Spatial Heterogeneity of Uplift Pattern in the Western European Alps
Revealed by InSAR Time-Series Analysis
Abstract
The Western European Alps display measurable surface deformation rates
from levelling and GNSS data. Based on the time-series analysis of 4
years of Sentinel-1 data, we propose for the first time an InSAR-based
mapping of the uplift pattern affecting the Western Alps on a
~350x175- km-wide area. This approach provides a denser
spatial distribution of vertical motion despite the high noise level
inherent to mountainous areas and the low expected deformation signal.
Our results show consistency with other geodetic measurements at the
regional scale, and reveal smaller-scale spatial variations in the
uplift pattern. Higher uplift rates are found within the external
crystalline massifs compared to surrounding areas, in agreement with the
variations expected from recent deglaciation and long-term exhumation
data. This work brings the first InSAR-based geodetic clue of
differential uplift within the Alpine belt in response to the surface
and deep processes affecting the belt.