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Covariation of Airborne Biogenic Tracers (CO 2 , COS, and CO) Supports Stronger Than Expected Growing Season Photosynthetic Uptake in the Southeastern US
Author(s) -
Parazoo Nicholas C.,
Bowman Kevin W.,
Baier Bianca C.,
Liu Junjie,
Lee Meemong,
Kuai Le,
Shiga Yoichi,
Baker Ian,
Whelan Mary E.,
Feng Sha,
Krol Maarten,
Sweeney Colm,
Runkle Benjamin R.,
Tajfar Elahe,
Davis Kenneth J.
Publication year - 2021
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 - 10.1029/2021gb006956
Subject(s) - biogeochemical cycle , environmental science , sink (geography) , atmospheric sciences , carbon sink , temperate climate , evergreen , deciduous , growing season , greenhouse gas , carbon cycle , ecosystem , climate change , chemistry , environmental chemistry , ecology , geography , oceanography , geology , cartography , biology
The Atmospheric Carbon Transport (ACT)‐America Earth Venture mission conducted five airborne campaigns across four seasons from 2016 to 2019, to study the transport and fluxes of Greenhouse gases across the eastern United States. Unprecedented spatial sampling of atmospheric tracers (CO 2 , carbon monoxide [CO], carbonyl sulfide [COS]) related to biospheric processes offers opportunities to improve our qualitative and quantitative understanding of seasonal and spatial patterns of biospheric carbon uptake. Here, we examine co‐variation of boundary layer enhancements of CO 2 , CO, and COS across three diverse regions: the crop‐dominated Midwest, evergreen‐dominated South, and deciduous broadleaf‐dominated Northeast. To understand the biogeochemical processes controlling these tracers, we compare the observed co‐variation to simulated co‐variation resulting from model‐ and satellite‐ constrained surface carbon fluxes. We found indication of a common terrestrial biogenic sink of CO 2 and COS and secondary production of CO from biogenic sources in summer throughout the eastern US, driven by stomatal conductance. Upper Midwest crops drive Δ CO 2 and Δ COS depletion from early to late summer. Northeastern temperate forests drive Δ CO 2 and Δ COS depletion in late summer. The unprecedented ACT‐America flask samples uncovered evidence that southern humid temperate forests photosynthesize and absorb CO 2 and COS, and emit CO precursors, deep into the growing season. Satellite‐ constrained carbon fluxes capture much of the observed seasonal and spatial variability, but underestimate the magnitude of net CO 2 and COS depletion in the South, indicating a stronger than expected net sink of CO 2 in late summer. Additional sampling of the South will more accurately constrain underlying biological processes and climate sensitivities governing southern carbon dynamics.