Zobrazeno 1 - 2
of 2
pro vyhledávání: '"J.C. Gallet (5)"'
Autor:
E. Barbaro (1), A. Spolaor (2), O. Karroca (2), K. Park (3), T. Martma (4), E. Isaksson (5), J. Kohler (5), J.C. Gallet (5), M.P. Bjorkman (6), D. Cappelletti (7), G. Spreen (8), R. Zangrando (1), C. Barbante (1, A. Gambaro (1
Publikováno v:
The Arctic as seen from Ny-Ålesund: research results, new proposals and overviews., pp. 92–92, Rome, 18-19/03/2019
info:cnr-pdr/source/autori:E. Barbaro (1), A. Spolaor (2), O. Karroca (2), K. Park (3), T. Martma (4), E. Isaksson (5), J. Kohler (5), J.C. Gallet (5), M.P. Bjorkman (6), D. Cappelletti (7), G. Spreen (8), R. Zangrando (1), C. Barbante (1,2), A. Gambaro (1,2)/congresso_nome:The Arctic as seen from Ny-Ålesund: research results, new proposals and overviews./congresso_luogo:Rome/congresso_data:18-19%2F03%2F2019/anno:2019/pagina_da:92/pagina_a:92/intervallo_pagine:92–92
info:cnr-pdr/source/autori:E. Barbaro (1), A. Spolaor (2), O. Karroca (2), K. Park (3), T. Martma (4), E. Isaksson (5), J. Kohler (5), J.C. Gallet (5), M.P. Bjorkman (6), D. Cappelletti (7), G. Spreen (8), R. Zangrando (1), C. Barbante (1,2), A. Gambaro (1,2)/congresso_nome:The Arctic as seen from Ny-Ålesund: research results, new proposals and overviews./congresso_luogo:Rome/congresso_data:18-19%2F03%2F2019/anno:2019/pagina_da:92/pagina_a:92/intervallo_pagine:92–92
The role of oceanic primary production on climate variability has long been debated. Defining changes in past oceanic primary production can help understanding of the important role that marine algae have in climate variability. The changes in primar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::eb006e1d749c18580daab3885eafe556
http://www.cnr.it/prodotto/i/426938
http://www.cnr.it/prodotto/i/426938
Autor:
A. Spolaor (1), Carlo Barbante (1)(2), E. Barbaro (1), F. Burgay (1), P. Bjorkman (3), D. Cappelletti (4), G. Cozzi (1), F. Dallo (1), G. Dreossi (1), J. Gabrieli (1), J.C. Gallet (5), A. Gambaro (2), J. Kohler (5), E. Isaksson (5), T. Martma (6), M. Maturilli (7), M. Vecchiato (2), M. Feltraco (2), N. Maffezzoli (1), F. Scoto(1), M. Vardè (1), R. Zangrando (1), A. Callegaro (1), C. Larousse (9), B. Luks (10), C. Zdanowich (11), B. Stenni (1)(2), C. Turetta (1)
Publikováno v:
The Arctic as seen from Ny-Ålesund: research results, new proposals and overviews. Rome 18th and 19th March 2019, pp. 40–41, Rome, 18-19/03/2019
info:cnr-pdr/source/autori:A. Spolaor (1), Carlo Barbante (1)(2), E. Barbaro (1), F. Burgay (1), P. Bjorkman (3), D. Cappelletti (4), G. Cozzi (1), F. Dallo (1), G. Dreossi (1), J. Gabrieli (1), J.C. Gallet (5), A. Gambaro (2), J. Kohler (5), E. Isaksson (5), T. Martma (6), M. Maturilli (7), M. Vecchiato (2), M. Feltraco (2), N. Maffezzoli (1), F. Scoto(1), M. Vardè (1), R. Zangrando (1), A. Callegaro (1), C. Larousse (9), B. Luks (10), C. Zdanowich (11), B. Stenni (1)(2), C. Turetta (1)/congresso_nome:The Arctic as seen from Ny-Ålesund: research results, new proposals and overviews. Rome 18th and 19th March 2019/congresso_luogo:Rome/congresso_data:18-19%2F03%2F2019/anno:2019/pagina_da:40/pagina_a:41/intervallo_pagine:40–41
info:cnr-pdr/source/autori:A. Spolaor (1), Carlo Barbante (1)(2), E. Barbaro (1), F. Burgay (1), P. Bjorkman (3), D. Cappelletti (4), G. Cozzi (1), F. Dallo (1), G. Dreossi (1), J. Gabrieli (1), J.C. Gallet (5), A. Gambaro (2), J. Kohler (5), E. Isaksson (5), T. Martma (6), M. Maturilli (7), M. Vecchiato (2), M. Feltraco (2), N. Maffezzoli (1), F. Scoto(1), M. Vardè (1), R. Zangrando (1), A. Callegaro (1), C. Larousse (9), B. Luks (10), C. Zdanowich (11), B. Stenni (1)(2), C. Turetta (1)/congresso_nome:The Arctic as seen from Ny-Ålesund: research results, new proposals and overviews. Rome 18th and 19th March 2019/congresso_luogo:Rome/congresso_data:18-19%2F03%2F2019/anno:2019/pagina_da:40/pagina_a:41/intervallo_pagine:40–41
The annual snow layer, during the winter, covers most of the Svalbard archipelago, becoming one of the most important factors influencing the Svalbard environment. The annual snow layer is an extremely dynamic portion of the Cryosphere and can be def
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::a15471e202f1cadc2e7e41241635612b
http://www.cnr.it/prodotto/i/426928
http://www.cnr.it/prodotto/i/426928