scholarly journals Multi-hazard assessment in Europe under climate change

2016 ◽  
Vol 137 (1-2) ◽  
pp. 105-119 ◽  
Author(s):  
Giovanni Forzieri ◽  
Luc Feyen ◽  
Simone Russo ◽  
Michalis Vousdoukas ◽  
Lorenzo Alfieri ◽  
...  
2020 ◽  
Vol 147 ◽  
pp. 105765 ◽  
Author(s):  
Amirhossein Shadmehri Toosi ◽  
Shahab Doulabian ◽  
Erfan Ghasemi Tousi ◽  
Giancarlo Humberto Calbimonte ◽  
Sina Alaghmand

Author(s):  
Edier Vicente Aristizábal Giraldo ◽  
Edwin García Aristizábal ◽  
Roberto Marín Sánchez ◽  
Federico Gómez Cardona ◽  
Juan Carlos Guzmán Martínez

Landslides triggered by rainfall are one of the most frequent causes of disasters in tropical countries and mountainous terrains. Recent studies show an upsurge in landslide occurrence as an expected impact of human-induced climate change. This paper presents the analysis and implementation of two different physically-based models, SHALSTAB and TRIGRS, to evaluate the effect of rainfall on landslide hazard assessment in the north-western Colombian Andes. Intensity-Duration-Frequency curves were used in climate change scenarios for different return periods. According to the results, although higher rainfall intensities increase, landslide occurrence does not escalate in a direct or proportional relationship. Considering a steady infiltration process (SHALSTAB), the results show an expansion of d unstable areas, compared with a transient infiltration process (TRIGRS). A greater influence of rainfall duration instead of rainfall intensity was observed. The results highlight the need for studies that incorporate the scenarios of variability and climate change in the hazard assessment and land planning in the long term.


2020 ◽  
Vol 125 (18) ◽  
Author(s):  
Pengcheng Xu ◽  
Dong Wang ◽  
Vijay P. Singh ◽  
Huayu Lu ◽  
Yuankun Wang ◽  
...  

2015 ◽  
Vol 160 ◽  
pp. 106-117 ◽  
Author(s):  
Won-Ho Nam ◽  
Michael J. Hayes ◽  
Mark D. Svoboda ◽  
Tsegaye Tadesse ◽  
Donald A. Wilhite

2022 ◽  
Vol 94 ◽  
pp. 102152
Author(s):  
Abdul Kadir Alhamid ◽  
Mitsuyoshi Akiyama ◽  
Hiroki Ishibashi ◽  
Koki Aoki ◽  
Shunichi Koshimura ◽  
...  

Author(s):  
M. A. Gusyev ◽  
Y. Kwak ◽  
M. I. Khairul ◽  
M. B. Arifuzzaman ◽  
J. Magome ◽  
...  

Abstract. This study introduces a flood hazard assessment part of the global flood risk assessment (Part 2) conducted with a distributed hydrological Block-wise TOP (BTOP) model and a GIS-based Flood Inundation Depth (FID) model. In this study, the 20 km grid BTOP model was developed with globally available data on and applied for the Ganges, Brahmaputra and Meghna (GBM) river basin. The BTOP model was calibrated with observed river discharges in Bangladesh and was applied for climate change impact assessment to produce flood discharges at each BTOP cell under present and future climates. For Bangladesh, the cumulative flood inundation maps were produced using the FID model with the BTOP simulated flood discharges and allowed us to consider levee effectiveness for reduction of flood inundation. For the climate change impacts, the flood hazard increased both in flood discharge and inundation area for the 50- and 100-year floods. From these preliminary results, the proposed methodology can partly overcome the limitation of the data unavailability and produces flood~maps that can be used for the nationwide flood risk assessment, which is presented in Part 2 of this study.


2021 ◽  
Author(s):  
Matilde García-Valdecasas Ojeda ◽  
Erika Coppola ◽  
Fabio Di Sante ◽  
Francesca Raffaele ◽  
Rita Nogherotto ◽  
...  

<p>A common way to study the impact of climate change on water resources is through hydrological models fed by precipitation from global or regional climate models (GCMs and RCMs, respectively). However, precipitation from climate models is usually affected by systematical biases that may produce inadequate streamflow estimations. For this reason, users find it necessary to apply some bias-corrected technique to reduce errors in precipitation before its use in hydrological simulations. Among the different methods, quantile mapping (QM) is a widely used method as it has shown satisfactory results for historical conditions.</p><p>In recent years, several studies have investigated the QM method, with a focus on mean precipitations. However, it remains quite uncertain how bias-corrected precipitation modifies river discharges, particularly the extreme discharges on a sub-daily timescale. In this framework, this study aims to quantify differences between simulated river discharges using corrected and uncorrected precipitation to feed a hydrological model in the context of flood hazard assessment in Italy.</p><p>To adequately estimate flood events, high spatiotemporal resolution data are required. Therefore, sub-daily precipitation outputs from the ICTP RegCM Regional Climate Model driven by the HadGEM2-ES model at 12 km were contemplated in this study. Precipitation outputs for the period 1976-2100 were bias-corrected concerning the observations from GRIPHO, which is a high-resolution observational product. Then, bias-corrected and uncorrected precipitations were used to feed the CETEMPS Hydrological Model (CHyM) completing thus, a set of hydrological simulations covering the entire Italian Territory, in both present-day and future conditions. Analyses focused on the comparison between simulated and observed discharges for present-day conditions, but also on the comparison between corrected and uncorrected values ​​in the future.</p><p>The results of this study could provide valuable information on whether the use of the QM method is appropriate for studying extreme discharges on a sub-daily scale, an essential issue for assessing the impacts of climate change on extreme hydrological events.</p><p><strong>Keywords</strong>: flood hazard assessment, quantile delta mapping, CHyM model, RegCM model, Italy</p><p><strong>Acknowledgments</strong>: The research reported in this work was supported by OGS and CINECA under HPC-TRES program award number 2020-02.</p>


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