HR: 0800h
AN: A21C-0882    [Abstracts]
TI: Alaskan Ice Core Shows Relationship Between Asian Dust Storm And The Stratosphere Troposphere Exchange
AU: * Yasunari, T J
EM: teppei@hms.lowtem.hokudai.ac.jp
AF: Graduate School of Environmental Science, Hokkaido University, Kita-10 Nishi-5, Sapporo, 060-0810 Japan
AU: Shiraiwa, T
EM: shiraiwa@chikyu.ac.jp
AF: Institute of Low Temperature Science, Hokkaido University, Kita-19 Nishi-8, Sapporo, 060-0819 Japan
AU: Kanamori, S
EM: kanasyo@pop.lowtem.hokudai.ac.jp
AF: Graduate School of Environmental Science, Hokkaido University, Kita-10 Nishi-5, Sapporo, 060-0810 Japan
AU: Fujii, Y
EM: fujii@pmg.nipr.ac.jp
AF: National Institute of Polar Research, Kaga 1-9-10, Itabashi-ku, Tokyo, Tokyo, 173-8515 Japan
AU: Igarashi, M
EM: igarashi@pmg.nipr.ac.jp
AF: National Institute of Polar Research, Kaga 1-9-10, Itabashi-ku, Tokyo, Tokyo, 173-8515 Japan
AU: Yamazaki, K
EM: yamazaki@ees.hokudai.ac.jp
AF: Graduate School of Environmental Science, Hokkaido University, Kita-10 Nishi-5, Sapporo, 060-0810 Japan
AU: Benson, C S
EM: benson@gi.alaska.edu
AF: Geophysical Institute, University of Alaska Fairbanks, 903 Koyukuk Drive, P.O.Box 757320, Fairbanks, AK 99775-7320 United States
AU: Hondoh, T
EM: hnd@hms.lowtem.hokudai.ac.jp
AF: Institute of Low Temperature Science, Hokkaido University, Kita-19 Nishi-8, Sapporo, 060-0819 Japan
AB: Atmospheric dust absorbs and scatters solar radiation, and affects global radiative balance. Dust storm in arid and semi-arid regions in East Asia is main dust source in the northern hemisphere. Asian dust has large effect on radiative balance in the northern hemisphere and its long range transport to Alaskan region frequently occurs in springtime. On the other hand, the stratosphere-troposphere exchange (STE) is a important phenomenon for material exchange among the spheres. Some parameters such as tritium, ozone and beryllium can be transferred from the stratosphere into the troposphere under some conditions such as tropopause folding outbreaks, cut-off low developing and cyclonic activities. STE has a seasonal exchange with maximum in springtime. In June 2003, a 50m ice core was drilled at the summit of Mount Wrangell volcano (60N, 144W, 4100 m), Alaska. Dust particle concentration, tritium content and ratio of stable hydrogen isotope were analyzed. Tritium is the stratospheric tracer recently because the effect of nuclear tests in 1960s has faded these days, and its concentration is highest north of 30th parallel. Therefore, the ice core drilled here is ideal to assess both the Asian dust transport and STE. The core covers 1992-2002 with divided four seasons (winter, spring, late-spring and summer). Fine dust less than one micro meter generally represents long range transport increased in springtime every year. The drastic fine and coarse dust flux increases after 2000 correspond to recent increase of Asian Dust outbreaks. These indicate that Asian dust storm largely affects Mount Wrangell every year. Here we show the fact that highest positive correlation between tritium and fine dust fluxes was seen in the term from late-spring to summer (also high correlation between tritium and coarse dust fluxes in this term), suggesting that the stratosphere-troposphere exchange was most intensified by Asian dust storms in this transient season from spring to summer. Asian dust and STE are dominant in springtime. However, our results showed that these activities related each other the most from late-spring to summer. Asian dust storm and STE are not active in summer. Hence, our results are assumed to mainly reflect late-spring relationship between Asian dust storm and STE. Asian dust outbreaks with severe weather would impact on vertical and horizontal material circulation from the stratosphere to the troposphere. Further studies for Asian dust and STE especially focused on late-spring may lead to elucidate the mechanism of material circulation and assess the radiative forcing of Asian dust in springtime.
UR: http://hgxpro1.lowtem.hokudai.ac.jp/english/index_eng.html
DE: 0305 Aerosols and particles (0345, 4801, 4906)
DE: 0700 CRYOSPHERE (4540)
DE: 0720 Glaciers
DE: 0724 Ice cores (4932)
DE: 3362 Stratosphere/troposphere interactions
SC: Atmospheric Sciences [A]
MN: Fall Meeting 2005