Final 2 weeks of class… Final exam will be posted on-line next week… Next week - Dale Lockwood: The “should ecologists be neutral or advocates” debate…

Slides:



Advertisements
Similar presentations
What can we learn about sink efficiencies from trends in CO 2 airborne fraction ? M. Gloor, J. Sarmiento, N. Gruber University of Leeds, Princeton University,
Advertisements

Regional trends in the land carbon cycle and the underlying mechanisms over the period, S. Sitch, P. Friedlingstein, G. Bonan, P. Canadell, P.
Short Background on Climate Change and Greenhouse Gases Dr Ruth Nussbaum ProForest Presentation to the RSPO GHG WG2 meeting in Feb 2010.
Michael B. McElroy ACS August 23rd, 2010.
1 Climate change impacts and adaptation: An international perspective Chris Field Carnegie Institution: Department of Global Ecology
1 Margaret Leinen Chief Science Officer Climos Oceans: a carbon sink or sinking ecosystems?
5.2: The Greenhouse Effect : Carbon cycle.
LTER Planning Process Science Task Force (STF) Report to NSF September 2005.
Ocean Circulation And Current Carbon Cycle For more detail see the course materials for Lynne Talley’s Course at SIO.
Carbon Cycle and Ecosystems Important Concerns: Potential greenhouse warming (CO 2, CH 4 ) and ecosystem interactions with climate Carbon management (e.g.,
Global Warming and Climate Sensitivity Professor Dennis L. Hartmann Department of Atmospheric Sciences University of Washington Seattle, Washington.
(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Ecosystems (from IPCC WG-2, Chapters 4,9-16) Ecosystems Primary Source: IPCC WG-2 Chapter 4 - Ecosystems, their.
Changing Nature of Rural Landscapes and Communities John Williams NSW Commissioner for Natural Resources.
Consequences of Climate Change for Rangelands: Unexpected Consequences of More Extreme Rainfall Patterns Alan K. Knapp Colorado State University Jana Heisler-White.
Earth Systems Science Chapter 1 I. CHANGES it is the nature of dynamic systems to change, often even in the absence of external “forcings”. Some important.
Course goals 1)Have you develop a firm understanding of the concepts and mechanisms of ecosystem ecology; 2)Have you enhance your understanding of how.
1 “Our Great Geophysical Experiment” Source: NOAA, Hurricane Katrina shortly before landfall.
Milankovitch Theory of Climate Change The Earth changes its: a)orbit (eccentricity), from ellipse to circle at 100,000 year cycles, b)wobble (precession),
QUESTIONS 1.How do elements in the lithosphere get transferred to the atmosphere? 2.Imagine an early Earth with a weak Sun and frozen ocean (“snowball.
CLIMATE CHANGE Global Temperatures: Past, Present, and Future.
BIOGEOSPHERIC CHANGE RESPONSE OF ECOSYSTEM STRUCTURE AND DISTRIBUTION TO ALTERED FORCING © 2007 T. Kittel Clarice Bassi - Anavilhanas.
1. How has the climate changed during the recent past? 2. What can we say about current climate change? 3. How do climate models work and what are their.
Essential Principles Challenge
Climate Change and Forestry Allan L. Carroll, Ph.D. Natural Resources Canada Canadian Forest Service Pacific Forestry Centre Victoria, Canada Senior Research.
The Science of Climate Change Why We Believe It and What Might Happen Dave Stainforth, University of Exeter Tyndall Centre for Climate Change Research.
IB BIOLOGY 5.2 The greenhouse effect. The Carbon Cycle Carbon exists in many forms:  Atmospheric gases (CO2 and Methane- CH4)  Dissolved CO2 in aquatic.
New Core Curriculum Foundations of Scientific Process Current Environmental Problems.
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
Climate Change Impacts & Resource Management Stephen T. Gray Water Resources Data System WY State Climate Office University of Wyoming.
European capacity building initiativeecbi Climate Change: an Introduction ecbi Workshops 2007 Claire N Parker Environmental Policy Consultant european.
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,
I.) WAYS OF KNOWING (Scientific Method, Observations, Technology, Informatics, Habits of Mind, Faith) “Reflection on how we know what we believe will help.
Global Megacycles and Trends: Setting the Agenda for 21 st Century Science Emerging Issues: Berrien Moore III University of New Hampshire New Challenges.
Climate Change and Ecosystems IV Presidential Meeting CGDD & IFHC Sao Paulo, Brazil March 7, 2009 Thomas E. Lovejoy Biodiversity Chair, The Heinz Center.
Chapter 10 Climate Change Geosystems 6e An Introduction to Physical Geography Robert W. Christopherson Charles E. Thomsen.
Modern Climate Change Darryn Waugh OES Summer Course, July 2015.
 Abiotic: nonliving parts  Biotic: living parts When these factors are altered in some way the ecosystem is affected.
CE 401 Climate Change Science and Engineering predictions from models global energy 22 February 2011 team selection and project topic proposal (paragraph):
Biotic and Abiotic Factors Chapters 3.3, 4.2 and 6.3)
Landscape Ecology: Conclusions and Future Directions.
Welcome Grant from National Science Foundation: Fire, Atmospheric pCO 2, and Climate as Alternative Primary Controls of C 4 -Grass Abundance: The Late-Quaternary.
UDnFmNTYhttps:// UDnFmNTY gmFa0r04https://
ATOC 220 Global Carbon Cycle Recent change in atmospheric carbon The global C cycle and why is the contemporary atmospheric C increasing? How much of the.
Climate Change: an Introduction ecbi Workshops 2007 Claire N Parker Environmental Policy Consultant european capacity building initiative initiative européenne.
Modelling the climate system and climate change PRECIS Workshop Tanzania Meteorological Agency, 29 th June – 3 rd July 2015.
Boreal forest resilience Some initial thoughts BNZ LTER meeting, March 2009 Terry Chapin & Jill Johnstone.
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.
CLIMATE CHANGE. CLIMATE IS: Long term Wide area Seasonal changes Measured over long spans of time CLIMATE is the average of many years of weather observation.
Metrics and MODIS Diane Wickland December, Biology/Biogeochemistry/Ecosystems/Carbon Science Questions: How are global ecosystems changing? (Question.
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
Chapter 4 Ecosystems and Communities. Copyright Pearson Prentice Hall 4-1 The Role of Climate.
SCI 256 mart Expect Success/sci256martdotcom
Earth2Class Workshops for Teachers Taro Takahashi Lamont-Doherty Earth Observatory of Columbia University November 21, 2009 State of Carbon Cycle in 2009.
Unit 15 – Ecology and Plant Life Functions
Chapter 19 Global Change.
The Human Component of the Global Carbon Cycle
Pre-anthropogenic C cycle and recent perturbations
Chapter 4: Ecosystems & Communities
Greenhouse Effect and Global Warming
Global Change Biology Objectives
DO NOW Turn in Review #25. Pick up notes and Review #26.
AVERAGE JANUARY TEMPERATURE (°F)
EVSC 1300 Global Warming.
Biodiversity and Climate Change
Chapter 19 Global Change.
Nutrient Cycles in Nature Ch. 3-3
Mitigation: Major Climate Change Can Be Avoided. Warren M
Recent Climate Change Chapter 14 Lesson 3.
Presentation transcript:

Final 2 weeks of class… Final exam will be posted on-line next week… Next week - Dale Lockwood: The “should ecologists be neutral or advocates” debate…

What is “Global Change”? Established in 1989 and codified in 1990 by the Global Change Research Act An Act - To require the establishment of a United States Global Change Research Program aimed at understanding and responding to global change, including the cumulative effects of human activities and natural processes on the environment, to promote discussions toward international protocols in global change research, and for other purposes. Global change—”changes in the environment that may alter the capacity of the Earth to sustain life”

Time series of departures from the 1961 to 1990 base period for an annual mean global temperature of 14.0°C (bars) and for a carbon dioxide mean of 334 ppmv (solid curve) during the base period, using data from ice cores and (after 1958) from Mauna Loa (4). Many other factors (such as the effects of volcanic eruptions and solar irradiance changes) are also important. (Karl and Trenberth 2003) What most people hear when you say Global Change (Global warming or increasing air temperatures…)

Dave Theobald

Reid & Miller (1989) the Scientific Basis for Conserving Biodiversity, World Resources Institute; Vitousek (1994) Ecology 75: ; National Oceanic and Atmospheric Administration (NOAA), USA. (Slide courtesy of Berrien Moore, USA) Climate change is only one aspect of Global Change D. Wall

Ecological Systems Goldewijk and Battjes (1997) Reid & Miller (1989) Vitousek (1994) NOAA Global Change J.A. Klein

But climate and CO 2, biodiversity and even land cover have varied in the past. Can’t we learn from the past? Paleoclimatic Studies Understanding how earth systems (biotic and physical) have changed on a range of time scales in the past can help us understand what the future may hold. But….

Overpeck et al The past can provide insight, but history provides few analogs for the type of climate change forecast… IPCC predictions

Ecological world today new global drivers of change rapid pace of change Global change “heading towards the unknown” Ecological world in textbooks natural systems in equilibrium local disturbance drives change Local change within a “backdrop of the known” Is the situation likely to get any better?

Updated from Le Quéré et al. 2009, Nature Geoscience; Data: NOAA 2010, CDIAC 2010 Key Diagnostic of the Carbon Cycle Evolution of the fraction of total emissions that remain in the atmosphere Total CO 2 emissions Atmosphere CO 2 Partitioning (PgC y -1 ) Time (y)

Fraction of total CO 2 emissions that remains in the atmosphere Airborne Fraction Updated from Le Quéré et al. 2009, Nature Geoscience; Raupach et al. 2008, Biogeosciences; Canadell et al. 2007, PNAS

Human Perturbation of the Global Carbon Budget Global Carbon Project 2010; Updated from Le Quéré et al. 2009, Nature Geoscience; Canadell et al. 2007, PNAS (PgC) atmospheric CO 2 ocean land fossil fuel emissions deforestation (Residual) Sink Source Time (y) CO 2 flux (PgC y -1 ) 2.3±0.4 (5 models) 4.1± ± ±

Fossil Fuel Emissions: Actual vs. IPCC Scenarios Updated from Raupach et al. 2007, PNAS; Data: Gregg Marland, Thomas Boden-CDIAC 2010; International Monetary Fund 2010 Fossil Fuel Emission (PgCy -1 ) Full range of IPCC individual scenarios used for climate projections A1B Models Average A1FI Models Average A1T Models Average A2 Models Average B1 Models Average B2 Models Average Observed Projected Time (y)

Appreciate that drivers “then” and drivers “now” may differ… Re-assess as well as push forward… Take advantage of this “global experiment”… Hang on tight… As Ecologists, what do we do?

No one is saying that this will be easy…

Opportunities afforded by Global Change that did not exist previously (when Ecology was “easy”) “The rates, scales, kinds, and combinations of changes occurring now are fundamentally different from those at any other time in history…” - Vitousek et al Some examples: Reassessing what we “know”…

Novel interactions Biotic change (species introductions) Abiotic change (Climate change and resource alterations)

Moving from a “disturbance centric” to a global change world Global change leads directly to resource alterations – new types of drivers of ecological dynamics. Define “Disturbance” CO 2 N H 2 O

Gradual change does not mean gradual response – responses are occurring quickly… Thresholds and alternative stable states have always existed, but thresholds are being crossed more frequently and alternative states are more commonly manifest today… Desertification…

Direct Climate Change Hypothesis Bonanza Creek LTER Total Area Burned Fire Season

Gradual warming Shift in Bark Beetle life cycle from two years to one –threshold response… Outbreak dynamics Increased fuel loads Indirect effect of warming Direct effect Biotic Interactions can accelerate responses to climate change…

Permafrost loss in the Arctic: another threshold response CO 2 CH 4 Warmer temperatures Unfrozen  Frozen Microbial decomposition of stored Carbon Biotic Interactions can feedback on drivers…

Evaluating Controls on Productivity in Ecosystems: Can we use successful exotic invasive species to learn more about abiotic controls and biotic constraints on productivity? (the Dov Sax approach: (2007) Trends in Ecology and Evolution 22: Ecological and evolutionary insights from species invasions)

Exotic “bluestems” invading native grassland in Kansas Response? Herbicide…

A Nightmare for Long-term Experiments… Can something “good” come out of something “bad”?

Productivity Abiotic Drivers & Resources Solar radiation Temperature Precipitation Edaphic Factors Environmental Nutrients Limitations Community Gene Pool  species  genes Biotic Interactions Competition Herbivory Predation Mutualisms Biotic Constraints Traditional ecological manipulations Invasive Exotic Species Determinants of Productivity in Ecosystems Autotrophs

A major challenge for research ecologists (you)… There are more fundamentally important questions to answer and more problems to solve than we have ecologists or resources available ($)… or (gulp) time (?). How do we prioritize? What if you were the “Czar of Global Ecological Crises”? How would you decide? Individual/Class exercise (Groups of 4) Provide specific prioritizing criteria that you think we should use to determine what ecological research we fund and what we do not… Rare vs. dominant? Unique vs. broadly applicable? Aesthetic vs. economic Urgent vs. best science?