Tidal Energy Resource Characterization, Velocity and Turbulence Measurements, Processed Data, Cook Inlet, AK, 2021
This submission contains processed datasets from a long-term deployment of 3 moorings and a transect survey of the proposed tidal energy site off the East Forelands in Cook Inlet, AK.
The long-term mooring datasets were created from 8 instruments mounted on a Terrasond High Energy Oceanographic Mooring (THEOM) bottom lander and two Mid-Water Mooring (MWM) Stablemoor buoys from 1 July 2021 to 31 August 2021 (60 days).
The west-most mooring (MWM1) was deployed at 60.720225 N, 151.436196 W in ~50 m of water.
The middle mooring (THEOM) was deployed at 60.720703 N, 151.429500 W in ~52 m of water.
The east-most buoy (MWM2) was deployed at 60.720081 N, 151.420896 W in ~50 m of water.
Each Stablemoor carried three instruments:
1. A Nortek Vector acoustic Doppler velocimeter (ADV) mounted at the Stablemoor's nose. Data were recorded at 8 Hz on a 5 minute duty cycle every 20 minutes. Data was motion-corrected using the internal IMU and external ADCP bottom-track data and then bin-averaged into 4 minute bins and converted to the Principal (streamwise, cross-stream, vertical) coordinate system. (Note: 30 seconds were trimmed from the beginning and end of each 5 minute duty cycle to account for the filter end-effects from turning on and turning off the IMU.)
2. A down-looking Nortek Signature 1000 kHz acoustic Doppler current profiler (ADCP) mounted in the first Stablemoor instrument well. Data were recorded in 2 Hz with 5-beam burst and bottom-track enabled. Processed data has been averaged into 10 minute bins and converted into the Principal coordinate system.
3. An up-looking Nortek Signature 1000 kHz acoustic Doppler current profiler (ADCP) mounted in the second Stablemoor instrument well. Data were recorded at 4 Hz with 5 beam burst enabled. Processed data has been averaged into 10 minute bins and converted into the Principal coordinate system.
Note: the down-facing ADCP on MWM1 failed on July 10th, 2021, only recording 9 days of data. Because ADV motion-correction required bottom track, the ADV from MWM1 also only has 9 days processed. Additionally, only 25 days of data were processed from the MWM2 ADV because it appeared to have been impacted by debris on 7/25.
Two instruments were mounted on the THEOM (see MHKDR link further below for THEOM raw data):
4. A Nortek Vector acoustic Doppler velocimeter (ADV). Data were recorded at 8 Hz on a 5 minute duty cycle every 20 minutes. Data was bin-averaged into 5 minute bins, and converted to the Principal coordinate system.
5. A Nortek Signature 500 kHz acoustic Doppler current profiler (ADCP). Data were recorded in 4 Hz in the beam coordinate system from all 5 beams. Processed data has been averaged into 10 minutes bins and converted to the Principal coordinate system.
Citation Formats
Pacific Northwest National Laboratory. (2021). Tidal Energy Resource Characterization, Velocity and Turbulence Measurements, Processed Data, Cook Inlet, AK, 2021 [data set]. Retrieved from https://dx.doi.org/10.15473/2007516.
McVey, James, Kilcher, Levi. Tidal Energy Resource Characterization, Velocity and Turbulence Measurements, Processed Data, Cook Inlet, AK, 2021. United States: N.p., 31 Aug, 2021. Web. doi: 10.15473/2007516.
McVey, James, Kilcher, Levi. Tidal Energy Resource Characterization, Velocity and Turbulence Measurements, Processed Data, Cook Inlet, AK, 2021. United States. https://dx.doi.org/10.15473/2007516
McVey, James, Kilcher, Levi. 2021. "Tidal Energy Resource Characterization, Velocity and Turbulence Measurements, Processed Data, Cook Inlet, AK, 2021". United States. https://dx.doi.org/10.15473/2007516. https://mhkdr.openei.org/submissions/475.
@div{oedi_6086, title = {Tidal Energy Resource Characterization, Velocity and Turbulence Measurements, Processed Data, Cook Inlet, AK, 2021}, author = {McVey, James, Kilcher, Levi.}, abstractNote = {This submission contains processed datasets from a long-term deployment of 3 moorings and a transect survey of the proposed tidal energy site off the East Forelands in Cook Inlet, AK.
The long-term mooring datasets were created from 8 instruments mounted on a Terrasond High Energy Oceanographic Mooring (THEOM) bottom lander and two Mid-Water Mooring (MWM) Stablemoor buoys from 1 July 2021 to 31 August 2021 (60 days).
The west-most mooring (MWM1) was deployed at 60.720225 N, 151.436196 W in ~50 m of water.
The middle mooring (THEOM) was deployed at 60.720703 N, 151.429500 W in ~52 m of water.
The east-most buoy (MWM2) was deployed at 60.720081 N, 151.420896 W in ~50 m of water.
Each Stablemoor carried three instruments:
1. A Nortek Vector acoustic Doppler velocimeter (ADV) mounted at the Stablemoor's nose. Data were recorded at 8 Hz on a 5 minute duty cycle every 20 minutes. Data was motion-corrected using the internal IMU and external ADCP bottom-track data and then bin-averaged into 4 minute bins and converted to the Principal (streamwise, cross-stream, vertical) coordinate system. (Note: 30 seconds were trimmed from the beginning and end of each 5 minute duty cycle to account for the filter end-effects from turning on and turning off the IMU.)
2. A down-looking Nortek Signature 1000 kHz acoustic Doppler current profiler (ADCP) mounted in the first Stablemoor instrument well. Data were recorded in 2 Hz with 5-beam burst and bottom-track enabled. Processed data has been averaged into 10 minute bins and converted into the Principal coordinate system.
3. An up-looking Nortek Signature 1000 kHz acoustic Doppler current profiler (ADCP) mounted in the second Stablemoor instrument well. Data were recorded at 4 Hz with 5 beam burst enabled. Processed data has been averaged into 10 minute bins and converted into the Principal coordinate system.
Note: the down-facing ADCP on MWM1 failed on July 10th, 2021, only recording 9 days of data. Because ADV motion-correction required bottom track, the ADV from MWM1 also only has 9 days processed. Additionally, only 25 days of data were processed from the MWM2 ADV because it appeared to have been impacted by debris on 7/25.
Two instruments were mounted on the THEOM (see MHKDR link further below for THEOM raw data):
4. A Nortek Vector acoustic Doppler velocimeter (ADV). Data were recorded at 8 Hz on a 5 minute duty cycle every 20 minutes. Data was bin-averaged into 5 minute bins, and converted to the Principal coordinate system.
5. A Nortek Signature 500 kHz acoustic Doppler current profiler (ADCP). Data were recorded in 4 Hz in the beam coordinate system from all 5 beams. Processed data has been averaged into 10 minutes bins and converted to the Principal coordinate system.}, doi = {10.15473/2007516}, url = {https://mhkdr.openei.org/submissions/475}, journal = {}, number = , volume = , place = {United States}, year = {2021}, month = {08}}
https://dx.doi.org/10.15473/2007516
Details
Data from Aug 31, 2021
Last updated Nov 18, 2024
Submitted Sep 29, 2023
Organization
Pacific Northwest National Laboratory
Contact
James McVey
206.528.3060
Authors
Original Source
https://mhkdr.openei.org/submissions/475Research Areas
Keywords
MHK, Marine, Hydrokinetic, energy, power, Cook Inlet, Alaska, tidal, water velocity, turbulence, transect survey, acoustic doppler current profiler, ADCP, mooring, acoustic doppler velocimeter, ADV, python, MATLAB, data, raw data, processed data, resource, current velocity, characterization, Marine Energy Resource Assessment and CharacterizationDOE Project Details
Project Name Model Validation and Site Characterization for Early Deployment MHK Sites and Establishment of Wave Classification Scheme
Project Lead Heather Spence
Project Number FY23 AOP 2.1.5.601