http://lod.bco-dmo.org/id/dataset/2458
eng; USA
utf8
dataset
Highest level of data collection, from a common set of sensors or instrumentation, usually within the same research project
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
2009-11-29
ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data
ISO 19115-2:2009(E)
ADCP data from the Long-Term Observation Program (LTOP) from Mooring site NH10 on the Oregon Shelf from 1997-2004 as part of the U.S. GLOBEC program (NEP project)
2007-04-13
publication
2007-04-13
revision
Marine Biological Laboratory/Woods Hole Oceanographic Institution Library (MBLWHOI DLA)
2019-10-31
publication
https://doi.org/10.1575/1912/bco-dmo.2458.1
Mike Kosro
Oregon State University
principalInvestigator
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
publisher
Cite this dataset as: Kosro, M. (2007) ADCP data from the Long-Term Observation Program (LTOP) from Mooring site NH10 on the Oregon Shelf from 1997-2004 as part of the U.S. GLOBEC program (NEP project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2007-04-13 [if applicable, indicate subset used]. doi:10.1575/1912/bco-dmo.2458.1 [access date]
ADCP data from the Long-Term Observation Program (LTOP) NH10 Mooring Dataset Description: <h4>ADCP U.S. GLOBEC Long-Term Observation Program (LTOP) NH10 Mooring</h4>
<p>A long-term mooring site on the Oregon shelf (44.6467N -124.3067E) was established in August 1997 and maintained with few gaps through December 2004 with U.S. GLOBEC funding. The mooring is at 81 m water depth, near the historical Newport Hydrographic Line. The nearest standard NH line station is NH10 (10 nautical miles off shore), so this mooring is referred to as Mooring NH10.</p>
<p>Upward looking acoustic Doppler current profilers have been used to measure vertical profiles of water velocity (insert actual sample interval here) at 2 or 4 m vertical intervals depending on instrument. The mooring is serviced in spring and fall: winter deployments generally use a Sontek 250 kHz profiler with 4 m vertical resolution; summer deployments use a Sontek 500 kHz profiler with 2 m resolution. There are a few data gaps.</p>
<p>Currents are processed using a cosine-Lanczos filter with a 40-hr half-power point. Six-hourly data included here are Eastward (u) and Northward (v) velocities in cm/s interpolated to 2 m depth bins.</p>
<p>The data were collected by Mike Kosro, 104 COAS Admin Bldg, COAS, Oregon State University, Corvallis, OR 97331-5503 (<a href="mailto:kosro@coas.oregonstate.edu">kosro@coas.oregonstate.edu</a>; Phone: 541-737-3079).</p>
<p>For further details about sampling/processing, see:</p>
<p>Kosro, M. 2003. Enhanced southward flow over the Oregon shelf in 2002: A conduit for subarctic water. Geophysical Research Letters, 30 (15), 8023, doi:10.1029/2003GL017436</p>
<p><em>Last modified: March 26, 2006</em></p> Methods and Sampling:
Funding provided by National Oceanic and Atmospheric Administration (NOAA) Award Number: unknown GB NOAA
Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-0000733 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=0000733
completed
Mike Kosro
Oregon State University
541-737-3079
104 COAS Admin Bldg
Corvallis
OR
97331-5503
USA
kosro@coas.oregonstate.edu
pointOfContact
asNeeded
Dataset Version: 1
Unknown
year
mooring
lat
long
depth_w
depth
julian_day
yrday0_gmt
month_gmt
day_gmt
time_gmt
u
v
Acoustic Doppler Current Profiler
theme
None, User defined
year
mooring identification
latitude
longitude
depth_w
depth
No BCO-DMO term
yrday0_gmt
month_gmt
day_gmt
time_gmt
velocity east
velocity north
featureType
BCO-DMO Standard Parameters
Acoustic Doppler Current Profiler
instrument
BCO-DMO Standard Instruments
NH10
service
Deployment Activity
Northeast Pacific
place
Locations
otherRestrictions
otherRestrictions
Access Constraints: none. Use Constraints: Please follow guidelines at: http://www.bco-dmo.org/terms-use Distribution liability: Under no circumstances shall BCO-DMO be liable for any direct, incidental, special, consequential, indirect, or punitive damages that result from the use of, or the inability to use, the materials in this data submission. If you are dissatisfied with any materials in this data submission your sole and exclusive remedy is to discontinue use.
U.S. GLOBal ocean ECosystems dynamics
http://www.usglobec.org/
U.S. GLOBal ocean ECosystems dynamics
U.S. GLOBEC (GLOBal ocean ECosystems dynamics) is a research program organized by oceanographers and fisheries scientists to address the question of how global climate change may affect the abundance and production of animals in the sea.
The U.S. GLOBEC Program currently had major research efforts underway in the Georges Bank / Northwest Atlantic Region, and the Northeast Pacific (with components in the California Current and in the Coastal Gulf of Alaska). U.S. GLOBEC was a major contributor to International GLOBEC efforts in the Southern Ocean and Western Antarctic Peninsula (WAP).
U.S. GLOBEC
largerWorkCitation
program
U.S. GLOBEC Northeast Pacific
http://nepglobec.bco-dmo.org
U.S. GLOBEC Northeast Pacific
<p><strong>Program in a Nutshell</strong></p>
<p><strong>Goal: </strong> To understand the effects of climate variability and climate change on the distribution, abundance and production of marine animals (including commercially important living marine resources) in the eastern North Pacific. To embody this understanding in diagnostic and prognostic ecosystem models, capable of capturing the ecosystem response to major climatic fluctuations.</p>
<p><strong>Approach: </strong>To study the effects of past and present climate variability on the population ecology and population dynamics of marine biota and living marine resources, and to use this information as a proxy for how the ecosystems of the eastern North Pacific may respond to future global climate change. The strong temporal variability in the physical and biological signals of the NEP will be used to examine the biophysical mechanisms through which zooplankton and salmon populations respond to physical forcing and biological interactions in the coastal regions of the two gyres. Annual and interannual variability will be studied directly through <strong>long-term observations</strong> and detailed <strong>process studies</strong>; variability at longer time scales will be examined through <strong>retrospective analysis</strong> of directly measured and proxy data. Coupled <strong>biophysical models</strong> of the ecosystems of these regions will be developed and tested using the process studies and data collected from the long-term observation programs, then further tested and improved by hindcasting selected retrospective data series.</p>
NEP
largerWorkCitation
project
eng; USA
oceans
Northeast Pacific
-124.3067
-124.3067
44.6467
44.6467
1997-10-21
2004-12-31
Northeast Pacific Ocean, Gulf of Alaska
0
BCO-DMO catalogue of parameters from ADCP data from the Long-Term Observation Program (LTOP) from Mooring site NH10 on the Oregon Shelf from 1997-2004 as part of the U.S. GLOBEC program (NEP project)
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
http://lod.bco-dmo.org/id/dataset-parameter/14261.rdf
Name: year
Units: dimensionless
Description: <p>Year.</p>
http://lod.bco-dmo.org/id/dataset-parameter/14262.rdf
Name: mooring
Units: dimensionless
Description: <p>Mooring ID (NH10 for this dataset).</p>
http://lod.bco-dmo.org/id/dataset-parameter/14263.rdf
Name: lat
Units: decimal degrees
Description: <p>Latitude in decimal degrees North</p>
http://lod.bco-dmo.org/id/dataset-parameter/14264.rdf
Name: long
Units: decimal degrees
Description: <p>Longitude in decimal degrees East</p>
http://lod.bco-dmo.org/id/dataset-parameter/14265.rdf
Name: depth_w
Units: meters
Description: <p>Water depth in meters</p>
http://lod.bco-dmo.org/id/dataset-parameter/14266.rdf
Name: depth
Units: meters
Description: <p>Depth of velocities in meters</p>
http://lod.bco-dmo.org/id/dataset-parameter/14267.rdf
Name: julian_day
Units: dimensionless
Description: <p>Julian day, where JD2440000 is 0000 hrs on 23 May 1968.</p>
http://lod.bco-dmo.org/id/dataset-parameter/14268.rdf
Name: yrday0_gmt
Units: dimensionless
Description: <p>Day of Year, where 0.5 is 1200 hrs on 1 January.</p>
http://lod.bco-dmo.org/id/dataset-parameter/14269.rdf
Name: month_gmt
Units: dimensionless
Description: <p>Month in GMT.</p>
http://lod.bco-dmo.org/id/dataset-parameter/14270.rdf
Name: day_gmt
Units: dimensionless
Description: <p>Day of Month in GMT.</p>
http://lod.bco-dmo.org/id/dataset-parameter/14271.rdf
Name: time_gmt
Units: dimensionless
Description: <p>Time of Day in GMT (HHMM).</p>
http://lod.bco-dmo.org/id/dataset-parameter/14272.rdf
Name: u
Units: centimeters/sec
Description: <p>Eastward Velocity (cm/s; Positive East)</p>
http://lod.bco-dmo.org/id/dataset-parameter/14273.rdf
Name: v
Units: centimeters/sec
Description: <p>Northward Velocity (cm/s; Positive North)</p>
GB/NERC/BODC > British Oceanographic Data Centre, Natural Environment Research Council, United Kingdom
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
23376759
https://darchive.mblwhoilibrary.org/bitstream/1912/24743/1/dataset-2458_nh10uv6hr__v1.tsv
download
https://doi.org/10.1575/1912/bco-dmo.2458.1
download
onLine
asNeeded
7.x-1.1
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
Acoustic Doppler Current Profiler
Acoustic Doppler Current Profiler
PI Supplied Instrument Name: Acoustic Doppler Current Profiler PI Supplied Instrument Description:Upward looking acoustic Doppler current profilers have been used to measure vertical profiles of water velocity (insert actual sample interval here) at 2 or 4 m vertical intervals depending on instrument. The mooring is serviced in spring and fall. winter deployments generally use a Sontek 250 kHz profiler with 4 m vertical resolution; summer deployments use a Sontek 500 kHz profiler with 2 m resolution. Instrument Name: Acoustic Doppler Current Profiler Instrument Short Name:ADCP 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). Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/115/
Deployment: NH10
NH10
Mooring NH10
mooring
NH10
Mike Kosro
Oregon State University
Mooring NH10
mooring