Updated Guidelines for Seadatanet ODV Production

Total Page:16

File Type:pdf, Size:1020Kb

Updated Guidelines for Seadatanet ODV Production EMODnet Thematic Lot n° 4 - Chemistry EMODnet Phase III Updated guidelines for SeaDataNet ODV production M. Lipizer, M. Vinci, A. Giorgetti, L. Buga, M. Fichault, J. Gatti, S. Iona, M. Larsen, R. Schlitzer, D. Schaap, M. Wenzer, E. Molina Date: 12/04/2018 EMODnet Thematic Lot n° 4 - Chemistry Updated guidelines for SDN ODV production Index EMODnet Phase III............................................................................................................................1 Updated guidelines for SeaDataNet ODV producton......................................................................1 Updated guidelines for SeaDataNet ODV producton..........................................................................1 Introducton......................................................................................................................................1 SeaDataNet ODV import format.......................................................................................................1 How to check your SeaDataNet ODV fle format?............................................................................6 Vocabulary........................................................................................................................................7 How to choose the correct P01?......................................................................................................8 Flagging of Data Below Detecton Limits and Data Below Limit of Quantfcatoni.......................13 Guidelines for SeaDataNet ODV producton for sediment data and contaminants in biota.............14 Contaminants in the Sediment.......................................................................................................14 Contaminants in Biota....................................................................................................................18 Partcular case in biota datai......................................................................................................18 Other general issues and inventory of common errors.................................................................21 Acknowledgements: We acknowledge the fundamental contribution of the British Oceanographic Data Centre (BODC) for the design, development and continuous management and update of the Vocabularies and for the provision of the webservices. How to cite this document: M. Lipizer, M. Vinci, A. Giorgetti, L. Buga, M. Fichault, J. Gatti, S. Iona, M. Larsen, R. Schlitzer, D. Shaap, M. Wenzer, E. Molina, 2018, EMODnet Phase III - Updated guidelines for SeaDataNet ODV production, 12/04/2018, 23 pp., DOI: 10.6092/259c43eb-4ba4- 419b-bb38-df00e189bd35 0 EMODnet Thematic Lot n° 4 - Chemistry Updated guidelines for SDN ODV production Updated guidelines for SeaDataNet ODV production Introduction EMODnet Chemistry uses SeaDataNet infrastructure (https://www.seadatanet.org/) for the technical set-up. In particular, it adopts: A set of Standards for metadata description and data formats: . SeaDataNet (SDN) Standards for metadata (https://www.seadatanet.org/Standards/Metadata-formats) . Common Vocabularies (i.e. standardised terms that cover a broad spectrum of disci- plines) to allow consistency and interoperability (https://www.seadatanet.org/Standards/Common-Vocabularies) . Common Data Index mechanism (CDI) to access data with data policy (https://www.seadatanet.org/Standards/Metadata-formats/CDI) . Ocean Data View format (ODV) for data exchange (https://www.seadatanet.org/Standards/Data-Transport-Formats) . Data Quality Control procedures (https://www.seadatanet.org/Standards/Data-Quality-Control) A set of software tools specifically developed for metadata and data formatting, data exchange and visualization: . MIKADO to prepare XML metadata files . NEMO to enable conversion from any type of ASCII format to the SeaDataNet ODV and Medatlas ASCII formats as well as the SeaDataNet NetCDF (CF) format . OCTOPUS to convert files in a given SeaDataNet format to another SeaDataNet format (e.g.: ODV to NetCDF, MedAtlas to NetCDF, MedAtlas to ODV) and to check the compli- ancy of SeaDataNet MedAtlas and ODV files format . ODV as the fundamental data analysis and visualisation software. DIVA to spatially interpolate (or analyse) observations on a regular grid in an optimal way SeaDataNet ODV import format All data entering EMODnet Chemistry must be converted to SeaDataNet ODV import format, which is the common standard format. Delivery of data to users requires common data trans- port formats, which interact with other SeaDataNet standards (Vocabularies, Quality Flag Scale) and SeaDataNet analysis & presentation tools (ODV, DIVA). Detailed guidelines on Data transport formats area for data in the water column and specific for biological data are avail- able on: https://www.seadatanet.org/Standards/Data-Transport-Formats (Fig. 1). All SDN ODV files are .txt files. 1 EMODnet Thematic Lot n° 4 - Chemistry Updated guidelines for SDN ODV production Fig. 1: SeaDataNet datafile formats documentation (https://www.seadatanet.org/Standards/Data-Transport-Formats) From: “SeaDatanet DATAFILE FORMATS”: The fundamental data model underlying the format is the ASCII spreadsheet (ODV spread- sheet files may contain comments, and the column separation character may be TAB or semi- colon, https://odv.awi.de/fileadmin/user_upload/odv/misc/odv4Guide.pdf ) : i.e. a collection of rows each having the same fixed number of columns. There are three different types of col- umn: . Metadata columns . Primary variable data columns (one column for the value plus one for the qualifying flag) . Data columns (one column for the value plus one for the qualifying flag) The metadata columns are stored at the left hand end of the row, followed by the primary variable columns and then the data columns. There are three different types of rows: . Comment rows 2 EMODnet Thematic Lot n° 4 - Chemistry Updated guidelines for SDN ODV production . Semantic header row . Column header row . Data row Comment lines start with two slashes //as first two characters of the line and may contain ar- bitrary text in free format. Comment lines may, in principle, appear anywhere in the file, most commonly, however, they are placed at the beginning of the file and contain descriptions of the data, information about the originator or definitions of the variables included in the file. The Semantic header consists in a set of ‘special’ mandatory comment lines that must appear before the column header row. Their function is to map the text strings used to label the meta- data and data columns to standardized SeaDataNet concepts, which is necessary if data files from different sources are to be combined in a meaningful way (Fig. 2, Fig. 3). Fig. 2: Example of SDN ODV file, with depth as primary variable (in column 10): Important: there MUST be exact correspondence between Semantic header and Header. The order of the first 9 metadata column MUST be respected (ie. Cruise; Station; Type; date-time; Long.; Lat.; Local_CDI_ID; EDMO_Code; Bot. Depth.). 3 EMODnet Thematic Lot n° 4 - Chemistry Updated guidelines for SDN ODV production The metadata values are followed by the primary variable value (on the 10th col- umn), its flag and then the data value plus qualifying flag pairs for each parameter. Flag values are taken from the SeaDataNet vocabulary for qualifying flags (L20 at http://vocab.ner- c.ac.uk/collection/L20/current). Fig. 3: Example of SDN ODV file showing correspondence between SDN_parameter_map- ping lines and measured parameters. The primary variable depends on the type of dataset: Time series: point time series have row_groups made up of measurements from a given in- strument at different times. The primary variable (column 10) is time. In case data come from samples taken in the same position and sampled at a fix frequency, the dataset type can be considered as “time series” and the SDN ODV file must provide time as primary variable in the 10th column. This is particularly suitable for regu- lar monitoring stations and is commonly used for mooring data (eg. oceanographic buoy). Vertical profile: profile data have row_groups made up of measurements at different depths. The primary variable (which is indicated in column 10) is the ‘z co-ordinate’, which is either depth in meters or pressure in decibars (in case of water column data), or depth below seabed (in case of sediment data). It is the choice for stations usually not repeated regularly over time, for which several depths are sampled. Typical ex- amples: CTD profiles, bottle stations (chemical data, chlorophyll, plankton,…) However, this distinction is not always clear and in cases of a same position, sampled over time at different depths, some data providers prefer to consider these as “repeated profiles” stations. 4 EMODnet Thematic Lot n° 4 - Chemistry Updated guidelines for SDN ODV production Lastly, when data are not available for the same position at more or less regular time periods, the dataset type is regarded as “vertical profiles” even if there is only 1 sampling depth and it is not a real profile. This can be the case of sediment samples taken during occasional surveys, for example. In order to produce correctly SDN ODV datasets for EMODnet Chemistry, the use NEMO software is STRONGLY RECCOMENDED. User Manual, NEMO presentation and NEMO examples are available on: https://www.seadatanet.org/Software/NEMO and lessons on NEMO given during EMODnet Chemistry 3 first training (18-19 May 2017, Trieste) are available on: http://www.emodnet-chemistry.eu/trieste_16-19_May_2017.html.
Recommended publications
  • Chinese Mooring and Buoy Observations in the Open-Ocean
    Chinese mooring and buoy observations in the open-ocean Chujin Liang Second Institute of Oceanography, SOA May 28, 2013 Seoul Main oceanographic institutions of China First Institute of Oceanography Qingdao State Oceanic Administration Second Institute of Oceanography Hangzhou /SOA Third Institute of Oceanography Xiamen Polar Institute of China ShanghaiFirst Institute of Oceanography, FIO Institute of Oceanography Qingdao Chinese Academy of Science /CAS South China Sea Institute of Oceanography GuangzhouSecond Institute of Oceanography, SIO China Ocean University, Xiamen University Qingdao/Third Institute of Oceanography,Ministry of Education TIO Xiamen Tongji University, East China Normal university, Shanghai/ Tsinghua University, Peiking University, etc. Beijing Second Institute of Oceanography State Oceanic Administration State Oceanic Administration, SOA First Institute of Oceanography, FIO Second Institute of Oceanography, SIO Third Institute of Oceanography, TIO Second Institute of Oceanography State Oceanic Administration FIO is operating 2 buoy stations and 1 mooring at 2 sites Long-term buoy station in eastern Indian Ocean operated by FIO FIO-AMFR 中国 海洋一所 FIO Progress Report 1. Surface buoy at (100E, 8S) • In place since 30 May 2010 • Daily data will be posted on PMEL and FIO website soon • Data includes the meteorological parameters: wind speed and direction, air temperature, relative humidity, air pressure, shortwave radiation, long wave radiation, unfortunately precipitation missed due to damage in the deployment • Data includes
    [Show full text]
  • SISP-4 a Metadata Convention for Processed Acoustic Data from Active Acoustic Systems
    SERIES OF ICES SURVEY PROTOCOLS SISP 4-TG-ACMETA NOVEMBER 2016 A metadata convention for processed acoustic data from active acoustic systems Version 1.10 ICES WGFAST Topic Group, TG-AcMeta International Council for the Exploration of the Sea Conseil International pour l’Exploration de la Mer H. C. Andersens Boulevard 44–46 DK-1553 Copenhagen V Denmark Telephone (+45) 33 38 67 00 Telefax (+45) 33 93 42 15 www.ices.dk [email protected] Recommended format for purposes of citation: ICES. 2016. A metadata convention for processed acoustic data from active acoustic systems. Series of ICES Survey Protocols SISP 4-TG-AcMeta. 48 pp. https://doi.org/10.17895/ices.pub.7434 The material in this report may be reused for non-commercial purposes using the rec- ommended citation. ICES may only grant usage rights of information, data, images, graphs, etc. of which it has ownership. For other third-party material cited in this re- port, you must contact the original copyright holder for permission. For citation of da- tasets or use of data to be included in other databases, please refer to the latest ICES data policy on the ICES website. All extracts must be acknowledged. For other repro- duction requests please contact the General Secretary. This document is the product of an Expert Group under the auspices of the International Council for the Exploration of the Sea and does not necessarily represent the view of the Council. https://doi.org/10.17895/ices.pub.7434 ISBN 978-87-7482-191-5 ISSN 2304-6252 © 2016 International Council for the Exploration of the Sea Background and Terms of reference The ICES Working Group on Fisheries Acoustics, Science and Technology (WGFAST) meeting in 2010, San Diego USA recommended the formation of a Topic Group that will bring together a group of expert acousticians to develop standardized metadata protocols for active acoustic systems.
    [Show full text]
  • MBARI's Buoy Based Seafloor Observatory Design (PDF)
    MBARI’s Buoy Based Seafloor Observatory Design Mark Chaffey, Larry Bird, Jon Mike Kelley, Lance McBride, Tom O’Reilly, Walter Paul*, Erickson, John Graybeal, Andy Ed Mellinger, Tim Meese, Mike Risi, and Wayne Hamilton, Kent Headley, Radochonski Monterey Bay Aquarium Research Institute * Dept. of Applied Ocean Physics and Engineering 7700 Sandholdt Road Woods Hole Oceanographic Institution Moss Landing CA 95039 Woods Hole, MA 02543 Abstract - There has been considerable discussion and planning in the oceanographic community toward the installation of long-term seafloor sites for scientific observation in the deep ocean. The Monterey Bay Aquarium Research Institute (MBARI) has designed a portable mooring system for deep ocean deployment that provides data and power connections to both seafloor and ocean surface instruments. The surface mooring collects solar and wind energy for powering instruments and transmits data to shore-side researchers using a satellite communications modem. A specialty anchor cable connects the surface mooring to a network of benthic instrumentation, providing the required data and power transfer. Design details and results of laboratory and field testing of the completed portions of the observatory system are described. I. INTRODUCTION Fig. 1 Buoy and seafloor network. MBARI has undertaken a major effort to develop the technology and techniques for building deep ocean of reliability, fault tolerance, and remote diagnostic seafloor observatories under the in-house Monterey capability. Ocean Observing System (MOOS) program. A key The overall functional and design requirements of the component of the overall observatory technology effort is MOOS mooring have previously been described in detail a moored surface buoy connected to the seafloor using [1] and can be summarized as a portable system, an anchor cable that incorporates mechanical strength configurable to a wide range of experiments, providing elements, copper conductors for power transfer, and episodic event response using on-board processing, and optical elements for communications.
    [Show full text]
  • The Official Magazine of The
    OceTHE OFFICIALa MAGAZINEn ogOF THE OCEANOGRAPHYra SOCIETYphy CITATION Smith, L.M., J.A. Barth, D.S. Kelley, A. Plueddemann, I. Rodero, G.A. Ulses, M.F. Vardaro, and R. Weller. 2018. The Ocean Observatories Initiative. Oceanography 31(1):16–35, https://doi.org/10.5670/oceanog.2018.105. DOI https://doi.org/10.5670/oceanog.2018.105 COPYRIGHT This article has been published in Oceanography, Volume 31, Number 1, a quarterly journal of The Oceanography Society. Copyright 2018 by The Oceanography Society. All rights reserved. USAGE Permission is granted to copy this article for use in teaching and research. Republication, systematic reproduction, or collective redistribution of any portion of this article by photocopy machine, reposting, or other means is permitted only with the approval of The Oceanography Society. Send all correspondence to: [email protected] or The Oceanography Society, PO Box 1931, Rockville, MD 20849-1931, USA. DOWNLOADED FROM HTTP://TOS.ORG/OCEANOGRAPHY SPECIAL ISSUE ON THE OCEAN OBSERVATORIES INITIATIVE The Ocean Observatories Initiative By Leslie M. Smith, John A. Barth, Deborah S. Kelley, Al Plueddemann, Ivan Rodero, Greg A. Ulses, Michael F. Vardaro, and Robert Weller ABSTRACT. The Ocean Observatories Initiative (OOI) is an integrated suite of instrumentation used in the OOI. The instrumented platforms and discrete instruments that measure physical, chemical, third section outlines data flow from geological, and biological properties from the seafloor to the sea surface. The OOI ocean platforms and instrumentation to provides data to address large-scale scientific challenges such as coastal ocean dynamics, users and discusses quality control pro- climate and ecosystem health, the global carbon cycle, and linkages among seafloor cedures.
    [Show full text]
  • (Mooring – Tide Gauge) Is ~22 Mm
    Updated Results from the In Situ Calibration Site in Bass Strait, Australia Christopher Watson1 , Neil White2,, John Church2 Reed Burgette1, Paul Tregoning 3, Richard Coleman 4 1 University of Tasmania ([email protected]) 2 Centre for Australian Weather and Climate Research, A partnership between CSIRO and the Australian Bureau of Meteorology 3 The Australian National University 4 The Institute of Marine and Antarctic Studies, UTAS OSTM/Jason-2 OST Science Team Meeting Updated Data Stream Presentation 1 San Diego OSTST Meeting October 2011 Impossible d'afficher l'image. Votre ordinateur manque peut-être de mémoire pour ouvrir l'image ou l'image est endommagée. Redémarrez l'ordinateur, puis ouvrez à nouveau le fichier. Si le x rouge est toujours affiché, vous devrez peut-être supprimer l'image avant de la réinsérer. Methods Recap Bass Strait • Primary site is located on Pass 088 in Bass Strait. Contributing bias estimates to the SWT/OSTST since the launch of T/P . • Secondary site along track in Storm Bay Storm Bay 2 Methods Recap • We adopt a purely geometric technique for determination of absolute bias. • The method is centred around the use of GPS buoys to define the datum ofhihf high preci si on ocean moori ngs. • Outside of available mooring data, all available mooring SSH data are used to correct tide gauge SSH to the comparison point. 3 Instrumentation (Bass Strait): Tide Gauge and CGPS • Tide gauge part of the Australian baseline array, located in Burnie. • Vertical velocity not significantly different from zero. • CGPS time series shows a quasi-annual periodic signal (amplitude ~3-4 mm).
    [Show full text]
  • Following Your Invitation 14Th January 2010 to Seadatanet To
    SeaDataNet Common Data Index (CDI) metadata model for Marine and Oceanographic Datasets November 2014 Document type: Standard Current status: Proposal Submitted by: Dick M.A. Schaap Technical Coordinator SeaDataNet MARIS The Netherlands Enrico Boldrini CNR-IIA Italy Stefano Nativi CNR-IIA Italy Michele Fichaut Coordinator SeaDataNet IFREMER France Title: SeaDataNet Common Data Index (CDI) metadata model for Marine and Oceanographic Datasets Scope: Proposal to acknowledge SeaDataNet Common Data Index (CDI) metadata profile of ISO 19115 as a standard metadata model for the documentation of Marine and Oceanographic Datasets. In particular, the proposal aims to promote CDI as a regional (i.e. European) standard. SeaDataNet CDI has been drafted and published as a metadata community profile of ISO 19115 by SeaDataNet, the leading infrastructure in Europe for marine & ocean data management. Its wide implementation, both by data centres within SeaDataNet and by external organizations makes it also a de-facto standard in the Europe region. The acknowledgement of SeaDataNet CDI as a standard data model by IODE/JCOMM will further favour interoperability and data management in the Marine and Oceanographic community. Envisaged publication type: The proposal target audience includes all the European bodies, programs, and projects that manage and exchange marine and oceanographic data. Besides, the proposed document informs all the international community dealing with marine and oceanographic data about the SeaDataNet CDI metadata model. Purpose and Justification: Provide details based wherever practicable. 1. Describe the specific aims and reason for this Proposal, with particular emphasis on the aspects of standardization covered, the problems it is expected to solve or the difficulties it is intended to overcome.
    [Show full text]
  • 2021 Connecticut Boater's Guide Rules and Resources
    2021 Connecticut Boater's Guide Rules and Resources In The Spotlight Updated Launch & Pumpout Directories CONNECTICUT DEPARTMENT OF ENERGY & ENVIRONMENTAL PROTECTION HTTPS://PORTAL.CT.GOV/DEEP/BOATING/BOATING-AND-PADDLING YOUR FULL SERVICE YACHTING DESTINATION No Bridges, Direct Access New State of the Art Concrete Floating Fuel Dock Offering Diesel/Gas to Long Island Sound Docks for Vessels up to 250’ www.bridgeportharbormarina.com | 203-330-8787 BRIDGEPORT BOATWORKS 200 Ton Full Service Boatyard: Travel Lift Repair, Refit, Refurbish www.bridgeportboatworks.com | 860-536-9651 BOCA OYSTER BAR Stunning Water Views Professional Lunch & New England Fare 2 Courses - $14 www.bocaoysterbar.com | 203-612-4848 NOW OPEN 10 E Main Street - 1st Floor • Bridgeport CT 06608 [email protected] • 203-330-8787 • VHF CH 09 2 2021 Connecticut BOATERS GUIDE We Take Nervous Out of Breakdowns $159* for Unlimited Towing...JOIN TODAY! With an Unlimited Towing Membership, breakdowns, running out GET THE APP IT’S THE of fuel and soft ungroundings don’t have to be so stressful. For a FASTEST WAY TO GET A TOW year of worry-free boating, make TowBoatU.S. your backup plan. BoatUS.com/Towing or800-395-2628 *One year Saltwater Membership pricing. Details of services provided can be found online at BoatUS.com/Agree. TowBoatU.S. is not a rescue service. In an emergency situation, you must contact the Coast Guard or a government agency immediately. 2021 Connecticut BOATER’S GUIDE 2021 Connecticut A digest of boating laws and regulations Boater's Guide Department of Energy & Environmental Protection Rules and Resources State of Connecticut Boating Division Ned Lamont, Governor Peter B.
    [Show full text]
  • Action Progress Report #1
    Project Information Project full title EuroSea: Improving and Integrating European Ocean Observing and Forecasting Systems for Sustainable use of the Oceans Project acronym EuroSea Grant agreement number 862626 Project start date and duration 1 November 2019, 50 months Project website https://www.eurosea.eu Deliverable information Deliverable number D9.1 Deliverable title Action Progress Report #1 Description EuroSea summary progress report for the external advisory boards Dec 2020 Work Package number 9 Work Package title Project Coordination, Management and strategic ocean observing alliance Lead beneficiary GEOMAR Lead authors Nicole Köstner, Toste Tanhua Contributors All work package leaders and task leaders Due date 31.12.2020 Submission date 22.12.2020 Comments This project has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement No. 862626. https://doi.org/10.3289/eurosea_d9.1 Action Progress Report #1 Reporting period: 1 Nov 2019 – 31 Dec 2020 https://doi.org/10.3289/eurosea_d9.1 Table of contents 1. Introduction to EuroSea ............................................................................................................................ 1 2. Summary of progress ................................................................................................................................. 2 3. Work package progress reports ................................................................................................................ 7 3.1. WP1 - Governance and
    [Show full text]
  • Project of Strategic Interest NEXTDATA Deliverable D1.3.5
    Project of Strategic Interest NEXTDATA Deliverable D1.3.5 Report on RR quality indexes and data transmission to archive and General Web Portal WP Coordinator: Nadia Pinardi INGV, Bologna Authors S. Simoncelli, C. Fratianni, N. Pinardi INGV, Bologna 1 Contents Abstract .............................................................................................................................................................................. 3 Introduction ..................................................................................................................................................................... 4 Validation Results .......................................................................................................................................................... 4 Sea Surface Temperature ...................................................................................................................................... 4 Temperature vertical structure .......................................................................................................................... 8 Salinity vertical structure .................................................................................................................................... 10 Sea surface height ................................................................................................................................................... 13 Gibraltar transport ................................................................................................................................................
    [Show full text]
  • Vertical Flow in the Southern Ocean Estimated from Individual Moorings
    SEPTEMBER 2015 S É VELLEC ET AL. 2209 Vertical Flow in the Southern Ocean Estimated from Individual Moorings F. SÉVELLEC,A.C.NAVEIRA GARABATO,J.A.BREARLEY,* AND K. L. SHEEN Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Southampton, United Kingdom (Manuscript received 14 February 2014, in final form 26 March 2015) ABSTRACT This study demonstrates that oceanic vertical velocities can be estimated from individual mooring mea- surements, even for nonstationary flow. This result is obtained under three assumptions: (i) weak diffusion (Péclet number 1), (ii) weak friction (Reynolds number 1), and (iii) small inertial terms (Rossby number 1). The theoretical framework is applied to a set of four moorings located in the Southern Ocean. For this site, the diagnosed vertical velocities are highly variable in time, their standard deviation being one to two orders of magnitude greater than their mean. The time-averaged vertical velocities are demonstrated to be largely induced by geostrophic flow and can be estimated from the time-averaged density and hori- zontal velocities. This suggests that local time-mean vertical velocities are primarily forced by the time- mean ocean dynamics, rather than by, for example, transient eddies or internal waves. It is also shown that, in the context of these four moorings, the time-mean vertical flow is consistent with stratified Taylor column dynamics in the presence of a topographic obstacle. 1. Introduction motions, and rectified mesoscale eddy flows along sloping isopycnals (Marshall and Speer 2012, and ref- Oceanic vertical flow is an important element of the erences therein). The latter two mechanisms are believed ocean circulation, playing a central role in the re- to extensively underpin vertical flow in the Southern distribution of water and tracers between (and within) Ocean, a region hosting a prominent large-scale vertical the upper-ocean mixed layer and the ocean interior.
    [Show full text]
  • In-Situ Calibration Results from Bass Strait
    In-Situ Calibration Results from Bass Strait Christopher Watson1 Neil White2,3 Reed Burgette1 Richard Coleman1,2,3 Paul Tregoning 4 John Church2,3 Jason Zhang4 1 University of Tasmania 2 CAWCR and CSIRO CMAR 3 Antarctic Climate and Ecosystems CRC 4 The Australian National University Jason-1 and OSTM/Jason-2 OST Science Team Updated Results Seattle OSTST Meeting June 2009 Overview Bass Strait is an absolute calibration site that adopts a purely geometric technique. The method is centred around the use of GPS buoys to define the datum of high precision ocean moorings. Mooring SSH also used to correct tide gauge SSH to the comparison point. Altimeter vs mooring SSH and tide gauge SSH to determine absolute bias. Bass Strait Calibration Site 1. The comparison point has been moved further offshore to avoid land contamination of the radiometer. 2. Different buoy design, longer deployment duration. 3. New tide gauge and collocated CGPS. 4. New inland CGPS site on bedrock (~5km from the gauge). 5. New episodic GPS at Stanley to minimise baseline length to GPS buoys. 6. Three new ocean moorings (two consecutive six month deployments and one twelve month deployment spanning the previous two). 7. FTLRS campaign (assess benefit of additional southern hemisphere SLR). Bass Strait Calibration Site Instrumentation: New Gauge Tide Gauge Bedrock CGPS (5km away) • Tide gauge is part of the Australian baseline array, provision for a radar gauge to be installed later in 2009. Run by the Australian National Tidal Centre (NTC). • Collocated CGPS at TG. • Bedrock CGPS ~5km away at Round Hill (RHPT).
    [Show full text]
  • J. Thomas Farrar
    J. Thomas Farrar December 10, 2008 Assistant Scientist Department of Physical Oceanography Woods Hole Oceanographic Institution Clark 212A, MS #29 508-289-2691 Woods Hole, MA 02543 [email protected] Research Interests Dynamics and thermodynamics of the upper ocean; tropical dynamics and equatorial waves; air-sea interaction and exchange; oceanic internal waves and eddies; satellite oceanography; ocean observing and instrumentation. These interests are pursued from an observational perspective using in situ observations, satellite observations, and, in some cases, laboratory and numerical models to test hypotheses and test or formulate simpli¯ed physical models that aid understanding. Education Massachusetts Institute of Technology- Ph.D., Physical Oceanography Woods Hole Oceanographic Institution (February 2007) (S.M., September 2003) Supervisor: Robert A. Weller, Ph.D., Woods Hole Oceanographic Institution. Ph.D. thesis title: Air-sea interaction at two contrasting sites in the eastern tropical Paci¯c: mesoscale variability and atmospheric convection at 10±N. GPA 4.5/5.0 (equivalent to 3.5/4.0) University of Oklahoma B.S., Physics B.A., Philosophy (June 2000) Supervisor: Eric Abraham, Ph.D. (Physics Department) Thesis title: Design and Construction of a Magneto-Optical Trap for Demonstration of Bose-Einstein Condensation. GPA 3.7/4.0 Selected Academic Honors: Outstanding Student Paper Award, 2006 AGU Ocean Sciences meeting MIT Presidential Fellowship, 2000-2001 Most Outstanding Physics Student, U. Oklahoma, 2000 Phi Beta Kappa Golden
    [Show full text]