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Greenland Ice Mapping Project: Ice Flow Velocity Variation at sub-monthly to decadal time scales
Ian Joughin1, Ben E Smith1, Ian Howat2
1Polar Science Center, Applied Physics Lab, University of Washington, 1013 NE 40th St., Seattle, WA 98105-6698, USA.
New ice velocity maps from the Greenland Ice Mapping Project (GIMP) reveal significant changes in glacier speeds. Jakobshavn Isbrae slowed in 2017, while other Greenland glaciers show regional speedup trends.
Area of Science:
- Glaciology
- Remote Sensing
- Climate Science
Background:
- The Greenland Ice Mapping Project (GIMP) has been instrumental in monitoring ice sheet dynamics.
- Understanding ice velocity is crucial for predicting sea-level rise.
Purpose of the Study:
- To present new ice velocity maps for Greenland using Landsat 8 and Copernicus Sentinel 1A/B data.
- To analyze changes in ice flow at specific sites and across broader regions of Greenland since 2000.
Main Methods:
- Utilized Landsat 8 and Copernicus Sentinel 1A/B satellite data to create ice velocity maps.
- Compared new velocity data with historical GIMP data dating back to 2000.
- Analyzed regional speedup trends and winter flow speed changes across Greenland's ice sheet.
Main Results:
- Jakobshavn Isbrae exhibited a substantial slowdown starting in 2017.
- Koge Bugt experienced two major slowdown events coinciding with terminus advances.
- Glaciers in northwest and southwest Greenland collectively continue to accelerate, with regional variations in peak speedup timing.
- Little statistically significant change was found in winter flow speeds along much of the southwest margin.
Conclusions:
- Ice velocity in Greenland shows complex behaviors, including localized slowdowns and regional accelerations.
- Satellite data consistency is generally good, but sensor resolution impacts accuracy in high strain rate areas.
- Users of GIMP data should consider sensor resolution effects for applications like model inversions.
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