Observations show that the increase of carbon dioxide is fully caused by human activities Pieter P. Tans NOAA Earth System Research Laboratory Boulder,

Slides:



Advertisements
Similar presentations
Some questions in current climate and CO 2 studies.
Advertisements

The Global Carbon Cycle Overview The atmospheric distribution Sources and sinks of anthropogenic CO 2 Sources and sinks of oxygen.
Activity 2.3 Team CarboEurope-IP Meeting, Posen, Poland, 7-12 Oktober, 2007 Flask network (A 2.3) Multiple species measurement What is expected from A.
GHG Verification & the Carbon Cycle 28 September 2010 JH Butler, NOAA CAS Management Group Meeting Page 1 Global Monitoring, Carbon Cycle Science, and.
Ocean Circulation And Current Carbon Cycle For more detail see the course materials for Lynne Talley’s Course at SIO.
Emissions de CO2 et objectifs climatiques
1 The Evolution of the Recent Atmospheric Methane Budget Lori Bruhwiler, Ed Dlugokencky, Steve Montzka, Pieter Tans Earth System Research Laboratory Boulder,
Sarmiento and Gruber (2002) Sinks for Anthropogenic Carbon Physics Today August
Combination of mechanisms responsible for the missing carbon sink using bottom-up approach Haifeng Qian March 29, A Carbon Cycle and Climate Past,
Air Pollutant Climate Forcings within the Big Climate Picture * Jim Hansen March 11, 2009 Climate Change Congress Global Risks, Challenges & Decisions.
Climate science in a world with global change David Noone Program in Atmospheric and Oceanic Sciences Cooperative Institute for Research in Environmental.
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.
Introduction to Sustainable Energy Technologies
SOURCES PUITS CO 2 Global Budget (GtC yr -1 ) (1 GtC = gC)
January 10, 2006 Global and Regional Climate Change: Causes, Consequences, and Vulnerability Climate Science in the Public Interest
Protecting our Health from Climate Change: a Training Course for Public Health Professionals Chapter 2: Weather, Climate, Climate Variability, and Climate.
The current causes of climate change: the human causes.
Anthropogenic Influences on the Global Carbon Cycle and its Implications for the Future Abstract Carbon makes up approximately 50% of the dry weight of.
Air Pollution and Global Warming. Air Pollution  Air pollution is the harmful materials into the Earth's atmosphere, causing disease, death to humans,
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 and the Carbon Cycle Gretchen Keppel-Aleks California Institute of Technology 16 October 2010.
Carbon Dioxide and Climate Pieter Tans NOAA Earth System Research Laboratory Boulder, Colorado National Science Teachers Association National Conference.
9 November 2002The North Texas SkepticsJohn Blanton, Curtis Severns Global Warming Science Solar Radiation Ozone and Oxygen absorb nm. Water.
Climate change and the carbon cycle David Schimel National Center for Atmospheric Research Boulder Colorado.
CESD 1 SAGES Scottish Alliance for Geoscience, Environment & Society Observing and Modelling Climate Change Simon Tett, Chair of Earth System Dynamics.
Weather Condition of the atmosphere at any particular time and place Air temperature, air pressure, humidity, clouds, precipitation, visibility, wind Climate.
Global Megacycles and Trends: Setting the Agenda for 21 st Century Science Emerging Issues: Berrien Moore III University of New Hampshire New Challenges.
A Decline in the Northern Hemisphere CO 2 Sink from John Miller 1, Pieter Tans 1, Jim White 2, Ken Masarie 1, Tom Conway 1, Bruce Vaughn 2,
Greenhouse Effect and Global Warming Greenhouse Effect Key Factors Earth-Sun Temperature Differences Greenhouse Gas Concentrations The atmosphere is.
Earth’s Changing Environment Lecture 13 Global Warming.
Climate Change 101. Everything I know about Climate Change I learned at the movies…
(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Biogochemistry & Climate (from IPCC WG-I, Chapter 7) Biogeochemistry & Climate Primary Source: IPCC WG-I Chapter.
CSI: Climate Status Investigations Teacher Training Institute April 16-21, 2008 Climate Change 101.
Ottawa Citizens’ Conference on Climate Change John M R Stone Carleton University.
The Global Effort to Understand Carbon Dioxide James R. Mahoney, Ph.D. Assistant Secretary of Commerce for Oceans and Atmosphere NOAA Deputy Administrator.
Remote input of nutrients in a changing climate
Investigating the Carbon Cycle in Terrestrial Ecosystems (ICCTE) Scott Ollinger * -PI, Jana Albrecktova †, Bobby Braswell *, Rita Freuder *, Mary Martin.
Long-term Observation of CO 2 concentration and its isotope ratios over the Western Pacific H. Mukai, Y. Nojiri, Y. Tohjima, T. Machida, Y. Shibata and.
THE CARBON CYCLE What Is Carbon? Carbon is a key element for life, composing almost half of the dry mass of the earth’s plants (that is, the mass when.
UDnFmNTYhttps:// UDnFmNTY gmFa0r04https://
The Earth and its atmosphere. The large H 2 O greenhouse effect is controlled by temperature – H 2 O saturation doubles with every 10°C Increase As a.
An alternative explanation to the size and location of the missing sink Robert Andres 1 Skee Houghton 2 1 Environmental Sciences Division, Oak Ridge National.
There can’t be life without it!.  Atomic Number 6  6 Protons  6 electrons  4 valence electrons.
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.
Simulations of historical and future anthropogenic CO 2 uptake from 12 global ocean models J.C. Orr, P. Monfray, O. Aumont, A. Yool, I. Totterdell, K.
Arne Winguth University of Wisconsin-Madison, USA Uwe Mikolajewicz, Matthias Gröger, Ernst Maier-Reimer, Guy Schurgers, Miren Vizcaíno Max-Planck-Institut.
Figure 1: Global time series plots of CH 4 and δ 13 C of CH 4 from The recent rise in CH 4 is concurrent with a decrease in δ 13 C of CH 4.
What is Climate Change?. Climate change refers to any significant change in the measures of climate lasting for an extended period of time. In other words,
KEY CONCEPT Fossil fuel emissions affect the biosphere.
Surprises in the anthropogenic carbon budget Why OCB is so important! Jorge Sarmiento Princeton University Co-lead author of the US Carbon Cycle Science.
Nitrous Oxide Focus Group Nitrous Oxide Focus Group launch event Friday February 22 nd, 2008 Dr Jan Kaiser Dr Parvadha Suntharalingam The stratospheric.
The Greenhouse Effect on Climate Change.  1. The sun’s rays warm up the land and the water.  2. Infrared rays bounce back to space.  3. Some are trapped.
ESF workshop on methane, April 10-12, years of methane : from global to regional P. Bousquet, S. Kirschke, M. Saunois, P. Ciais, P. Peylin, R.
CO2 RECORDS. Source: ^ Trends in Atmospheric Carbon Dioxide - Mauna Loa. National Oceanic & Atmospheric Administration.^Trends in Atmospheric Carbon Dioxide.
Climate Change 101. Everything I know about Climate Change, I learned at the movies…
Post 2035: Fossil Emissions and the Paris Agreement
Climate Change: Science and Society
Pre-anthropogenic C cycle and recent perturbations
Clicker quiz: Carbon and the climate created by Sarah Wise, CIRES Education and Outreach, for use by faculty at U. of Colorado at Boulder for Focus.
Introduction: Carbon Cycle
CARBON CYCLE Presented By: Stefanie Spayd Janet Fang.
EVSC 1300 Global Warming.
Roger Pielke, Sr, Director
Dr. Matthias Lüdeke, Potsdam Institut für Klimafolgenforschung
by Philip S. Ringrose Petroleum Geoscience Volume 23(3):
Mitigation: Major Climate Change Can Be Avoided. Warren M
The global carbon cycle for the 1990s, showing the main annual fluxes in GtC yr–1: pre-industrial ‘natural’ fluxes in black and ‘anthropogenic’ fluxes.
The global carbon cycle for the 1990s, showing the main annual fluxes in GtC yr–1: pre-industrial ‘natural’ fluxes in black and ‘anthropogenic’ fluxes.
Greenhouse Gases & their effect on earth
(a) Global CO2 emissions from fossil-fuel combustion, cement manufacture, and gas flaring and global population, 1800 – 2014 (sources: carbon emissions.
Presentation transcript:

Observations show that the increase of carbon dioxide is fully caused by human activities Pieter P. Tans NOAA Earth System Research Laboratory Boulder, Colorado AGU fall meeting 10 December 2007

Fossil fuel data: CDIAC and BP DECADAL MASS BALANCE OF CARBON

Pulse response: CO2 ATM = exp( -t /363) exp( -t /74) exp ( -t /17) exp( -t /1.9) DECADAL MASS BALANCE OF CARBON Hamburg Ocean Carbon Cycle Model, E.Maier-Reimer, 1987

sources: David Etheridge, CSIRO, Australia; ESRL DECADAL MASS BALANCE OF CARBON

GtC Cumulative fossil fuel emissions (Jan. 2007)331 ± 25 (source: CDIAC) Observed atmospheric increase (Jan. 2007)214 ± 8 (source: ESRL) Observed ocean increase through ± 19 (Sabine et al., Science 2004) oceans, extrapolated through DECADAL MASS BALANCE OF CARBON fossil fuel emissions + terrestrial sources = atmospheric increase + ocean

DECADAL MASS BALANCE OF CARBON fossil fuel emissions + terrestrial sources = atmospheric increase + ocean Hamburg Ocean Carbon Cycle Model, E. Maier-Reimer, 1987

DECADAL MASS BALANCE OF CARBON fossil fuel emissions + terrestrial sources = atmospheric increase + ocean Princeton Ocean Carbon Cycle Model, J. Sarmiento, 1992

DECADAL MASS BALANCE OF CARBON fossil fuel emissions + terrestrial sources = atmospheric increase + ocean Bern Model (HILDA), F. Joos, 2005

Conclusions: The observed increase in atmospheric carbon dioxide since pre-industrial times is entirely due to human activities. The measured increases in the atmosphere and oceans add up to the cumulative fossil fuel emissions. The relative contribution of NET changes in terrestrial biomass and organic matter has dwindled over time and is now relatively small. DECADAL MASS BALANCE OF CARBON

Use of isotopic ratios to distinguish sources 13 C/ 12 C sample – 13 C/ 12 C reference 13 C/ 12 C reference 14 C/C sample δ 13 C 13 C/ 12 C ratio 14 C/C reference (approximate) (approximate) Atmosphere -8 ‰ From oceans -8 ‰ Terrestrial biosphere -26 ‰ Coal -24 ‰ Oil -28 ‰ Natural gas -45 ‰ ISOTOPIC RATIO SIGNATURES

Sources: Friedli (1986), Francey (1999 ), and ESRL & INSTAAR ISOTOPIC RATIO SIGNATURES

RECENT RATES OF CHANGE

more uptake

RECENT RATES OF CHANGE

5-year averaged, centered on 2000 (Gton C/year) 5-year averaged, centered on 2005 (Gton C/year) fossil emissions atmos. increase total uptake, of which: oceans terrestrial RECENT RATES OF CHANGE carbon budgets

CO2 GROWTHRATE and CLIMATE ANOMALIES

CO2 GROWTHRATE and CLIMATE ANOMALIES

Conclusion: 2/3 of the interannual variance of the CO2 growth rate is explained by the delayed response of the terrestrial biosphere to interannual variations of temperature and precipitation. CO2 GROWTHRATE and CLIMATE ANOMALIES