Lecture 1: OCN520 Chemical Oceanography Prof: Jim Murray.

Slides:



Advertisements
Similar presentations
Carbon Theme Report and Implementation 23 April April 2004 Tokyo, Japan Berrien Moore III Institute for the Study of Earth, Oceans, and Space University.
Advertisements

Climate Change and the Oceans
Global Carbon Cycle Sabine et al. (2004) SCOPE Ocean sequester ~30% of fossil fuel CO 2 Human perturbations overlay large natural background C cycle Climate.
Carbonate System and pH
March 23, th IGM/SPG/Symposium, Canberra Cape Grim: A 28-year record of the changing atmosphere Graeme Pearman CSIRO.
Carbon Cycle. Carbon Carbonic acid ( HCO 3 − ) Carbonate rocks (limestone and coral = CaCO 3 ) Deposits of Fossil fuels Carbon exists in the nonliving.
Carbon Cycle. Carbon Carbon exists in the nonliving environment as: Carbon dioxide (CO2) Carbonic acid ( HCO 3 − ) Carbonate rocks (limestone and coral.
Ocean Circulation And Current Carbon Cycle For more detail see the course materials for Lynne Talley’s Course at SIO.
Factors Shaping Long- Term Future Global Energy Demand and Carbon Emissions 7 th International Carbon Dioxide Conference September 25-30, 2005 Jae Edmonds,
2. Land-Use Change (primarily tropical deforestation) 1. Burning of fossil fuels How Are We Increasing the CO 2 Concentration?
The Ocean’s Role in the Carbon Cycle in Relation to Increased Atmospheric CO 2 Paul Loikith.
Properties of Seawater Monday we talked about properties of water (Table 7.2) - dissolves solids and gases readily (“universal solvent”) Last time (Wednesday)
Determining the magnitude and variability of the anthropogenic CO 2 uptake rate by the oceans. Dick Feely (NOAA/PMEL/JISAO) Chris Sabine (NOAA/PMEL/JISAO)
The Anthropogenic Ocean Carbon Sink Alan Cohn March 29, 2006
Effects of global warming on the world’s oceans Ashley A. Emerson.
The uptake, transport, and storage of anthropogenic CO 2 by the ocean Nicolas Gruber Department of Atmospheric and Oceanic Sciences & IGPP, UCLA.
Where has all the Carbon Gone? Atmospheric oxygen, carbon fluxes and the implications for climate change. Mark Battle (Bowdoin College) Michael Bender.
Climate and the Carbon Cycle Gretchen Keppel-Aleks California Institute of Technology 16 October 2010.
GEOF236 CHEMICAL OCEANOGRAPHY (HØST 2012) Christoph Heinze University of Bergen, Geophysical Institute and Bjerknes Centre for Climate Research Prof. in.
Global Warming Fact and Fiction. Some Critical Findings Global temperatures have increased C the past 100 years Global temperatures have increased.
Ocean Carbon Cycle Figure credit US-OCB Program.
Climate Change: 4 Lectures The Science - Today –The climate system –Historical records and evidence of climate change –Direct and indirect greenhouse gases.
The NH Climate Action Plan The Transportation and Land Use Connection Strafford Region Planning Commission May 28, 2009 Thomas S. Burack Commissioner NH.
Global Megacycles and Trends: Setting the Agenda for 21 st Century Science Emerging Issues: Berrien Moore III University of New Hampshire New Challenges.
Ocean Acidification Victoria J. Fabry and Andrew G. Dickson
The Other Carbon Dioxide Problem Ocean acidification is the term given to the chemical changes in the ocean as a result of carbon dioxide emissions.
Greenhouse Effect and Global Warming Greenhouse Effect Key Factors Earth-Sun Temperature Differences Greenhouse Gas Concentrations The atmosphere is.
Fall 2011 Writing 20:Ocean Acidification August 31, 2011 Lecture 1: “Introduction to Ocean Acidification” Some of this lecture obtained from
The Global Effort to Understand Carbon Dioxide James R. Mahoney, Ph.D. Assistant Secretary of Commerce for Oceans and Atmosphere NOAA Deputy Administrator.
SAILING INTO A SEA OF EXCITEMENT: An Earth System Perspective on Marine Research in the Next Decade Will Steffen Executive Director, IGBP Royal Swedish.
Global connections between aeolian dust, climate and ocean biogeochemistry at the present day and at the last glacial maximum Maher et al., 2010, Earth-Science.
1 UIUC ATMOS 397G Biogeochemical Cycles and Global Change Lecture 6: Earth System / Modeling Don Wuebbles Department of Atmospheric Sciences University.
The Carbon Cycle within the Oceans Allyn Clarke With much help from Ken Denman, Glen Harrison and others.
Working Group 3: What aspects of coastal ecosystems are significant globally? Coastal Zone Impacts on Global Biogeochemistry NCAR, June 2004 Contributed.
UDnFmNTYhttps:// UDnFmNTY gmFa0r04https://
Investigating the Carbon Cycle in Terrestrial Ecosystems (ICCTE) A joint program between: The University of New Hampshire, USA AND Charles University,
13,000 km 3 15,300,000 km 3 1,350,000,000 km 3 71,000 km 3 33,000,000 km 3 425,000 km 3 40,000 km 3.
WORLDRESOURCESINSTITUTE Data Source: C.D. Keeling and T.P. Whorf, Atmospheric CO2 Concentrations (ppmv) derived from in situ air samples collected at Mauna.
Data Source: C.D. Keeling and T.P. Whorf, Atmospheric CO2 Concentrations (ppmv) derived from in situ air samples collected at Mauna Loa Observatory, Hawaii,
Lecture 1: OCN400 Chemical Oceanography Prof: Jim Murray TAs: Tessa McGee Susanna Michael 1.Introduce Murray 2. Who are the Students? 3. Syllabus / Text.
CO 2 and Climate Change. Lisiecki & Raymo,
ESYS 10 Introduction to Environmental Systems February 28
Lecture 11 Principles of Mass Balance Simple Box Models The modern view about what controls the composition of sea water.
Factors contributing to variability in pCO 2 and omega in the coastal Gulf of Maine. J. Salisbury, D. Vandemark, C. Hunt, C. Sabine, S. Musielewicz and.
Chapter 6 The Carbon Cycle © 2013 Elsevier, Inc. All rights reserved. From Fundamentals of Ecosystem Science, Weathers, Strayer, and Likens (eds).
Goal of this course: What determines the abundance of different elements in the ocean? How does their distribution depend on physical circulation and biological.
Core Theme 5 – WP 17 Overview on Future Scenarios - Update on WP17 work (5 european modelling groups : IPSL, MPIM, Bern, Bergen, Hadley) - Strong link.
Coral Growth in Response to Increased Atmospheric CO 2 Jim Billingsley Biology 881 University of Nebraska, Kearney.
Finzi Born Finzi Graduates High School Finzi Teaches First BU Course Source:
Greenhouse Gas: Carbon Dioxide Thuan, Marko. Carbon Dioxide (CO 2 ) Colorless & odorless gas Ice Age (400 kyBCE) ppm Preindustrial (1700s)
Mobile Energy Centre. Raw materials Production Distribution Use Phase Disposal Re-use Raw materials Production Distribution Use.
Oceans & Anthropogenic CO 2 V.Y. Chow EPS 131.  CO 2 exchange across sea surfaces in the oceans  Measurement methods of anthropogenic CO 2  Distributions.
Lecture 1: GEOL330/634 Chemical Oceanography Prof: Jim Murray 1.Introduce Murray 2. Who are the Students? 3. Syllabus / Text (Emerson and Hedges) 4. Course.
Carbon Cycle Ocean Systems.
Carbonate System and pH Why study the carbonate system? Why study the carbonate system? Involves carbonic acid – an example of an acid-base reaction Involves.
CARBON CYCLE Presented By: Stefanie Spayd Janet Fang.
CH19: Carbon Sinks and Sources
CH19: Carbon Sinks and Sources
Carbon cycle theme The Earth’s carbon cycle has a stabilizing mechanism against sudden addition of CO2 to the atmosphere About 50% of carbon emission is.
The Oceanic Sink Uptake in the mixed layer
The Carbon Cycle.
משאב אוויר עד כמה חיוני האוויר לחיינו ?????? גוף האדם- מסוגל להתקיים:
Stable Carbon Cycle–Climate Relationship During the Late Pleistocene
~90 ppmv -Cooler oceans decrease CO2 by 22 ppmv -Saltier oceans increase CO2 by 11 ppmv.
CO2 Concentration (ppm)
Environmental Chemistry
GLOBE Carbon Cycle: The Carbon Cycle
Chapter 11 The Global Carbon Cycle
Chapter 19 Global Change.
(a) Global CO2 emissions from fossil-fuel combustion, cement manufacture, and gas flaring and global population, 1800 – 2014 (sources: carbon emissions.
Presentation transcript:

Lecture 1: OCN520 Chemical Oceanography Prof: Jim Murray

Four Main Themes 1.Global Carbon Cycle 2.Are humans changing the chemistry of the ocean? 3.What are chemical controls on biological production? 4. What is the fate of organic matter made by biological production?

Global Carbon Cycle

Mauna Loa CO 2 record – Started by David Keeling (SIO) NOAA-ERL Data

Source: C. D. Keeling and T. P. Whorf; Etheridge et.al.; Barnola et.al.; (PAGES / IGBP); IPCC (BP 1950) Projected (2100) Current (2001) CO 2 Concentration (ppmv) Vostok Record Law Dome Record Mauna Loa Record IPCC IS92a Scenario

Global Carbon Cycle Sabine et al. (2004) SCOPE Reservoirs and Fluxes

Are Humans Changing the Composition of the Ocean: Ocean Acidification

Because the ocean mixes slowly, half of the anthropogenic CO 2 stored in the oceans is found in the upper 10% of the ocean. Sabine et al. Science (2004) Global Anthropogenic CO 2 Inventory = 118±19 Pg C

Chemistry, Biology and Circulation

Nitrate concentrations High Nutrient-Low Chlorophyll regions:

Fate of Organic Matter

Source: JGOFS / IGBP CO 2 Preindustrial CO2: maximum strength bio pump: 160 ppm Preindustrial CO2: Physical pump alone: 400 ppm Oceanic Primary Production: Sept. 97 – Aug. 98 CO 2 Biological PumpPhysical (solubility) Pump