Zobrazeno 1 - 10
of 52
pro vyhledávání: '"Renato R Colucci"'
Autor:
Michele Petrini, Florence Colleoni, Nina Kirchner, Anna L. C. Hughes, Angelo Camerlenghi, Michele Rebesco, Renata G. Lucchi, Emanuele Forte, Renato R. Colucci, Riko Noormets
Publikováno v:
Scientific Reports, Vol 8, Iss 1, Pp 1-9 (2018)
Abstract The Barents Sea Ice Sheet was a marine-based ice sheet, i.e., it rested on the Barents Sea floor during the Last Glacial Maximum (21 ky BP). The Bjørnøyrenna Ice Stream was the largest ice stream draining the Barents Sea Ice Sheet and is r
Externí odkaz:
https://doaj.org/article/0142988d9e2143e9a6179ea6734ac79f
Publikováno v:
Scientific Reports, Vol 7, Iss 1, Pp 1-7 (2017)
Abstract We document the occurrence in December 2015 of unprecedented high monthly mean temperatures in the observational record of mountain sites in the eastern Alps. For the first time in the last 150 years mean December temperature exceeded 0 °C
Externí odkaz:
https://doaj.org/article/1990a90d040440798877deb58b05295a
Autor:
Renato R. Colucci, Manja Žebre, Csaba Zsolt Torma, Neil F. Glasser, Eleonora Maset, Costanza Del Gobbo, Simone Pillon
Publikováno v:
Atmosphere, Vol 12, Iss 2, p 263 (2021)
Very small glaciers (2) account for more than 80% of the total number of glaciers and more than 15% of the total glacier area in the European Alps. This study seeks to better understand the impact of extreme snowfall events on the resilience of very
Externí odkaz:
https://doaj.org/article/1ef881f645b247dd84c3a38cb44b8f97
Publikováno v:
Progress in Physical Geography: Earth and Environment. 46:422-440
This study investigates the application of a terrestrial structure from motionmulti-view stereo (SfM-MVS) approach combined with ground-penetrating radar (GPR) surveys for monitoring the surface topographic change of two permanent ice deposits in cav
Publikováno v:
Geodetski Vestnik, Vol 58, Iss 2, Pp 274-313 (2014)
Three very small Alpine glaciers in the Julian Alps are presented: the Eastern and the Western Canin glaciers in Italy and the Triglav glacier in Slovenia. The history of measurements using a measuring tape and via geodetic means on Canin glaciers is
Externí odkaz:
https://doaj.org/article/24bdaa66868e410ab4a170c227cca918
The Last Glacial Maximum (LGM) is a global event that occurred 26 to 21 ka BP and was characterized by lower temperatures (3 to 6 °C globally) and different precipitation regimes. The environment was marked by extended glaciers which released a larg
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::36e19a95811ca93533cc36292fea210d
https://doi.org/10.5194/ems2022-655
https://doi.org/10.5194/ems2022-655
Autor:
Emanuele Forte, Carlotta Zanettini, Mauro Guglielmin, Manja Žebre, Eleonora Maset, Renato R. Colucci
Publikováno v:
Geomorphology (Amst.) 330 (2019): 177–189. doi:10.1016/j.geomorph.2019.02.002
info:cnr-pdr/source/autori:Colucci R.R.; Forte E.; Zebre M.; Maset E.; Zanettini C.; Guglielmin M./titolo:Is that a relict rock glacier?/doi:10.1016%2Fj.geomorph.2019.02.002/rivista:Geomorphology (Amst.)/anno:2019/pagina_da:177/pagina_a:189/intervallo_pagine:177–189/volume:330
info:cnr-pdr/source/autori:Colucci R.R.; Forte E.; Zebre M.; Maset E.; Zanettini C.; Guglielmin M./titolo:Is that a relict rock glacier?/doi:10.1016%2Fj.geomorph.2019.02.002/rivista:Geomorphology (Amst.)/anno:2019/pagina_da:177/pagina_a:189/intervallo_pagine:177–189/volume:330
The distribution of rock glaciers is often used to investigate the occurrence of permafrost in mountain areas and to understand their climate and paleoclimate evolution. This requires the creation of regional and global inventories capable of discrim
Autor:
Michele Petrini, Emanuele Forte, Michele Rebesco, Nina Kirchner, Riko Noormets, Florence Colleoni, Angelo Camerlenghi, Renata G. Lucchi, Anna L.C. Hughes, Jan Mangerud, Renato R. Colucci
Publikováno v:
Petrini, M, Colleoni, F, Kirchner, N, Hughes, A L C, Camerlenghi, A, Rebesco, M, Lucchi, R G, Forte, E, Colucci, R R, Noormets, R & Mangerud, J 2020, ' Simulated last deglaciation of the Barents Sea Ice Sheet primarily driven by oceanic conditions ', Quaternary Science Reviews, vol. 238, 106314 . https://doi.org/10.1016/j.quascirev.2020.106314
Quaternary Science Reviews, 238
Quaternary Science Reviews
Quaternary Science Reviews, 238
Quaternary Science Reviews
The Barents Sea Ice Sheet was part of an interconnected complex of ice sheets, collectively referred to as the Eurasian Ice Sheet, which covered north-westernmost Europe, Russia and the Barents Sea during the Last Glacial Maximum (around 21 ky BP). D
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b949fe587d76960c5d80f85ca04c04de
https://hdl.handle.net/11368/2973556
https://hdl.handle.net/11368/2973556