fresh water inflow from glaciers and rivers
Changes in surface climate of the tropical Pacific
Changes in surface climate of the tropical Pacific
Changes in surface climate of the tropical Pacific
Presentation transcript:

Global Warming Status 1. Knowledge Gap Between - What is Understood (science) - What is Known (public/policymakers) 2. Planetary Emergency - Climate Inertia Warming in Pipeline - Tipping Points Could Lose Control 3. Good News & Bad News - Safe Level of CO 2 < 350 ppm - Multiple Benefits of Solution

Basis of Understanding 1. Earths Paleoclimate History 2. On-Going Climate Changes 3. Climate Models

Green Triangle = Volcano; Red Box = El Nino; Blue Semicircle= La Nina

Metrics for Dangerous Change Extermination of Animal & Plant Species 1. Extinction of Polar and Alpine Species 2. Unsustainable Migration Rates Ice Sheet Disintegration: Global Sea Level 1. Long-Term Change from Paleoclimate Data 2. Ice Sheet Response Time Regional Climate Disruptions 1. Increase of Extreme Events 2. Shifting Zones/Freshwater Shortages

Tipping Point Definitions 1. Tipping Level - Climate forcing (greenhouse gas amount) reaches a point such that no additional forcing is required for large climate change and impacts 2. Point of No Return - Climate system reaches a point with unstoppable irreversible climate impacts (irreversible on a practical time scale) Example: disintegration of large ice sheet

Extent (million sq km)

Observations: Domingues, C.M. et al., Nature 453, , Model: Hansen, J. et al., Science 308, , 2005.

Arctic Sea Ice Criterion* 1. Restore Planetary Energy Balance CO 2 : 385 ppm ppm 2. Restore Sea Ice: Aim for -0.5 W/m 2 CO 2 : 385 ppm ppm Range based on uncertainty in present planetary energy imbalance (between 0.5 and 1 W/m 2 ) * Assuming near-balance among non-CO 2 forcings

Konrad Steffen and Russell Huff, CIRES, University of Colorado at Boulder Greenland Total Melt Area – 2007 value exceeds last maximum by 10%

Melt descending into a moulin, a vertical shaft carrying water to ice sheet base. Source: Roger Braithwaite, University of Manchester (UK) Surface Melt on Greenland

Jakobshavn Ice Stream in Greenland Discharge from major Greenland ice streams is accelerating markedly. Source: Prof. Konrad Steffen, Univ. of Colorado

Greenland Mass Loss – From Gravity Satellite

Sea Level Criterion* 1. Prior Interglacial Periods CO 2 <~ 300 ppm 2. Cenozoic Era CO 2 <~ 300 ppm 3. Ice Sheet Observations CO 2 < 385 ppm * Assuming near-balance among non-CO 2 forcings

Pier on Lake Mead.

Rongbuk Glacier Rongbuk glacier in 1968 (top) and The largest glacier on Mount Everests northern slopes feeds Rongbuk River.

Black bar: ice loss in Curve:years until ice gone, at that loss rate. Paul, F. et al., Geophys. Res. Lett. 31, L21402, Ice Loss

Coral Reef off Fiji (Photo: Kevin Roland) Stresses on Coral Reefs

Assessment of Target CO 2 Phenomenon Target CO 2 (ppm) 1. Arctic Sea Ice Ice Sheets/Sea Level Shifting Climatic Zones Alpine Water Supplies Avoid Ocean Acidification Initial Target CO 2 = 350* ppm *assumes CH 4, O 3, Black Soot decrease

Target CO 2 : < 350 ppm To preserve creation, the planet on which civilization developed

The fraction of CO 2 remaining in the air, after emission by fossil fuel burning, declines rapidly at first, but 1/3 remains in the air after a century and 1/5 after a millennium (Atmos. Chem. Phys. 7, , 2007).

Initial Target CO 2 : 350 ppm Technically Feasible (but not if business-as-usual continues) Quick Coal Phase-Out Critical (long lifetime of atmospheric CO 2 ) (must halt construction of any new coal plants that do not capture & store CO 2 )

(a) Fraction of each fossil fuel in 2007 CO2 emissions (b) Fraction of each in todays airborne CO2 amount

Fraction = Coal / (Coal + Oil + Natural Gas)

Free Will Alternative 1. Phase Out Coal CO 2 Emissions - by 2025/2030 developed/developing countries 2. Rising Carbon Price - discourages unconventional fossil fuels & extraction of every last drop of oil (Arctic, etc.) 3. Soil & Biosphere CO 2 Sequestration - improved farming & forestry practices 4. Reduce non-CO 2 Forcings - reduce CH 4, O 3, trace gases, black soot

Carbon Tax & 100% Dividend 1. Tax Large & Growing (but get it in place!) - tap efficiency potential & life style choices 2. Entire Tax Returned - equal monthly deposits in bank accounts 3. Limited Government Role - keep hands off money! - eliminate fossil subsidies - let marketplace choose winners - change profit motivation of utilities - watch U.S. modernize & emissions fall!

Key Elements in Transformation Low-Loss Electric Grid Clean Energy by 2020 (West) & 2030 Allows Renewable Energy Ascendancy Carbon Tax and 100% Dividend Tax at First Sale of Coal/Oil/Gas Tax Can Rise & Spur Transformations 100% or Fight! No Alligator-Shoes!

Basic Conflict Fossil Fuel Special Interests vs Young People & Nature (Animals) Fossil Interests: God-given fact that all fossil fuels will be burned (no free will) Young People: Hey! Not so fast! Nice planet you are leaving us!

What are the Odds? Fossil Interests: have influence in capitals world-wide Young People: need to organize, enlist others (parents, e.g.), impact elections Animals: not much help (dont vote, dont talk)

The Challenge We can avoid destroying creation! (+cleaner planet, + good jobs!) We have to figure out how to live without fossil fuels someday… Why not now?

Whats the Problem?* 1. No Strategic Approach %CO 2 Reduction Approach Doomed 2. No Leadership for Planet & Life Businesses Rule in Capitals 3. Greenwash Replaces Strategy * Just my opinions, of course

Web Site includes Letter to Prime Minister Fukuda Global Warming Twenty Years Later: Tipping Points Near (todays statement) Target Atmospheric CO 2 : Where Should Humanity Aim?