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doi:10.1016/j.gca.2004.02.010 O effects in the hydrologic cycle: Indirect evidence and implications
 

Summary: doi:10.1016/j.gca.2004.02.010
Kinetic 17
O effects in the hydrologic cycle: Indirect evidence and implications
ALON ANGERT,1,
* CHRISTOPHER D. CAPPA,2
and DONALD J. DEPAOLO
3,4
1
Berkeley Atmospheric Sciences Center, University of California, Berkeley, CA 94720-4767, USA
2
Department of Chemistry, University of California, Berkeley, CA 94720-1460, USA
3
Department of Earth and Planetary Science, University of California, Berkeley, CA 94720-4767, USA
4
Earth Sciences Division, E. O. Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA
(Received July 7, 2003; accepted in revised form February 9, 2004)
Abstract--The abundances of 18
O and deuterium in the present and past hydrologic cycle have proven to be
an important tool in Earth systems science. In contrast, the abundance of 17
O in precipitation has thus far been

  

Source: Alon, Angert - Institute of Earth Sciences, Hebrew University of Jerusalem

 

Collections: Geosciences