Spatial variability of climate and past atmospheric circulation patterns from central West Antarctic glaciochemistry

David B. Reusch, Paul A. Mayewski, Sallie I. Whitlow, Iqbal I. Pittalwala, Mark S. Twickler

Research output: Contribution to journalArticle

20 Citations (Scopus)

Abstract

Atmospheric circulation patterns and the spatial variability of atmospheric chemistry and moisture transport in central West Antarctica are investigated using new 40 year long (1954-1994 A.D.) glaciochemical and accumulation rate records developed from four firn cores from this region. The core sites lie on a 200 km traverse from 82° 22′ S, 119° 17′ W to 81° 22′ S, 107° 17′ W. The glaciochemical records represent the major ionic species present in Antarctic snow: Na+, K+, Mg2+, Ca2+, Cl-, NO3-, and SO42-. High spatial variability appears in comparisons of full record averages and poor intersite linear correlation results. Accumulation rates show 50-100% changes over distances of 50-100 km and sea-salt concentrations drop by 50% between the middle two sites. One likely contributor to the high variability seen at this spatial scale is variability in synoptic- and finer-scale meteorology. Empirical orthogonal function (EOF) analysis shows that 80% or more of the variance in site chemistry can be attributed to two types of air masses: winter season air (50-70% of site variance) with a strong marine signature (heavy loading of sea-salt species) and summer season air (21% of the variance), marked by marine biogenic non-sea-salt SO4 plus NO3. This pattern of winter and summer regimes appears at other West Antarctic sites suggesting it may apply to the entire region. We show that a general picture of the patterns of variability in West Antarctica can best be drawn by using an analysis technique that fully exploits high resolution, multiparameter, multisite data sets.

Original languageEnglish (US)
Article number1998JD200056
Pages (from-to)5985-6001
Number of pages17
JournalJournal of Geophysical Research Atmospheres
Volume104
Issue numberD6
DOIs
StatePublished - Mar 27 1999

Fingerprint

glaciochemistry
atmospheric circulation
climate
Salts
sea salt
accumulation rate
Air
Atmospheric chemistry
Orthogonal functions
Antarctic regions
atmospheric moisture
salts
Meteorology
firn
air
winter
Antarctica
atmospheric chemistry
summer
Snow

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Forestry
  • Oceanography
  • Aquatic Science
  • Ecology
  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth-Surface Processes
  • Atmospheric Science
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science
  • Palaeontology

Cite this

Reusch, D. B., Mayewski, P. A., Whitlow, S. I., Pittalwala, I. I., & Twickler, M. S. (1999). Spatial variability of climate and past atmospheric circulation patterns from central West Antarctic glaciochemistry. Journal of Geophysical Research Atmospheres, 104(D6), 5985-6001. [1998JD200056]. https://doi.org/10.1029/1998JD200056
Reusch, David B. ; Mayewski, Paul A. ; Whitlow, Sallie I. ; Pittalwala, Iqbal I. ; Twickler, Mark S. / Spatial variability of climate and past atmospheric circulation patterns from central West Antarctic glaciochemistry. In: Journal of Geophysical Research Atmospheres. 1999 ; Vol. 104, No. D6. pp. 5985-6001.
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Spatial variability of climate and past atmospheric circulation patterns from central West Antarctic glaciochemistry. / Reusch, David B.; Mayewski, Paul A.; Whitlow, Sallie I.; Pittalwala, Iqbal I.; Twickler, Mark S.

In: Journal of Geophysical Research Atmospheres, Vol. 104, No. D6, 1998JD200056, 27.03.1999, p. 5985-6001.

Research output: Contribution to journalArticle

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AU - Reusch, David B.

AU - Mayewski, Paul A.

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AU - Twickler, Mark S.

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AB - Atmospheric circulation patterns and the spatial variability of atmospheric chemistry and moisture transport in central West Antarctica are investigated using new 40 year long (1954-1994 A.D.) glaciochemical and accumulation rate records developed from four firn cores from this region. The core sites lie on a 200 km traverse from 82° 22′ S, 119° 17′ W to 81° 22′ S, 107° 17′ W. The glaciochemical records represent the major ionic species present in Antarctic snow: Na+, K+, Mg2+, Ca2+, Cl-, NO3-, and SO42-. High spatial variability appears in comparisons of full record averages and poor intersite linear correlation results. Accumulation rates show 50-100% changes over distances of 50-100 km and sea-salt concentrations drop by 50% between the middle two sites. One likely contributor to the high variability seen at this spatial scale is variability in synoptic- and finer-scale meteorology. Empirical orthogonal function (EOF) analysis shows that 80% or more of the variance in site chemistry can be attributed to two types of air masses: winter season air (50-70% of site variance) with a strong marine signature (heavy loading of sea-salt species) and summer season air (21% of the variance), marked by marine biogenic non-sea-salt SO4 plus NO3. This pattern of winter and summer regimes appears at other West Antarctic sites suggesting it may apply to the entire region. We show that a general picture of the patterns of variability in West Antarctica can best be drawn by using an analysis technique that fully exploits high resolution, multiparameter, multisite data sets.

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