SIZONET Surface Albedo Transects

Wavelength integrated surface albedo was monitored every 2.5 meters along two 200 meter transects using a pair of Kipp and Zonen radiometers. Measurements are taken daily or every few days from 5/21-6/25/2009, spanning the time from snow melt through unsafe ice conditions. The transects are on shore...

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Format: Dataset
Language:unknown
Published: Arctic Data Center 2009
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Online Access:https://search.dataone.org/view/urn:uuid:852ceb1b-9c83-4ab1-9e21-6e0de97e39b5
id dataone:urn:uuid:852ceb1b-9c83-4ab1-9e21-6e0de97e39b5
record_format openpolar
spelling dataone:urn:uuid:852ceb1b-9c83-4ab1-9e21-6e0de97e39b5 2024-01-03T20:45:49+01:00 SIZONET Surface Albedo Transects ENVELOPE(156.0,157.0,72.0,71.0) BEGINDATE: 2009-04-14T00:00:00Z ENDDATE: 2009-06-25T00:00:00Z 2009-11-24T10:15:15Z https://search.dataone.org/view/urn:uuid:852ceb1b-9c83-4ab1-9e21-6e0de97e39b5 unknown Arctic Data Center EARTH SCIENCE > CRYOSPHERE > SNOW/ICE > ALBEDO EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > SPECTROMETERS/RADIOMETERS > RADIOMETERS > RADIOMETERS FIELD SURVEY TRANSECT 1 METER TO 30 METERS DAILY TO WEEKLY Dataset 2009 dataone:urn:node:ARCTIC 2024-01-03T20:03:57Z Wavelength integrated surface albedo was monitored every 2.5 meters along two 200 meter transects using a pair of Kipp and Zonen radiometers. Measurements are taken daily or every few days from 5/21-6/25/2009, spanning the time from snow melt through unsafe ice conditions. The transects are on shorefast seasonal ice near the Mass Balance Site. The South transect was on flat, mostly undeformed ice. The Eastern end of the line appeared to be intact ice which had formed under calmer conditions, while the Western half had rafted when a few centimeters thick and appeared to have formed in dirtier, more turbulent seas. The South transect ran from Universal Transverse Mercator (UTM) 587519.70W 7920274.01N (zone 4) to 587718.92W 7920261.68N and was roughly a hundred meters offshore from the Mass Balance Site. The North transect was about a kilometer north toward Point Barrow from the Mass Balance site, on a separate floe, running from 7920510.88N 588422.251W to 7920471.49N 588226.646W, again UTM zone 4. The East end of this line was on level ice very similar to the west end of the south line. There was evidence of rafting during early growth and significant sediment was entrained in the ice. The West end of this North transect was ridged and rubbly ice which had been deformed when the ice was 5-10 cm thick, with significant snow drifts. Data Citation: Eicken, H., R. Gradinger, T. Heinrichs, M. Johnson, A. Lovecraft, and C. Polashenski. (2012). Surface Albedo Transects (SIZONET). UCAR/NCAR - CISL - ACADIS. http://www.aoncadis.org/dataset/sizonet_surface_albedo_transects.html Dataset Point Barrow Arctic Data Center (via DataONE) ENVELOPE(156.0,157.0,72.0,71.0)
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
topic EARTH SCIENCE > CRYOSPHERE > SNOW/ICE > ALBEDO
EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > SPECTROMETERS/RADIOMETERS > RADIOMETERS > RADIOMETERS
FIELD SURVEY
TRANSECT
1 METER TO 30 METERS
DAILY TO WEEKLY
spellingShingle EARTH SCIENCE > CRYOSPHERE > SNOW/ICE > ALBEDO
EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > SPECTROMETERS/RADIOMETERS > RADIOMETERS > RADIOMETERS
FIELD SURVEY
TRANSECT
1 METER TO 30 METERS
DAILY TO WEEKLY
SIZONET Surface Albedo Transects
topic_facet EARTH SCIENCE > CRYOSPHERE > SNOW/ICE > ALBEDO
EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > SPECTROMETERS/RADIOMETERS > RADIOMETERS > RADIOMETERS
FIELD SURVEY
TRANSECT
1 METER TO 30 METERS
DAILY TO WEEKLY
description Wavelength integrated surface albedo was monitored every 2.5 meters along two 200 meter transects using a pair of Kipp and Zonen radiometers. Measurements are taken daily or every few days from 5/21-6/25/2009, spanning the time from snow melt through unsafe ice conditions. The transects are on shorefast seasonal ice near the Mass Balance Site. The South transect was on flat, mostly undeformed ice. The Eastern end of the line appeared to be intact ice which had formed under calmer conditions, while the Western half had rafted when a few centimeters thick and appeared to have formed in dirtier, more turbulent seas. The South transect ran from Universal Transverse Mercator (UTM) 587519.70W 7920274.01N (zone 4) to 587718.92W 7920261.68N and was roughly a hundred meters offshore from the Mass Balance Site. The North transect was about a kilometer north toward Point Barrow from the Mass Balance site, on a separate floe, running from 7920510.88N 588422.251W to 7920471.49N 588226.646W, again UTM zone 4. The East end of this line was on level ice very similar to the west end of the south line. There was evidence of rafting during early growth and significant sediment was entrained in the ice. The West end of this North transect was ridged and rubbly ice which had been deformed when the ice was 5-10 cm thick, with significant snow drifts. Data Citation: Eicken, H., R. Gradinger, T. Heinrichs, M. Johnson, A. Lovecraft, and C. Polashenski. (2012). Surface Albedo Transects (SIZONET). UCAR/NCAR - CISL - ACADIS. http://www.aoncadis.org/dataset/sizonet_surface_albedo_transects.html
format Dataset
title SIZONET Surface Albedo Transects
title_short SIZONET Surface Albedo Transects
title_full SIZONET Surface Albedo Transects
title_fullStr SIZONET Surface Albedo Transects
title_full_unstemmed SIZONET Surface Albedo Transects
title_sort sizonet surface albedo transects
publisher Arctic Data Center
publishDate 2009
url https://search.dataone.org/view/urn:uuid:852ceb1b-9c83-4ab1-9e21-6e0de97e39b5
op_coverage ENVELOPE(156.0,157.0,72.0,71.0)
BEGINDATE: 2009-04-14T00:00:00Z ENDDATE: 2009-06-25T00:00:00Z
long_lat ENVELOPE(156.0,157.0,72.0,71.0)
genre Point Barrow
genre_facet Point Barrow
_version_ 1787109162107273216