Observations of Near-Bottom Currents with Low-Cost SeaHorse Tilt Current Meters

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DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Observations of Near-Bottom Currents with Low-Cost SeaHorse Tilt Current Meters Vitalii A. Sheremet Graduate School of Oceanography University of Rhode Island Narragansett, Rhode Island 02882 Telephone: (401) 874-6939, Fax: (401) 874-6728 Email: vsheremet@gso.uri.edu Grant Number: N00014-09-1-0993 http://www.gso.uri.edu/~sheremet/seahorse LONG-TERM GOALS The SeaHorse TCM is a low-cost, easy to use, robust current meter based on the drag principle. Use of a large number of low-cost instruments would result in a new high spatial resolution view of the processes and to improve the ocean state prediction. The ultimate goal is to improve this technology by including expendable option with automatic data relay after deployment and to develop a global scale program of near-bottom current observations. OBJECTIVES The objectives are to improve the design of the instrument, evaluate its performace in comparison with other standard current meters, accumulate experience in its deployment/recovery/operation and to promote the use of such an instrument in various applications. APPROACH We propose to evaluate this instrument in a number of settings in comparison with standard oceanographic equipment, to demonstrate the instrument s capabilities and to analyze its performance. Specifically, we identified several organizations and researches interested and willing to try these instruments or assist in their evaluations: 1. Chris Weidman at Waquoit Bay Natural Estuary Research Reservation (WEBNERR) will assist in deploying arrays of these instruments within the bay in order to study circulation and sediment transport. 2. Steve Lentz (WHOI) agreed to deploy several Tilt Current Meters alongside his tripods carrying bottom mounted ADCPs and other instrumentation at the Marthas Vineyard Observatory. 3. Rocky Geyer (WHOI) is interested to try a very short version of this instrument to complement his project of studying circulation on tidal flats, sponsored by ONR. 1

Report Documentation Page Form Approved OMB No. 0704-0188 Public reporting burden for the collection of information is estimated to average 1 hour per response, including the time for reviewing instructions, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing the collection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing this burden, to Washington Headquarters Services, Directorate for Information Operations and Reports, 1215 Jefferson Davis Highway, Suite 1204, Arlington VA 22202-4302. Respondents should be aware that notwithstanding any other provision of law, no person shall be subject to a penalty for failing to comply with a collection of information if it does not display a currently valid OMB control number. 1. REPORT DATE 30 SEP 2009 2. REPORT TYPE Annual 3. DATES COVERED 00-00-2009 to 00-00-2009 4. TITLE AND SUBTITLE Observations Of Near-Bottom Currents With Low-Cost SeaHorse Tilt Current Meters 5a. CONTRACT NUMBER 5b. GRANT NUMBER 5c. PROGRAM ELEMENT NUMBER 6. AUTHOR(S) 5d. PROJECT NUMBER 5e. TASK NUMBER 5f. WORK UNIT NUMBER 7. PERFORMING ORGANIZATION NAME(S) AND ADDRESS(ES) University of Rhode Island,Graduate School of Oceanography,Narragansett,RI,02882 8. PERFORMING ORGANIZATION REPORT NUMBER 9. SPONSORING/MONITORING AGENCY NAME(S) AND ADDRESS(ES) 10. SPONSOR/MONITOR S ACRONYM(S) 12. DISTRIBUTION/AVAILABILITY STATEMENT Approved for public release; distribution unlimited 13. SUPPLEMENTARY NOTES 11. SPONSOR/MONITOR S REPORT NUMBER(S) 14. ABSTRACT The SeaHorse TCM is a low-cost, easy to use, robust current meter based on the drag principle. Use of a large number of low-cost instruments would result in a new high spatial resolution view of the processes and to improve the ocean state prediction. The ultimate goal is to improve this technology by including expendable option with automatic data relay after deployment and to develop a global scale program of near-bottom current observations. 15. SUBJECT TERMS 16. SECURITY CLASSIFICATION OF: 17. LIMITATION OF ABSTRACT a. REPORT b. ABSTRACT c. THIS PAGE Same as Report (SAR) 18. NUMBER OF PAGES 4 19a. NAME OF RESPONSIBLE PERSON Standard Form 298 (Rev. 8-98) Prescribed by ANSI Std Z39-18

4. R.-S. Tseng and Y.-H. Wang (National San Yat Sen University, Taiwan) with whom PI established scientific collaboration during participation in the NLIWI project are interested to deploy these instruments off Taiwan and in South China Sea to study shelf circulation and internal wave solitons. PI will be responsible for assembling and modifying the instruments and required moorings, will participate in deployment/recovery and will analyze the observational data. PI will also collect and analyze the instrument performance information (pertaining, for example, to bio fouling, potential data telecommunication, internal motion-driven power generation) required for future development. WORK COMPLETED PI received a limited amount of funding in FY09, nonetheless the project is progressing according to its original scientific plan: 1) The experiment in the Waquoit Bay will be conducted starting Nov 2009 and will last till April 2010; 2) Steve Lenz (WHOI) has deployed one instrument at the at the Marthas Vineyard Observatory. It will be recovered in January 2010; 3). Rocky Geyer (WHOI) did a test deployment in a tidal flats environment and provided data for analysis. 4). R.S Tseng (National San Yat Sen University, Taiwan) is currently maintaining a small array of instruments deployed in the Nan Wan Bay (south Taiwan). We conducted test deployments off URI/GSO dock in about 10m depth (Fig. 1). There is a range of tidal currents of about 50 cm/s in both directions. The purpose of these tests is to calibrate several models of SeaHorse TCM of varying length 50cm, 1m, 2m long and of varying sensitivity ballasted for 50 cm/s to 10 cm/s currents against acoustic Doppler velocity measurements (SonTek/ArgonautMD). The ACM is mounted vertically, upward looking, in a stainless steel cage. The cage is supported in a vertical position by three aluminum legs. The legs are loaded with lead weights. The ACM settings are blanking distance 0.5m and varying bin size corresponding to the length of the instrument. The TCM was attached to a narrow aluminum pole extending above the cage, with the buoyant PVC pipe starting at the same level as the sampling bin of the ACM. Thus the velocity measurements were acquired essentially in the same fluid volume, above and without the interference from the cage or the tripod. The ACM were sampling every 1 sec, while TCM was programmed for sampling ranging from 1 sec to 2 min depending of the deployment duration (from 6 hours to 1 month). The deployments were conducted with the help of GSO student divers as part of a diving course taught by Mark Gustafson (a GSO diving instructor and small boat manager). The presence of divers was very helpful in ensuring that the tripod is landed properly. 2

Figure 1. The calibration tests off GSO dock. The SonTek ArgonautMD acoustic current meter mounted in a tripod and SeaHorse Tilt Current Meters of different lengths (50 cm, 1m, and 2m) in preparation for deployments (right). The ArgonautMD records are shown in blue while the SeaHorse records are shown in red. RESULTS The calibration tests allowed us to construct an empirical relationship between the tilt angle of the instrument and the ambient velocity. The plots in Figure 1 show excellent agreement between the records. Note that the tidal current is asymmetric, predominantly southward. This is probably caused by dock pilings blocking northward flow. Note also that the tidal signal does not have a sinusoidal shape but has a sharp peak instead. This is a characteristic feature of tides in shallow waters due to nonlinear effects. These tests allowed us to improve the empirical calibration function that relates the ambient current and the tilt angle of the SeaHorse (Fig. 2). The sensitivity of the instrument depends slightly on its length (the end effect) but more on its ballasting (or buoyancy of the pipe). Data corresponding to different instrument are marked by different colors: SeaHorse length 25cm (red), 50cm (green), 1m (blue), 1m ballasted (magenta). A rule of thumb is that the tilt of the instrument in degrees corresponds roughly to the ambient velocity in cm/s. Another important result is the dependence of the vortex shedding regime on the ballasting on the instrument. As seen in Figure 2 small kinks in the drag curves correspond to transition from a regular Karman vortex street pattern to a chaotic pattern of eddy shedding which affects the drag coefficient (Clift 1978, Hoerner 1965). For the properly ballasted instrument the eddy shedding is reduced and the instrument performance is improved. 3

Figure 2. The empirical relationship between the ambient velocity and the tilt of the instrument: SeaHorse length 25cm (red), 50cm (green), 1m (blue), 1m ballasted (magenta). IMPACT/APPLICATIONS Study of the drag coefficient of this instrument has a potential future impact for other submerged applications: such as moored near-bottom buoys. REFERENCES Clift, R., J. R. Grace, and M. E. Weber, 1978: Bubbles, Drops, and Particles. Academic Press, 381pp. Hoerner, S. F., 1965: Fluid-Dynamic Drag: Practical Information on Aerodynamic Drag and Hydrodynamic Resistance. 4