Petermann Fjord EK80 sonar data, Greenland, July 30 - August 10, 2015

The contributed data represents watercolumn backscatter data collected with a Simrad EK80 Wide-band Transceiver (WBT) transmitting through a Simrad ES18-11 scientific split-beam echosounder on the Icebreaker Oden during Petermann Glacier 2015 Expedition. The EK80 WBT was installed by UNH on the ODEN...

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Bibliographic Details
Main Author: Larry Mayer
Format: Dataset
Language:unknown
Published: Arctic Data Center 2018
Subjects:
Online Access:https://doi.org/10.18739/A2HG5J
id dataone:doi:10.18739/A2HG5J
record_format openpolar
spelling dataone:doi:10.18739/A2HG5J 2024-06-03T18:46:51+00:00 Petermann Fjord EK80 sonar data, Greenland, July 30 - August 10, 2015 Larry Mayer Transit from Thule Greenland to Petermann Fjord and return plus thirty days of data collection in Petermann Fjord, Hall Basin, Kennedy Channel, Robeson Channel all off northwestern Greenland. ENVELOPE(-67.0,-61.0,82.0,80.5) BEGINDATE: 2015-07-30T00:00:00Z ENDDATE: 2015-08-10T00:00:00Z 2018-04-11T00:00:00Z https://doi.org/10.18739/A2HG5J unknown Arctic Data Center Instruments/Sensors>EK80>Broadband Watercolumn Acoustic Data Dataset 2018 dataone:urn:node:ARCTIC https://doi.org/10.18739/A2HG5J 2024-06-03T18:11:05Z The contributed data represents watercolumn backscatter data collected with a Simrad EK80 Wide-band Transceiver (WBT) transmitting through a Simrad ES18-11 scientific split-beam echosounder on the Icebreaker Oden during Petermann Glacier 2015 Expedition. The EK80 WBT was installed by UNH on the ODEN especially for this program. The data were collected over a band of approximately 16 - 26 kHz providing extremely high resolution imagery of the water column. The water-column data showed revealed a distinct mid-water scattering layer whose spatial distribution and presence and absence appears to be associated with the distribution and circulation of water masses in the region. Files are named according to the format: PETERMANN2015-{Date}-{Time}.raw. "PETERMANN2015" indicates that the measurements were taken during the Petermann Glacier 2015 Expedition. {Date} corresponds to the date that this 24-hour cycle of measurements concluded and {Time} is the number of hours, minutes, and seconds (in this format: HHMMSS) since this cycle of measurements began. For example, "PETERMANN2015-D20150806-T020343.raw" contains data recorded during the Petermann Glacier 2015 Expedition taken during the 2015-08-06 cycle 02:03:43 after the cycle began. Dataset glacier Greenland Hall Basin Kennedy channel oden Petermann Fjord Petermann glacier Robeson channel Thule Arctic Data Center (via DataONE) Greenland Kennedy Channel ENVELOPE(-66.139,-66.139,80.919,80.919) Petermann Fjord ENVELOPE(-61.500,-61.500,81.167,81.167) Robeson Channel ENVELOPE(-61.473,-61.473,81.995,81.995) Hall Basin ENVELOPE(-62.992,-62.992,81.502,81.502) ENVELOPE(-67.0,-61.0,82.0,80.5)
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
topic Instruments/Sensors>EK80>Broadband Watercolumn Acoustic Data
spellingShingle Instruments/Sensors>EK80>Broadband Watercolumn Acoustic Data
Larry Mayer
Petermann Fjord EK80 sonar data, Greenland, July 30 - August 10, 2015
topic_facet Instruments/Sensors>EK80>Broadband Watercolumn Acoustic Data
description The contributed data represents watercolumn backscatter data collected with a Simrad EK80 Wide-band Transceiver (WBT) transmitting through a Simrad ES18-11 scientific split-beam echosounder on the Icebreaker Oden during Petermann Glacier 2015 Expedition. The EK80 WBT was installed by UNH on the ODEN especially for this program. The data were collected over a band of approximately 16 - 26 kHz providing extremely high resolution imagery of the water column. The water-column data showed revealed a distinct mid-water scattering layer whose spatial distribution and presence and absence appears to be associated with the distribution and circulation of water masses in the region. Files are named according to the format: PETERMANN2015-{Date}-{Time}.raw. "PETERMANN2015" indicates that the measurements were taken during the Petermann Glacier 2015 Expedition. {Date} corresponds to the date that this 24-hour cycle of measurements concluded and {Time} is the number of hours, minutes, and seconds (in this format: HHMMSS) since this cycle of measurements began. For example, "PETERMANN2015-D20150806-T020343.raw" contains data recorded during the Petermann Glacier 2015 Expedition taken during the 2015-08-06 cycle 02:03:43 after the cycle began.
format Dataset
author Larry Mayer
author_facet Larry Mayer
author_sort Larry Mayer
title Petermann Fjord EK80 sonar data, Greenland, July 30 - August 10, 2015
title_short Petermann Fjord EK80 sonar data, Greenland, July 30 - August 10, 2015
title_full Petermann Fjord EK80 sonar data, Greenland, July 30 - August 10, 2015
title_fullStr Petermann Fjord EK80 sonar data, Greenland, July 30 - August 10, 2015
title_full_unstemmed Petermann Fjord EK80 sonar data, Greenland, July 30 - August 10, 2015
title_sort petermann fjord ek80 sonar data, greenland, july 30 - august 10, 2015
publisher Arctic Data Center
publishDate 2018
url https://doi.org/10.18739/A2HG5J
op_coverage Transit from Thule Greenland to Petermann Fjord and return plus thirty days of data collection in Petermann Fjord, Hall Basin, Kennedy Channel, Robeson Channel all off northwestern Greenland.
ENVELOPE(-67.0,-61.0,82.0,80.5)
BEGINDATE: 2015-07-30T00:00:00Z ENDDATE: 2015-08-10T00:00:00Z
long_lat ENVELOPE(-66.139,-66.139,80.919,80.919)
ENVELOPE(-61.500,-61.500,81.167,81.167)
ENVELOPE(-61.473,-61.473,81.995,81.995)
ENVELOPE(-62.992,-62.992,81.502,81.502)
ENVELOPE(-67.0,-61.0,82.0,80.5)
geographic Greenland
Kennedy Channel
Petermann Fjord
Robeson Channel
Hall Basin
geographic_facet Greenland
Kennedy Channel
Petermann Fjord
Robeson Channel
Hall Basin
genre glacier
Greenland
Hall Basin
Kennedy channel
oden
Petermann Fjord
Petermann glacier
Robeson channel
Thule
genre_facet glacier
Greenland
Hall Basin
Kennedy channel
oden
Petermann Fjord
Petermann glacier
Robeson channel
Thule
op_doi https://doi.org/10.18739/A2HG5J
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