The Global Carbon Cycle “It’s not just for scientists anymore…”

Slides:



Advertisements
Similar presentations
Trees and Climate Change. Global Warming the recent increase of the mean temperatures in the earth’s atmosphere and oceans which is predominantly caused.
Advertisements

Sources and Sinks Climate Change
Carbon Sequestration Akilah Martin Fall Outline Pre-Assessment  Student learning goals  Carbon Sequestration Background  Century Model Overview.
Anthropocene Introduction to Meteorology, spring 2011 Observations –Trace gases –Temperature, land and ocean –Precipitation –Sea level Attribution Models.
Your Name Your Title Your Organization (Line #1) Your Organization (Line #2) Global warming.: Matthieu BERCHER, Master M.I.G.S., University of Burgundy,
Global Climate Change: What Controversies? Bryan C. Weare Atmospheric Science Program University of California, Davis.
Explaining the Evidence Activity 2: Clearing the Air.
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
1 THE CARBON CYCLE AND GLOBAL WARMING. 2 CARBON CYCLE Movement of carbon between the atmosphere, oceans, biosphere, and geosphere Movement of carbon between.
Climate Change: Carbon footprints and cycles. What is climate change? What do you think climate change is? What do we actually mean when we talk about.
Turn Down the Heat: State of the Climate (and Australia) February 2014 Damien Lockie.
How is the average temperature of Earth determined? Jot down a few ideas Sketch a map of the room. Show the locations of each water container. When directed,
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
G lobal warming For past climate change see Paleoclimatology and Geologic temperature record. For scientific and political disputes, see Global warming.
European capacity building initiativeecbi Climate Change: an Introduction ecbi Workshops 2007 Claire N Parker Environmental Policy Consultant european.
Climate change and the carbon cycle David Schimel National Center for Atmospheric Research Boulder Colorado.

Samayaluca Dune Field, south of Juarez, Chihuahua Global Climate Change.
Greenhouse Effect and Global Warming Greenhouse Effect Key Factors Earth-Sun Temperature Differences Greenhouse Gas Concentrations The atmosphere is.
Global Warming By Daniel Htwe. Introduction the Earth's temperature has risen by 1 degree Fahrenheit in the past century, with accelerated warming during.
Lecture 34: Anthropogenic Inputs of Greenhouse Gases in the Past 200 Years Ch. 18.
Chapter 19 Global Change. Global change-Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures.
PROSPERIDAD J. ABONETE JULY 3, 2003 Understanding Climate Change.
Carbon Cycle Gr 9 Science. Carbon Cycle Fourth most abundant element in universe Building block of all living things Main Pathway– in and out of living.
Anthropogenic Climate Change. Global Temperature is Increasing.
Climate Change 101. What Is Climate? What Is the Greenhouse Effect?
Climate Change Pre-Quiz 1.What is the “greenhouse effect”? 2.What are examples of greenhouse gases? 3.Is climate change natural or human- made? How do.
Unit 5 Seminar Carbon dioxide. The Carbon Cycle Carbon comes into the living world through the plants, algae, and bacteria that take in atmospheric carbon.
INTERGOVERNMENTAL PANEL ON CLIMATE CHANGE (IPCC) Working Group I Working Group I Contribution to the IPCC Fourth Assessment Report Climate Change 2007:
Carbon Cycle Jeopardy Water Rocks!. Carbon Sources Effects of Climate Change Greenhouse Gases $100 $500 $400 $500 $400 $300 $200 $100 $500 $300 $200 $100.
Carbon cycle and Human activity. Carbon cycle Carbon cycles though the atmosphere, living things, soils, and the ocean.Carbon cycles though the atmosphere,
Nutrient Cycles Ecosystems have an essentially inexhaustible supply of energy But chemical elements are available in limited amounts Life therefore depends.
THE CARBON CYCLE AND GLOBAL WARMING
Anthropocene physical basis of climate spring 2011 Introduction and UNEP reports Observations –Emissions and other natural forcingsEmissions and other.
Global Warming.
SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.
MonthDayLectureActivityChap. Nov.21Ecosystems IIServices56 26Global C cycle56 Dec.3Thinking ecologically I 5Thinking ecologically II Eco. literacy 10Exam.
Climate Change: an Introduction ecbi Workshops 2007 Claire N Parker Environmental Policy Consultant european capacity building initiative initiative européenne.
Chapter 13 Section 3 Global Warming Environmental Science Spring 2011.
 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.
© Yann Arthus-Bertrand / Altitude The Summary for PolicyMakers - final plenary The Summary for PolicyMakers - final plenary Michael Prather, LA, Chapter.
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).
Schematic framework of anthropogenic climate change drivers, impacts and responses to climate change, and their linkages (IPCC, 2007).
Chapter 19 Global Change.
Carbon Sequestration Akilah Martin Fall 2005.
Chapter 19 Global Change.
Chapter 19 Global Change.
REMOVE THIS SLIDE BEFORE PRESENTING
Chapter 19 Global Change.
DO NOW Turn in Review #25. Pick up notes and Review #26.
Chapter 19 Global Change.
DO NOW Pick up notes and Review #25..
Climate Change CH 19.
Cycles Within an Ecosystem
Intergovernmental Panel on Climate Change
The Global Carbon Cycle
Chapter 19 Global Change.
The Global Carbon Cycle
Schematic framework of anthropogenic climate change drivers, impacts and responses to climate change, and their linkages (IPCC, 2007).
Chapter 15 Global Change.
Chapter 19 Global Change.
Nutrient Cycles in Nature Ch. 3-3
The Cycling of Matter.
Chapter 19 Global Change.
Integrated B Midterm -study guide
Presentation transcript:

The Global Carbon Cycle “It’s not just for scientists anymore…”

What we wish to learn: 1.How does the carbon cycle help to explain increasing temperatures on Earth? 2.What are the major controls on the C cycle, and what methods of study can we use to determine these controls? 3. Can we use natural ecosystem processes related to the carbon cycle in order to slow the rate of greenhouse gas accumulation in our atmosphere?

Surface Temperature Variation (top) Past 140 years, global (bottom) Past 1000 years, N. Hemisphere only The “Hockey Stick” of change

Greenhouse gas increases are driving temperature rise ftp://ftp.cmdl.noaa.gov/ccg/co2/trends/co2_mm_mlo.txt

The rate of CO 2 increase is accelerating ftp://ftp.cmdl.noaa.gov/ccg/co2/trends/co2_mm_mlo.txt

Source: IPCC TAR 2001 Indicators of the Human Influence on the Atmosphere during the Industrial Era CO 2, CH 4, N 2 O It’s a “hockey team” Now commonly referred to as the next geological epoch, the “Anthropocene”

Human- caused greenhouse gas increases have warmed the world Observations IPCC 2007: WG1-AR4 Models using only natural forcing Models using both natural and human forcing Global and Continental Climate Change – observations and models

“The understanding of anthropogenic warming and cooling influences on climate has improved…, leading to very high confidence that the global average net effect of human activities since 1750 has been one of warming.” “The global increases in carbon dioxide concentration are due primarily to fossil fuel use and land use change, while those of methane and nitrous oxide are primarily due to agriculture.” “Warming of the climate system is unequivocal, as is now evident from observations of increases in global average air and ocean temperatures, widespread melting of snow and ice, and rising global average sea level.” Intergovernmental Panel on Climate Change, IPCC Summary statements from the 4 th Assessment Report, 2007

Open Letter on the President’s Position on Climate Change, 7 February 2007: “Our emissions performance since 2000 is among the best in the world. According to the International Energy Agency, from , as our population increased and our economy grew by nearly 10%, U.S. carbon dioxide emissions increased by only 1.7%. During the same period, European Union carbon dioxide emissions grew by 5%, with lower economic growth.” "Research is basically a question of revealing truths about ourselves and our surroundings, be these manmade or natural. But research does not simply come about of its own accord, it has to be financed. This means that the problems to be investigated are influenced, to some degree, by the interests of those who finance the research." pp. 36 in Lomborg, B The Skeptical Environmentalist: Measuring the Real State of the World. Cambridge Press, 540 pp. Scientists must support themselves financially, and the hyping of global warming leads to more research grants. Beware the Arguments and Ploys of Skeptics and Politicians 1. Personal or professional gain 2. Selective use of data (cherry-picking) 1. 2.

Index of Greenhouse Gas Emissions for the U.S. and European Union from 1990 to 2004 (Index=100 for 1990, U.N. baseline agreement) The ploy of “cherry-picking data” 1992 “Rio” 1997 “Kyoto” 2001 “9/11 recession” +15% -1%

The CO 2 concentration in the atmosphere is strongly correlated with the Earth’s surface temperature but, there are aspects of the carbon cycle that we don’t understand…

Understanding Global Element Cycles A Method of analysis: 1. Accounting 2. Cycling and Pathways 3. Controls (This method applies to all element cycles)

The Global Carbon Cycle 1. Accounting (x g C) Rocks 65,000,000 Oceans 39,000 Soils 1,580 Atmosphere 860 Land Plants 610 Carbon Forms include: Inorganic C (e.g., HCO 3 - ) Organic C (e.g., CHO compounds) Gases (CO 2, CH 4, CO) The carbon in the atmosphere is 99.6% CO 2

Atmospheric CO ppmv) Vegetation 610 Soils Ocean Stock = Billion metric tons Flow = Billion metric tons per year Global Carbon Carbon Cycle Cycle per year ~1.4 Net flux +7.9 per year ~1.7 Net flux River Transport

2. Cycling (a) Pathways (previous slide) (in “Peta grams”, Pg = g (b) Fluxes (in “Peta grams”, Pg = g = “gigaton” = billion metric tons) = “gigaton” = billion metric tons) g/year (i) Photosynthesis = (ii) Respiration = (iii) Net Ocean Uptake = (iv) Fossil Fuels = +6.3 (v) Biomass Burning = +1.6

(c) Mass Balance (of the atmosphere) Net change = Input + Output + Internal Change 3.2= ( ) + ( ) = (117.9) - (112.7) 3.2= 5.2 * Need a “sink” of (5.2 – 3.2) = 2.0 Pg C / year to balance the global C budget. Where is the sink? Probably in the soils and plants of the Northern Hemisphere

3. Controls (a) Volcanic Activity Strong controls over long periods of time, Weak controls over short periods of time. (b) Weathering Strong controls over long periods of time, Weak controls over short periods of time. (c) Biological controls Strong controls over the patterns of carbon flux over short periods of time (e.g., seasonal) (d) Human influence Weak controls over long periods of time, Strong controls over short periods of time.

(a) Volcanic Activity has a Strong Influence on Atmospheric CO 2 over Long Periods of Time

Over Short Periods of Time, Volcanic Activity has a Weak Influence on Atmospheric CO 2 Volcanic Emissions = 0.05 Pg C /yr Anthropogenic emissions = 8 Pg C /yr Therefore, human influences are ~160 times more important than volcanoes today.

(b) Weathering Reactions Control CO 2 in the Atmosphere over long Geologic Time

Respiration Photosynthetic uptake N. Hemisphere S. Hemisphere (c) Biological controls – affect seasonal patterns Global distribution of CO

Projected CO 2 Emissions will be tied to Population Growth (d) Human Influence – CO 2 emissions from fossil fuels and land-use change

Model predictions 95% confidence intervals (uncertainty) Projected Changes in Annual Temperatures for from different GCM models (A2 emission scenario). Note that the temperature increases are all greater than the uncertainty. From IPCC 2007 Deg C Dec, Jan, Feb

1.The “Geritol Fix” – adding Fe to the Southern Oceans to stimulate algae to take up more CO 2 C:Fe = 106: Carbon Sequestration – can something as simple as planting trees be the solution? How do we solve problems associated with our altered C cycle and increasing CO 2 in the atmosphere? C:N:P:Fe (!) Element cycles interact!

Can’t we just plant a bunch of trees? CO 2 uptake = 50 CO 2 (with 1 N) Plant C:N = 50 Soil C:N = 25 OM decomposition 25 CO 2 1 N +25 CO 2 Net atm change = (25 – 50) = -25

Take-home message: “There are no magic fixes for the CO 2 problem”

Summary: 1.The global carbon cycle is closely tied to Earth’s temperature through carbon-based greenhouse gases (CO 2 and CH 4 ). 2.The recent modification of the carbon cycle by humans has warmed our globe considerably more than accounted for by background climate variation. 3.Understanding the carbon cycle requires an accounting of where the C is stored, the pathways that it travels through the geosphere and biosphere, and the controls on the rates of C cycling. 4.Volcanoes and weathering exert control over the global C cycle only on very long time scales, whereas humans exert control over very short time scales. 5.There are no simple fixes for the CO 2 increases, in part because element cycles (C, N, P, Fe) are linked and interact.