Sea ice dynamics influence halogen deposition to Svalbard (Articolo in rivista)

Type

• Articolo in rivista (Classe)
• Prodotto della ricerca (Classe)

Label

• Sea ice dynamics influence halogen deposition to Svalbard (Articolo in rivista) (literal)

Anno

• 2013-01-01T00:00:00+01:00 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi

• 10.5194/tc-7-1645-2013 (literal)

Alternative label

• Spolaor, A.; Gabrieli, J.; Martma, T.; Kohler, J.; Bjorkman, M. B.; Isaksson, E.; Varin, C.; Vallelonga, P.; Plane, J. M. C.; Barbante, C. (2013)
  Sea ice dynamics influence halogen deposition to Svalbard
  in The cryosphere (Print)
  (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori

• Spolaor, A.; Gabrieli, J.; Martma, T.; Kohler, J.; Bjorkman, M. B.; Isaksson, E.; Varin, C.; Vallelonga, P.; Plane, J. M. C.; Barbante, C. (literal)

Pagina inizio

• 1645 (literal)

Pagina fine

• 1658 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume

• 7 (literal)

Rivista

• ?The ?cryosphere (Rivista)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali

• 14 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo

• 5 (literal)

Note

• ISI Web of Science (WOS) (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni

• Universita Ca Foscari Venezia; Universita Ca Foscari Venezia; Tallinn University of Technology; Norwegian Polar Res Inst; University of Oslo; Niels Bohr Institute; Curtin University of Technology; University of Leeds (literal)

Titolo

• Sea ice dynamics influence halogen deposition to Svalbard (literal)

Abstract

• Sea ice is an important parameter in the climate system and its changes impact upon the polar albedo and atmospheric and oceanic circulation. Iodine (I) and bromine (Br) have been measured in a shallow firn core drilled at the summit of the Holtedahlfonna glacier (Northwest Spitsbergen, Svalbard). Changing I concentrations can be linked to the March-May maximum sea ice extension. Bromine enrichment, indexed to the Br / Na sea water mass ratio, appears to be influenced by changes in the seasonal sea ice area. I is emitted from marine biota and so the retreat of March-May sea ice coincides with enlargement of the open-ocean surface which enhances marine primary production and consequent I emission. The observed Br enrichment could be explained by greater Br emissions during the Br explosions that have been observed to occur mainly above first year sea ice during the early springtime. In this work we present the first comparison between halogens in surface snow and Arctic sea ice extension. Although further investigation is required to characterize potential depositional and post-depositional processes, these preliminary findings suggest that I and Br can be linked to variability in the spring maximum sea ice extension and seasonal sea ice surface area. (literal)

Prodotto di

• Institute for the Dynamics of Environmental Processes (IDPA) (Istituto)
• Ambiente e clima: processi, cambiamenti globali e contaminazione chimica in aree polari, remote e antropizzate (TA.P02.024.001) (Modulo)

Autore CNR

• CARLO BARBANTE (Persona)

Incoming links:

Prodotto

• Institute for the Dynamics of Environmental Processes (IDPA) (Istituto)
• Ambiente e clima: processi, cambiamenti globali e contaminazione chimica in aree polari, remote e antropizzate (TA.P02.024.001) (Modulo)

Autore CNR di

• CARLO BARBANTE (Persona)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#rivistaDi

• ?The ?cryosphere (Rivista)