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Constraining surface carbon fluxes using in situ measurements of carbonyl sulfide and carbon dioxide
Author(s) -
Berkelhammer M.,
Asaf D.,
Still C.,
Montzka S.,
Noone D.,
Gupta M.,
Provencal R.,
Chen H.,
Yakir D.
Publication year - 2014
Publication title -
global biogeochemical cycles
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.512
H-Index - 187
eISSN - 1944-9224
pISSN - 0886-6236
DOI - 10.1002/2013gb004644
Subject(s) - carbonyl sulfide , environmental science , carbon dioxide , tracer , photosynthetically active radiation , diurnal cycle , soil water , carbon cycle , atmospheric sciences , eddy covariance , trace gas , chemistry , biogeochemical cycle , carbon sink , flux (metallurgy) , environmental chemistry , photosynthesis , ecosystem , soil science , ecology , geology , sulfur , organic chemistry , biology , physics , biochemistry , nuclear physics
Understanding the processes that control the terrestrial exchange of carbon is critical for assessing atmospheric CO 2 budgets. Carbonyl sulfide (COS) is taken up by vegetation during photosynthesis following a pathway that mirrors CO 2 but has a small or nonexistent emission component, providing a possible tracer for gross primary production. Field measurements of COS and CO 2 mixing ratios were made in forest, senescent grassland, and riparian ecosystems using a laser absorption spectrometer installed in a mobile trailer. Measurements of leaf fluxes with a branch‐bag gas‐exchange system were made across species from 10 genera of trees, and soil fluxes were measured with a flow‐through chamber. These data show (1) the existence of a narrow normalized daytime uptake ratio of COS to CO 2 across vascular plant species of 1.7, providing critical information for the application of COS to estimate photosynthetic CO 2 fluxes and (2) a temperature‐dependent normalized uptake ratio of COS to CO 2 from soils. Significant nighttime uptake of COS was observed in broad‐leafed species and revealed active stomatal opening prior to sunrise. Continuous high‐resolution joint measurements of COS and CO 2 concentrations in the boundary layer are used here alongside the flux measurements to partition the influence that leaf and soil fluxes and entrainment of air from above have on the surface carbon budget. The results provide a number of critical constraints on the processes that control surface COS exchange, which can be used to diagnose the robustness of global models that are beginning to use COS to constrain terrestrial carbon exchange.