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During the first couple of decades of our professional life we have worked extensively with landslides risk assessment and monitoring in the European Alps, mostly in Switzerland and Italy.
At the beginning “risk” was not yet the buzz-word it became later. Clients and governments were seeing hazards impinging on population and infrastructure like transportation, hydropower and bulk-storage facilities. Engineering “repairs” were the most obvious paths.
Nevertheless, in 1997 Riskope’s founder Franco Oboni participated in an IUGS workshop in Honolulu. The goal of the event was to define a glossary of risk-related technical terms specific to slopes and landslides. In short, the IUGS Working Group on Landslides, Committee on Risk Assessment, produced a glossary for quantitative risk assessment for slopes and landslides. The glossary of risk-related technical terms has continued to evolve. It is now applicable to other fields of business and industries and the latest version is freely available online.
Discussing landslides risk assessment and monitoring
Today we return to our “first love” to discuss a few points related to landslides risk assessment and monitoring.
One of our latest books is:
And our chapter in that book is “Holistic geoethical slope portfolio risk assessment”. We endeavour to show how sustainability and ethics can be fostered by using rational, repeatable, transparent quantitative risk assessment applicable at the local scale as well as on a large scale. Among the case histories we present, one deals with the Cassass landslide in North Western Italy.
A few references on the Cassass landslide
Before the book cited above came out, we published various papers on the Cassass Landslide and the studies we performed. The related references below in chronological order.
Space observation new tools
At Riskope we have used space observation results such as:
for a number of cases in the mining industry and landslides and/or man-made slopes. Here are a couple of references.
In those papers we already cautioned users on a few issues we have encountered. Happily, we were working with experienced and friendly suppliers that not only helped us solve the issues, but also pointed out possible “traps”, potentially leading to hazardous misinterpretations.
So, we approached with keen interest the newly published and publicly available European Ground Motion (EGM portal https://land.copernicus.eu/pan-european/european-ground-motion-service manual: https://land.copernicus.eu/user-corner/technical-library/egms-end-user-interface-manual ).
We looked at the Cassass Landslide (Loc 45.06567, 6.90520) between the beginning of November 2016 and November 2020.
The image below shows an example of the results the platform delivered.
Comments on the results
On one hand, we are satisfied for having mitigated the sliding activity to such an extent, but on the other we have to admit we do not really believe these results. Too little yearly average movement, not enough “red dots” on the slope! Indeed, the original slope had spikes at more than 10cm/yr and was moving “en masse”, of course with significant variabilities across and along its surface.
So we asked the publisher of the EGM a couple of questions which unfortunately remain to this date unanswered. We hope 2023 will bring some replies on this subject.
We then asked Paolo Mazzanti, who is a specialist of SAR Interferometry and PhotoMonitoring technologies. His reply confirmed our views. We summarize it as follows:
Closing remarks on landslides risk assessment and monitoring
At the end of the day, a large scale publicly available platform like EGM should be used with care and its limits should be recognized to avoid blunders.
It is possible to seamlessly link advanced land-based monitoring devices, space observation tools and other imagery results with quantitative risk analysis of slopes.
In order to avoid the surprise effects of extreme events and climate change the quantitative risk assessments should include projections based on the best available data and predictions.