Abstract
This chapter focuses on the aridification of the Asian interior during the Late Cenozoic, with an emphasis on modern dust and black carbon, and examines global iron connections which originate from dust derived from the arid interior of Asia. The modern formation of Asian dust, the connection of black carbon, paleofires and climate change, and relationships among dust, global iron cycles, marine productivity and climate change were discussed. The aridification history of the Asian interior were reconstructed from Chinese loess record.
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Notes
- 1.
As more chemical data have become available, Asian dust is now known to actually contain about 7 % Al (and 4 % Fe) by weight Zhang, X.Y., Gong, S.L., Shen, Z.X., Mei, F.M., Xi, X.X., Liu, L.C., Zhou, Z.J., Wang, D., Wang, Y.Q., Cheng, Y., 2003a. Characterization of soil dust aerosol in China and its transport/distribution during 2001 ACE-Asia. 1. Network Observations. J. Geophys. Res 108, doi:10.1029/1004 2002JD002632.
- 2.
Mineral dust also absorbs sunlight but due to its strong reflective characteristics, it is generally thought to be an agent of atmospheric cooling.
- 3.
Radiative forcing is the change in stratospherically adjusted radiative flux at the tropopause, compared to 1750AD as defined by the Intergovernmental Panel on Climate Change Forster, P.V., Ramaswamy, V., Artaxo, P., Berntsen, T., Betts, R., Fahey, D.W., Haywood, J., Lean, J., Lowe, D.C., Myhre, G., Nganga, J., R. Prinn, Raga, G., Schulz, M., Dorland, R.V., 2007. Changes in atmospheric constituents and in radiative forcing. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA.
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Zhang, X., Han, Y., Sun, Y., Cao, J., An, Z. (2014). Asian Dust, Eolian Iron and Black Carbon—Connections to Climate Changes. In: An, Z. (eds) Late Cenozoic Climate Change in Asia. Developments in Paleoenvironmental Research, vol 16. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-7817-7_4
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