Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Salvatore M.C.[1]"'
Autor:
Cerrato R.[1], Salvatore M.C.[1, Gunnarson B.E.[3], Linderholm H.W.[4], Carturan L.[5], Brunetti M.[6], Baroni C.[1
Publikováno v:
Journal of Glaciology 66 (2020): 714–726. doi:10.1017/jog.2020.40
info:cnr-pdr/source/autori:Cerrato R.[1], Salvatore M.C.[1,2], Gunnarson B.E.[3], Linderholm H.W.[4], Carturan L.[5], Brunetti M.[6], Baroni C.[1,2]/titolo:Pinus cembra L. tree-ring data as a proxy for summer mass-balance variability of the Careser Glacier (Italian Rhaetian Alps)/doi:10.1017%2Fjog.2020.40/rivista:Journal of Glaciology/anno:2020/pagina_da:714/pagina_a:726/intervallo_pagine:714–726/volume:66
info:cnr-pdr/source/autori:Cerrato R.[1], Salvatore M.C.[1,2], Gunnarson B.E.[3], Linderholm H.W.[4], Carturan L.[5], Brunetti M.[6], Baroni C.[1,2]/titolo:Pinus cembra L. tree-ring data as a proxy for summer mass-balance variability of the Careser Glacier (Italian Rhaetian Alps)/doi:10.1017%2Fjog.2020.40/rivista:Journal of Glaciology/anno:2020/pagina_da:714/pagina_a:726/intervallo_pagine:714–726/volume:66
Glacial extent and mass balance are sensitive climate proxies providing solid information on past climatic conditions. However, series of annual mass-balance measurements of more than 60 years are scarce. To our knowledge, this is the first time the
Autor:
Cerrato R.[1], Salvatore M.C.[1, Gunnarson B.E.[3], Linderholm H.W.[4], Carturan L.[5], Brunetti M.[6], De Blasi F.[5], Baroni C.[1
Publikováno v:
Dendrochronologia (Verona) 53 (2019): 22–31. doi:10.1016/j.dendro.2018.10.010
info:cnr-pdr/source/autori:Cerrato R.[1], Salvatore M.C.[1,2], Gunnarson B.E.[3], Linderholm H.W.[4], Carturan L.[5], Brunetti M.[6], De Blasi F.[5], Baroni C.[1,2]/titolo:A Pinus cembra L. tree-ring record for late spring to late summer temperature in the Rhaetian Alps, Italy/doi:10.1016%2Fj.dendro.2018.10.010/rivista:Dendrochronologia (Verona)/anno:2019/pagina_da:22/pagina_a:31/intervallo_pagine:22–31/volume:53
info:cnr-pdr/source/autori:Cerrato R.[1], Salvatore M.C.[1,2], Gunnarson B.E.[3], Linderholm H.W.[4], Carturan L.[5], Brunetti M.[6], De Blasi F.[5], Baroni C.[1,2]/titolo:A Pinus cembra L. tree-ring record for late spring to late summer temperature in the Rhaetian Alps, Italy/doi:10.1016%2Fj.dendro.2018.10.010/rivista:Dendrochronologia (Verona)/anno:2019/pagina_da:22/pagina_a:31/intervallo_pagine:22–31/volume:53
Ongoing climate change strongly affects high-elevation environments in the European Alps, influencing the cryosphere and the biosphere and causing widespread retreat of glaciers and changes in biomes. Nevertheless, high-elevation areas often lack lon
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b573a523b75f49432914b58b45de14ce
http://hdl.handle.net/11577/3291127
http://hdl.handle.net/11577/3291127
Autor:
Baroni C.[1, Gennaro S.[1], Salvatore M.C.[1, Ivy-Ochs S.[3], Christl M.[3], Cerrato R.[1], Orombelli G.[4]
Publikováno v:
Quaternary Science Reviews, 255
Quaternary science reviews 255 (2021). doi:10.1016/j.quascirev.2021.106815
info:cnr-pdr/source/autori:Baroni C.[1,2], Gennaro S.[1], Salvatore M.C.[1,2], Ivy-Ochs S.[3], Christl M.[3], Cerrato R.[1], Orombelli G.[4]/titolo:Last Lateglacial glacier advance in the Gran Paradiso Group reveals relatively drier climatic conditions established in the Western Alps since at least the Younger Dryas/doi:10.1016%2Fj.quascirev.2021.106815/rivista:Quaternary science reviews/anno:2021/pagina_da:/pagina_a:/intervallo_pagine:/volume:255
Quaternary science reviews 255 (2021). doi:10.1016/j.quascirev.2021.106815
info:cnr-pdr/source/autori:Baroni C.[1,2], Gennaro S.[1], Salvatore M.C.[1,2], Ivy-Ochs S.[3], Christl M.[3], Cerrato R.[1], Orombelli G.[4]/titolo:Last Lateglacial glacier advance in the Gran Paradiso Group reveals relatively drier climatic conditions established in the Western Alps since at least the Younger Dryas/doi:10.1016%2Fj.quascirev.2021.106815/rivista:Quaternary science reviews/anno:2021/pagina_da:/pagina_a:/intervallo_pagine:/volume:255
The Late Pleistocene to Holocene transition in the Northern Hemisphere was characterized by abrupt millennial-scale climatic changes testified in the Alpine Chain by proxy records derived from glacial landforms and deposits. A detailed reconstruction
Autor:
Bini M.[1, Isola I.[2, 3] Zanchetta G.[1, 2] Pappalardo M.[1], Ribolini A.[1], Ragaini L.[1], Baroni C.[1, Boretto G.[4], Fuck E.[5], Morigi C.[1], Salvatore M.C.[1, Bassi D.[6] Marzaioli F.[7], Terrasi F. [7]
Publikováno v:
SEDICI (UNLP)
Universidad Nacional de La Plata
instacron:UNLP
Holocene (Lond. Online) 28 (2018): 56–64. doi:10.1177/0959683617714596
info:cnr-pdr/source/autori:Bini M.[1,2], Isola I.[2,3] Zanchetta G.[1,2] Pappalardo M.[1], Ribolini A.[1], Ragaini L.[1], Baroni C.[1,3], Boretto G.[4], Fuck E.[5], Morigi C.[1], Salvatore M.C.[1,3], Bassi D.[6] Marzaioli F.[7], Terrasi F. [7]/titolo:Mid-Holocene relative sea-level changes along Atlantic Patagonia: New data from Camarones, Chubut, Argentina/doi:10.1177%2F0959683617714596/rivista:Holocene (Lond. Online)/anno:2018/pagina_da:56/pagina_a:64/intervallo_pagine:56–64/volume:28
Universidad Nacional de La Plata
instacron:UNLP
Holocene (Lond. Online) 28 (2018): 56–64. doi:10.1177/0959683617714596
info:cnr-pdr/source/autori:Bini M.[1,2], Isola I.[2,3] Zanchetta G.[1,2] Pappalardo M.[1], Ribolini A.[1], Ragaini L.[1], Baroni C.[1,3], Boretto G.[4], Fuck E.[5], Morigi C.[1], Salvatore M.C.[1,3], Bassi D.[6] Marzaioli F.[7], Terrasi F. [7]/titolo:Mid-Holocene relative sea-level changes along Atlantic Patagonia: New data from Camarones, Chubut, Argentina/doi:10.1177%2F0959683617714596/rivista:Holocene (Lond. Online)/anno:2018/pagina_da:56/pagina_a:64/intervallo_pagine:56–64/volume:28
This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast derived from sea-level index points whose elevation was determined by a differential global position system (DGPS). Bio encrustations from outcrops locat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2082dd8589942efb90b8094c84bdc18a
http://hdl.handle.net/11392/2381984
http://hdl.handle.net/11392/2381984
Publikováno v:
Quaternary science reviews 197 (2018): 352–367. doi:10.1016/j.quascirev.2018.07.003
info:cnr-pdr/source/autori:Baroni C.[1,2], Guidobaldi G.[1], Salvatore M.C.[1,2], Christl M.[3], Ivy-Ochs S.[3]/titolo:Last glacial maximum glaciers in the Northern Apennines reflect primarily the influence of southerly storm-tracks in the western Mediterranean/doi:10.1016%2Fj.quascirev.2018.07.003/rivista:Quaternary science reviews/anno:2018/pagina_da:352/pagina_a:367/intervallo_pagine:352–367/volume:197
info:cnr-pdr/source/autori:Baroni C.[1,2], Guidobaldi G.[1], Salvatore M.C.[1,2], Christl M.[3], Ivy-Ochs S.[3]/titolo:Last glacial maximum glaciers in the Northern Apennines reflect primarily the influence of southerly storm-tracks in the western Mediterranean/doi:10.1016%2Fj.quascirev.2018.07.003/rivista:Quaternary science reviews/anno:2018/pagina_da:352/pagina_a:367/intervallo_pagine:352–367/volume:197
During the Local Last Glacial Maximum (LLGM), the Northern Apennines hosted more than 100 valley and mountain glaciers covering collectively more than 260 km2. Cosmogenic 10Be exposure ages obtained for the first time along the Apenninic range constr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e1b5e9c41c9c0879464a5b1aef09a923
http://www.cnr.it/prodotto/i/393436
http://www.cnr.it/prodotto/i/393436
Autor:
Bini M.[1, 2] Zanchetta G.[1, 2] Ribolini A.[1], Salvatore M.C.[1, 3] Baroni C.[1, Pappalardo M.[1], Isola I.[2], Isla F.I.[4] Fucks E.[5], Boretto G.[6] Morigi C.[1, Ragaini L.[1], Marzaioli F.[8], Passariello I.[8]
Publikováno v:
Geografia fisica e dinamica quaternaria (Testo stamp.) 40 (2017): 29–39. doi:10.4461/GFDQ2017.40.3
info:cnr-pdr/source/autori:Bini M.[1,2] Zanchetta G.[1,2] Ribolini A.[1], Salvatore M.C.[1,3] Baroni C.[1,3], Pappalardo M.[1], Isola I.[2], Isla F.I.[4] Fucks E.[5], Boretto G.[6] Morigi C.[1,7], Ragaini L.[1], Marzaioli F.[8], Passariello I.[8]/titolo:Last Interglacial Sea-level highstand deduced from notches and inner margins of marine terraces at Puerto Deseado, Santa Cruz Province, Argentina/doi:10.4461%2FGFDQ2017.40.3/rivista:Geografia fisica e dinamica quaternaria (Testo stamp.)/anno:2017/pagina_da:29/pagina_a:39/intervallo_pagine:29–39/volume:40
info:cnr-pdr/source/autori:Bini M.[1,2] Zanchetta G.[1,2] Ribolini A.[1], Salvatore M.C.[1,3] Baroni C.[1,3], Pappalardo M.[1], Isola I.[2], Isla F.I.[4] Fucks E.[5], Boretto G.[6] Morigi C.[1,7], Ragaini L.[1], Marzaioli F.[8], Passariello I.[8]/titolo:Last Interglacial Sea-level highstand deduced from notches and inner margins of marine terraces at Puerto Deseado, Santa Cruz Province, Argentina/doi:10.4461%2FGFDQ2017.40.3/rivista:Geografia fisica e dinamica quaternaria (Testo stamp.)/anno:2017/pagina_da:29/pagina_a:39/intervallo_pagine:29–39/volume:40
A detailed geomorphological survey was undertaken in the area of Puerto Deseado (Santa Cruz Province, Argentina) to reconstruct the Relative Sea-level (RSL) position during the Last Interglacial highstand. The presence of active and well-preserved ab
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::6a6a6150444174a5c3403e7fac9d25fd
Publikováno v:
International Symposium held in Torino (Italy) 18-21 September, 2014 For celebrating 100 years of the Bulletin of the Italian Glaciological Committee, pp. 97–104, Torino (Italy), 18-21 September 2014
info:cnr-pdr/source/autori:Baroni C.[1,2,3], Salvatore M.C.[1,2]/congresso_nome:International Symposium held in Torino (Italy) 18-21 September, 2014 For celebrating 100 years of the Bulletin of the Italian Glaciological Committee/congresso_luogo:Torino (Italy)/congresso_data:18-21 September 2014/anno:2015/pagina_da:97/pagina_a:104/intervallo_pagine:97–104
info:cnr-pdr/source/autori:Baroni C.[1,2,3], Salvatore M.C.[1,2]/congresso_nome:International Symposium held in Torino (Italy) 18-21 September, 2014 For celebrating 100 years of the Bulletin of the Italian Glaciological Committee/congresso_luogo:Torino (Italy)/congresso_data:18-21 September 2014/anno:2015/pagina_da:97/pagina_a:104/intervallo_pagine:97–104
The International Symposium "The future of the glaciers: from the past to the next 100 years" was held in Torino (Italy) from 18 to 21 September, 2014 for celebrating the centenary of the Bulletin of the Italian Glaciological Committee. The "Bulletin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::b4c941def03651dd5456d555807d2e1c
Autor:
Salvatore M.C.[1, Zanoner T.[1, Baroni C.[1, 2, Carton A.[1, 3, Banchieri F.A.[1], Viani C.[1, Giardino M.[1, Perotti L.[1
Publikováno v:
Geografia fisica e dinamica quaternaria (Testo stamp.) 38 (2015): 175–198. doi:10.4461/GFDQ.2015.38.16
info:cnr-pdr/source/autori:Salvatore M.C.[1,2], Zanoner T.[1,3], Baroni C.[1,2,4], Carton A.[1,3,5], Banchieri F.A.[1], Viani C.[1,6], Giardino M.[1,6], Perotti L.[1,6]/titolo:The state of Italian glaciers: A snapshot of the 2006-2007 hydrological period/doi:10.4461%2FGFDQ.2015.38.16/rivista:Geografia fisica e dinamica quaternaria (Testo stamp.)/anno:2015/pagina_da:175/pagina_a:198/intervallo_pagine:175–198/volume:38
info:cnr-pdr/source/autori:Salvatore M.C.[1,2], Zanoner T.[1,3], Baroni C.[1,2,4], Carton A.[1,3,5], Banchieri F.A.[1], Viani C.[1,6], Giardino M.[1,6], Perotti L.[1,6]/titolo:The state of Italian glaciers: A snapshot of the 2006-2007 hydrological period/doi:10.4461%2FGFDQ.2015.38.16/rivista:Geografia fisica e dinamica quaternaria (Testo stamp.)/anno:2015/pagina_da:175/pagina_a:198/intervallo_pagine:175–198/volume:38
In this study, we present a snapshot of Italian glaciers that outlines the hydrological years of 2006 and 2007 and was derived from the interpretation of high-resolution orthophotographs. The results are freely available and downloadable on the websi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::7d24be79520ba09342b0beabdd0ecab7
https://publications.cnr.it/doc/463284
https://publications.cnr.it/doc/463284
Autor:
Baroni C.[1, Pieruccini P.[3], Bini M.[1], Coltorti M.[3], Fantozzi P.L.[3], Guidobaldi G.[1], Nannini D.[1], Ribolini A.[1], Salvatore M.C.[1]
Publikováno v:
Geografia fisica e dinamica quaternaria (Testo stamp.) 38 (2015): 201–227. doi:10.4461/GFDQ.2015.38.17
info:cnr-pdr/source/autori:Baroni C.[1,2], Pieruccini P.[3], Bini M.[1], Coltorti M.[3], Fantozzi P.L.[3], Guidobaldi G.[1], Nannini D.[1], Ribolini A.[1], Salvatore M.C.[1]/titolo:Geomorphological and neotectonic map of the Apuan Alps (Tuscany, Italy)/doi:10.4461%2FGFDQ.2015.38.17/rivista:Geografia fisica e dinamica quaternaria (Testo stamp.)/anno:2015/pagina_da:201/pagina_a:227/intervallo_pagine:201–227/volume:38
info:cnr-pdr/source/autori:Baroni C.[1,2], Pieruccini P.[3], Bini M.[1], Coltorti M.[3], Fantozzi P.L.[3], Guidobaldi G.[1], Nannini D.[1], Ribolini A.[1], Salvatore M.C.[1]/titolo:Geomorphological and neotectonic map of the Apuan Alps (Tuscany, Italy)/doi:10.4461%2FGFDQ.2015.38.17/rivista:Geografia fisica e dinamica quaternaria (Testo stamp.)/anno:2015/pagina_da:201/pagina_a:227/intervallo_pagine:201–227/volume:38
Renowned since the Roman Period for the extraction of precious marble, the Apuan Alps (northern Tuscany) are an extraordinary region of natural and cultural heritage in the Mediterranean basin and contain a large number of geosites of international a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::d60d229111e7f7f51597bae906072b31
Autor:
Lorenzini S.[1], Baroni C.[1, Baneschi I.[2], Salvatore M.C.[1], Fallick A.E.[3], Hall B.L.[4]
Publikováno v:
Palaeogeography, palaeoclimatology, palaeoecology 395 (2014): 21–28. doi:10.1016/j.palaeo.2013.12.014
info:cnr-pdr/source/autori:Lorenzini S.[1], Baroni C.[1,2], Baneschi I.[2], Salvatore M.C.[1], Fallick A.E.[3], Hall B.L.[4]/titolo:Adelie penguin dietary remains reveal Holocene environmental changes in the western Ross Sea (Antarctica)/doi:10.1016%2Fj.palaeo.2013.12.014/rivista:Palaeogeography, palaeoclimatology, palaeoecology/anno:2014/pagina_da:21/pagina_a:28/intervallo_pagine:21–28/volume:395
info:cnr-pdr/source/autori:Lorenzini S.[1], Baroni C.[1,2], Baneschi I.[2], Salvatore M.C.[1], Fallick A.E.[3], Hall B.L.[4]/titolo:Adelie penguin dietary remains reveal Holocene environmental changes in the western Ross Sea (Antarctica)/doi:10.1016%2Fj.palaeo.2013.12.014/rivista:Palaeogeography, palaeoclimatology, palaeoecology/anno:2014/pagina_da:21/pagina_a:28/intervallo_pagine:21–28/volume:395
Carbon and nitrogen stable isotope analyses were performed on modern and Holocene Adelie penguin guano samples collected from ornithogenic soils along the Scott Coast (Southern Victoria Land, Antarctica), from Cape Irizar to Dunlop Island, and at Cap
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bc46c8c57f1965b09fa19a58d561f0ac
http://hdl.handle.net/11568/335267
http://hdl.handle.net/11568/335267