Select Northern Hemisphere Glacier Velocity Maps Using Customized autoRIFT and PlanetScope Imagery, Version 1
Data set id:
NSIDC-0801
DOI: 10.5067/VHFVXHZHOO6P
This is the most recent version of these data.
Version Summary
Version Summary
Initial release
Overview
This data set consists of velocity maps and error estimates for five surge-type glaciers: Nàłùdäy/Lowell Glacier, Canada; Medvezhiy Glacier, the Pamir mountains; South Rimo Glacier, the Karakoram; Sít' Kusá Glacier, Alaska; and Aavatsmarkbreen Glacier, Spitsbergen, Svalbard.
The maps are generated using CautoRIFT, a pipeline that improves temporal coverage during periods of rapid glacier motion by adding pre-processed, daily high-resolution PlanetScope images and customized feature tracking parameters for each glacier to NASA's autonomous Repeat Image Feature Tracking (autoRIFT) algorithm for Sentinel-2 and Landsat imagery.
Stable surface masks, area of interest (AOI) and glacier outlines, and ancillary data are also available for each glacier site.
Parameter(s):
ICE VELOCITY
Platform(s):
LANDSAT-8
LANDSAT-9
PlanetScope
Sentinel-2A
Sentinel-2B
Sensor(s):
OLI
OLI-2
PS2
PS2.SD
PSB.SD
Sentinel-2 MSI
Data Format(s):
GeoTIFF
Shapefile
CSV
Temporal Coverage:
- 5 March 2019 to 26 December 2022
- 18 March 2019 to 31 December 2022
- 16 January 2020 to 16 October 2021
- 10 March 2020 to 28 September 2021
- 19 January 2021 to 27 November 2022
Temporal Resolution:
- Varies
Spatial Resolution:
- 100 m
- 100 m
Spatial Reference System(s):
- WGS 84 / UTM zone 7NEPSG:32607
- WGS 84 / UTM zone 8NEPSG:32608
- WGS 84 / UTM zone 33NEPSG:32633
- WGS 84 / UTM zone 42NEPSG:32642
- WGS 84 / UTM zone 43NEPSG:32643
Spatial Coverage:
- N:78.7800952S:78.6133048E:12.7046985W:11.5497732
- N:60.4731365S:60.1011977E:-137.8206057W:-138.6933945
- N:38.7041022S:38.6037845E:72.2802216W:72.1118897
- N:60.2800575S:59.9016126E:-139.4144551W:-140.175999
- N:35.4419895S:35.2267909E:77.6655226W:77.3183406
Blue outlined yellow areas on the map below indicate the spatial coverage for this data set.
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