Radar monitoring data collected at two locations in June, 2009, Breidamerkurjokull

5-MHz ground-based radar system was located on two places on Breidamerkurjokull for several days to measure temporal changes of englacial and subglacial properties. The data file includes two structures: Site A and Site B. Each structure includes two radar waveforms (ch0 for a wider amplitude range...

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Bibliographic Details
Main Authors: Howard Conway, Kenichi Matsuoka
Format: Dataset
Language:unknown
Published: Arctic Data Center 2013
Subjects:
Online Access:https://doi.org/10.18739/A2M03XW73
id dataone:doi:10.18739/A2M03XW73
record_format openpolar
spelling dataone:doi:10.18739/A2M03XW73 2024-10-03T18:46:12+00:00 Radar monitoring data collected at two locations in June, 2009, Breidamerkurjokull Howard Conway Kenichi Matsuoka NORTHERN EUROPE > ICELAND ENVELOPE(-16.35,16.33,64.1,64.08) BEGINDATE: 2009-06-22T00:00:00Z ENDDATE: 2009-06-28T00:00:00Z 2013-02-22T00:00:00Z https://doi.org/10.18739/A2M03XW73 unknown Arctic Data Center EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIERS EARTH REMOTE SENSING INSTRUMENTS > ACTIVE REMOTE SENSING > PROFILERS/SOUNDERS > RADAR SOUNDERS > RADAR ECHO SOUNDERS FIELD SURVEY STATION POINT 1 MINUTE TO 1 HOUR geoscientificInformation Dataset 2013 dataone:urn:node:ARCTIC https://doi.org/10.18739/A2M03XW73 2024-10-03T18:11:14Z 5-MHz ground-based radar system was located on two places on Breidamerkurjokull for several days to measure temporal changes of englacial and subglacial properties. The data file includes two structures: Site A and Site B. Each structure includes two radar waveforms (ch0 for a wider amplitude range and ch1 for a narrower amplitude range), corresponding two-way travel time, and time when each radar data was collected (julian day, hour, minute, second, and timestamp = jday + (hour + minute./60 + second./3600)./24). We replaced the batteries of the radar system every day, which is not frequent enough to collect the data continuously. The users of this dataset should pay attention to temporal changes of the radar-transmitting power. Amplitudes of the direct wave can be used to measure this feature caused by decreased voltage of the power supply. Coordinates of two monitoring sites are: Site A: 64.0961N, 16.3441W (WGS84 decimal degrees) Site B: 64.0891N, 16.3357W (WGS84 decimal degrees) Dataset Iceland Arctic Data Center (via DataONE) ENVELOPE(-16.35,16.33,64.1,64.08)
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
topic EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIERS
EARTH REMOTE SENSING INSTRUMENTS > ACTIVE REMOTE SENSING > PROFILERS/SOUNDERS > RADAR SOUNDERS > RADAR ECHO SOUNDERS
FIELD SURVEY
STATION
POINT
1 MINUTE TO 1 HOUR
geoscientificInformation
spellingShingle EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIERS
EARTH REMOTE SENSING INSTRUMENTS > ACTIVE REMOTE SENSING > PROFILERS/SOUNDERS > RADAR SOUNDERS > RADAR ECHO SOUNDERS
FIELD SURVEY
STATION
POINT
1 MINUTE TO 1 HOUR
geoscientificInformation
Howard Conway
Kenichi Matsuoka
Radar monitoring data collected at two locations in June, 2009, Breidamerkurjokull
topic_facet EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIERS
EARTH REMOTE SENSING INSTRUMENTS > ACTIVE REMOTE SENSING > PROFILERS/SOUNDERS > RADAR SOUNDERS > RADAR ECHO SOUNDERS
FIELD SURVEY
STATION
POINT
1 MINUTE TO 1 HOUR
geoscientificInformation
description 5-MHz ground-based radar system was located on two places on Breidamerkurjokull for several days to measure temporal changes of englacial and subglacial properties. The data file includes two structures: Site A and Site B. Each structure includes two radar waveforms (ch0 for a wider amplitude range and ch1 for a narrower amplitude range), corresponding two-way travel time, and time when each radar data was collected (julian day, hour, minute, second, and timestamp = jday + (hour + minute./60 + second./3600)./24). We replaced the batteries of the radar system every day, which is not frequent enough to collect the data continuously. The users of this dataset should pay attention to temporal changes of the radar-transmitting power. Amplitudes of the direct wave can be used to measure this feature caused by decreased voltage of the power supply. Coordinates of two monitoring sites are: Site A: 64.0961N, 16.3441W (WGS84 decimal degrees) Site B: 64.0891N, 16.3357W (WGS84 decimal degrees)
format Dataset
author Howard Conway
Kenichi Matsuoka
author_facet Howard Conway
Kenichi Matsuoka
author_sort Howard Conway
title Radar monitoring data collected at two locations in June, 2009, Breidamerkurjokull
title_short Radar monitoring data collected at two locations in June, 2009, Breidamerkurjokull
title_full Radar monitoring data collected at two locations in June, 2009, Breidamerkurjokull
title_fullStr Radar monitoring data collected at two locations in June, 2009, Breidamerkurjokull
title_full_unstemmed Radar monitoring data collected at two locations in June, 2009, Breidamerkurjokull
title_sort radar monitoring data collected at two locations in june, 2009, breidamerkurjokull
publisher Arctic Data Center
publishDate 2013
url https://doi.org/10.18739/A2M03XW73
op_coverage NORTHERN EUROPE > ICELAND
ENVELOPE(-16.35,16.33,64.1,64.08)
BEGINDATE: 2009-06-22T00:00:00Z ENDDATE: 2009-06-28T00:00:00Z
long_lat ENVELOPE(-16.35,16.33,64.1,64.08)
genre Iceland
genre_facet Iceland
op_doi https://doi.org/10.18739/A2M03XW73
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