TY - JOUR
T1 - Evaluating Oceanic Uptake of Atmospheric CCl4
T2 - A Combined Analysis of Model Simulations and Observations
AU - Suntharalingam, Parvadha
AU - Buitenhuis , E
AU - Carpenter, Lucy Jane
AU - Andrews, Stephen Joseph
AU - Hackenberg, Sina
AU - BUTLER, J
AU - Messias , MJ
PY - 2019/1/16
Y1 - 2019/1/16
N2 - We provide new estimates of the air‐sea flux of CCl4 using simulations from a global ocean biogeochemistry model (NEMO‐PlankTOM) in combination with depth‐resolved CCl4 observations from global oceanic databases. Estimates of global oceanic CCl4 uptake are derived from a range of model analyses, including prescribed parameterizations using reported values on hydrolysis and degradation, and analyses optimized using the global observational databases. We evaluate the sensitivity of our results to uncertainties in air‐sea gas exchange parameterization, estimation period, and circulation processes. Our best constrained estimate of ocean CCl4 uptake for the period 1996–2000 is 20.1 Gg/year (range 16.6–22.7), corresponding to estimates of the partial atmospheric lifetime with respect to ocean uptake of 124 (110–150) years. This new oceanic lifetime implies higher emissions of CCl4 than currently estimated and therefore a larger missing atmospheric source of CCl4.
AB - We provide new estimates of the air‐sea flux of CCl4 using simulations from a global ocean biogeochemistry model (NEMO‐PlankTOM) in combination with depth‐resolved CCl4 observations from global oceanic databases. Estimates of global oceanic CCl4 uptake are derived from a range of model analyses, including prescribed parameterizations using reported values on hydrolysis and degradation, and analyses optimized using the global observational databases. We evaluate the sensitivity of our results to uncertainties in air‐sea gas exchange parameterization, estimation period, and circulation processes. Our best constrained estimate of ocean CCl4 uptake for the period 1996–2000 is 20.1 Gg/year (range 16.6–22.7), corresponding to estimates of the partial atmospheric lifetime with respect to ocean uptake of 124 (110–150) years. This new oceanic lifetime implies higher emissions of CCl4 than currently estimated and therefore a larger missing atmospheric source of CCl4.
KW - air-sea fluxes
KW - carbon tetrachloride
KW - halocarbon
KW - ozone-depleting substance
UR - http://www.scopus.com/inward/record.url?scp=85059902016&partnerID=8YFLogxK
U2 - 10.1029/2018GL080612
DO - 10.1029/2018GL080612
M3 - Article
SN - 0094-8276
VL - 46
SP - 472
EP - 482
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 1
ER -