Reconstructing the past variability of Arctic sea ice provides an essential context for recent multi-year sea ice decline, although few quantitative reconstructions cover the Holocene period prior to the earliest historical records 1,200 years ago. Photochemical recycling of bromine is observed over first-year, or seasonal, sea ice in so-called “bromine explosions” and we employ a 1-D chemistry transport model to quantify processes of bromine enrichment over first-year sea ice and depositional transport over multi-year sea ice and land ice.
Original Source [2]
Technology Partners: MimirTech
Links:
[1] http://admin.indiaenvironmentportal.org.in/feature-article/canadian-arctic-sea-ice-reconstructed-bromine-greenland-neem-ice-core
[2] http://www.nature.com/articles/srep33925
[3] http://admin.indiaenvironmentportal.org.in/category/author/andrea-spolaor
[4] http://admin.indiaenvironmentportal.org.in/category/author/paul-vallelonga
[5] http://admin.indiaenvironmentportal.org.in/category/author/clara-turetta-et-al
[6] http://admin.indiaenvironmentportal.org.in/category/journal/scientific-reports
[7] http://admin.indiaenvironmentportal.org.in/category/thesaurus/greenland
[8] http://admin.indiaenvironmentportal.org.in/category/thesaurus/arctic
[9] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-change
[10] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-science
[11] http://admin.indiaenvironmentportal.org.in/category/thesaurus/canada
