@article{fdi:010079035, title = {{M}apping rainstorm erosion associated with an individual storm from {I}n{SAR} coherence loss validated by field evidence for the {A}tacama {D}esert}, author = {{C}abre, {A}. and {R}{\'e}my, {D}ominique and {A}guilar, {G}. and {C}arretier, {S}{\'e}bastien and {R}iquelme, {R}.}, editor = {}, language = {{ENG}}, abstract = {{E}xtreme high-magnitude and low-frequency storm events in arid zones provide the necessary runoff to entrain sediments from source areas and therefore dictate the linkages between hillslopes and channels. {N}evertheless, the erosive impact of large storms remains difficult to predict. {M}ost of the uncertainty lies in the lack of topographic change maps associated with single hydro-meteorological events. {C}onsequently, event-based erosion models are poorly constrained and their extrapolation over long time periods remains uncertain. {I}n this study, a 15-month {S}entinel-1{A} coherence time series, optical and field data are used to map the spatial patterns of erosion after the 5-day storm occurred on {M}arch 2015, in the {A}tacama {D}esert. {T}he coherence change detection ({CCD}) analysis suggests that temporal loss of coherence is related to variations in soil moisture, while permanent loss of coherence is related to modification of soil texture by erosion and sedimentation. {I}mportantly, permanent loss of coherence is more apparent on gentle rather than steeper slopes, likely reflecting differences in regolith cover and thickness. {T}hese findings can contradict the landscape models predicting higher erosion on steeper hillslopes. {T}he {CCD} technique represents a promising tool for analysing and modelling sediment connectivity in arid areas, giving a clear picture of the relation between sediment sources and sink pathways.}, keywords = {erosion ; coherence loss ; flash floods ; sediment connectivity ; {I}n{SAR} ; {CHILI} ; {ATACAMA} ; {ATACAMA} {DESERT}}, booktitle = {}, journal = {{E}arth {S}urface {P}rocesses and {L}andforms}, volume = {45}, numero = {9}, pages = {2091--2106}, ISSN = {0197-9337}, year = {2020}, DOI = {10.1002/esp.4868}, URL = {https://www.documentation.ird.fr/hor/fdi:010079035}, }