Halogen-based reconstruction of Russian Arctic sea ice area from the Akademii Nauk ice core (Severnaya Zemlya)

• Published in: The Cryosphere
• Main Authors: Spolaor, Andrea, VARIN, Cristiano, KIRCHGEORG, TORBEN, VALLELONGA, PAUL TRAVIS, Opel, T., Mcconnell, J. R., Maselli, O. J., Spreen, G., Fritzsche, D., Saiz Lopez, A.
• Other Authors: Varin, Cristiano, Kirchgeorg, Torben, Vallelonga, PAUL TRAVIS
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2016
• Subjects: MASS-SPECTROMETRY; IODINE EMISSIONS; BOUNDARY-LAYER; WEDDELL SEA; NORDIC SEAS; VARIABILITY; ANTARCTICA; BROMINE; CLIMATE; RECORD; Settore CHIM/01 - Chimica Analitica; Arctic; Weddell Sea; Laptev Sea; Weddell; Severnaya Zemlya; albedo; Antarc*; Antarctica; ice core; laptev; Nordic Seas; Sea ice
• Online Access: http://hdl.handle.net/10278/3665335; https://doi.org/10.5194/tc-10-245-2016

The role of sea ice in the Earth climate system is still under debate, although it is known to influence albedo, ocean circulation, and atmosphere-ocean heat and gas exchange. Here we present a reconstruction of 1950 to 1998AD sea ice in the Laptev Sea based on the Akademii Nauk ice core (Severnaya Zemlya, Russian Arctic). The chemistry of halogens bromine (Br) and iodine (I) is strongly active and influenced by sea ice dynamics, in terms of physical, chemical and biological process. Bromine reacts on the sea ice surface in autocatalyzing "bromine explosion" events, causing an enrichment of the Br/Na ratio and hence a bromine excess (Br-exc) in snow compared to that in seawater. Iodine is suggested to be emitted from algal communities growing under sea ice. The results suggest a connection between Br-exc and spring sea ice area, as well as a connection between iodine concentration and summer sea ice area. The correlation coefficients obtained between Br-exc and spring sea ice (r = 0.44) as well as between iodine and summer sea ice (r = 0.50) for the Laptev Sea suggest that these two halogens could become good candidates for extended reconstructions of past sea ice changes in the Arctic.