Landsat Images showing Ice Scours in the Caspian Sea
Image 1: This is a Landsat 8 image of the Caspian sea
acquired on April 16th, 2016. The image clearly shows a strange
seabed scouring phenomena in the region of Tyuleni Archipelago (the light
colored lines that break up the darker green vegetation visible on the seabed).
One thing that makes them curious is that groups of scours are often parallel
to each other and appear to be formed by objects traveling in the same
direction. The initial cause of these features was confusing to analysts, one
possible proposal is that they were human in origin - the result of seafloor
trawling. It was not until this image was compared to the second image, taken
in January, that the origin of the scours was identified as gouging caused by
sea ice starting to break up.
Image 2: A Landsat 8 image that shows the same region in
winter. In the northeastern portion of the image the ice is starting to break
up and it is possible to see the scour marks which occur behind the leading
edge of shrinking ice floes. This occurs because the Caspian sea is very shallow
and the sea ice that develops there is relatively warm and thin. This means the
ice pieces are easily moved by wind and currents and are often pushed together,
causing some of them to tilt, forming structures called “hummocks.” In the
shallow water, the “keels” of these hummocks can become wedged in the sediment,
causing scouring as the ice bed is moved. Once the ice melts, only the scour
marks persist in the spring and summer, creating the pattern seen in the first
image. The parallel nature of groups of lines in the first image can be
explained by several ice pieces all being dragged along a similar path by the
same wind/current.
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