API src

Found 2 results.

Other language confidence: 0.9928877075879629

High-resolution subsidence maps and data for whole Afghanistan, and, in a higher resolution, for Kabul and Ghazni provinces (2015-2022)

We present high-resolution subsidence maps for whole Afghanistan, and, in a higher resolution, for Kabul and Ghazni provinces. These data are complemented by wells water level time-series and precipitation data of Kabul, and time-series of mapped solar panel arrays, mapped Kariz networks, mapped desiccation cracks of 2022, and the Normalized Difference Vegetation Index (NDVI) of Ghazni province. The subsidence maps result from a small-baseline (SBAS) time-series analysis (Lazecky et al., 2020; Morishita et al., 2020; Yunjun et al., 2019) of ~7 years of freely available Sentinel-1 radar data. The monthly wells water level time-series 2013-2022 were digitized from the log data of the Afghan Ministry of Water and Energy. The NDVI data 2015-2022 were derived from Sentinel-2 optical imagery. The solar panel arrays were mapped on high-resolution online Google Earth Pro imagery data in 2016, 2019 and 2022. More details of data processing and methods can be found in (Kakar et al., 2023), currently under review at AGU Water Resources. The jupyter notebook documents the creation of key figures.

Supplement to: Quantifying groundwater exploitation induced subsidence in the Rafsanjan Plain, southeastern Iran, using InSAR time-series and in situ measurements

This data publication provides supplementary material to Motagh et. al (2017), which presents the results of an InSAR time series analysis obtained by the exploitation of Envisat, ALOS and Sentinel-1 (S1) SAR data archives between June 2004, and May 2016. The study investigates land subsidence due to groundwater overexploitation for agriculture and industrial development in the Rafsanjan plain of southeastern Iran. Datasets included are a list of SAR data used for the study and the Line of Sight (LOS) displacement rates from Envisat, ALOS and Sentinel 1 (S1) satellites in ASCII format. More in formation is avalable in Motagh-et-al-2017-Supplementary_Material_readme.pdf.

1