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Journal articles on the topic 'Torrential processe'

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1

Marchi, Lorenzo, and Sylvie Brochot. "Les cônes de déjection torrentiels dans les Alpes françaises. Morphométrie et processus de transport solide torrentiel." Revue de géographie alpine 88, no. 3 (2000): 23–38. http://dx.doi.org/10.3406/rga.2000.2999.

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2

Ballandras, Stéphane. "Le « Remblaiement Historique » dans les bassins versants torrentiels des Alpes françaises/The « historical filling-up » in torrential catchments of French Alps." Géomorphologie : relief, processus, environnement 4, no. 1 (1998): 65–77. http://dx.doi.org/10.3406/morfo.1998.942.

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3

Burtin, Arnaud, Niels Hovius, and Jens M. Turowski. "Seismic monitoring of torrential and fluvial processes." Earth Surface Dynamics 4, no. 2 (2016): 285–307. http://dx.doi.org/10.5194/esurf-4-285-2016.

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Abstract. In seismology, the signal is usually analysed for earthquake data, but earthquakes represent less than 1 % of continuous recording. The remaining data are considered as seismic noise and were for a long time ignored. Over the past decades, the analysis of seismic noise has constantly increased in popularity, and this has led to the development of new approaches and applications in geophysics. The study of continuous seismic records is now open to other disciplines, like geomorphology. The motion of mass at the Earth's surface generates seismic waves that are recorded by nearby seismo
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4

Kovačević-Majkić, Jelena, Dragoljub Štrbac, Jelena Ćalić, Marko V. Milošević, Milovan Milivojević, and Siniša Polovina. "Fluvial processes and landforms as indicators in torrential flood hazard assessment." GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY 17, no. 4 (2025): 26–34. https://doi.org/10.24057/2071-9388-2024-3378.

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Torrential flood hazard assessment is always a challenge, especially if the aim is to do it on the level of the whole watershed. When there are no required data available, there are traces in nature, morphological indicators, that show the extent of previous floods, in period longer then instrumental period. Therefore, in this paper we deal with fluvial and slope both erosional and accumulation processes and landforms, which doubtlessly indicate torrential flood prone areas. We have selected eight indicators and grouped them into three segments: erosional process, morphometric characteristics
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5

Sodnik, Jošt, Matjaž Mikoš, and Nejc Bezak. "Torrential Hazards’ Mitigation Measures in a Typical Alpine Catchment in Slovenia." Applied Sciences 13, no. 20 (2023): 11136. http://dx.doi.org/10.3390/app132011136.

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Different sediment-related disasters due to torrential hazards, such as flash floods, debris flows, and landslides, can occur in an Alpine torrential catchment. When protecting infrastructure and human lives, different structural and non-structural protection measures can be used to mitigate permanent and future risks. An overview of the mitigation measures constructed near the Krvavec ski resort in northwest Slovenia (Central Europe) is presented. In May 2018, an extreme debris flood occurred in this area, causing significant economic damage. After the May 2018 event, different field investig
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6

Hübl, Johannes. "Conceptual Framework for Sediment Management in Torrents." Water 10, no. 12 (2018): 1718. http://dx.doi.org/10.3390/w10121718.

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Torrential catchments are complex systems showing a huge diversity of sediment and flow regime reactions. Therefore, it seems reasonable to decrease the complexity by introducing a conceptual framework to obtain a general idea of the torrential system’s behavior. The aim of the manuscript is to provide a conceptual framework and a stepwise procedure to develop a reproducible sediment management concept. This involves starting with a definition of torrential process types. These processes are then routed through the drainage system, which is divided into homogeneous reaches. Each reach transfer
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7

Coviello, V., M. Arattano, and L. Turconi. "Detecting torrential processes from a distance with a seismic monitoring network." Natural Hazards 78, no. 3 (2015): 2055–80. http://dx.doi.org/10.1007/s11069-015-1819-2.

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8

Huang, Yongjie, and Xiaopeng Cui. "Dominant cloud microphysical processes of a torrential rainfall event in Sichuan, China." Advances in Atmospheric Sciences 32, no. 3 (2015): 389–400. http://dx.doi.org/10.1007/s00376-014-4066-7.

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9

Garitte, Gilles, and Philippe Lahousse. "Contribution à l'évaluation de l'aléa torrentiel dans le bassin versant du Riou Chanal (Alpes-de-Haute-Provence, France) / Contribution to the torrential hazard assessment in the Riou Chanal catchment area (Alpes-de Haute-Provence, France)." Géomorphologie : relief, processus, environnement 8, no. 1 (2002): 61–70. http://dx.doi.org/10.3406/morfo.2002.1128.

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10

Kummert, Mario, and Reynald Delaloye. "Regional-scale inventory of periglacial moving landforms connected to the torrential network system." Geographica Helvetica 73, no. 4 (2018): 357–71. http://dx.doi.org/10.5194/gh-73-357-2018.

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Abstract. When connected to torrential channels, periglacial moving landforms (including rock glaciers, push moraines and high-altitude landsliding masses) may constitute important active sediment sources for gravitational and torrential transfer processes such as debris flows. However, still very little is known about the location and the number of such types of sedimentary connection in given regions, as well as about the typical sediment transfer rates that can be expected. Therefore, this contribution aims at (i) describing a new methodology developed to identify and characterize moving la
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11

Mao, Jiahua, Fan Ping, Lei Yin, and Xinfa Qiu. "A Study of Cloud Microphysical Processes Associated With Torrential Rainfall Event Over Beijing." Journal of Geophysical Research: Atmospheres 123, no. 16 (2018): 8768–91. http://dx.doi.org/10.1029/2018jd028490.

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12

Hürlimann, Marcel, Vicente Husmann, Roger Ruiz-Carulla, Laura Molano, and José Moya. "Monitoring and modelling of debris-flow erosion in the Rebaixader catchment (Pyrenees, Spain)." E3S Web of Conferences 415 (2023): 03011. http://dx.doi.org/10.1051/e3sconf/202341503011.

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Debris flow and other torrential processes can entrain large volumes of sediments along their runout path. Since the debris-flow hazard strongly depends on the volume, the research on the entrainment is relevant and has been analysed by multiple approaches in the past. In this study, the erosion volume due to torrential processes has been monitored in the Rebaixader catchment (Spain) by digital elevation models obtained from Uncrewed Aerial Vehicle (UAV) surveys and by the instrumental monitoring system installed in the channel reach. In addition, the entrainment of debris flows has been model
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13

Mară, M., and Oana Dârlău. "Types and Forms of Relief on Gherasim Torrential Valley, Târgu Ocna." Present Environment and Sustainable Development 8, no. 2 (2014): 209–24. http://dx.doi.org/10.2478/pesd-2014-0036.

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Abstract The present study brings new data regarding the landforms occurring on gypsum rocks through the action of denudation processes. The landforms signaled complement the domain literature with natural dams, vertical shafts and reappearing springs, developed at the contact between the Subcarpathians and Berzunţi Mts. The presence of the gypsum dam has slowed down the intensity of erosion processes upstream, in comparison to the neighboring valleys. The analyzed area has also an educational importance, offering sufficient objectives for the knowledge of the local characteristics or for fiel
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14

Di Bella, Letizia, Martina Pierdomenico, Cristiano Bove, Daniele Casalbore, and Domenico Ridente. "Benthic Foraminiferal Response to Sedimentary Processes in a Prodeltaic Environment: The Gulf of Patti Case Study (Southeastern Tyrrhenian Sea)." Geosciences 11, no. 5 (2021): 220. http://dx.doi.org/10.3390/geosciences11050220.

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Analyses of benthic foraminiferal assemblages were carried out on sediment samples collected in the Gulf of Patti (NE Sicily, Tyrrhenian Sea), where high sedimentation rates in front of the Mazzarrà River led to the growth of a prodelta. The frequency of riverine sedimentary fluxes is testified by the widespread occurrence of erosional and depositional bedforms indicative of high-energy processes on the prodelta slope.The frequency of riverine sedimentary fluxes suggests the widespread occurrence of erosional and depositional bedforms indicative of high-energy processes on the prodelta slope.
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15

Ristic, Ratko, Boris Radic, Zoran Nikic, et al. "Erosion control and protection from torrential floods in Serbia-spatial aspects." Spatium, no. 25 (2011): 1–6. http://dx.doi.org/10.2298/spat1125001r.

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Torrential floods represent the most frequent phenomenon within the category of ?natural risks? in Serbia. The representative examples are the torrential floods on the experimental watersheds of the rivers Manastirica (June 1996) and Kamisna (May 2007). Hystorical maximal discharges (Qmaxh) were reconstructed by use of ?hydraulics flood traces? method. Computations of maximal discharges (Qmaxc), under hydrological conditions after the restoration of the watersheds, were performed by use of a synthetic unit hydrograph theory and Soil Conservation Service methodology. Area sediment yields and in
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16

MARINESCU, Emil, and Oana MITITELU-IONUȘ. "Correlations between the hydrological regime and the morphodynamic processes in the Gilort river basin." Annals of the University of Craiova Series Geography 23, no. 1 (2022): 5–20. http://dx.doi.org/10.52846/aucsg.23.1.01.

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This study highlights the relationship between the dynamics of the hydrological regime in a river basin and the morphodynamic potential that appears in the context of increasing frequency and intensity of current climatic phenomena. Climate change characterized by the high frequency and intensity of torrential rains and floods, especially in the last decade, with a maximum amplitude in the summer months (June-July), alternating with periods of drought have brought to a series of geomorphological changes in the Gilort river basin. These processes are amplified by the high degree of fragmentatio
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17

Kostadinov, Stanimir, Slavoljub Dragićević, Tomislav Stefanović, Ivan Novković, and Ana M. Petrović. "Torrential flood prevention in the Kolubara river basin." Journal of Mountain Science 14, no. 11 (2017): 2230–45. http://dx.doi.org/10.1007/s11629-017-4575-9.

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18

Wang, Shuaiwei, Weichao Sun, Xiuyan Wang, Lin Sun, and Songbo Liu. "The Role of Geological Methods in the Prevention and Control of Urban Flood Disaster Risk: A Case Study of Zhengzhou." Applied Sciences 14, no. 5 (2024): 1839. http://dx.doi.org/10.3390/app14051839.

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The frequent occurrence of urban flood disasters is a major and persistent problem threatening the safety of cities in China and elsewhere in the world. As this issue is so pervasive, exploring new methods for more effective risk prevention and urban flood disaster control is now being prioritized. Taking the case of the city of Zhengzhou as an example, this paper proposes using geological, hydrogeological, ecological, and environmental conditions together with appropriate engineering designs to address the problem of urban flooding. The strategy includes integrating urban sponge–hydrogeologic
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19

Badea, L., and D. Balteanu. "La movilidad tectonica y los procesos geomorfologicos actuales de los subcarpatos de rumania." Cuadernos de Investigación Geográfica 8 (May 21, 2013): 19–36. http://dx.doi.org/10.18172/cig.893.

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The Subcarpathians of Rumania, integrated by folded neogen molasses associated locally to the paleogenic flysch, are affected by possitive tectonic movements of variable intensity which have an obvious injluence in the present geomorphologic processes in a mild-continental climate. The shaping of the slopes is essentially caused by mass movements (landslides, mud flows) together with intense processes of overland flows. Extreme factors (torrential rainfall, earthquakes) play the most important role in the cause and intensity of mass movements. According to the research carried out we can appre
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20

Shen, Xinyong, Jia Liu, and Xiaofan Li. "Torrential rainfall responses to ice microphysical processes during pre-summer heavy rainfall over southern China." Advances in Atmospheric Sciences 29, no. 3 (2012): 493–500. http://dx.doi.org/10.1007/s00376-011-1122-4.

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21

Costandache, Cristinel, Lucian Dinca, Laurentiu Popovici, and Ciprian Tudor. "The role of forest vegetation in the mitigation of the ecological imbalances resulting from climate change in the Putna-Vrancea river basin." SIMI 2019, Abstract Book, SIMI 2019 (September 20, 2019): 98–106. http://dx.doi.org/10.21698/simi.2019.fp13.

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"Climatic changes displayed through extremes (thermic or hydric) correlated with uncontrolled anthropic interventions exercised over time on land usages are the main factors that emphasize ecological and hydric disequilibrium from the South, East part of Romania. Specific of our country, the torrential precipitation regime generates rapid floods in mountain and hill areas. Torrential and land degrading processes occur on slopes and on the main hydrographic network as a result of torrential runoffs. Their consequences extend on a larger area than the one on which they occur. This happens especi
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22

Luino, F., L. Turconi, G. Paliaga, F. Faccini, and F. Marincioni. "Torrential floods in the upper Soana Valley (NW Italian Alps): Geomorphological processes and risk-reduction strategies." International Journal of Disaster Risk Reduction 27 (March 2018): 343–54. http://dx.doi.org/10.1016/j.ijdrr.2017.10.021.

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23

Xu, Huiyan, Rui Liu, Guoqing Zhai, and Xiaofan Li. "Torrential rainfall responses of Typhoon Fitow (2013) to radiative processes: A three-dimensional WRF modeling study." Journal of Geophysical Research: Atmospheres 121, no. 23 (2016): 14,127–14,136. http://dx.doi.org/10.1002/2016jd025479.

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24

Wang, Pengyun, and Jing Yang. "Observation and Numerical Simulation of Cloud Physical Processes Associated with Torrential Rain of the Meiyu Front." Advances in Atmospheric Sciences 20, no. 1 (2003): 77–96. http://dx.doi.org/10.1007/bf03342052.

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25

Viel, Vincent, Monique Fort, Candide Lissak, et al. "Debris-flow functioning and their contribution to sedimentary budgets: the Peynin subcatchment of the Guil River (Upper Queyras, Southern French Alps)." Landform Analysis 36 (December 30, 2018): 71–84. http://dx.doi.org/10.12657/landfana.036.007.

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The Peynin catchment (15 km2) is prone to catastrophic floods (June 1957 – Recurrence Interval R.I.>100 yr), June 2000 (R.I.-30 yr) with serious damages to infrastructure and buildings located at the outlet. In this paper, PIT tags tracers and Vensim modelling software are used to better assess the sediment delivery unsteadiness, and more specifically to evaluate the respective role of geomorphological processes on sediment supply during flood event. For the last 20 years, our results highlight a significant variability in sediment delivery from a tributary to another one. According to our
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26

Hashimoto, Akihiro, Akira Tai, and Toshimitsu Komatsu. "Clarification and Application of Inundation Processes in Basins with Insufficient Observation Devices Installed." Journal of Disaster Research 10, no. 3 (2015): 495–502. http://dx.doi.org/10.20965/jdr.2015.p0495.

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Torrential rain possibly due to climate change has begun causing disasters annually, with water and sediment resulting from heavy rainfall in relatively narrow upper basins often arising in short periods. Because most of these basins are traversed by class B rivers administered by local governments, data on disasters are not accumulated comprehensively. Targeting the Sumiyo River basin on Amami Oshima Island, this study involved field surveys and numerical simulations to clarify inundation features in areas short on data based on hearings from investigation results. Calculation results have re
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27

Zhou, Yushu, Liping Liu, and Guo Deng. "Comparisons of the Generalized Potential Temperature in Moist Atmosphere with the Equivalent Potential Temperature in Saturated Moist Atmosphere." Advances in Meteorology 2009 (2009): 1–9. http://dx.doi.org/10.1155/2009/105265.

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The real tropospheric atmosphere is neither absolutely dry nor completely saturated. It is in general moist but not saturated. Here the generalized potential temperature (GPT) was introduced to describe this humid feature of real moist atmosphere. GPT's conservation property in moist adiabatic process was discussed and proved. Comparisons of GPT in moist atmosphere with the equivalent potential temperature (EPT) in saturated moist atmosphere were made by analyzing three torrential rain cases occurring over Jianghuai Valleys in 2003, the north China in 2004, and with the typhoon Fung-Wong in 20
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28

Kalińska, Edyta. "The Role of Morphogenetic and Anthropogenic Processes in The Development of Gullies and Methods of Their Prevention (On The Example of The Vicinity of Kazimierz Dolny)." Miscellanea Geographica 12, no. 1 (2006): 103–10. http://dx.doi.org/10.2478/mgrsd-2006-0012.

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Abstract The vicinity of Kazimierz Dolny is characterised by the occurrence of large denivelations and thick loess covers. Due to that, as well as to the characteristic properties of loess and frequent occurrences of torrential rains, the region is marked by numerous dissections by valleys. Not without importance is agriculture, whose intensification brought about the creation of new relief forms. Gully erosion is a serious threat for the inhabitants of the region; on the other hand, it is impossible to eliminate it. For that reason it is necessary to use modern anti-erosion measures.
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29

Kummert, Mario, and Reynald Delaloye. "Mapping and quantifying sediment transfer between the front of rapidly moving rock glaciers and torrential gullies." Geomorphology 309 (May 2018): 60–76. http://dx.doi.org/10.1016/j.geomorph.2018.02.021.

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30

Francos, Marcos, Xavier Úbeda, and Paulo Pereira. "Impact of torrential rainfall and salvage logging on post-wildfire soil properties in NE Iberian Peninsula." CATENA 177 (June 2019): 210–18. http://dx.doi.org/10.1016/j.catena.2019.02.014.

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31

Xu, Huiyan, and Xiaofan Li. "Torrential rainfall processes associated with a landfall of Typhoon Fitow (2013): A three‐dimensional WRF modeling study." Journal of Geophysical Research: Atmospheres 122, no. 11 (2017): 6004–24. http://dx.doi.org/10.1002/2016jd026395.

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32

Gerdjikov, Ianko, Stelian Dimitrov, Zornitsa Dotseva, Martin Iliev, and Dian Vangelov. "Mapping and classification of heavy rainfall-induced hazards in the Petrich town area (SW Bulgaria)." Review of the Bulgarian Geological Society 83, no. 3 (2022): 229–31. http://dx.doi.org/10.52215/rev.bgs.2022.83.3.229.

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The torrential catchments located on the northern slopes of Belasitsa Mountain (SW Bulgaria), in the area of Petrich town were affected by an intense rainfall event in December 2021 that triggered a cascade of hazard processes like floods, landslides, debris flows/floods that caused major damage to the road network, properties, and buildings, showing the urgent need to take hazard and risk assessment and mitigation measures. For assessment purposes, we perform field and UAV-based analysis, and mapping of the affected areas, the geomorphological changes after the flooding event, and the differe
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33

Babič, Matej, Dušan Petrovič, Jošt Sodnik, et al. "Modeling and Classification of Alluvial Fans with DEMs and Machine Learning Methods: A Case Study of Slovenian Torrential Fans." Remote Sensing 13, no. 9 (2021): 1711. http://dx.doi.org/10.3390/rs13091711.

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Alluvial (torrential) fans, especially those created from debris-flow activity, often endanger built environments and human life. It is well known that these kinds of territories where human activities are favored are characterized by increasing instability and related hydrological risk; therefore, treating the problem of its assessment and management is becoming strongly relevant. The aim of this study was to analyze and model the geomorphological aspects and the physical processes of alluvial fans in relation to the environmental characteristics of the territory for classification and predic
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34

Schmucki, Gregor Rafael, Perry Bartelt, Yves Bühler, et al. "Photogrammetrically UAV based terrain data generation and automatic extraction of torrential properties." E3S Web of Conferences 415 (2023): 03026. http://dx.doi.org/10.1051/e3sconf/202341503026.

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Debris flows are a severe hazard in mountainous regions. However, cost-effective long-term studies of debris flows are seldom, which leads to substantial uncertainties in hazard mitigation methods. This paper investigates whether cost-effective remote sensing techniques can be applied to assess the hazards of mountain torrents and to gather accurate long-term information on the development of the watershed. Torrents that are prone to debris flows are often devoid of vegetation and can thus be well surveyed using photogrammetric methods based on uncrewed aerial vehicle (UAV) surveys. The possib
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Flez, Christophe, and Philippe Lahousse. "La gestion du risque torrentiel à Serre-Chevalier : acteurs et enjeux." Espace géographique 31, no. 2 (2002): 163. http://dx.doi.org/10.3917/eg.312.0163.

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36

Ahlborn, Marieke, Moshe Armon, Yoav Ben Dor, et al. "Increased frequency of torrential rainstorms during a regional late Holocene eastern Mediterranean drought." Quaternary Research 89, no. 2 (2018): 425–31. http://dx.doi.org/10.1017/qua.2018.9.

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AbstractIdentifying climates favoring extreme weather phenomena is a primary aim of paleoclimate and paleohydrological research. Here, we present a well-dated, late Holocene Dead Sea sediment record of debris flows covering 3.3 to 1.9 cal ka BP. Twenty-three graded layers deposited in shallow waters near the western Dead Sea shore were identified by microfacies analysis. These layers represent distal subaquatic deposits of debris flows triggered by torrential rainstorms over the adjacent western Dead Sea escarpment. Modern debris flows on this escarpment are induced by rare rainstorms with int
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37

Ravanel, Ludovic, Pierre-Allain Duvillard, Laurent Astrade, et al. "The Taconnaz Rockfall (Mont-Blanc Massif, European Alps) of November 2018: A Complex and At-Risk Rockwall-Glacier-Torrent Morphodynamic Continuum." Applied Sciences 13, no. 17 (2023): 9716. http://dx.doi.org/10.3390/app13179716.

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The glacial and torrential basin of Taconnaz (Mont-Blanc massif, France) dominates the Chamonix valley. It is one of the major paths for snow avalanches in the Alps, often triggered by serac falls from the Taconnaz glacier. On 24 November 2018, the basin’s multi-risk nature was further accentuated by a new type of hazard with a rockfall triggered at c. 2700 m a.s.l. It travelled down over a distance of 1.85 km and stopped 165 m away from the construction site of a micro-hydroelectric power station. We studied the triggering conditions at the permafrost lower limit, the effects of the supra-gla
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Sugiyama, Ayumi, Suguru Masuda, Kazuyo Nagaosa, Maki Tsujimura, and Kenji Kato. "Tracking the direct impact of rainfall on groundwater at Mt. Fuji by multiple analyses including microbial DNA." Biogeosciences 15, no. 3 (2018): 721–32. http://dx.doi.org/10.5194/bg-15-721-2018.

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Abstract. A total of 2 to 3 million tons of spring water flushes out from the foot of Mt. Fuji, the largest volcanic mountain in Japan. Based on the concept of piston flow transport, residence time of stored groundwater at Mt. Fuji was estimated at ∼ 15–30 years by the 36Cl ∕ Cl ratio (Tosaki et al., 2011). This range, however, represents the average residence time of groundwater that was mixed before it flushed out. To elucidate the route of groundwater in a given system, we determined signatures of direct impacts of rainfall on groundwater, using microbial, stable isotopic (δ18O), and chemic
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39

Conesa-García, C., F. López-Bermúdez, and R. García-Lorenzo. "Bed stability variations after check dam construction in torrential channels (South-East Spain)." Earth Surface Processes and Landforms 32, no. 14 (2007): 2165–84. http://dx.doi.org/10.1002/esp.1521.

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40

Xo‘janova, Tamara. "AXBOROT URUSHI TUSHUNCHASINING G‘OYAVIY TABIATI VA MAFKURAVIY XUSUSIYATLARI." TAMADDUN NURI JURNALI 7, no. 58 (2024): 231–35. http://dx.doi.org/10.69691/n84mkx92.

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The article provides a scientific basis for the concept of information warfare, its ideological nature and ideological features. Since globalization processes and information society trends have a negative impact on people's consciousness in every region, an important task is to eliminate it and enhance its positive impact. It is impossible to adapt to this phenomenon without studying it deeply and, if necessary, changing its direction accordingly. Failure to thoroughly study the threats in the modern global world, failure to develop a strategy, tactics and technologies for their elimination a
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41

Costache, Romulus, Haoyuan Hong, and Yi Wang. "Identification of torrential valleys using GIS and a novel hybrid integration of artificial intelligence, machine learning and bivariate statistics." CATENA 183 (December 2019): 104179. http://dx.doi.org/10.1016/j.catena.2019.104179.

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42

Petrović, Ana M., Stanimir Kostadinov, and Sanja Mustafić. "THE IMPACT OF DEPOPULATION ON REDUCTION OF THE PEAKS OF TORRENTIAL FLOODS IN SELECTED WATERSHEDS OF THE SOUTHEASTERN SERBIA." Academic Perspective Procedia 5, no. 2 (2022): 201–9. http://dx.doi.org/10.33793/acperpro.05.02.5841.

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Petrović, Ana M., Stanimir Kostadinov, and Sanja Manojlović. "The Impact of Depopulation on Reduction of the Peaks of Torrential Floods in Selected Watersheds of the Southeastern Serbia." Academic Perspective Procedia 5, no. 2 (2022): 387–95. http://dx.doi.org/10.33793/acperpro.05.02.9300.

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44

Zhou, Yushu, and Chunguang Cui. "A modeling study of surface rainfall processes associated with a torrential rainfall event over Hubei, China, during July 2007." Advances in Atmospheric Sciences 28, no. 6 (2011): 1459–70. http://dx.doi.org/10.1007/s00376-010-0119-8.

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45

PAEZ, Luciano Gagliardi. "SPATIAL RESTRUCTURING IN THE SCALE DEBATE BASED ON DECISION-MAKING PROCESSES ON CLIMATE CHANGE: FROM GLOBAL TO LOCAL." Boletim de Conjuntura (BOCA) 14, no. 41 (2023): 585–94. https://doi.org/10.5281/zenodo.7992425.

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Climate change already affects everyone. Anthropogenic actions produce planetary impacts and accelerate global warming. Municipalities around the world have been suffering from heat waves, prolonged droughts, torrential rains, tornadoes, cyclones, hurricanes, among others, which are increasingly recurrent. The objective of this essay is to show that cities have a strategic role, both in facing these atmospheric changes that we are experiencing, as well as in the decision-making power for coping actions. For this, we use the concept of geographic scale as a methodology, as a conceptual tool to
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46

Gournelos, Theodoros, and Hampik Maroukian. "Geomorphological observations concerning the evolution of the Basin of Athens." Geologica Balcanica 20, no. 6 (1990): 15–24. http://dx.doi.org/10.52321/geolbalc.20.6.15.

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Tectonism is an important element in the determination of the present landscape of Greece. It has shaped and is shaping the numerous highlands and depressions and consequently settlement patterns of the country. One such area is the Greater Athens region, a triangular basin, opening to the sea in the southwest and surrounded by four mountain masses. The presence of an old planation surface on the surrounding mountains; of thick lateritic soils in the basin overlain by Miocene and Pliocene marls, marly limestones, sands and conglomerates; Pleistocene fluvio-torrential deposits; alluvial fans; a
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Gems, Bernhard, Bruno Mazzorana, Thomas Hofer, Michael Sturm, Roman Gabl, and Markus Aufleger. "3-D hydrodynamic modelling of flood impacts on a building and indoor flooding processes." Natural Hazards and Earth System Sciences 16, no. 6 (2016): 1351–68. http://dx.doi.org/10.5194/nhess-16-1351-2016.

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Abstract. Given the current challenges in flood risk management and vulnerability assessment of buildings exposed to flood hazards, this study presents three-dimensional numerical modelling of torrential floods and its interaction with buildings. By means of a case study application, the FLOW-3D software is applied to the lower reach of the Rio Vallarsa torrent in the village of Laives (Italy). A single-family house on the flood plain is therefore considered in detail. It is exposed to a 300-year flood hydrograph. Different building representation scenarios, including an entire impervious buil
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Turconi, Laura, Domenico Tropeano, Gabriele Savio, et al. "Torrential Hazard Prevention in Alpine Small Basin through Historical, Empirical and Geomorphological Cross Analysis in NW Italy." Land 11, no. 5 (2022): 699. http://dx.doi.org/10.3390/land11050699.

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Debris flow is one of the most dangerous natural processes in mountain regions and it occur in a wide variety of environments throughout the world. In the Italian Alps, some tens of thousands of damaging debris flow and, in general, torrential floods associated to intense sediment transport in secondary catchments have been documented in the last 300 years. These have caused socio-economic damage, damage to anthropogenic structures or infrastructures and in many cases casualties. Often, in the same basins, the occurrence of debris-flow processes recurs many years later. Prediction can often be
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Milanesi, L., M. Pilotti, R. Ranzi, and G. Valerio. "Methodologies for hydraulic hazard mapping in alluvial fan areas." Proceedings of the International Association of Hydrological Sciences 364 (September 16, 2014): 267–72. http://dx.doi.org/10.5194/piahs-364-267-2014.

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Abstract. Hydraulic hazards in alluvial fan areas are mainly related to torrential floods and debris flows. These processes are characterized by their fast time evolution and relevant sediment load. Rational approaches for the estimation of hazard levels in flood-prone areas make use of the maps of depth and velocity, which are provided by numerical simulations of the event. This paper focuses on national regulations regarding quantitative debris-flow hazard mapping and compares them to a simple conceptual model for the quantification of the hazard levels on the basis of human stability in a f
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Wang, Donghai, Xiaofan Li, Wei-Kuo Tao, Ying Liu, and Haiguang Zhou. "Torrential rainfall processes associated with a landfall of severe tropical storm Bilis (2006): A two-dimensional cloud-resolving modeling study." Atmospheric Research 91, no. 1 (2009): 94–104. http://dx.doi.org/10.1016/j.atmosres.2008.07.005.

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