The Global Tropical Moored Buoy Array: Status & Plans Mike McPhaden OCO Review 3-5 Sept 2008 RAMA PIRATA TAO/TRITON.

Slides:



Advertisements
Similar presentations
OceanSITES: Status and Plans M. J. McPhaden, NOAA/PMEL 18 February 2006 Honolulu, Hawaii Nuku Hiva, Marquesas Islands 1)TAO Transition 2)New NOAA funding.
Advertisements

Evolution of the El Niño : The Role of Intraseasonal to Interannual Time Scale Dynamics Michael J. McPhaden NOAA/PMEL Seattle, Washington CLIVAR.
Uganda’s climate: change and variability Prof Chris Reason, UCT & Lead Author, WG1 AR5 Regional circulation and climate Climate variability Long-term projections.
Semyon A. Grodsky and James A. Carton, University of Maryland, College Park, MD The PIRATA (PIlot Research Array moored in the Tropical Atlantic) project.
» Data buoys measure air pressure, temperature (sea-surface & air), ocean current velocity and wind velocity across all oceans. These observations are.
Towards a Global Tropical Ocean Moored Buoy Array for Climate
Tropical Ocean-Global Atmosphere (TOGA) Tropical Atmosphere Ocean (TAO) Array Mira Losic Dec 2, 2010.
El Nino – Southern Oscillation - Southern Oscillation (atmosphere) - El Nino (ocean) - change in equatorial Pacific circulation - produces global climate.
Modes of Tropical Climate Variability El Niño / Southern Oscillation Atlantic Niño Atlantic and Pacific Meridional Modes Indian Ocean Dipole  Observational.
Yukio Masumoto (RIGC, JAMSTEC). Outline  Indian Ocean Observing System - Background and present status  Examples of key phenomena observed by IndOOS.
Modes of Pacific Climate Variability: ENSO and the PDO Michael Alexander Earth System Research Lab michael.alexander/publications/
NOAA’s Global Ocean Observations for Climate
RAMA Research Moored Array for African-Asian-Australian Monsoon Analysis and Prediction M. J. McPhaden and G. Meyers, K. Ando,Y. Masumoto, V. S. N. Murty,
Seasonal outlook of the East Asian Summer in 2015 Motoaki Takekawa Tokyo Climate Center Japan Meteorological Agency May th FOCRAII 1.
Mike McPhaden NOAA/PMEL Seattle, Washington
SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean.
Report of the Tropical Moored Buoy Implementation Panel to the 24 rd Session of the Data Buoy Cooperation Panel October 13-16, 2008 Cape Town, South Africa.
Shang-Ping Xie, Dept of Meteorology & IPRC Research interest: Climate variability and change, Ocean’s role in climate Major funding sources: NASA, NOAA.
Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag and Mike McPhaden NOAA/PMEL NOAA Climate Observation Program 3 rd Annual System.
Indian Ocean Science Drivers Improved description, understanding and ability to predict:  Seasonal monsoon variability  Monsoon ENSO interactions  Indian.
Development of an Indian Ocean Moored Buoy Array for Climate*
El Niño/Southern Oscillation Major climatic perturbation on the planet Coupled atmosphere ocean process Key is the western tropical Pacific – Ascending.
Discussion issues from the Tropical Moored Buoy Implementation Panel for the 4th Session of the JCOMM OCG April 18-20, 2011 Hobart, Australia.
ENSO Prediction and Policy Why Predict ENSO? How do we predict ENSO? Why is it possible ? What information do predictions offer? What to do with this information?
Observation program for role of the Indian Ocean in the climate system Gary Meyers Co-Chair CLIVAR/GOOS Indian Ocean Panel With Contributions from IOP.
1. Global monsoon features Australian monsoon South American monsoon North American monsoon African monsoon Asian monsoon 2. Northern China winter drought.
Current status of TRITON buoy array and Past, Present, and Future Collaborations Ken Ando and Yasu Ishihara, JAMSTEC.
2: PIRATA ( Pilot Research moored Array in the Tropical Atlantic ) ( ?) Tripartite Programme as a contribution to CLIVAR, GCOS and GOOS : - FRANCE.
NEP Presentation Transition of the Tropical Atmosphere Ocean (TAO) Project from research to operations Chet Koblinsky NOAA Climate Office 08 January 2004.
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.
ODINAFRICA/GLOSS Sea Level Training Course Regional Oceanography and Climate (West Africa) November 2006, Oostende Angora AMAN.
Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.
PredIction and Research mooring Array in the Tropical Atlantic PIRATA Dr. Domingos Urbano National Institute for Space Research - INPE OceanSITES meeting.
Equatorial Circulation and Tropical Atlantic Variability during the Tropical Atlantic Climate Experiment Peter Brandt 1, Andreas Funk 2, Alexis Tantet.
Recent Progress Towards an Indian Ocean Observing System for Climate
Report of the Tropical Moored Buoy Implementation Panel to the 23 rd Session of the Data Buoy Cooperation Panel October 15-19, 2007 Jeju, Korea.
Progress of US CLIVAR during Reasons for recapping progress: - Present advances in scientific understanding of the climate system - Demonstrate.
Development of an Indian Ocean Moored Buoy Array for Climate* Mike McPhaden NOAA/Pacific Marine Environmental Laboratory Seattle, Washington Sustained.
Report of the Tropical Moored Buoy Implementation Panel to the 20 th Session of the Data Buoy Cooperation Panel October 18-22, 2004 Chennai, India Nuku.
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.
FORSGC/JAMSTEC Indian Ocean Activities
Bifurcation Dynamics L. Gourdeau (1), B. Kessler (2) 1), LEGOS/IRD Nouméa, New Caledonia, 2) NOAA/PMEL, Seattle, USA Why is it important to study the bifurcation.
State of the Oceans Albert Fischer OOPC-12 Paris, France, 2-5 May 2007.
IGY and the Origins of El Niño/Southern Oscillation (ENSO) Research
Variations in the Activity of the Madden-Julian Oscillation:
Climate Change El-Nino Southern Oscillation (ENSO)Phenomena.
Climate Variability and Basin Scale Forcing over the North Atlantic Jim Hurrell Climate and Global Dynamics Division National Center for Atmospheric Research.
TAO Project Mission: To provide real-time data from moored ocean buoys for improved detection, understanding, and prediction of El Niño and La Niña Customers:
KORDI’s observation project focusing on the tropical western Pacific Jae Hak Lee () Jae Hak Lee ( 李載學 ) Korea Ocean Research and Development Institute.
Tropical Moored Buoy Implementation Panel 25th Session of the Data Buoy Cooperation Panel Report of the Tropical Moored Buoy Implementation Panel to the.
Michael J. McPhaden NOAA/Pacific Marine Environmental Laboratory Seattle, Washington IAPSO Dynamic Planet Symposium Cairns, Australia 24 August 2005 ENSO.
TAO Project Mission: To provide real-time data from moored ocean buoys for improved detection, understanding, and prediction of El Niño and La Niña Customers:
Impact of TAO observations on Impact of TAO observations on Operational Analysis for Tropical Pacific Yan Xue Climate Prediction Center NCEP Ocean Climate.
Development of an Indian Ocean Moored Buoy Array for Climate Michael J. McPhaden NOAA/PMEL Outline:  Scientific background  Status of Implementation.
Interannual Variability (Indian Ocean Dipole) P. N. Vinayachandran Centre for Atmospheric and Oceanic Sciences (CAOS) Indian Institute of Science (IISc)
Strategic Plan for the TAO Project M. J. McPhaden, NOAA/PMEL Goal: To implement and maintain a global tropical moored buoy array in support of research.
Southern California Coast Observed Temperature Anomalies Observed Salinity Anomalies Geostrophic Along-shore Currents Warming Trend Low Frequency Salinity.
Report to CLIVAR SSG-14 CLIVAR/GOOS Indian Ocean Panel Gary Meyers (IOP Chair) & Mike McPhaden With Contributions from IOP Members and Friends Buenos Aires,
Tropical Moored Buoy Arrays in Support of Climate Research and Forecasting Contributions to the Global Ocean Observing System Nuku Hiva, Marquesas Islands.
Research Moored Array for African-Asian-Australian Monsoon Analysis and Prediction (RAMA): Rationale, Design, First Results, Status & Plans Mike McPhaden.
NAME SWG th Annual NOAA Climate Diagnostics and Prediction Workshop State College, Pennsylvania Oct. 28, 2005.
Report of the Tropical Moored Buoy Implementation Panel to the 22 nd Session of the Data Buoy Cooperation Panel October 16-20, 2006 San Diego, United States.
Michael J. McPhaden, NOAA/PMEL Dongxiao Zhang, University of Washington and NOAA/PMEL Circulation Changes Linked to ENSO- like Pacific Decadal Variability.
 El Niño and La Niña: Their Impacts on Global Climate and Geomorphic Systems Kathy Lipschultz.
Climate Prediction: Products, Research, Outreach Briefing for NOAA’s Science Advisory Board March 19, 2002 National Weather Service Climate Prediction.
TAV / PIRATA-17 Meeting, Kiel, Germany
LONG RANGE FORECAST SW MONSOON
El Niño / Southern Oscillation
LONG RANGE FORECAST SW MONSOON
LONG RANGE FORECAST SW MONSOON
Presentation transcript:

The Global Tropical Moored Buoy Array: Status & Plans Mike McPhaden OCO Review 3-5 Sept 2008 RAMA PIRATA TAO/TRITON

Global Tropical Moored Buoy Array: A coordinated, sustained, multi-national effort to develop and implement moored buoy observing systems for climate research and forecasting throughout the global tropics A contribution to GOOS, GCOS, and GEOSS

Indian Ocean RAMA

DJF JJA The Monsoon Half the world’s population depends on monsoon rainfall for agriculture ITCZ

Indian Ocean Climate Science Drivers  Seasonal monsoons  Cyclones and synoptic scale events  Intraseasonal Madden Julian Oscillation (  ENSO, west coast US weather, hurricanes)  Interannual variations: the Indian Ocean Dipole  Decadal variability  Warming trends since the 1970s  Complex ocean circulation  Poorly understood biogeochemistry Indian Ocean Dipole

 Plan developed by the CLIVAR/GOOS Indian Ocean Panel in 2004 as part of IndOOS  Basin scale, upper ocean (~500 m) focus.  Design supported by numerical model observing system simulation studies. RAMA McPhaden et al, 2008: RAMA. Bull. Am. Met. Soc., accepted.

RAMA: Present Status 47% of sites occupied by end of 2008 (22 of 46; 15 involve PMEL) Resource Formula: Partners provide ship time (~ days) NOAA provides most equipment

2006 Indian Ocean Dipole Neutral=±0.5°C

Comparison of Oct-Nov 2004 (Normal) & Oct-Nov 2006 (Dipole) NormalDipole

Subsurface Temperature leads SST: A Source of Indian Ocean Dipole Predictability? Horii et al, 2008, GRL Thermocline temperature anomalies mediated by wind forced upwelling Kelvin waves.

Dynamics of Wyrtki Jets Overbar: depth integral from surface to H=175 m ~0 Use RAMA, Argo, QuikSCAT data to assess linear dynamical balance at 0°, 80.5°E (f=0): Nagura & McPhaden, 2008, GRL Oct 2004Sept 2006 Zonal velocity Zonal transport

Cyclone Nargis Qscat Wind 28 Apr 2008 TMI/AMSR SST 2 May °N, 90°E Spot Hourly Data (~ 8 per day)

International Cooperation USA (NOAA) and Indonesia (DKP and BPPT) sign MOU in 2007 China (SOA) and Indonesia (DKP) sign MOU in 2007 USA (NOAA) and Japan (JAMSTEC) sign MOU in 2008 USA (NOAA) and India (MoES) sign MOU in 2008 U. Paris and U. Capetown are committing ship time to expand RAMA into SW Indian Ocean/MOU’s under discussion Tsunami/RAMA cruise RV Baruna Jaya III Sept 2007

RAMA Field Work cruises, 6 ships, 5 countries ~100 sea days In 2009: 130 sea days available (73 from India), enough to add 9 more ATLAS moorings  31 or 46 sites (67% complete)

Atlantic Ocean PIRATA

PIRATA Courtesy, P. Chang Partners Brazil (INPE & DHN) & France (IRD & Meteo-France) provide logistic support & most ship time: ~300 sea days during USA (NOAA) provides most mooring equipment & data processing Focus: Tropical Atlantic Climate Variability-- 1)Atlantic meridional mode 2)Atlantic warm events 3)Climatic conditions in “hurricane alley”

Prediction & Research Moored Array in the Tropical Atlantic (PIRATA) NE Extension begins SW Extension begins 2005 SE Extension begins 2006 Status in 2008 Status in 2004 CLIVAR/GOOS Review of PIRATA, 2006: “..the main backbone of the Tropical Atlantic Observing System”

Pilot Research Moored Array in the Tropical Atlantic PIRATA Introduced October 1998 Pilot Research Moored Array in the Tropical Atlantic (PIRATA)

Pilot Research Moored Array in the Tropical Atlantic PIRATA Introduced October 1998 Pilot Research Moored Array in the Tropical Atlantic (PIRATA) Prediction and Research Moored Array in the Tropical Atlantic PIRATA Redefined August 2008

Pacific Ocean TAO/TRITON

TAO/TRITON TAO/TRITON Array & the El Ni ñ o/Southern Oscillation (ENSO) Cycle  Implemented as part of TOGA  Presently a U.S./Japan collaboration  Transition to operations at NDBC underway

Current Conditions

Status--  FY 05: NDBC assumes responsibility for TAO management  FY 06: TAO DAC transferred to NDBC  FY 07: TAO field operations transferred to NDBC  FY Initial tests of NDBC prototype ATLAS refresh mooring system (COTS)  FY 09: If prototypes work, parallel testing next to legacy ATLAS in Pacific for 1 yr  FY 10: Evaluation and verification of refresh ATLAS system performance  FY 11-12: capitalization and replacement of all 55 legacy ATLAS with refreshed ATLAS TAO Transition The Plan: 3-year transition starting in FY 05 and ending in FY 07 CONCLUSION: TAO Transition will take at least 8 years to complete, not 3. QUESTIONS: 1)What went wrong with the original plan? 2)Will the transition be successful? 3)Is TAO transition a good model for future transitions? 4)Should the climate community be concerned?