Most of the attenuation is in the winter-months, which for this part of Norway and this elevation is from November to March.

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Ground-Based Differential Interferometric Radar Monitoring of Unstable Mountain Blocks in a Coastal Environment.

Received: 27 April 2018 Revised: 1 June 2018 Accepted: 5 June 2018 Published: 9 June 2018.

The circle to the left marks the location of the radar, and the 6 circles to the right marks the monitored mountain area.

There are three sites in the mountain with two reflectors at each.

The numbering of the six reflectors is indicated below each reflector.

The triangular corner reflectors are located from 740 to 1000 m AMSL.

The three areas (Sites 13) are marked with white circles.

Site 1, showing the vertical fault and the location of reflector 1 and 2.

Reflector 1 is the main reflector, and 2 is the reference reflector.

The white arrow indicates the anticipated motional direction of the block.

The pressure is kept constant at 1013.25 mbar.

The International Standard Atmosphere according to ISO 2314 is marked with a red cross-hair (The ISO 1314 Standard Atmosphere is defined as Temperature 15C, Humidity 60 and Pressure 1013.25 mbar at Sea Level).

Radar 10 Crack