HR: 1340h
AN: PP13A-0577    [Abstracts]
TI: Atmospheric Circulation and Climate Variability over the Last 200 Years from Talos Dome (East Antarctica) Dust Record
AU: Sala, M
EM: bdelmonte@nest.it
AF: University of Milano-Bicocca, DISAT, Dept. Environmental Sciences, Piazza della Scienza 1 , milano, 20126 Italy
AU: * Marino, F
EM: federica.marino@unimib.it
AF: University of Milano-Bicocca, DISAT, Dept. Environmental Sciences, Piazza della Scienza 1 , milano, 20126 Italy
AU: Delmonte, B
EM: bdelmonte@nest.it
AF: University of Milano-Bicocca, DISAT, Dept. Environmental Sciences, Piazza della Scienza 1 , milano, 20126 Italy
AU: Uglietti, C
EM: ugliettichiara@yahoo.it
AF: University of Milano-Bicocca, DISAT, Dept. Environmental Sciences, Piazza della Scienza 1 , milano, 20126 Italy
AU: Maggi, V
EM: valter.maggi@unimib.it
AF: University of Milano-Bicocca, DISAT, Dept. Environmental Sciences, Piazza della Scienza 1 , milano, 20126 Italy
AB: Aeolian dust concentration and size distribution measurements performed on the first 30 m of the Talos Dome (East Antarctica, 72ø48'S, 159ø06'E) firn core, drilled during the 1996 PNRA-ITASE (Programma Nazionale di Ricerche in Antartide-International Trans-Antarctic Scienticic Expedition) traverse, provide a record of recent climatic and atmospheric history over the East Antarctic sector facing the Ross Sea-Oates Coast (Southern Ocean). Talos Dome (2316 m a.s.l.) is located in the Northern Victoria Land at the topoghraphic summit of a dome (Frezzotti et al., 1998). More than 500 samples analyzed from 1.5 to 30 m allowed to obtain a record of atmospheric mineral dust at high temporal resolution (sub-annual) for the last ~200 years. The average dust concentration and size distribution levels, as well as their variability, are higher from early 1800 to the mid-1900 with respect to the most recent part of the record, with a sharp decrease occurring around 1950-55. The concentration and size distribution of microparticles almost covary over the period investigated, high dust concentrations being generally associated to coarser dust and vice versa. Moreover, average modal value of the volume (mass) background dust size distribution and total dust concentration are slightly higher that typical Holocene values for other East Antarctic sites (Delmonte et al., 2004). These evidences suggest that mixing of fine-grained atmospheric dust from long-range transport with more local sources such as the rock outcrops of the Northern Victoria Land, for example, cannot be excluded. A possible local contribution for dust was also suggested by Maggi and Petit (1998) from earlier dust investigations on a firn core drilled in the Northern Victoria Land close to the Transantarctic Mountains (Hercules Nev‚, 73ø06'S; 165ø27'E). Interestingly, the dust concentration and size distribution profiles are embedded by clear cycles having periodicity of 7-8 years on average overall the 200 years of the record. The magnitude of these variations is a factor of 10 to 100 for the concentration and a factor 3 for the mode. Assuming the arrivals of coarse (fine) -grained dust having high (low) concentration directly related to the easier (more difficult) penetration of troposphere air masses to Talos Dome and hence to the pattern of meridional wind, our data evidence that a modulation of the atmospheric circulation at these timescales does exist. This periodicity corresponds to the time taken by the Antarctic Circumpolar Wave (White and Peterson, 1996) to encircle the Southern Ocean. We hypothesize the cyclic pattern observed as linked to the circumpolar propagation of ocean-sea ice-atmosphere anomalies in the Southern Ocean, imprinted particularly in the Ross Sea region, modulating the atmospheric circulation pattern at interannual timescale and finally the atmospheric dust advection to the site. The Talos Dome dust record, therefore, can be considered as first-order indicator capable to mirror the past Southern Ocean-atmosphere coupled mode of variability.
DE: 9310 Antarctica
DE: 3309 Climatology (1620)
DE: 1610 Atmosphere (0315, 0325)
DE: 1620 Climate dynamics (3309)
DE: 0305 Aerosols and particles (0345, 4801)
SC: Paleoceanography and Paleoclimatology [PP]
MN: 2004 AGU Fall Meeting