[1] | Montanari, A., Nguyen, H., Rubinetti, S., Ceola, S., et al. (2023). Why the 2022 Po River drought is the worst in the past two centuries. Sci Adv. 9, eadg8304. |
[2] | Varlas, G., Pytharoulis, I., Steeneveld, G.J., Katsafados, P., and Papadopoulos, A. (2023). Investigating the impact of sea surface temperature on the development of the Mediterranean tropical-like cyclone “Ianos” in 2020. Atmos Res. 291, 106827. |
[3] | Qiu, J., Cao, B., Park, E., Yang, X., et al. (2021). Flood monitoring in rural areas of the Pearl River Basin (China) using Sentinel-1 SAR. Remote Sens. 13, 1384. |
[4] | Xu, H. (2006). Modification of Normalised Difference Water Index (NDWI) to enhance open water features in remotely sensed imagery. Int. J. Remote. Sens. 27, 3025−3033. |
[5] | Ashoor, A.A.R. (2022). Estimation of the surface runoff depth of Wadi Derna Basin by integrating the geographic information systems and Soil Conservation Service (SCS-CN) model. J. Pure. Appl. Sci. 21, 90−100. |
Qiu J., Zhao W., Brocca L., et al., (2023). Storm Daniel revealed the fragility of the Mediterranean region. The Innovation Geoscience 1(3), 100036. https://doi.org/10.59717/j.xinn-geo.2023.100036 |
(a) Rainfall monitoring using GPM; (b) Flood monitoring in Thessaly region using S1 images from Sep 6th to 7th and L8 images on Sep 8th; (c) Flood monitoring in Libya using S2 images; (d) VHR image in Derna before the flood; (e) VHR image in Derna after the flood. GPM, S1, S2, L8, and ESA WorldCover 10m 2021 data were obtained from the Google Earth Engine platform.