Pine Island Glacier rift: 50,000,000 Elvis Fans Can’t Be Wrong

The rift of Pine Island glacier was captured by Sentinel-2A several times since Sentinel-2A is watching Antarctica. However I was not sure if the crack was growing by looking at the images only.

The answer is not obvious from a simple image comparison since this part of the glacier is moving at 10 m per day in summer. The best solution would be to use a GIS software and digitalize the whole crack to compute its length [1] … but my PhD students were already busy. So I made this small online survey. The participants were asked to choose the image which they think has the longest rift without knowing the acquisition dates. The result are unambiguous. The most recent image was selected by 95% of the 63 voters. This means that the rift is actually expanding… unless you think that argumentum ad populum is not a definitive proof of scientific truth?

 In the same period the western part also seems to have expanded a little.

Update: a more recent image acquired on Jan 06 shows that the crack is now opening faster in the west (click on the image below to see the animation)

 Footnote:[1] See this other disturbing rift in the Larsen C ice shelf, which is now making the headlines https://youtu.be/Sf8kedzFLGI

Plus d'actualités

Autumn snow drought on Mount Damavand

« We are currently experiencing the driest autumn the country has experienced in 50 years » said Iran’s meteorological organisation. Near Tehran, Mount Damavand, the highest peak in Iran (5609 m) was reported to be « unusually bare of snow ». I checked this statement using my MODIS snow cover data processing algorithm implemented in Google Earth Engine (Gascoin […]

IOTA2 software mailing list

Hello everyone, We have just created a mailing list for users of the IOTA2 software (iota2 — iota2 documentation). The tool will undergo significant developments in the coming months, and the purpose of this list is to communicate with the community to support these changes and to maintain the processing workflows needed by the users. […]

Evolution des glaciers du Vignemale sous l’œil des satellites Pléiades (2013-2025)

Grâce à DINAMIS, un couple d’images stéréoscopiques a été acquis par Pléiades 1B le 14 septembre 2025. Le modèle numérique de surface (MNS) produit à partir de ces images peut être comparé à un autre MNS de septembre 2013 produit à partir des images Pléiades 1A commandées par Marti et al. (2014). Le glacier d’Ossoue […]

Rechercher