Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali,...
-
Upload
julius-flowers -
Category
Documents
-
view
214 -
download
1
Transcript of Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali,...
![Page 1: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/1.jpg)
Development of an Indian Ocean Moored Buoy Array for Climate
Paul FreitagNOAA/PMEL
SEACORM
Bali, Indonesia
7-9 June 2006
![Page 2: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/2.jpg)
Scientific Background and Societal Context
![Page 3: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/3.jpg)
Indian Ocean Science DriversImproved description, understanding and prediction of:
Seasonal monsoon variability
Monsoon <=> ENSO interactions
Indian Ocean Dipole (El Niño-like phenomenon in the Indian Ocean)
Intraseasonal oscillations and both near and far field impacts (Asian monsoon active/break periods; west coast US rainfall, Atlantic hurricane formation, ENSO)
SST warming trends since the 1970s
Indonesian Throughflow
General ocean circulation, ocean heat transport, and their variability
Indian Ocean Dipole
Webster et al, 1999, Nature
![Page 4: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/4.jpg)
Efforts to develop an Indian Ocean component to the Global Ocean Observing system for climate studies are accelerating
Compelling unanswered scientific questions;
Potential societal benefits from development of skillful monsoon prediction models;
One of the most poorly sampled regions of the world ocean;
Growing ocean science investments from India, Japan, and U.S., and nations surrounding the Indian Ocean;
Inauguration of plans for the Global Earth Observing System of Systems (GEOSS) in 2003;
Inauguration of a CLIVAR/GOOS Indian Ocean Panel in 2004;
![Page 5: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/5.jpg)
Network Design
All Components
Moored Array
![Page 6: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/6.jpg)
CLIVAR/GOOS Indian Ocean PanelProgress on Sustained Observing System● Basin scale mooring array
● Integrated approach to moorings, Argo floats, XBT lines, drifters, and satellites
● Alternative observational strategies assessed by observing system simulations
● Report: The role of the Indian Ocean in the climate system—implementation plan for sustained observations
http://eprints.soton.ac.uk/20357/
![Page 7: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/7.jpg)
Integrated, Multi-platform Ocean Observing System
Carbon/hydro cruise
High density XBT
Frequently repeated XBT
Enhanced XBT lines to monitor Indonesian Throughflow, inflow to western boundary, Java upwelling and 10°S thermocline ridge
Emphasis on ocean, but will provide surface met data as well
Argo floats 3°x 3° Drifters 5°x 5°
~20 real-time tide gauges for IOTWS
Regional mooring arrays
![Page 8: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/8.jpg)
Satellite and In Situ Obs
Satellite remote sensing of SST, wind, sea level, ocean color, precipitation, and salinity* is critical
Spatial and temporal coverage of surface properties
In situ measurements provide the 3-dimensional perspective
Combined observations used for model validation & development, initialization of climate & weather forecasts, and ocean state estimation.
* First salinity remote sensing satellites will fly in 2007 (ESA/SMOS) and in 2009 NASA/Aquarius)
Cloud penetrating capabilities of TMI yields an SST data suitable for intraseasonal analysis
![Page 9: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/9.jpg)
Draft Strategy for Indian Ocean Moored Buoy Array
*Actual sea days in 2006: involves more than just mooring work
![Page 10: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/10.jpg)
Moored Measurement Suite
Standard
Met: Wind, RH, AT, SWR, Rain
Ocean: SST, SSS, T(z:10 depths), S(z: 5 depths), P (z: 2 depths); v (10 m)
Flux Sites: Standard plus--
Met: LWR, BP
Ocean: Additional T(z), S(z), v (z) in upper 100 m
All data transmitted to shore in real-time via Service Argos
![Page 11: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/11.jpg)
Design Considerations
![Page 12: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/12.jpg)
Indian Ocean “Dipole” or “Zonal Mode”
First reported in Nature by Saji et al and
Webster et al in 1999
![Page 13: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/13.jpg)
Ocean Circulation and its Relation to SST
• Cross-equatorial transport carried by-- Somali Current north-- Ekman transport south
• What is relative strength of the different upwelling centers? How do they vary from intraseasonal to decadal time scales?
• What is relation of ITF to general circulation in the Indian Ocean?
Schott et al., 2002
![Page 14: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/14.jpg)
Intraseasonal & MJO Variations“Building Block for the Monsoons”
Elongated zone between 0°-10°S exhibits elevated intraseasonal SST, wind, and OLR variance
Air-sea interaction & mixed layer dynamics are critical to understanding and predicting variations in this region.
Band-passed (30-90 day periods) standard deviation for DJF
TOP: SST (color), wind speed (m/s)
BOT: SST (color), OLR (W/m2)
![Page 15: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/15.jpg)
Rationale for Flux Sites
Courtesy of Lisan Yu, WHOI
![Page 16: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/16.jpg)
Implementation of Moored Array and Initial Data
![Page 17: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/17.jpg)
41 Day Cruise 4 ATLAS & 1 ADCP mooring
Mooring ImplementationORV Sagar Kanya Cruise
9 October – 17 November 2004
PMEL in collaboration with the National Institute of Oceanography (NIO) and the National Center for Antarctic and Ocean Research (NCAOR), Goa, India. http://www.pmel.noaa.gov/tao/disdel/
![Page 18: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/18.jpg)
Meteorological Data at 0°, 90°E
![Page 19: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/19.jpg)
ATLAS at 0, 80.5E
MLD based on =0.15 kg m-3 from surface value
Transition winds (Nov-Dec)
Northeast Monsoon (Feb-Mar)
Wyrtki Jet (Nov-Dec)
Northeast Monsoon Current (Feb-Mar)
O(1°C) week-to-week and seasonal SST changes
50 m intraseasonal MLD changes (Nov-Jan)
Shallow and steady during NE monsoon (Feb-Mar)
![Page 20: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/20.jpg)
Preliminary ResultsIndo/US TAO Mooring
Mixed layer heat balance
Surface heat fluxes
![Page 21: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/21.jpg)
Indian Ocean Moored Buoy Data Assembly Center (DAC)
Modeled after TAO/ TRITON and PIRATA data processing and dissemination systems.
PMEL and JAMSTEC initial contributors.
Hosted at PMEL; potential for mirror sites outside the US (e.g. in Indonesia).
http://www.pmel.noaa.gov/tao/disdel/disdel.html
![Page 22: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/22.jpg)
Challenges & Plans
![Page 23: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/23.jpg)
FY06 Budget for NOAAClimate Observations and Services
“…[Funds] to expand the Tropical Atmosphere Ocean array… into the Indian Ocean. This expansion will enhance NOAA's capability to accurately document the state of ocean climactic conditions and improve seasonal forecasting capability.”(http://www.noaanews.noaa.gov/stories2005/s2386.htm)
Other activities covered by this funding:
Add salinity sensors to the TAO array to improve seasonal-interannual forecasting. Upgrades for 4 TAO and 3 PIRATA moorings to ocean reference station quality. Provide 4 additional buoys for the PIRATA array in the hurricane-genesis region of the Atlantic Ocean for improved understanding of ocean-atmosphere interactions on hurricane development. Support the technological development of the next generation of moored buoys
![Page 24: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/24.jpg)
New 2006 JAMSTEC Budget Initiative
JAMSTEC received a new 5-year budget starting in Japanese FY2005 for promoting the Indian Ocean mooring array as a part of "JEPP: Japan EOS (Earth Observation System) Promotion Program" which is a new program of Japanese government related GEOSS. JEPP will enable the development of new small size TRITON buoy and the continuation of the present TRITON sites in the Indian Ocean.
![Page 25: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/25.jpg)
Challenges: Ship Time
Requirements:
> 140 days per year to maintainfull array
Must be available routinely and with regularity
Assumes 1-year mooring design lifetime and annual servicing cruises
![Page 26: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/26.jpg)
Ship time needs based on these hypthetical tracks
![Page 27: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/27.jpg)
Near-Term Mooring Array PlansRV Baruna Jaya
2006 (BRKT/NOAA)
ORV Sagar Kanya August 2006
RV Suroit February 2007
(CIRENE)
RV Mirai Nov 2006 (MISMO)
SOA/NOAA Cooperation (?)
![Page 28: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/28.jpg)
Near-Term Mooring Array Plans
•Deploy 2 new ATLAS moorings (4ºN, 8ºN)
•Repair 2 existing ATLAS
moorings (0º, 1.5ºN if required)
•Jakarta to Padang
•14 days for transit and mooring operations (assuming 10 kt)
![Page 29: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/29.jpg)
Summary
The international community has developed plans for an integrated Indian Ocean observing system for climate research and forecasting.
The array design is based on observing, understanding, and predicting key ocean and climate phenomena that have significant socio-economics impacts on countries surrounding the basin and that affect global climate variability.
The plan has been endorsed by CLIVAR and GOOS; implementation is underway.
The newest component of the observing system is a basin scale moored buoy array, with initial contributions from the U.S., India, and Japan.
There are many challenges to full implementation of this array, but success promises significant scientific and societal benefits.
![Page 30: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/30.jpg)
Issues
Developing partnerships that enable efficient and sustained implementation of the array
Identifying and overcoming resource limitations, especially ship time
Building capacity for transfer of scientific and technical expertise in mooring operations and data analysis to regional partners
Coordinating international contributions (underway through CLIVAR/GOOS IOP and through bilateral agreements)
Ensuring integration and dissemination of all observing system data for climate research, model development and forecasting
Leveraging available resources for development of multi-hazard warning systems, e.g. for climate, weather, tsunami*, etc.
* see McKinnie talk for tsunami
![Page 31: Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.](https://reader036.fdocuments.us/reader036/viewer/2022062719/56649ef35503460f94c052ee/html5/thumbnails/31.jpg)
Thank You