Meridional transport and deposition of atmospheric 10 Be

By U. Heikkilä, J. Beer, Johann Feichter. 2008

154 citations recorded by the source corpus.

Be concentrations measured in ice cores exhibit larger temporal variability than expected based on theoretical production calculations. To investigate whether this is due to atmospheric transport a general circulation model study is performed with the 10 Be production divided into strato- spheric, tropospheric tropical, tropospheric subtropical and tropospheric polar sources. A control run with present day 10 Be production rate is compared with a run during a geo- magnetic minimum. The present 10 Be production rate is 4-5 times higher at high latitudes than in the tropics whereas dur- ing a period of no geomagnetic dipole field it is constant at all latitudes. The 10 Be deposition fluxes, however, show a very similar latitudinal distribution in both the present day and the geomagnetic minimum run indicating that 10 Be is well mixed in the atmosphere before its deposition. This is also con- firmed by the fact that the contribution of 10 Be produced in the stratosphere is dominant (55%-70%) and relatively con- stant at all latitudes. The contribution of stratospheric 10 Be is approximately 70% in Greenland and 60% in Antarctica reflecting the weaker stratosphere-troposphere air exchange in the Southern Hemisphere.

Subfields: Astronomy and Astrophysics, Atmospheric Science, Radiological and Ultrasound Technology

View Paper: https://www.semanticscholar.org/paper/2f01613d030823aca79830f4fc247707becfc3fb

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In Astronomy and Astrophysics

  1. E. Bard
  2. G. Delaygue

In Atmospheric Science

  1. C. Hoose
  2. Ulrike Lohmann
  3. P. Stier
  4. Johann Feichter
  5. Sylvaine Ferrachat
  6. A. Donkelaar
  7. E. Bard
  8. Randall V. Martin

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