Diel carbon monoxide cycling in the upper Sargasso Sea near Bermuda at the onset of spring and in midsummer

Oliver C. Zafiriou, Huixiang Xie, Norman B. Nelson, Raymond G. Najjar, Wei Wang

Research output: Contribution to journalArticle

42 Citations (Scopus)

Abstract

Rapid bio-oxidation of carbon monoxide (CO), a photoproduct of dissolved organic matter, results in diel cycles reflecting photochemical-biogeochemical- physical interactions. These cycles were characterized by timeseries studies of hydrography, meteorology, insolation, optics, and CO concentration ([CO]). Diel patterns of near-surface [CO] generally varied little seasonally, despite different forcings. In summer 30% of CO was below the mixed layer (ML); ML depths and optics indicate that two-layer photochemistry is common elsewhere. [CO] decayed at similar rates in both isolated layers. In spring CO extended to 150 m, reflecting nocturnal mixing. Cruise-average profiles indicated a shallower ML defined by CO than that defined by density, illustrating short-lived CO's sensitivity to recent mixing. Below the ML, [CO] dropped exponentially with depth on scales controlled by photoproduction in summer but mixing in spring. Mass-balance modeling of diurnal variations in CO column burden (CB) gave similar production rates in summer and spring (∼50 μmol m-2 d-1 CO), but different biooxidation rates, 1.5 ± 0.2 d-1 (summer, 0-50 m) and 0.52-0.66 d-1 (spring, 0-200 m). Outgassing averaged 4% of bio-oxidation in summer and 14% in spring. Similar production and differing sinks resulted in different CBs: 39.3 μmol m-2 (summer) versus 94.9 μmol m-2 (spring). Insolation-normalized CO productions were 1.8 times those in the oligotrophic equatorial Pacific. Improved, well-blanked analyses found [CO] at 200 m always <0.1 nmol L-1 in summer, and usually in spring. Prior reports of [CO] systematically ≥0.2 nmol L-1 at depth in well-stratified, oxic blue waters may be high because of method artifacts.

Original languageEnglish (US)
Pages (from-to)835-850
Number of pages16
JournalLimnology and Oceanography
Volume53
Issue number2
DOIs
StatePublished - Mar 2008

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Sargasso Sea
Bermuda
carbon monoxide
summer
mixed layer
insolation
optics
sea
solar radiation
oxidation
photochemistry
hydrography
dissolved organic matter
diurnal variation
meteorology
hydrology
artifact

All Science Journal Classification (ASJC) codes

  • Oceanography
  • Aquatic Science

Cite this

Zafiriou, Oliver C. ; Xie, Huixiang ; Nelson, Norman B. ; Najjar, Raymond G. ; Wang, Wei. / Diel carbon monoxide cycling in the upper Sargasso Sea near Bermuda at the onset of spring and in midsummer. In: Limnology and Oceanography. 2008 ; Vol. 53, No. 2. pp. 835-850.
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abstract = "Rapid bio-oxidation of carbon monoxide (CO), a photoproduct of dissolved organic matter, results in diel cycles reflecting photochemical-biogeochemical- physical interactions. These cycles were characterized by timeseries studies of hydrography, meteorology, insolation, optics, and CO concentration ([CO]). Diel patterns of near-surface [CO] generally varied little seasonally, despite different forcings. In summer 30{\%} of CO was below the mixed layer (ML); ML depths and optics indicate that two-layer photochemistry is common elsewhere. [CO] decayed at similar rates in both isolated layers. In spring CO extended to 150 m, reflecting nocturnal mixing. Cruise-average profiles indicated a shallower ML defined by CO than that defined by density, illustrating short-lived CO's sensitivity to recent mixing. Below the ML, [CO] dropped exponentially with depth on scales controlled by photoproduction in summer but mixing in spring. Mass-balance modeling of diurnal variations in CO column burden (CB) gave similar production rates in summer and spring (∼50 μmol m-2 d-1 CO), but different biooxidation rates, 1.5 ± 0.2 d-1 (summer, 0-50 m) and 0.52-0.66 d-1 (spring, 0-200 m). Outgassing averaged 4{\%} of bio-oxidation in summer and 14{\%} in spring. Similar production and differing sinks resulted in different CBs: 39.3 μmol m-2 (summer) versus 94.9 μmol m-2 (spring). Insolation-normalized CO productions were 1.8 times those in the oligotrophic equatorial Pacific. Improved, well-blanked analyses found [CO] at 200 m always <0.1 nmol L-1 in summer, and usually in spring. Prior reports of [CO] systematically ≥0.2 nmol L-1 at depth in well-stratified, oxic blue waters may be high because of method artifacts.",
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Diel carbon monoxide cycling in the upper Sargasso Sea near Bermuda at the onset of spring and in midsummer. / Zafiriou, Oliver C.; Xie, Huixiang; Nelson, Norman B.; Najjar, Raymond G.; Wang, Wei.

In: Limnology and Oceanography, Vol. 53, No. 2, 03.2008, p. 835-850.

Research output: Contribution to journalArticle

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AB - Rapid bio-oxidation of carbon monoxide (CO), a photoproduct of dissolved organic matter, results in diel cycles reflecting photochemical-biogeochemical- physical interactions. These cycles were characterized by timeseries studies of hydrography, meteorology, insolation, optics, and CO concentration ([CO]). Diel patterns of near-surface [CO] generally varied little seasonally, despite different forcings. In summer 30% of CO was below the mixed layer (ML); ML depths and optics indicate that two-layer photochemistry is common elsewhere. [CO] decayed at similar rates in both isolated layers. In spring CO extended to 150 m, reflecting nocturnal mixing. Cruise-average profiles indicated a shallower ML defined by CO than that defined by density, illustrating short-lived CO's sensitivity to recent mixing. Below the ML, [CO] dropped exponentially with depth on scales controlled by photoproduction in summer but mixing in spring. Mass-balance modeling of diurnal variations in CO column burden (CB) gave similar production rates in summer and spring (∼50 μmol m-2 d-1 CO), but different biooxidation rates, 1.5 ± 0.2 d-1 (summer, 0-50 m) and 0.52-0.66 d-1 (spring, 0-200 m). Outgassing averaged 4% of bio-oxidation in summer and 14% in spring. Similar production and differing sinks resulted in different CBs: 39.3 μmol m-2 (summer) versus 94.9 μmol m-2 (spring). Insolation-normalized CO productions were 1.8 times those in the oligotrophic equatorial Pacific. Improved, well-blanked analyses found [CO] at 200 m always <0.1 nmol L-1 in summer, and usually in spring. Prior reports of [CO] systematically ≥0.2 nmol L-1 at depth in well-stratified, oxic blue waters may be high because of method artifacts.

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