Barrow’s Arctic Ocean Developing a Cabled Seafloor Observatory to Complement the Barrow Global Climate Change Facility the “BGCCRF” Developing a Cabled.

Slides:



Advertisements
Similar presentations
John A. Orcutt Deputy Director, SIO Ocean Observations Initiative NSF MREFC Chair, NSF/CORE DEOS Comm.
Advertisements

MeDON Phase II - Outline MeDON Partners Meeting, Plymouth. March 8 th 2012 Chris Gallienne, PML An initial investigation of potential development of MeDON.
January 2011 The MARS Deep-Sea Observatory in Monterey Bay Yanwu Zhang, James Bellingham, Gene Massion, Craig Dawe, Steve Etchemendy, and Christopher Scholin.
NVC0901 Maritime Alliance Symposium San Diego, August 2011 By: Michael Broadbent Fugro Pelagos Inc. Seafloor Mapping Technologies.
Concepts for Integrating Ocean Science Sensors on Submarine Cables.
Deep Seafloor Features Mapping the seafloor – Bathymetry- study and mapping of seafloor elevations – Techniques Early explorers measured depth with rope.
Ocean Technology Test Bed Colin Bradley, University of Victoria John Roston, McGill University NEPTUNE Canada VENUS.
Bathymetry Lab Adam Fox Coastal Carolina University.
INTRODUCTION TO GENERAL OCEANOGRAPHY (GEOL 1033) “Few people stand at the edge of the sea without feeling awed by its size and power, and without wondering.
Oil Spill Detection and Tracking Technologies Aircraft and Autonomous Aircraft Detection Methods Autonomous Surface Vessel Tracking Methods Autonomous.
Seafloor Mapping In Partnership with Colleen Peters By: Ashley Landis.
SHELL ALASKA Program Update March 2015.
GEO/OC 103 Exploring the Deep …. Today’s Tune “ Sink to the Bottom” Fountains of Wayne.
Mapping the Seafloor. Depth Soundings The earliest soundings were made with a hand line of rope weighted at one end. The earliest soundings were made.
Introduction to future synergy options Uli Katz ECAP, Univ. Erlangen Deep Ocean Cabled Observatories Amsterdam, May 2012.
Essential Questions What are some of the different types of remote sensing? How are satellites and sonar used to map Earth’s surface and its oceans? What.
Section 2.3 Remote Sensing
Inductive Power System for Autonomous Underwater Vehicles
Partnership in Unmanned Marine Systems GATE Electronics TR Technologies TURKEY.
Remote Sensing Section 2.3. Landsat Satellite The process of gathering data about Earth using satellites, airplanes, or ships is called remote sensing.
Marine Autonomous and Robotic Systems Facility at NOC 20 th March David White 20 th March
Section 1: The Water Planet
Copyright 2005SIEP B.V.Shell Exploration & ProductionEPT-EIP0 Shell Exploration & Production 1 End user requirements (2) – some examples Alaska summer.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Image: MODIS Land Group, NASA GSFC March 2000 Center for Satellite Applications.
Sensors and Samplers Modern Oceanographic Tools (Content and Images from Woods Hole Oceanographic Institute Sensors and Samplers Section)
1 Development of a Long Term Observatory Based on ESONET, VENUS, MARS and NEPTUNE Sponsored by StatOil To quantify fluid flow and carbon/methane oxidation.
U.S. Geological Survey Woods Hole Field Center Background, Data & Visualization Background, Data & Visualization Matthew Arsenault USGS Woods Hole Science.
The role of gliders in sustained observations of the ocean Deliverable 4.1 or WP 4.
Lesson 23: Technology II. Strides in underwater research Did you know that most of the ocean (>95%) still hasn’t been explored? Technologies developed.
Alaska Ocean Observing System Regional association under IOOS Part of coastal GOOS Ocean component of GEOSS IPY opportunity.
Physical Oceanography Chapter Branches of Oceanography Physical Oceanography - study of the motions of seawater, particularly waves currents and.
Understanding Earth Chapter 17: Earth Beneath the Oceans Copyright © 2004 by W. H. Freeman & Company Frank Press, Raymond Siever, John Grotzinger, and.
Structure of Ocean Basins Chapter 4. Focus now on structure  Problem of the ocean being remote  First “soundings” were made with a weight attached to.
HOW DO WE STUDY THE SEAFLOOR?. 1. Line-sounding – starting around 85 B.C. lead weighted ropes were dropped over the side of the boat and the depth was.
Laura Beranzoli Istituto Nazionale di Geofisica e Vulcanologia October 5-7, 2009ESONET NoE - 2nd All Region Workshop WP4 – Demonstration Missions.
General Assembly Meeting – SA Session | Crete Oct SA Observatory 15 PYLOS – Southern Ionian Sea water column and seabed observations to access deep.
The Alaska Ocean Observing System (AOOS) The Alaska Ocean Observing System (AOOS) A Regional Coastal Observing System within the Integrated Ocean Observing.
IES Integration of research activities on a long-term perspective Co-operation between universities, research institutes, enterprises and technology organisations.
June 2011_ M. DEL BRENNAProperty of Prysmian SUBMARINE CABLE INSTALLATION Data required for effective design 13° Meeting of Marine Observation and Data.
Understanding Earth Chapter 17: Earth Beneath the Oceans Copyright © 2004 by W. H. Freeman & Company John Grotzinger, Thomas H. Jordan, Frank Press and.
Labs Start Next Week Don’t forget your lab book!!!  Read through labs ahead of time  Exploring the Deep: GEO/OC 103 Lab Manual by Hall-Wallace et al.
Monterey Accelerated Research System
The Global Ocean The Vast World Ocean.
Winter Lead Convection The Study of Environmental Arctic Change (SEARCH) and the Barrow Cabled Observatory Presentation at Science and Education Opportunities.
Irish Sea Public domain: From Irish National Tidegauge NetworkIrish National Tidegauge Network Mean spring tides.
Department of the Interior uses NOAA Hydrographic Services data, products and services Susan Russell-Robinson Acting Program Coordinator, USGS Coastal.
Hydrographic Services Review Panel October 2010 David Fox Oregon Department of Fish & Wildlife Marine Resources Program Use of seafloor mapping data in.
Future needs and plans for ocean observing in the Arctic AOOS Arctic Town Hall Futur Zdenka Willis Integrated Ocean Observing System National Program Office.
Ocean Exploration & Energy Capitol Hill Oceans Week 2003 June 11, 2003 Art A. Kleiner, Hydrographer C & C Technologies, Inc.
SIDE SCAN OVERVIEW. Sidescan Survey Overview A sidescan sonar can be used for a wide variety of survey operations. Search and recovery Geological Identification.
© 2002 Brooks/Cole, a division of Thomson Learning, Inc. BATHYMETRY New technology, such as this bathyscaphe, allows scientists to study deep-ocean basins.
Some of the types of equipment oceanographers use to do research.
5th Workshop on "SMART Cable Systems: Latest Developments and Designing the Wet Demonstrator Project" ( Dubai, UAE, April 2016) Implementation Topics.
© 2014 Pearson Education, Inc. Marine Provinces Chapter 1 Clickers Essentials of Oceanography Eleventh Edition Alan P. Trujillo Harold V. Thurman © 2014.
Mapping Technology.
Section 3: Remote Sensing
Bathymetry of the Sea Floor
USS Hawkbill, Pearl Harbor, Hawaii
Mapping the Seafloor.
Understanding Earth Fourth Edition Chapter 17:
Mapping the Seafloor.
Future of Deep-Ocean Observatories
CHALLENGES IN PROVIDING MARINE DATA IN FORMATS DESIGNED FOR LAND-BASED DATA Karen Douglas|
The Missing Piece of Wegener’s Continental Drift Puzzle
The feasibility of Measuring Abyssal Ocean Temperature with Thermometers Embedded in the Trans-Ocean Communication Cables David Murphy, Bruce Howe, Roger.
Users will plan and build sensor networks for simulated cabled ocean observatories.
Oceanography.
Lesson 23: Technology II.
Exploring the Ocean Floor & Its Features
Presentation transcript:

Barrow’s Arctic Ocean Developing a Cabled Seafloor Observatory to Complement the Barrow Global Climate Change Facility the “BGCCRF” Developing a Cabled Seafloor Observatory to Complement the Barrow Global Climate Change Facility the “BGCCRF”

BGCCRF Design Process Developed through a series of meetings with user groups Original Design included Seawater Intake Developed through a series of meetings with user groups Original Design included Seawater Intake

Seawater Intake Meeting Held at MBARI October 10, 2003 Approximately 30 attendees Discussed multiple uses Constraints on seawater intake Use as a “cable run” for Seafloor Observatories How to install it? Held at MBARI October 10, 2003 Approximately 30 attendees Discussed multiple uses Constraints on seawater intake Use as a “cable run” for Seafloor Observatories How to install it?

Everyone was excited about the potential for Seafloor Observatories……..  Broadband Acoustic Monitoring - marine mammals, acoustic tomography, volcanic activity  Visual Monitoring - scheduled, triggered or remotely triggered  Seafloor Seismometers  Oceanographic - monitor water column  Active Acoustic - observe currents and ice  Tethered -reeled in and out  Autonomous Underwater Vehicle Docking  Intercommunication between nodes  Broadband Acoustic Monitoring - marine mammals, acoustic tomography, volcanic activity  Visual Monitoring - scheduled, triggered or remotely triggered  Seafloor Seismometers  Oceanographic - monitor water column  Active Acoustic - observe currents and ice  Tethered -reeled in and out  Autonomous Underwater Vehicle Docking  Intercommunication between nodes

….and nervous about the cost  Slant drilling for 4-5 km is near the limit for the technology  Not Cheap  The Seawater intake has been eliminated from the design.  Slant drilling for 4-5 km is near the limit for the technology  Not Cheap  The Seawater intake has been eliminated from the design.

Spin Cycle “On”  Elimination of the Seawater Intake is an Opportunity  Permits us to select optimum Site for Installation  Where is it?  Elimination of the Seawater Intake is an Opportunity  Permits us to select optimum Site for Installation  Where is it?

Land-Based Sea Ice Radar at Barrow, AK data courtesy of Andy Mahoney-UAF  10 kW X-Band marine radar  level ice, open water and radar shadows appear black  detects ice floes up to 10 km from shore  captures detailed development of landfast sea ice

Edge of landfast ice; courtesy Andy Mahoney-UAF

High-Resolution Bathymetry off Barrow

Data Needs to identify best Cable Location Multi-beam Bathymetric Survey identify bottom features to avoid or exploit Sidescan Survey map ice gouges Chirp sub-bottom profiler Survey estimate penetration depth of ice keels Repeat identify the active areas