HR: 0830h
AN: A31C-0056 [PDF]
TI: Evaluation of Tephra Found in the Law Dome Ice Core, East Antarctica
AU: * Kurbatov, A V
EM: akurbatov@maine.edu
AF: Climate Change Institute, 303 Bryand GCS, Orono, ME 04473 United States
AU: Dunbar, N W
EM: nelia@nmt.edu
AF: N.M.B.M.M.R./E\ &ES Department, New Mexico Tech, 801 Leroy Place, Socorro, NM 87801 United States
AU: Zielinski, G A
EM: gzielinski@maine.edu
AF: Climate Change Institute, 303 Bryand GCS, Orono, ME 04473 United States
AU: Mayewski, P A
EM: paul.mayewski@maine.edu
AF: Climate Change Institute, 303 Bryand GCS, Orono, ME 04473 United States
AU: Curran, M A
EM: mark.curran@utas.edu.au
AF: University of Tasmania, Antarctic CRC PO Box 252-80, Hobart, 7001
Australia
AU: Morgan, V
EM: vin.morgan@utas.edu.au
AF: University of Tasmania, Antarctic CRC PO Box 252-80, Hobart, 7001
Australia
AU: van Ommen, T D
EM: tas.van.ommen@utas.edu.au
AF: University of Tasmania, Antarctic CRC PO Box 252-80, Hobart, 7001
Australia
AB: The presence of tephra in several sections of the Law Dome ice core, collected in East Antarctica, has enabled us to expand
on the glaciochemical record of volcanic events detected in that core (Palmer et al., JGR, 2001). High snow accumulation,
low summer temperatures that inhibit melting and relatively moderate winds that limit the amount of post-depositional mixing
of snow at the coring site has helped produce a well-dated, and highly-resolved chronology of past volcanic activity. We
expanded on this chronology by filtering continuous meltwater samples covering the last 700 years and by analyzing volcanic
glass shards found in these sections with an electron microprobe with the objective of identifying the volcanic sources. We
found rhyolitic glass in 15 different layers and are presently working on identification of the source volcanoes. The lack
of significant populations of shards at many of these depths make the interpretation of these shards as time-stratigraphic
makers equivocal. However, the compositions are not known to occur in Antarctica volcanic systems, thus we believe that they
represent either southern hemisphere mid-latitude or equatorial eruptions. Several potential sources include rhyolitic
volcanoes in New Zealand or South America.
These results, in combination with the tephra analyses that we performed on the Antarctica Siple Dome and Taylor Dome ice
cores, suggest that in addition to the stratospheric transport of volcanic debris from South America and New Zealand to
Antarctica, tropospherically transported material may be another source of tephra particles found in Antarctica ice cores.
Large particles sizes as well as thickness of the several tephra layers combined with results of satellite observations on
propagation of volcanic clouds from recent eruptions of South American volcanoes allowed us to suspect this tropospheric mode
of transport. This work provides interesting new evidence on past circulation patterns in the Southern Hemisphere and on the
climatic-forcing capabilities of volcanic eruptions.
DE: 0370 Volcanic effects (8409)
DE: 1000 GEOCHEMISTRY (New field, replaces Rock Chemistry)
DE: 3319 General circulation
DE: 8409 Atmospheric effects (0370)
SC: Atmospheric Sciences [A]
MN: 2003 Fall Meeting