Monitoring the Endeavour – Middle Valley Hydrothermal Systems: Integrated heat and mass fluxes and the response of biogeochemical and physical processes.

Slides:



Advertisements
Similar presentations
The Terrestrial Planets
Advertisements

Mooring Activities at SAMS NERC 4 th Moorings Workshop 15 th /16 th May 2008 Mooring Activities at SAMS NERC 4 th Moorings Workshop 15 th /16 th May 2008.
Fourth Annual Conference on Carbon Capture & Sequestration Developing Potential Paths Forward Based on the Knowledge, Science and Experience to Date Geologic.
Lesson 12: Technology I Technology matters Most of the topics we’ve learned so far rely on measurement and observation: – Ocean acidification – Salinity.
Fourier law Conservation of energy The geotherm
MoMAR* : suivi à long terme des systèmes hydrothermaux de la dorsale Médio Atlantique près des Açores. * Monitoring the Mid Atlantic Ridge.
Heat Flow in Young Oceanic Crust: Is Earth’s Heat Flux 44 TW or 31 TW 2008 Joint Assembly, Ft. Lauderdale T21A-01, May 27, 2008 T-21A Thermotectonic Models.
THE STUDY OF BIOGEOCHEMICAL CYCLES AND RELATED SEDIMENT FLUXES: THE IOC-BSRC PROJECT PROPOSAL Could such a project idea be developed into an EC FP Integrated.
Physical Oceanography and Endeavour Regional Circulation Moorings ONC NEPTUNE Canada Science Steve Mihaly, ONC Rick Thomson, DFO.
Jacob Adams ME 340 Winter The Problem: Long complex boiling equations Numerous cases and different variations can be confusing Evaluation takes.
Coupled microbiological and biogeochemical studies of the deep crustal biosphere along the Juan de Fuca Ridge flank.
Ocean Features.
TREX-NET TRibal Environmental eXchange Network.
Ocean Networks Canada Endeavour Site Sampling for CRUISE FALL 2012 – now scheduled for 2013 Equipment List for Thompson ADCP ADCP Echo sounder Echo sounder.
Mid-Ocean Ridges: A Connected System Hydrothermal circulation links ocean, seafloor, and crust, including vent communities How is fluid circulation controlled.
Spatial and Temporal Variability of Hydrography in the Vicinity of the Main Endeavour Field Scott Veirs, Christian Sarason, Russell McDuff, Fritz Stahr,
3 Types of Metamorphism Miss Holl Rowland High School October 24, 2006.
Parameters and instruments A. Proshutinsky, Woods Hole Oceanographic Institution Science and Education Opportunities for an Arctic Cabled Seafloor Observatory.
It’s a microbial world (And was and will be to the end)
* Institut de Physique du Globe Paris
Recent interests Discovery of hydrothermal vent The link between global warming & ocean: the Carbon story Microbial loop Industrialized mariculture: Peter.
Summary and background: Thorough characterization of microbial habitats within submarine volcanoes demands that fluid flow models include the chemical.
Extant models: Thorough characterization of microbial habitats within submarine volcanoes demands that fluid flow models include the chemical reactions.
$100 $400 $300$200$400 $200$100$100$400 $200$200$500 $500$300 $200$500 $100$300$100$300 $500$300$400$400$500.
ASCOS ice camp Oden ”Met Alley & Ocean ”Open Lead” 5700 meter 3200 meter.
OET Nautilus Workshop University of Rhode Island, ISC 6–9 May 2013 OET Nautilus Workshop University of Rhode Island, ISC 6–9 May 2013 AT25-04: Hydrogeologic,
Heat Transfer Important: This chapter follows mainly on chapter 4 in Turcotte and Schubert textbook.
MoMAR : a coordinated and multidisciplinary long-term study of hydrothermal ecosystems at the Mid-Atlantic Ridge close to the Azores archipelago. Hydrothermal.
Measurements in the Ocean Peter Challenor University of Exeter and National Oceanography Centre.
Life in Extreme Environments: A Study of the Prevalence of life in the Depths of an Underwater Rift Zone.
ROSCOE Vicki Ferrini: Data Representative/Team Leader Breea Govenar: Research Scientist/Data Representative Laishona Vitelli: K-12 Educator David Reeder:
NEPTUNE Canada Hydrothermal Experiments at Main Endeavour: Status Report Dave Butterfield, Univ. of Washington and NOAA/PMEL Marv Lilley, University of.
Little Diomede Island, Bering Strait BERING STRAIT THROUGHFLOW ARC Comparison of Water Properties and Flows in the U.S. and Russian Channels of.
Laura Beranzoli Istituto Nazionale di Geofisica e Vulcanologia October 5-7, 2009ESONET NoE - 2nd All Region Workshop WP4 – Demonstration Missions.
Using satellite observations to measure the direct climate impacts of oil palm expansion in Indonesia Natalie Schultz Heat budget group meeting June 13,
SCIENTIFIC DRILLING OF THE MUTNOVSKY MAGMA-HYDROTHERMAL SYSTEM (KAMCHATKA, RUSSIA): TESTING THE MAGMA-HYDROTHERMAL CONNECTION Alexey V. Kiryukhin 1, J.
Walker River Basin Project Agriculture, Restoration, and Plant/Soil/Water Interactions Tasks 4 & 5 Summary2008.
IES Integration of research activities on a long-term perspective Co-operation between universities, research institutes, enterprises and technology organisations.
Autosub 7 m long x 0.9 m dia 2,700 kg in air Maximum Depth: 1600 m. Speed: 1 to 4 knots Endurance: Up to700 km depending on speed, hotel load etc. Large.
IV. Modern Plate Tectonic Theory
Flow Mow - a study of hydrothermal heat flux Who: Russ McDuff, Fritz Stahr, Scott Veirs, Christian Sarason - (UW); Ko-ichi Nakamura - (GSJ); Al Bradley,
MoMAR : a coordinated and multidisciplinary long-term study of hydrothermal environments at the Mid- Atlantic Ridge / MoMAR-Fr The MOMAR (“Monitoring the.
Southern Sierra Critical Zone Observatory Integrating measurements for advances in hydrology & geochemistry A research platform for studying Earth surface.
 The Importance of Hydrothermal Vents. Completely changed our view of life.  Chemosynthesis.  “Extreme’ life forms.  New ideas on the origin of life.
Serving Multidisciplinary Data For Ridge2000 and MARGINS Programs William B. F. Ryan, Suzanne Carbotte and MGDS Team.
What is a metamorphic rock? How is it formed? Metamorphic Rock Chapter 6, Section 3 Scripps Classroom Connection.
Chapter 12: The Seafloor. Introduction The seafloor makes up the largest part of the Earth’s surface.
Extant models: Thorough characterization of microbial habitats within submarine volcanoes demands that physical flow models be combined with models of.
Intensive water and chemistry flux site: paired canopy and open-canopy sites Water flux site: paired canopy and open-canopy sites Pyronmeter Throughfall.
Introduction Diffuse flow is detected using remote acoustic imaging. It is traditionally difficult to measure because it has a lower temperature and velocity.
Profiling and Moored Instrumentation: Applications for Aquatic Ecosystems Sally MacIntyre Marine Science Institute University of California at Santa Barbara.
O ET Central question: How do plumes and currents interact above the Main Endeavour vent field to affect the measurement of hydrothermal heat flux? Approach.
Boundary layer models of Martian hydrothermal systems Kate Craft 11/2/2007.
Image from
Metamorphic Rocks In Greek the word morphos means form or shape. The word metamorphism means the change of form. Within the Earth we find temperatures.
$200 $400 $600 $800 $1000 $200 $400 $600 $800 $1000 $200 $400 $600 $800 $1000 $200 $400 $600 $800 $1000 $200 $400 $600 $800 $1000 $200.
Honors Chemistry Podcast 2.3 Joule Problems Q = mc  T.
University of New Mexico
CHEMICAL OCEANOGRAPHY AT THE UNIVERSITY OF WASHINTON
Amanda Williams, Scott Glenn, Josh Kohut,
P6314: Field Oceanography Cruise Report
What are hydrothermal Vents?
COM – LMGEM CPPM Tamburini C., Robert A., Fuda JL., Lefèvre D…
Hydrology of a Dynamic Earth March 2007
Heat Transfer Important: This chapter follows mainly on chapter 4 in Turcotte and Schubert textbook.
Calorimetry Practice 1. If a 1.45 g sample of iron at 95.0 ˚C is placed into water at 21.6 ˚C , if the final temperature of the water and iron is 26.7.
Range of Variables Currently Received
What amount of heat is required to increase the temperature of 75
CREST CAChE Student Poster Template
Evaluate the integral {image}
Presentation transcript:

Monitoring the Endeavour – Middle Valley Hydrothermal Systems: Integrated heat and mass fluxes and the response of biogeochemical and physical processes to perturbations Kathryn Gillis, Neil Banerjee, David Butterfield, Laurence Coogan, John Delaney, Mark Hannington, Deborah Kelley, Marv Lilley, Russ McDuff, Steven Mihaly, Karlis Muehlenbachs, Adam Schultz, Rick Thomson

What are the impacts of tectonic and magmatic perturbations on biogeochemical and hydrological processes in ridge crest environments and the overlying water column? What are the total fluxes of heat, chemistry, and biomass out of a hydrothermal system? Endeavour Node

Instrument Update High T vent sites: microbial incubator – in progress, no contract temperature-hydrogen-resistivity probe – in progress, no contract Imaging sonar system –2010? Low T vent sites: tempo-mini – camera, temperature probes, O probes; recently tested at VENUS fluid sampler – in progress, no contract camera – ?? Regional circulation moorings: CTD, ADCP, current metres – almost ready?