Zobrazeno 1 - 10
of 71
pro vyhledávání: '"Hakan Tanyas"'
Publikováno v:
Scientific Data, Vol 11, Iss 1, Pp 1-12 (2024)
Abstract Cryospheric hazards - in this case, thaw slumps (TS) and thermo-erosion gullies (TEG) - are phenomena typical of permafrost-dominated landscapes. Open datasets informing about their spatial, temporal and size distributions in the Arctic are
Externí odkaz:
https://doaj.org/article/713396ce65f04a13b65d54ad4ead6146
Autor:
Mustafa Y. Kaya, Guillaume Dupont-Nivet, Joost Frieling, Chiara Fioroni, Alexander Rohrmann, Sevinç Özkan Altıner, Ezgi Vardar, Hakan Tanyaş, Mehmut Mamtimin, Guo Zhaojie
Publikováno v:
Communications Earth & Environment, Vol 3, Iss 1, Pp 1-10 (2022)
The Eurasian Epicontinental Sea sequestered 720–1300 Gt of organic carbon during the Palaeocene-Eocene Thermal Maximum, according to a palaeogeographic reconstruction and multi-proxy data from a sedimentary sequence in the Tarim Basin, China.
Externí odkaz:
https://doaj.org/article/357c21986bfb4d6f91e12cfd2fadf039
Autor:
Marco Loche, Gianvito Scaringi, Ali P. Yunus, Filippo Catani, Hakan Tanyaş, William Frodella, Xuanmei Fan, Luigi Lombardo
Publikováno v:
Scientific Reports, Vol 12, Iss 1, Pp 1-11 (2022)
Abstract The patterns and controls of the transient enhanced landsliding that follows strong earthquakes remain elusive. Geostatistical models can provide clues on the underlying processes by identifying relationships with a number of physical variab
Externí odkaz:
https://doaj.org/article/1daadef51a4c4801a656f68f02c4cbea
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Earthquakes do not only trigger landslides in co-seismic phases but also elevate post-seismic landslide susceptibility either by causing a strength reduction in hillslope materials or by producing co-seismic landslide deposits, which are prone to fur
Externí odkaz:
https://doaj.org/article/4f857b8fad304b07ae33b962af74edec
Publikováno v:
Communications Earth & Environment, Vol 5, Iss 1, Pp 1-14 (2024)
Abstract The weakening of hillslopes during strong earthquakes increases landsliding rates in post-seismic periods. However, very few studies have addressed the amount of coseismic reduction in shear strength of hillslope materials. This makes estima
Externí odkaz:
https://doaj.org/article/cbe3c0b2f2b24d4b98fa5d3fe93d5ab1
Autor:
Mahnoor Ahmed, Hakan Tanyas, Raphaël Huser, Ashok Dahal, Giacomo Titti, Lisa Borgatti, Mirko Francioni, Luigi Lombardo
Publikováno v:
International Journal of Applied Earth Observations and Geoinformation, Vol 125, Iss , Pp 103593- (2023)
The initial inception of the landslide susceptibility concept defined it as a static property of the landscape, explaining the proneness of certain locations to generate slope failures. Since the spread of data-driven probabilistic solutions though,
Externí odkaz:
https://doaj.org/article/926836b2260749f9a537857947328a64
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Externí odkaz:
https://doaj.org/article/15aae63228f345b0b76273f320b90a1f
Publikováno v:
Remote Sensing, Vol 14, Iss 17, p 4357 (2022)
Rapid and accurate identification of landslides is an essential part of landslide hazard assessment, and in particular it is useful for land use planning, disaster prevention, and risk control. Recent alternatives to manual landslide mapping are movi
Externí odkaz:
https://doaj.org/article/7567c9eb9ba04778b53ce87cd9e60ebf
Publikováno v:
Remote Sensing, Vol 14, Iss 6, p 1321 (2022)
To understand the factors that make certain areas especially prone to landslides, statistical approaches are typically used. The interpretation of statistical results in areas characterised by complex geological and geomorphological patterns can be c
Externí odkaz:
https://doaj.org/article/5bab4331c5f24fefac6aa8d792a94ad1
Publikováno v:
Stochastic environmental research and risk assessment, 36(8), 2031-2048. Springer
For more than three decades, the part of the geoscientific community studying landslides through data-driven models has focused on estimating where landslides may occur across a given landscape. This concept is widely known as landslide susceptibilit