|Savidge, William||Skidaway Institute of Oceanography (SkIO)||Principal Investigator|
|Brandes, Jay||Skidaway Institute of Oceanography (SkIO)||Co-Principal Investigator|
|Edwards, Catherine||Skidaway Institute of Oceanography (SkIO)||Co-Principal Investigator|
|Stubbins, Aron||Skidaway Institute of Oceanography (SkIO)||Co-Principal Investigator|
|Copley, Nancy||Woods Hole Oceanographic Institution (WHOI BCO-DMO)||BCO-DMO Data Manager|
Tidal water velocities were measured at two stations in Groves Creek salt marsh, Skidaway Island Georgia, USA from August 2013 to July 2014.
Model Serial # (Hz) Nortek ADPs were used to sample water velocities in the tidal creeks. (Initial compass setting procedure. Other setup details?) Bins were set to 30 or 40 cm with a blanking distance of XXX. ADP transducer heads were coated with a mixture of cayenne pepper and petroleum jelly to discourage hard fouling.
Units were affixed to a concrete plate that was lowered from a small boat by hand and rope to the bottom of the creek channel. Deployments were blind: effort was made to assure that the units were oriented channel-parallel and on flat bottom, but the exact location and orientation of each deployment depended greatly on the swing of the boat’s anchor in the current. The a priori objective of each deployment was to locate a unit in the center of a straight section of creek seaward of the water quality sampling stations. Each ADP mount was fixed to a weighted line that ran to the nearest shoreline where it was anchored and marked with a buoy. Individual deployments lasted ~A to B months. Units were recovered by retrieving the line at the shore and hand-hauling it to the surface.
ADPs were returned to the lab for cleaning, downloading data, charging batteries and setting up the unit for the next deployment. Units were re-deployed at the next convenient opportunity. Gaps in the record were on the order of a week to a month.
BCO-DMO Processing notes:
- added conventional header with dataset name, PI name, version date
- modified parameter names to conform with BCO-DMO naming conventions
- added station, lat, lon, date, time, ISO_DateTIme columns
- ISO Date format generated from date and time values
- reduced decimal places of lat and lon to 5; reduced depth to 2
|lat||latitude; north is positive||decimal degrees|
|lon||longitude; east is positive||decimal degrees|
|date||UTC date formatted as yyyy-mm-dd||unitless|
|time||UTC time; formatted as hh:mm||unitless|
|ISO_DateTime_UTC||Date/Time (UTC) ISO formatted based on ISO 8601:2004(E) with format YYYY-mm-ddTHH:MM:SS[.xx]Z||unitless|
|datenum_matlab||MATLAB formatted datenum||unitless|
|pitch||orientation (pitch) of measurement platform by inclinometer||degrees|
|roll||orientation (roll angle) of measurement platform by inclinometer||degrees|
|heading||compass direction (0 being north, 90 being east, etc.)||degrees|
|soundspeed||speed of sound through water||meters/second?|
|Dataset-specific Instrument Name|| |
|Generic Instrument Name|| |
Acoustic Doppler Current Profiler
|Generic Instrument Description|| |
The ADCP measures water currents with sound, using a principle of sound waves called the Doppler effect. A sound wave has a higher frequency, or pitch, when it moves to you than when it moves away. You hear the Doppler effect in action when a car speeds past with a characteristic building of sound that fades when the car passes. The ADCP works by transmitting "pings" of sound at a constant frequency into the water. (The pings are so highly pitched that humans and even dolphins can't hear them.) As the sound waves travel, they ricochet off particles suspended in the moving water, and reflect back to the instrument. Due to the Doppler effect, sound waves bounced back from a particle moving away from the profiler have a slightly lowered frequency when they return. Particles moving toward the instrument send back higher frequency waves. The difference in frequency between the waves the profiler sends out and the waves it receives is called the Doppler shift. The instrument uses this shift to calculate how fast the particle and the water around it are moving. Sound waves that hit particles far from the profiler take longer to come back than waves that strike close by. By measuring the time it takes for the waves to bounce back and the Doppler shift, the profiler can measure current speed at many different depths with each series of pings. (More from WHOI instruments listing).
Groves Creek - SkIO
|Start Date|| |
|End Date|| |
Studies of temporal and compositional changes in exported material in a saltmarsh, both the quantity and quality of dissolved organic matter (DOM) and particulate organic matter (POM) exported from Groves Creek.
This document is created by info v 4.1f 5 Oct 2018 from the content of the BCO-DMO metadata database. 2020-02-17 16:11:16