Lecture 22 Deployment Strategies Fixed Platforms Collin Roesler 18 July 2007.

Slides:



Advertisements
Similar presentations
Day 3 Platforms Biological sensors Chemical sensors.
Advertisements

Future Directions and Initiatives in the Use of Remote Sensing for Water Quality.
High Resolution Time Series Measurements of Bio- optical and Physical Variability in the Coastal Ocean as Part of HyCODE Dickey Mooring.
Observatory # 23 Filchner – Ronne Weddell Sea Antarctica Svein Østerhus UNI Climate
Carmen E. Morales - Samuel Hormazabal Isabel Andrade - Marco Correa-Ramírez Universidad de Concepción P. Universidad Católica de Valparaíso CHILE (FONDECYT.
Falmouth High School Freshman Science School Grounds Survey Project Kimberly Blenk Gary Glick Chris Moore Summer 2011.
Tim Smyth and Jamie Shutler Assessment of analysis and forecast skill Assessment using satellite data.
SIO 210: I. Observational methods and II. Data analysis (combined single lecture) Fall 2013 Remote sensing In situ T, S and tracers Velocity Observing.
1 Current CTD-Satellite Relay Data Logger (CTD-SRDL) with CTD head (black) based on an inductive cell (2). Bottom left picture shows a CTD-SRDL deployed.
Brown Bag Lunch Lecture ABI Calibration
Bio-optical Gliders and Profiling floats in the Mediterranean ARGO SCIENCE WORKSHOP – MARCH 13 – 18, 2006 Fabrizio D’Ortenzio 1, Katarzyna Niewiadomska.
GoMOOS G ulf of M aine O cean O bserving S ystem Telemetry System Design for Reliability Robert Stessel GoMOOS / University of Maine.
Radiometric and Geometric Errors
AOSC 634 Air Sampling and Analysis Lecture 1 Measurement Theory Performance Characteristics of instruments Nomenclature and static response Copyright Brock.
Seasonal to Interannual Variability in Phytoplankton Biomass and Diversity on the New England Shelf Heidi M. Sosik Hui Feng In Situ Time Series for Validation.
RAPID-MOC Mooring Array Instrumentation l Instrument types and specifications l Telemetry.
Calibration and Status of MOBY Dennis Clark, NOAA/NESDIS Carol Johnson, NIST Steve Brown, NIST Mark Yarbrough, MLML Stephanie Flora, MLML Mike Feinholz,
Aquarius/SAC-D Mission Validation Working Group Summary Gary Lagerloef 6 th Science Meeting; Seattle, WA, USA July 2010.
Temporal and Spatial Variability of Physical and Bio-optical Properties on the New York Bight Inner Continental Shelf G. C. Chang, T. D. Dickey Ocean Physics.
Parameters and instruments A. Proshutinsky, Woods Hole Oceanographic Institution Science and Education Opportunities for an Arctic Cabled Seafloor Observatory.
Satellite Drifter Technology Dr. Sergey Motyzhev.
Problem Description: To develop an autonomous network for monitoring aquatic environment Problem Description: To develop an autonomous network for monitoring.
OSMOSIS Primary Production from Seagliders April-September 2013 Victoria Hemsley, Stuart Painter, Adrian Martin, Tim Smyth, Eleanor Frajka-Williams.
Real-time Monitoring of the Derwent and Huon Estuaries in Southern Tasmania Greg Timms Senior Research Scientist Tasmanian ICT Centre, CSIRO 20 May 2009.
Southern Ocean Air-Sea Flux Observations Eric Schulz, CAWCR, BoM.
Why We Care or Why We Go to Sea.
Brief Review of Lecture 1 Understanding Science, Oceanography, Physical Oceanography Descriptive or Dynamical Approaches Eulerian or Lagrangian techniques.
Measurements in the Ocean Peter Challenor University of Exeter and National Oceanography Centre.
UNDERWATER GLIDERS.
Norm Nelson, UCSB Chantal Swan, UCSB / ETH with assistance of: Julia Gauglitz, Teresa Serrano Catala, Erica Aguilera UltraPath in the Oligotrophic Ocean.
Earth Observation from Satellites GEOF 334 MICROWAVE REMOTE SENSING A brief introduction.
The role of gliders in sustained observations of the ocean Deliverable 4.1 or WP 4.
Interdisciplinary Integration and Research Directions CMOP possesses a wide range of interdisciplinary research assets - Biological - Chemical - Physical.
Salinometer Thermosalinograph (TSG) CTD
”MOBY-Net, an ocean color vicarious calibration system” PI: Kenneth Voss, Physics Dept., Univ of Miami Co-I’s: Carol Johnson (NIST), Mark Yarbrough (MLML),
Soe Hlaing *, Alex Gilerson, Samir Ahmed Optical Remote Sensing Laboratory, NOAA-CREST The City College of the City University of New York 1 A Bidirectional.
Final General Assembly – Paris, France – September 19, 2014 FP7-Infra : Design studies for European Research Infrastrutures 1st October 2011.
Chlorophyll Results Ocean Optics 2004 Mike Sauer & Eric Rehm.
OOI Annual Review Year 2 May 16 – 20, 2011 Ocean Observatories Initiative Surface and Subsurface Mooring Telemetry Inductive and acoustic technology and.
CONRAD BLUCHER INSTITUTE ACTIVITIES SUPPORTING TEXAS PORTS AND WATERWAYS OPERATIONS Two Inter-related Services to the Port Community: 1. The Texas Coastal.
1 Quality Control of Phycoerythrin Data from The Columbia River Estuary Development of a Correction for Turbidity Artifacts. Observation ● Prediction ●
An Inexpensive Deployable Acoustic Snow Observing Sensor (IDASOS) Sean Helfrich NESDIS Snow and Ice Product Area Lead National.
Context Events Situation Limits Strategy Glider Observation of Suspended Particle Dynamics in the Gulf of Lions Gaël MANY 1, François Bourrin 1, Romaric.
Ocean Color Remote Sensing Pete Strutton, COAS/OSU.
Why We Care or Why We Go to Sea.
Ice Tethered Profiler (ITP) Moorings WHOI Principle Investigators John Toole Rick Krishfield Andrey Proshutinsky WHOI Principle Investigators John Toole.
Update on Ferrybox Improvement of process understanding through the use of high frequent Ferrybox observations Henning Wehde, Dominique Durand, Pierre.
VIIRS Product Evaluation at the Ocean PEATE Frederick S. Patt Gene C. Feldman IGARSS 2010 July 27, 2010.
CHAPTER 5: Data sampling design, data quality, calibration, presentation Sampling Physical variables are continuous, but samples (water samples) and digital.
Lecture 22: Deployment strategies for different optical sampling platforms: mobile platforms (AKA “ALPS) What are mobile platforms? Why use them? Some.
SeaWiFS Calibration & Validation Strategy & Results Charles R. McClain SeaWiFS Project Scientist NASA/Goddard Space Flight Center February 11, 2004.
03/24/2004 Broadband Seismometer Workshop, Lake Tahoe 1 Akiteru Takamori Earthquake Research Institute, University of Tokyo In Collaboration with: Alessandro.
CIOSS Ocean Optics Aug 2005 Ocean Optics, Cal/Val Plans, CDR Records for Ocean Color Ricardo M Letelier Oregon State University Outline - Defining Ocean.
Ocean-Tune: A Community Ocean Testbed for Underwater Wireless Networks Puget Sound Deployment Revision 0.1 July 19, 2012 Sumit Roy, Payman Arabshahi
Seasonal to Interannual Variability in Phytoplankton Biomass and Diversity on the New England Shelf Heidi M. Sosik Hui Feng In Situ Time Series for Validation.
SIO 218A Observational techniques in physical oceanography Goals/methods: Learn currently used methods and instruments Understand principles of observation/technique.
Overview of Climate Observational Requirements for GOES-R Herbert Jacobowitz Short & Associates, Inc.
USB_DAQ (PGA309EVM) for Real Sensor Application Iven Xu May. 20 th,
UNDERWATER WIRELESS COMMUNICATION
Incorporating Satellite Time-Series data into Modeling Watson Gregg NASA/GSFC/Global Modeling and Assimilation Office Topics: Models, Satellite, and In.
© NERC All rights reserved EGU2016:Information in Earth Sciences A solution for handling time-series data Visualisation and the questions around uncertainty.
Deep Observing Network
WHOTS ALOHA Roger Lukas*, Fernando Santiago-Mandujano*, Robert Weller#, Albert Plueddemann# * SOEST/University of Hawaii # Woods Hole Oceanographic.
IMAGERY DERIVED CURRENTS FROM NPP Ocean Color Products 110 minutes!
5th Workshop on "SMART Cable Systems: Latest Developments and Designing the Wet Demonstrator Project" (Dubai, UAE, April 2016) Contribution of.
Instrument Considerations
Consistent calibration of VIRR onboard FY-3A to FY-3C
Space and time scales in satellite oceanography
OCB Plenary II Q: How is climate change affecting Southern Ocean?
Presentation transcript:

Lecture 22 Deployment Strategies Fixed Platforms Collin Roesler 18 July 2007

Issues related to fixed platform observatories, examples from the Gulf of Maine Ocean Observing System Moored array issues System Integration Instrument characterization/calibration Biofouling Data Analysis

Moored Arrays Motivation Space/time (x, y, z, t) sampling strategies Advantages –highly resolved time scales –real time telemetry (line of site wireless, cell phone, satellite, irridium) –6 month deployments (TOGA TAO 12 months) Disadvantages –no spatial information without other data sources (modeling, remote sensing, mobile platforms, shipboard surveys) –biofouling

Time and Space Scales

Moored Arrays Motivation Space/time (x, y, z, t) sampling strategies Advantages –highly resolved time scales –real time telemetry (line of site wireless, cell phone, satellite, irridium) –6 month deployments (TOGA TAO 12 months) Disadvantages –no spatial information without other data sources/arrays (modeling, remote sensing, mobile platforms, shipboard surveys, arrays) –biofouling

System Integration Mooring types –subsurface float vs. surface expression –taut vs. elastic vs. scoping

System Integration Mooring types –subsurface float vs. surface expression –taut vs. elastic vs. scoping System control –centralized control (wired vs. inductive modem) –centralized vs. local data storage Power –centralized power vs. local power –solar cells, traditional batteries, on board generation Real estate –everyone wants the surface positions –flow and drag simulations Data telemetry –band width limitations –onboard processing –redundant telemetry

Calibrations Instrument characterization/calibration pure water cals total offset biofouling instrument drift time cal value - Post-recovery post-clean calibration (3) biofouling = (3) – (2) drift = (3) – (1) - Re-deployment calibration (4) - Pre-deployment calibration (1) - Post-recovery pre-clean calibration (2) Total offset = (2) – (1)

Calibrations Instrument characterization/calibration pure water cals total offset biofouling instrument drift time In situ value - Validation (new deploy – corrected) - Linear trend - Step function trend

Instrument characterization/calibration Calibrations Environmental characterization –temperature –salinity –pressure –irradiance

Chlorophyll Fluorometer Characterization

Chlorophyll Fluorometer Characterization Temperature Dependence Slope is the warmup effect Deployment Temperature Effect

Range 1 to 5 counts/ o C Chlorophyll Fluorometer Characterization Temperature Dependence The temperature dependence, of course, varies between sensors and between sensor type

Chlorophyll Fluorometer Characterization Correction for Temperature Dependence ~0.25  g/l Compounding Issue: The biggest temperature effect occurs in the winter (  T), and that is when chlorophyll is lowest.

Biofouling

Prevention –toxic coatings –copper shutters –copper tape –copper tubing

Biofouling Identification –Long term trends

Biofouling Identification –Long term trends –Redundancy

Biofouling Identification –Long term trends –Redundancy

Biofouling Identification –Long term trends –Redundancy –Temporal patterns

Biofouling Correction –after the fact: calibrations –real time redundancy signal separation flagging

Biofouling Correction –after the fact: calibrations a(676) corrected F chl (mg/m 3 ) / (m 2 /mg)

Biofouling Correction –after the fact: calibrations –real time Redundancy (is signal real?) Signal separation (is it one component?) Flagging (pretty sure it is an artifact)

Calibrated Chlorophyll Fluorescence Time Series A B E I