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AGU: Geophysical Research Letters

 

Index Terms

  • Atmospheric Composition and Structure: Constituent sources and sinks
  • Global Change: Remote sensing
  • Meteorology and Atmospheric Dynamics: Climatology
  • Meteorology and Atmospheric Dynamics: Ocean/atmosphere interactions
  • Meteorology and Atmospheric Dynamics: Remote sensing

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 31, L16114, 4 PP., 2004
doi:10.1029/2004GL020655

Frost flowers on sea ice as a source of sea salt and their influence on tropospheric halogen chemistry

L. Kaleschke

Institute of Environmental Physics, University of Bremen, Germany

A. Richter

Institute of Environmental Physics, University of Bremen, Germany

J. Burrows

Institute of Environmental Physics, University of Bremen, Germany

O. Afe

Institute of Environmental Physics, University of Bremen, Germany

G. Heygster

Institute of Environmental Physics, University of Bremen, Germany

J. Notholt

Institute of Environmental Physics, University of Bremen, Germany

A. M. Rankin

British Antarctic Survey, Natural Environment Research Council, Cambridge, UK

H. K. Roscoe

British Antarctic Survey, Natural Environment Research Council, Cambridge, UK

J. Hollwedel

Institute of Environmental Physics, University of Heidelberg, Germany

T. Wagner

Institute of Environmental Physics, University of Heidelberg, Germany

H.-W. Jacobi

Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany

Frost flowers grow on newly-formed sea ice from a saturated water vapour layer. They provide a large effective surface area and a reservoir of sea salt ions in the liquid phase with triple the ion concentration of sea water. Recently, frost flowers have been recognised as the dominant source of sea salt aerosol in the Antarctic, and it has been speculated that they could be involved in processes causing severe tropospheric ozone depletion events during the polar sunrise. These events can be explained by heterogeneous autocatalytic reactions taking place on salt-laden ice surfaces which exponentially increase the reactive gas phase bromine (“bromine explosion”). We analyzed tropospheric bromine monoxide (BrO) and the sea ice coverage both measured from satellite sensors. Our model based interpretation shows that young ice regions potentially covered with frost flowers seem to be the source of bromine found in bromine explosion events.

Received 2 June 2004; accepted 2 August 2004; published 25 August 2004.

Citation: Kaleschke, L., et al. (2004), Frost flowers on sea ice as a source of sea salt and their influence on tropospheric halogen chemistry, Geophys. Res. Lett., 31, L16114, doi:10.1029/2004GL020655.

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