Supplementary animations supporting "South-east Greenland Ice Sheet short term response to environmental conditions"

Animation S1: Animation showing MODIS imagery and edge detection for Kangerdlugssuaq glacier. Left hand plot shows band 1 surface reflectance of Kangerdlugssuaq and the surrounding area for each cloud free day, which forms a single frame of the animation; axis units are km. Central top figure shows...

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Main Author: Seale, Anthony
Format: Dataset
Language:unknown
Published: University of Cambridge 2017
Subjects:
Online Access:https://doi.org/10.17863/CAM.9653
https://www.repository.cam.ac.uk/handle/1810/264246
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record_format openpolar
spelling ftunivcam:oai:www.repository.cam.ac.uk:1810/264246 2023-07-30T04:03:15+02:00 Supplementary animations supporting "South-east Greenland Ice Sheet short term response to environmental conditions" Seale, Anthony 2017-05-15T15:29:20Z Video player video/vnd.avi https://doi.org/10.17863/CAM.9653 https://www.repository.cam.ac.uk/handle/1810/264246 unknown University of Cambridge https://doi.org/10.17863/CAM.9652 doi:10.17863/CAM.9653 https://www.repository.cam.ac.uk/handle/1810/264246 All Rights Reserved https://www.rioxx.net/licenses/all-rights-reserved/ Dataset 2017 ftunivcam https://doi.org/10.17863/CAM.965310.17863/CAM.9652 2023-07-10T21:39:59Z Animation S1: Animation showing MODIS imagery and edge detection for Kangerdlugssuaq glacier. Left hand plot shows band 1 surface reflectance of Kangerdlugssuaq and the surrounding area for each cloud free day, which forms a single frame of the animation; axis units are km. Central top figure shows surface reflectance of the 'active region', the area within which edge detection takes place; axis units are km. Second central figure down shows detected edge pixels (white) over the active region using the Sobel method; axis units are km. Third central figure down shows frequency of detected edge pixels (y-axis) using the Sobel method along the length of the glacier (x-axis, km). High frequencies signify likely calving margin positions. Central bottom figure shows gradient (y-axis) of across-glacier averaged surface reflectance along the length of the glacier (x-axis, km), used as part of the brightness profiling method of calculating margin position. High brightness gradient locations signify likely calving margin locations. Right hand plot shows detected margin positions after consolidation of the two detection methods and noise removal procedures; x-axis is relative margin position in km, y-axis is time in years beginning. A horizontal line travels down the plot to signify animation location within time. Animation S2: Plots are the same as in Supplementary Animation S1, but for Helheim Glacier. Plot details are described in the caption for S1. Dataset East Greenland glacier Greenland Ice Sheet Apollo - University of Cambridge Repository Greenland Sobel ENVELOPE(20.500,20.500,69.618,69.618)
institution Open Polar
collection Apollo - University of Cambridge Repository
op_collection_id ftunivcam
language unknown
description Animation S1: Animation showing MODIS imagery and edge detection for Kangerdlugssuaq glacier. Left hand plot shows band 1 surface reflectance of Kangerdlugssuaq and the surrounding area for each cloud free day, which forms a single frame of the animation; axis units are km. Central top figure shows surface reflectance of the 'active region', the area within which edge detection takes place; axis units are km. Second central figure down shows detected edge pixels (white) over the active region using the Sobel method; axis units are km. Third central figure down shows frequency of detected edge pixels (y-axis) using the Sobel method along the length of the glacier (x-axis, km). High frequencies signify likely calving margin positions. Central bottom figure shows gradient (y-axis) of across-glacier averaged surface reflectance along the length of the glacier (x-axis, km), used as part of the brightness profiling method of calculating margin position. High brightness gradient locations signify likely calving margin locations. Right hand plot shows detected margin positions after consolidation of the two detection methods and noise removal procedures; x-axis is relative margin position in km, y-axis is time in years beginning. A horizontal line travels down the plot to signify animation location within time. Animation S2: Plots are the same as in Supplementary Animation S1, but for Helheim Glacier. Plot details are described in the caption for S1.
format Dataset
author Seale, Anthony
spellingShingle Seale, Anthony
Supplementary animations supporting "South-east Greenland Ice Sheet short term response to environmental conditions"
author_facet Seale, Anthony
author_sort Seale, Anthony
title Supplementary animations supporting "South-east Greenland Ice Sheet short term response to environmental conditions"
title_short Supplementary animations supporting "South-east Greenland Ice Sheet short term response to environmental conditions"
title_full Supplementary animations supporting "South-east Greenland Ice Sheet short term response to environmental conditions"
title_fullStr Supplementary animations supporting "South-east Greenland Ice Sheet short term response to environmental conditions"
title_full_unstemmed Supplementary animations supporting "South-east Greenland Ice Sheet short term response to environmental conditions"
title_sort supplementary animations supporting "south-east greenland ice sheet short term response to environmental conditions"
publisher University of Cambridge
publishDate 2017
url https://doi.org/10.17863/CAM.9653
https://www.repository.cam.ac.uk/handle/1810/264246
long_lat ENVELOPE(20.500,20.500,69.618,69.618)
geographic Greenland
Sobel
geographic_facet Greenland
Sobel
genre East Greenland
glacier
Greenland
Ice Sheet
genre_facet East Greenland
glacier
Greenland
Ice Sheet
op_relation https://doi.org/10.17863/CAM.9652
doi:10.17863/CAM.9653
https://www.repository.cam.ac.uk/handle/1810/264246
op_rights All Rights Reserved
https://www.rioxx.net/licenses/all-rights-reserved/
op_doi https://doi.org/10.17863/CAM.965310.17863/CAM.9652
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