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On the detection of summertime terrestrial photosynthetic variability from its atmospheric signature
Authors
Baldocchi
Barford
+24 more
Bonan
Boville
Collatz
Céline Bonfils
Dai
Dickinson
Durre
Durre
Farquhar
Friedlingstein
Hicke
Inez Fung
Jasmin John
Karl
Kiehl
Levis
Randerson
Schimel
Schwartz
Schwartz
Scott Doney
Sellers
Sellers
Thompson
Publication date
11 May 2004
Publisher
'American Geophysical Union (AGU)'
Doi
Cite
Abstract
Author Posting. © American Geophysical Union, 2004. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 31 (2004): L09207, doi:10.1029/2004GL019453.We identify the climatic signatures of the summertime terrestrial photosynthesis variability using a long simulation of pre-industrial climate performed with the NCAR coupled global climate-carbon model. Since plant physiology controls simultaneously CO2 uptake and surface fluxes of water, changes in photosynthesis are accompanied by changes in numerous climate variables: daily maximum temperature, diurnal temperature range, Bowen ratio, canopy temperature and tropospheric lapse rate. Results show that these climate variables may be used as powerful proxies for photosynthesis activity for subtropical vegetation and for tropical vegetation when photosynthetic variability may be limited by water availability.Support for this work was provided by National Science Foundation grant ATM-9987457, NASA EOS-IDS grant NAG5-9514, WHOI contribution #11077 and the NCAR Climate Simulation Laboratory (CSL)
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