Admiralty Inlet Advanced Turbulence Measurements: May 2015
This data is from measurements at Admiralty Head, in Admiralty Inlet (Puget Sound) in May of 2015. The measurements were made using Inertial Motion Unit (IMU) equipped ADVs mounted on a 'StableMoor' (Manufacturer: DeepWater Buoyancy) buoy and a Tidal Turbulence Mooring (TTM). These platforms position ADV heads above the seafloor to make mid-depth turbulence measurements. The inertial measurements from the IMU allows for removal of mooring motion in post processing.
The mooring and buoy motion has been removed from the stream-wise and vertical velocity signals (u, w). The lateral (v) velocity has some 'persistent motion contamination' due to mooring sway.
The TTM was deployed with one ADV, it's position was: 48 09.145', -122 41.209'
The StableMoor was deployed twice, the first time it was deployed in 'wing-mode' with two ADVs ('Port' and 'Star') at: 48 09.166', -122 41.173'
The second StableMoor deployment was in 'Nose' mode with one ADV at: 48 09.166', -122 41.174'
Units
-----
- Velocity data (_u, urot, uacc) is in m/s.
- Acceleration (Accel) data is in m/s^2.
- Angular rate (AngRt) data is in rad/s.
- The components of all vectors are in 'ENU' orientation. That is, the first index is True East, the second is True North, and the third is Up (vertical).
- All other quantities are in the units defined in the Nortek Manual.
Motion correction and rotation into the ENU earth reference frame was performed using the Python-based open source DOLfYN library (http://lkilcher.github.io/dolfyn/). Details on motion correction can be found there.
Additional details on TTM measurements at this site can be found in the included Marine Energy Technology Symposium paper.
Citation Formats
TY - DATA
AB - This data is from measurements at Admiralty Head, in Admiralty Inlet (Puget Sound) in May of 2015. The measurements were made using Inertial Motion Unit (IMU) equipped ADVs mounted on a 'StableMoor' (Manufacturer: DeepWater Buoyancy) buoy and a Tidal Turbulence Mooring (TTM). These platforms position ADV heads above the seafloor to make mid-depth turbulence measurements. The inertial measurements from the IMU allows for removal of mooring motion in post processing.
The mooring and buoy motion has been removed from the stream-wise and vertical velocity signals (u, w). The lateral (v) velocity has some 'persistent motion contamination' due to mooring sway.
The TTM was deployed with one ADV, it's position was: 48 09.145', -122 41.209'
The StableMoor was deployed twice, the first time it was deployed in 'wing-mode' with two ADVs ('Port' and 'Star') at: 48 09.166', -122 41.173'
The second StableMoor deployment was in 'Nose' mode with one ADV at: 48 09.166', -122 41.174'
Units
-----
- Velocity data (_u, urot, uacc) is in m/s.
- Acceleration (Accel) data is in m/s^2.
- Angular rate (AngRt) data is in rad/s.
- The components of all vectors are in 'ENU' orientation. That is, the first index is True East, the second is True North, and the third is Up (vertical).
- All other quantities are in the units defined in the Nortek Manual.
Motion correction and rotation into the ENU earth reference frame was performed using the Python-based open source DOLfYN library (http://lkilcher.github.io/dolfyn/). Details on motion correction can be found there.
Additional details on TTM measurements at this site can be found in the included Marine Energy Technology Symposium paper.
AU - Kilcher, Levi
DB - Marine and Hydrokinetic Data Repository
DP - Open EI | National Renewable Energy Laboratory
DO - 10.15473/1245826
KW - MHK
KW - Marine
KW - Hydrokinetic
KW - energy
KW - power
KW - Turbulence
KW - Admiralty Inlet
KW - Puget Sound
KW - water velocity
KW - Tidal Turbulence Mooring
KW - TTM
KW - mid-depth turbulence
KW - measurements
KW - StableMoor
KW - DOLfYN
KW - Matlab
KW - data
KW - Python
KW - code
KW - vector files
KW - resource
KW - effectiveness
KW - safety
KW - technology
KW - ocean
KW - IMU
KW - buoy
KW - University of Washington
KW - PNNL
KW - NREL
KW - raw data
KW - pre-processed
KW - ADV
KW - measurement
KW - Nortek Vector
KW - VEC
KW - acceleration
KW - angular rate
KW - field test
KW - DeepWater Buoyancy
KW - processed data
LA - English
DA - 2015/05/18
PY - 2015
PB - National Renewable Energy Laboratory
T1 - Admiralty Inlet Advanced Turbulence Measurements: May 2015
UR - https://doi.org/10.15473/1245826
ER -
Kilcher, Levi. Admiralty Inlet Advanced Turbulence Measurements: May 2015. National Renewable Energy Laboratory, 18 May, 2015, Marine and Hydrokinetic Data Repository. https://doi.org/10.15473/1245826.
Kilcher, L. (2015). Admiralty Inlet Advanced Turbulence Measurements: May 2015. [Data set]. Marine and Hydrokinetic Data Repository. National Renewable Energy Laboratory. https://doi.org/10.15473/1245826
Kilcher, Levi. Admiralty Inlet Advanced Turbulence Measurements: May 2015. National Renewable Energy Laboratory, May, 18, 2015. Distributed by Marine and Hydrokinetic Data Repository. https://doi.org/10.15473/1245826
@misc{MHKDR_Dataset_51,
title = {Admiralty Inlet Advanced Turbulence Measurements: May 2015},
author = {Kilcher, Levi},
abstractNote = {This data is from measurements at Admiralty Head, in Admiralty Inlet (Puget Sound) in May of 2015. The measurements were made using Inertial Motion Unit (IMU) equipped ADVs mounted on a 'StableMoor' (Manufacturer: DeepWater Buoyancy) buoy and a Tidal Turbulence Mooring (TTM). These platforms position ADV heads above the seafloor to make mid-depth turbulence measurements. The inertial measurements from the IMU allows for removal of mooring motion in post processing.
The mooring and buoy motion has been removed from the stream-wise and vertical velocity signals (u, w). The lateral (v) velocity has some 'persistent motion contamination' due to mooring sway.
The TTM was deployed with one ADV, it's position was: 48 09.145', -122 41.209'
The StableMoor was deployed twice, the first time it was deployed in 'wing-mode' with two ADVs ('Port' and 'Star') at: 48 09.166', -122 41.173'
The second StableMoor deployment was in 'Nose' mode with one ADV at: 48 09.166', -122 41.174'
Units
-----
- Velocity data (_u, urot, uacc) is in m/s.
- Acceleration (Accel) data is in m/s^2.
- Angular rate (AngRt) data is in rad/s.
- The components of all vectors are in 'ENU' orientation. That is, the first index is True East, the second is True North, and the third is Up (vertical).
- All other quantities are in the units defined in the Nortek Manual.
Motion correction and rotation into the ENU earth reference frame was performed using the Python-based open source DOLfYN library (http://lkilcher.github.io/dolfyn/). Details on motion correction can be found there.
Additional details on TTM measurements at this site can be found in the included Marine Energy Technology Symposium paper.},
url = {https://mhkdr.openei.org/submissions/51},
year = {2015},
howpublished = {Marine and Hydrokinetic Data Repository, National Renewable Energy Laboratory, https://doi.org/10.15473/1245826},
note = {Accessed: 2025-05-05},
doi = {10.15473/1245826}
}
https://dx.doi.org/10.15473/1245826
Details
Data from May 18, 2015
Last updated Jul 30, 2020
Submitted Sep 23, 2015
Organization
National Renewable Energy Laboratory
Contact
Levi Kilcher
303.384.7192
Authors
Keywords
MHK, Marine, Hydrokinetic, energy, power, Turbulence, Admiralty Inlet, Puget Sound, water velocity, Tidal Turbulence Mooring, TTM, mid-depth turbulence, measurements, StableMoor, DOLfYN, Matlab, data, Python, code, vector files, resource, effectiveness, safety, technology, ocean, IMU, buoy, University of Washington, PNNL, NREL, raw data, pre-processed, ADV, measurement, Nortek Vector, VEC, acceleration, angular rate, field test, DeepWater Buoyancy, processed dataDOE Project Details
Project Name Advanced Turbulence Measurement Techniques for Current Device Field Deployments Collab with UW
Project Lead Alison LaBonte
Project Number FY16 AOP 132401
