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This Landsat image from 6 September 2010 shows a small part of the
intertidal Wadden Sea and two shallow, artificial lakes in the
Netherlands. Visible in the image is the Afsluitdijk – a causeway that
creates a division between the Wadden Sea to the north and the former
Zuiderzee bay to the south. After the dike was built, the Dutch were
able to reclaim land from the sea – like the lighter coloured areas in
the lower-central part of the image. Zooming in, we can see the
patchwork of agricultural land plots.
ESA supports the Landsat series as a Third Party Mission, meaning it
uses its ground infrastructure and expertise to acquire, process and
distribute Landsat data to users. Credits: USGS/ESA
Cut off from the Wadden Sea by a causeway, the shallow IJsselmeer lake is lined by dikes that protect the surrounding land from rising water levels.
In a recently completed Terrafirma study, the IJsselmeer dikes were checked using Envisat radar data for the period 2003–10.
Results show that a large stretch of the dike near the town of Medemblik is subsiding up to 5 mm per year.
These numbers are normal for dikes with recent reconstruction works.
Other areas also show some subsidence, but overall the dikes appear
stable.
The study was just the first step in a project that combines satellite
data, information on subsurface structure and the knowledge of dike
managers for the early detection of weak spots in dikes.
Dike management authorities Wetterskip Fryslân and Hoogheemraadschap
Hollands Noorderkwartier are enthusiastic about the first results
generated by the project.
“For us, the benefit of satellite monitoring is that it tracks down
small anomalies that we can’t see with the naked eye,” said Fryslân
water authority manager Harry Boon.
“This is a highly promising approach, and a valuable addition to our usual physical inspections.”
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Along the Netherlands’ IJsselmeer dikes, Envisat’s radar detected subsidence of 5 mm per year (in red) during 2003–10.
Credits: GMES/Terrafirma; Envisat ASAR data: ESA.
In a more recent way of processing satellite radar images called
Persistent Scatterer Interferometry (PSI), movements over wide areas can
be detected and monitored with even greater sensitivity.
PSI typically works best with hard structures such as buildings, roads, railways or dikes with a hard cover.
This technique is therefore particularly useful in monitoring stability
and tracing weak spots in dikes with a hard cover, like stone or
asphalt.
Roald van Gameren, a dike manager with Hoogheemraadschap Hollands
Noorderkwartier, says that the technology has already proven its worth
during a previous study looking at the Hondsbossche en Pettemer Sea
Dike.
“The results show that satellite observations are very useful for
designing dike upgrades, for testing dikes and for detecting
instability.
“The results also show that the data density is still too low for
practical purposes when it comes to grass dikes. We see this as an
avenue for improvements to the technology.”
In 2013, ESA plans to launch the first satellite of the Sentinel
missions. Owing to the Sentinels’ high revisit rate over the
Netherlands, more data will be available on the dikes.
The satellites are planned to make several passes over the dikes each
week. After every series of passes, new products can be produced on the
dikes’ status, helping managers to decide where additional inspections
are needed, or where maintenance has the highest priority.
The Sentinels are being developed for Europe’s Global Monitoring for Environment and Security (GMES) programme.
ESA
Guillermo Gonzalo Sánchez Achutegui
ayabaca@gmail.comayabaca@hotmail.comayabaca@yahoo.com
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