Global Ocean Observing System (GOOS) Environmental Context for CoML Some cautions and a quick picture of elements of the system Edward Harrison, Chair,

Slides:



Advertisements
Similar presentations
LRF Training, Belgrade 13 th - 16 th November 2013 © ECMWF Sources of predictability and error in ECMWF long range forecasts Tim Stockdale European Centre.
Advertisements

Ocean Biogeochemistry (C, O 2, N, P) Achievements and challenges Nicolas Gruber Environmental Physics, ETH Zürich, Zurich, Switzerland. Using input from.
Literature Review Kathryn Westerman Oliver Smith Enrique Hernandez Megan Fowler.
Climate Change & Global Warming: State of the Science overview December 2009 Nathan Magee.
Climate Change Science
Global Warming  The Evidence  Potential for change?  Can anthropogenic change be separated from natural change?  Can the world collectively.
CO2 (ppm) Thousands of years ago Carbon dioxide concentrations over the last.
Climate Signal Detection from Multiple Satellite Measurements Yibo Jiang, Hartmut H. Aumann Jet Propulsion Laboratory, Californian Institute of Technology,
Climate case study. Outline The challenge The simulator The data Definitions and conventions Elicitation Expert beliefs about climate parameters Expert.
Outline Further Reading: Detailed Notes Posted on Class Web Sites Natural Environments: The Atmosphere GE 101 – Spring 2007 Boston University Myneni L29:
Ocean Heat Uptake Gregory C. Johnson 1,2, John M. Lyman 3,1, & Sarah G. Purkey 2,1 1 NOAA/Pacific Marine Environmental Laboratory, 2 University of Washington.
Climate Change: An Overview of the Science Anthony J. Broccoli Director, Center for Environmental Prediction Department of Environmental Sciences Rutgers.
Where is Our SWWA Climate Headed? Bryson C. Bates Director, CSIRO CLIMATE.
Chang enefits of educing nthropogenic limate B EN S ANDERSON C LAUDIA T EBALDI B RIAN O’N EILL K IETH O LESON BRACEBRACE When can we expect to see the.
Alan F. Hamlet Philip W. Mote Martyn Clark Dennis P. Lettenmaier JISAO/SMA Climate Impacts Group and Department of Civil and Environmental Engineering.
Protecting our Health from Climate Change: a Training Course for Public Health Professionals Chapter 2: Weather, Climate, Climate Variability, and Climate.
 Myth: What global warming? Earth has actually been cooling since ◦ 1998 was the warmest summer  It’s been cooler since then ◦ Not supported by.
Global warming indicates the increase in the average temperature of Earth's atmosphere and oceans. It is one of the kinds of global climate change and.
(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Observed Surface & Atmosphere (from IPCC WG-I, Chapter 3) Observed Changes in Surface and Atmosphere Climate.
Climate Variability & Change - Past & Future Decades Brian Hoskins Director, Grantham Institute for Climate Change, Imperial College London Professor of.
Comparative analysis of climatic variability characteristics of the Svalbard archipelago and the North European region based on meteorological stations.
What is the Difference Between Weather and Climate?
Global Interannual Upper Ocean Heat Content Variability Gregory C. Johnson (NOAA/PMEL), John M. Lyman (UH/JIMA & NOAA/PMEL), Josh K. Willis (NASA/JPL),
CHAPTER 14: Nonparametric Methods
The role of gliders in sustained observations of the ocean Deliverable 4.1 or WP 4.
The AMOC in the Kiel Climate Model WP 3.1 Suitability of the ocean observation system components for initialization PI: Mojib Latif With contribution from:
Inter-annual to decadal climate prediction Mojib Latif, Leibniz Institute of Marine Sciences at Kiel University.
Final General Assembly – Paris, France – September 19, 2014 FP7-Infra : Design studies for European Research Infrastrutures 1st October 2011.
Changes in the Seasonal Cycle of Sea Surface Salinity from Jim Reagan 1,2, Tim Boyer 2, John Antonov 2,3, Melissa Zweng 2 1 University of Maryland.
Modern Climate Change Darryn Waugh OES Summer Course, July 2015.
ENSO Variability in SODA: SULAGNA RAY BENJAMIN GIESE TEXAS A&M UNIVERSITY WCRP 2010, Paris, Nov
International Environment Forum Conference Ottawa October 12 th, 2007 John M R Stone Carleton University.
Modern Era Retrospective-analysis for Research and Applications: Introduction to NASA’s Modern Era Retrospective-analysis for Research and Applications:
Components of the Global Climate Change Process IPCC AR4.
Measurements of atmospheric O 2 in relation to the ocean carbon cycle Ralph Keeling Scripps Institution of Oceanography.
IndOOS—a sustained ocean observing system in the Indian Ocean for climate research Howard Cattle for Gary Meyers Co-Chair CLIVAR/GOOS Indian Ocean Panel.
Australian Climate: The Past 50 Years of Change Mr Bruce Stewart Assistant Director (Climate and Oceans)
Temporal Variability of Thermosteric & Halosteric Components of Sea Level Change, S. Levitus, J. Antonov, T. Boyer, R. Locarnini, H. Garcia,
Instrumental Surface Temperature Record Current Weather Data Sources Land vs. Ocean Patterns Instrument Siting Concerns Return Exam II For Next Class:
What is the Difference Between Weather and Climate?
CE 401 Climate Change Science and Engineering evolution of climate change since the industrial revolution 9 February 2012
Impacts of Climate Change on Physical Systems Lesson Plan 4 – Day 2 PPT
Climate Change and Global Warming Michael E. Mann Department of Environmental Sciences University of Virginia Waxter Environmental Forum Sweet Briar College.
Continental-scale temperature variability during the past two millennia, Pages 2k consortium Not enough data in Africa.
Burning issues at climate science – policy interface Judith Curry.
The State of the Ocean Climate: climate indices and their uncertainty as a measure of our ability to observe the ocean Albert Fischer, Ed Harrison, Gildas.
What is the Difference Between Weather and Climate?
ENVIRONMENTAL SCIENCE TEACHERS’ CONFERENCE ENVIRONMENTAL SCIENCE TEACHERS’ CONFERENCE, Borki Molo, Poland, 7-10 February 2007 The warming trend for the.
Schematic framework of anthropogenic climate change drivers, impacts and responses to climate change, and their linkages (IPCC, 2007).
The Greenhouse Effect often has a negative connotation with it but without it we could not survive on Earth. Too much Greenhouse gasses are a problem,
Spatial Modes of Salinity and Temperature Comparison with PDO index
Global Warming Michael E. Mann, Department of Environmental Sciences
Schematic framework of anthropogenic climate change drivers, impacts and responses to climate change, and their linkages (IPCC, 2007; 2014).
Instrumental Surface Temperature Record
What Has Caused the Observed Warming over Recent Decades? Pressure?
Dynamics of ENSO Complexity and Sensitivity
Candyce Clark JCOMM Observations Programme Area Coordinator
Energy accumulation and surface warming
Workshop 1: GFDL (Princeton), June 1-2, 2006
Instrumental Surface Temperature Record
Proxy Measures of Past Climates
Effects of Temperature and Precipitation Variability on Snowpack Trends in the Western U.S. JISAO/SMA Climate Impacts Group and the Department of Civil.
Emerging signals at various spatial scales
Schematic framework of anthropogenic climate change drivers, impacts and responses to climate change, and their linkages (IPCC, 2007).
Is the rate of recent warming greater than observed in the past?
ARGO, Profiling Floats, and Iridium
Get out a piece of paper and title it “Ocean Currents”
Instrumental Surface Temperature Record
Schematic framework of anthropogenic climate change drivers, impacts and responses to climate change, and their linkages (IPCC, 2007).
Schematic framework of anthropogenic climate change drivers, impacts and responses to climate change, and their linkages (IPCC, 2007).
Presentation transcript:

Global Ocean Observing System (GOOS) Environmental Context for CoML Some cautions and a quick picture of elements of the system Edward Harrison, Chair, climate component of GOOS planning

Historical Ocean Sampling The global ocean has been under sampled in the past, physically and biologically Available evidence shows much decadal variability with complex sub-basin scale structure Short-term trends may mislead Global average uncertainties hard to estimate

Temp Data Distributions since Caution! Blue colors mean fewer than 20% of months had any observations! 300m 500m

Running 20yr Temp Trends at 300m 55-75, , , Red – warming Blue – cooling Caution! 95% of regions change sign!

90% Significant Temp Trends m, , , 1000 Caution: Little of the ocean has reliable trend! Opportunity: Match biological analyses to regions with well-established trends

Moorings and Surface Drifters January 2007 (~1300) Many will begin to report multiple times/day in 2007

Argo profiling floats January 2007 (~2800)

Concluding Questions Can CoML focus some of its studies for 2010 on parts of the ocean with best observations for physical and environmental variables? Can CoML plan activities for CoML II ( ) that benefit from likely evolution of physical and environmental observing plans? Opportunity: 2008 SCOR conference on Ocean in a High CO2 World 6-8 October 2008 (talk with Ed Urban)