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ITS_LIVE Python Library Demo: Time Series of Ice Flow Speed at a Point

ITS_LIVE (Intermission Time Series of Land Ice Velocity and Elevation, http:itslive.jpl.nasa.gov) maintains an archive of ice flow speeds for glaciers and ice sheets. These speeds are determined from pairs of satellite images by tracking how far features move from the first image in a pair to the second image in a pair.

As a result, the time series of ice motion at a single location on a glacier consist of measurements of the average speed of the ice at that point over the time interval between the two images used. In the plot generated below, color represents the time separation of the two images used (also visible as the length of the line segment for each point), the vertical position of that line segment shows the average speed over that interval in meters per year, and dates of the two images determine the start and end points of the line segment.

<Figure size 1600x1000 with 2 Axes>

The time series is too long for this plot to show all the detail, so we replot it below but limit it to 2018-2023

(17532.0, 19358.0)
<Figure size 1600x1000 with 2 Axes>

Shorter (blue) line segments are from image pairs only separated in time by a few to a few tens of days. These shorter segments can reveal rapid transients in ice flow speed due to rain storms or strong melt events.

Longer segments (red in this plot) average out these transients, but provide a less noisy picture of ice flow speed.

Note that we have selected 90 days as the longest time interval shown in this plot (max_dt = 90 above) - ITS_LIVE processes image pairs out to 545 days time separation, which can provide longer-term average ice flow speed, but the ability to track features over longer times successfully is limited by changes in the surface of the ice, so the numer of longer time measurements is significantly smaller than the shorter intervals.