Open AccessCarbonaceous species and humic like substances (HULIS) in Arctic snowpack during OASIS field campaign in Barrow
Author(s) -
Voisin Didier,
Jaffrezo JeanLuc,
Houdier Stéphan,
Barret Manuel,
Cozic Julie,
King Martin D.,
France James L.,
Reay Holly J.,
Grannas Amanda,
Kos Gregor,
Ariya Parisa A.,
Beine Harry J.,
Domine Florent
Publication year - 2012
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2011jd016612
Subject(s) - snowpack , snow , dissolved organic carbon , arctic , environmental science , environmental chemistry , albedo (alchemy) , total organic carbon , flux (metallurgy) , deposition (geology) , atmospheric sciences , chemistry , geology , sediment , oceanography , geomorphology , art , organic chemistry , performance art , art history
Snowpacks contain many carbonaceous species that can potentially impact on snow albedo and arctic atmospheric chemistry. During the OASIS field campaign, in March and April 2009, Elemental Carbon (EC), Water insoluble Organic Carbon (WinOC) and Dissolved Organic Carbon (DOC) were investigated in various types of snow: precipitating snows, remobilized snows, wind slabs and depth hoars. EC was found to represent less than 5% of the Total Carbon Content (TCC = EC + WinOC + DOC), whereas WinOC was found to represent an unusual 28 to 42% of TCC. Snow type was used to infer physical processes influencing the evolution of different fractions of DOC. DOC is highest in soil influenced indurated depth hoar layers due to specific wind related formation mechanisms in the early season. Apart from this specific snow type, DOC is found to decrease from precipitating snow to remobilized snow to regular depth hoar. This decrease is interpreted as due to cleaving photochemistry and physical equilibration of the most volatile fraction of DOC. Depending on the relative proportions of diamond dust and fresh snow in the deposition of the seasonal snowpack, we estimate that 31 to 76% of DOC deposited to the snowpack is reemitted back to the boundary layer. Under the assumption that this reemission is purely photochemical, we estimate an average flux of VOC out of the snowpack of 20 to 170 μ g C m −2 h −1 . Humic like substances (HULIS), short chain diacids and aldehydes are quantified, and showed to represent altogether a modest (<20%) proportion of DOC, and less than 10% of DOC + WinOC. HULIS optical properties are measured and could be consistent with aged biomass burning or a possible marine source.