Was the Enhanced CO2 Sink Following the Mt. Pinatubo Eruption Driven by an Increase in Diffuse Radiation?

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ADS bibcode: 2004AGUFM.B33A0241A
year: 2004
Listed Authors: Angert, A.; Biraud, S.; Bonfils, C.; Buermann, W.; Fung, I.
Listed Institutions: Berkeley Atmospheric Sciences Center, University of California, Berkeley., 307 McCone Hall, Berkeley, CA 94720-4767 United States; Berkeley Atmospheric Sciences Center, University of California, Berkeley., 307 McCone Hall, Berkeley, CA 94720-4767 United States; Berkeley Atmospheric Sciences Center, University of California, Berkeley., 307 McCone Hall, Berkeley, CA 94720-4767 United States; Berkeley Atmospheric Sciences Center, University of California, Berkeley., 307 McCone Hall, Berkeley, CA 94720-4767 United States; Berkeley Atmospheric Sciences Center, University of California, Berkeley., 307 McCone Hall, Berkeley, CA 94720-4767 United States

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University of California, Berkeley