On the coefficients of small eddy and surface divergence models for the air-water gas transfer velocity

2015 ◽  
Vol 120 (3) ◽  
pp. 2129-2146 ◽  
Author(s):  
Binbin Wang ◽  
Qian Liao ◽  
Joseph H. Fillingham ◽  
Harvey A. Bootsma
Keyword(s):  
Gas Transfer ◽  
Transfer Velocity ◽  
Gas Transfer Velocity ◽  
Water Gas ◽  
Small Eddy

scholarly journals Statistics of surface divergence and their relation to air-water gas transfer velocity

2012 ◽  
Vol 117 (C5) ◽  
pp. n/a-n/a ◽  
Author(s):  
William E. Asher ◽  
Hanzhuang Liang ◽  
Christopher J. Zappa ◽  
Mark R. Loewen ◽  
Moniz A. Mukto ◽  
...  
Keyword(s):  
Gas Transfer ◽  
Transfer Velocity ◽  
Gas Transfer Velocity ◽  
Water Gas

scholarly journals Changes in gross oxygen production, net oxygen production, and air-water gas exchange during seasonal ice melt in the Bras d'Or Lake, a Canadian estuary

2017 ◽  
Author(s):  
Cara C. Manning ◽  
Rachel H. R. Stanley ◽  
David P. Nicholson ◽  
Brice Loose ◽  
Ann Lovely ◽  
...  
Keyword(s):  
Gas Exchange ◽  
Open Water ◽  
Gas Transfer ◽  
Polar Regions ◽  
Oxygen Production ◽  
Transfer Velocity ◽  
Gas Transfer Velocity ◽  
Ice Melt ◽  
Wide Range ◽  
Water Gas

Abstract. Sea ice is an important control on gas exchange and primary production in polar regions. We measured net oxygen production and gross oxygen production using near-continuous measurements of the O2 / Ar gas ratio and discrete measurements of the triple isotopic composition of O2 in the Bras d'Or Lake, an estuary in Nova Scotia, Canada, as the bay transitioned from ice-covered to ice-free conditions. The volumetric gross oxygen production was 5.4(+2.8−1.6) mmol O2 m−3 d−1, similar at the beginning and end of the time-series, and likely peaked at the end of the ice melt period. Net oxygen production displayed more temporal variability and the system was on average net autotrophic during ice melt and net heterotrophic following the ice melt. We performed the first field-based dual tracer release experiment in ice-covered water to quantify air-water gas exchange. The gas transfer velocity at > 90 % ice cover was 6 % of the rate for nearly ice-free conditions. Published studies have shown a wide range of results for gas transfer velocity in the presence of ice, and this study indicates that gas transfer through ice is much slower than the rate of gas transfer through open water. The results also indicate that both primary producers and heterotrophs are active in Whycocomagh Bay during spring while it is covered in ice.

Estimating the air-sea gas transfer velocity from a statistical reconstruction of ocean turbulence observations

2021 ◽  
Author(s):  
Giulia Carella ◽  
Leonie Esters ◽  
Martí Galí Tàpias ◽  
Carlos Gomez Gonzalez ◽  
Raffaele Bernardello
Keyword(s):  
Kinetic Energy ◽  
Gas Transfer ◽  
Multiple Sources ◽  
Ocean Turbulence ◽  
Transfer Velocity ◽  
Gas Transfer Velocity ◽  
Statistical Reconstruction ◽  
Gp Model ◽  
The Relationship ◽  
Small Eddy

<p>Although the air-sea gas transfer velocity k is usually parameterized with wind speed, the so-called small-eddy model suggests a relationship between k and the ocean surface turbulence in the form of the dissipation rate of turbulent kinetic energy ε. However, available observations of ε from oceanographic cruises are spatially and temporally sparse. In this study, we use a Gaussian Process (GP) model to investigate the relationship between the observed profiles of ε and co-located atmospheric and oceanic fields from the ERA5 reanalysis. The model is then used to construct monthly maps of ε and to estimate the climatological air-sea gas transfer velocity from existing parametrizations. As an independent  validation,  the same model is also trained on EC-Earth3 outputs with the objective of reproducing the temporal and spatial patterns of turbulence kinetic energy as simulated by EC-Earth3. The ability to predict ε is instrumental to achieve better estimates of air-sea gas exchange that take into account multiple sources of upper ocean turbulence beyond wind stress.</p>

scholarly journals A Structure Function Model Recovers the Many Formulations for Air-Water Gas Transfer Velocity

2018 ◽  
Vol 54 (9) ◽  
pp. 5905-5920 ◽  
Author(s):  
Gabriel Katul ◽  
Ivan Mammarella ◽  
Tiia Grönholm ◽  
Timo Vesala
Keyword(s):  
Structure Function ◽  
Gas Transfer ◽  
Function Model ◽  
Transfer Velocity ◽  
Gas Transfer Velocity ◽  
The Many ◽  
Water Gas

scholarly journals Changes in gross oxygen production, net oxygen production, and air-water gas exchange during seasonal ice melt in Whycocomagh Bay, a Canadian estuary in the Bras d'Or Lake system

2019 ◽  
Vol 16 (17) ◽  
pp. 3351-3376
Author(s):  
Cara C. Manning ◽  
Rachel H. R. Stanley ◽  
David P. Nicholson ◽  
Brice Loose ◽  
Ann Lovely ◽  
...  
Keyword(s):  
Gas Exchange ◽  
Gas Transfer ◽  
Polar Regions ◽  
Oxygen Production ◽  
Transfer Velocity ◽  
Gas Transfer Velocity ◽  
Ice Melt ◽  
Lake System ◽  
Wide Range ◽  
Water Gas

Abstract. Sea ice is an important control on gas exchange and primary production in polar regions. We measured net oxygen production (NOP) and gross oxygen production (GOP) using near-continuous measurements of the O2∕Ar gas ratio and discrete measurements of the triple isotopic composition of O2, during the transition from ice-covered to ice-free conditions, in Whycocomagh Bay, an estuary in the Bras d'Or Lake system in Nova Scotia, Canada. The volumetric gross oxygen production was 5.4+2.8-1.6 mmol O2 m−3 d−1, similar at the beginning and end of the time series, and likely peaked at the end of the ice melt period. Net oxygen production displayed more temporal variability and the system was on average net autotrophic during ice melt and net heterotrophic following the ice melt. We performed the first field-based dual tracer release experiment in ice-covered water to quantify air–water gas exchange. The gas transfer velocity at >90 % ice cover was 6 % of the rate for nearly ice-free conditions. Published studies have shown a wide range of results for gas transfer velocity in the presence of ice, and this study indicates that gas transfer through ice is much slower than the rate of gas transfer through open water. The results also indicate that both primary producers and heterotrophs are active in Whycocomagh Bay during spring while it is covered in ice.

scholarly journals Multiple mechanisms generate a universal scaling with dissipation for the air-water gas transfer velocity

2017 ◽  
Vol 44 (4) ◽  
pp. 1892-1898 ◽  
Author(s):  
Gabriel Katul ◽  
Heping Liu
Keyword(s):  
Gas Transfer ◽  
Transfer Velocity ◽  
Gas Transfer Velocity ◽  
Universal Scaling ◽  
Water Gas

scholarly journals Spatiotemporal variability of gas transfer velocity in a tropical high‐elevation stream using two independent methods

Ecosphere ◽  
2021 ◽  
Vol 12 (7) ◽  
Author(s):  
Keridwen M. Whitmore ◽  
Nehemiah Stewart ◽  
Andrea C. Encalada ◽  
Esteban Suárez ◽  
Diego A. Riveros‐Iregui
Keyword(s):  
High Elevation ◽  
Spatiotemporal Variability ◽  
Gas Transfer ◽  
Transfer Velocity ◽  
Gas Transfer Velocity

scholarly journals Sea-to-air and diapycnal nitrous oxide fluxes in the eastern tropical North Atlantic Ocean

2012 ◽  
Vol 9 (3) ◽  
pp. 957-964 ◽  
Author(s):  
A. Kock ◽  
J. Schafstall ◽  
M. Dengler ◽  
P. Brandt ◽  
H. W. Bange
Keyword(s):  
Nitrous Oxide ◽  
Gas Exchange ◽  
Mixed Layer ◽  
North Atlantic Ocean ◽  
Gas Transfer ◽  
Potential Contribution ◽  
Transfer Velocity ◽  
N2o Production ◽  
Gas Transfer Velocity ◽  
Upwelled Water

Abstract. Sea-to-air and diapycnal fluxes of nitrous oxide (N2O) into the mixed layer were determined during three cruises to the upwelling region off Mauritania. Sea-to-air fluxes as well as diapycnal fluxes were elevated close to the shelf break, but elevated sea-to-air fluxes reached further offshore as a result of the offshore transport of upwelled water masses. To calculate a mixed layer budget for N2O we compared the regionally averaged sea-to-air and diapycnal fluxes and estimated the potential contribution of other processes, such as vertical advection and biological N2O production in the mixed layer. Using common parameterizations for the gas transfer velocity, the comparison of the average sea-to-air and diapycnal N2O fluxes indicated that the mean sea-to-air flux is about three to four times larger than the diapycnal flux. Neither vertical and horizontal advection nor biological production were found sufficient to close the mixed layer budget. Instead, the sea-to-air flux, calculated using a parameterization that takes into account the attenuating effect of surfactants on gas exchange, is in the same range as the diapycnal flux. From our observations we conclude that common parameterizations for the gas transfer velocity likely overestimate the air-sea gas exchange within highly productive upwelling zones.

scholarly journals Surfactant control of gas transfer velocity along an offshore coastal transect: results from a laboratory gas exchange tank

2016 ◽  
Vol 13 (13) ◽  
pp. 3981-3989 ◽  
Author(s):  
R. Pereira ◽  
K. Schneider-Zapp ◽  
R. C. Upstill-Goddard
Keyword(s):  
Organic Matter ◽  
Gas Exchange ◽  
Trace Gas ◽  
Gas Transfer ◽  
Transfer Velocity ◽  
Chl A ◽  
Gas Transfer Velocity ◽  
Biogeochemical Models ◽  
Sea Surface Microlayer ◽  
Laboratory Water

Abstract. Understanding the physical and biogeochemical controls of air–sea gas exchange is necessary for establishing biogeochemical models for predicting regional- and global-scale trace gas fluxes and feedbacks. To this end we report the results of experiments designed to constrain the effect of surfactants in the sea surface microlayer (SML) on the gas transfer velocity (kw; cm h−1), seasonally (2012–2013) along a 20 km coastal transect (North East UK). We measured total surfactant activity (SA), chromophoric dissolved organic matter (CDOM) and chlorophyll a (Chl a) in the SML and in sub-surface water (SSW) and we evaluated corresponding kw values using a custom-designed air–sea gas exchange tank. Temporal SA variability exceeded its spatial variability. Overall, SA varied 5-fold between all samples (0.08 to 0.38 mg L−1 T-X-100), being highest in the SML during summer. SML SA enrichment factors (EFs) relative to SSW were  ∼  1.0 to 1.9, except for two values (0.75; 0.89: February 2013). The range in corresponding k660 (kw for CO2 in seawater at 20 °C) was 6.8 to 22.0 cm h−1. The film factor R660 (the ratio of k660 for seawater to k660 for “clean”, i.e. surfactant-free, laboratory water) was strongly correlated with SML SA (r ≥ 0.70, p ≤ 0.002, each n = 16). High SML SA typically corresponded to k660 suppressions  ∼  14 to 51 % relative to clean laboratory water, highlighting strong spatiotemporal gradients in gas exchange due to varying surfactant in these coastal waters. Such variability should be taken account of when evaluating marine trace gas sources and sinks. Total CDOM absorbance (250 to 450 nm), the CDOM spectral slope ratio (SR = S275 − 295∕S350 − 400), the 250 : 365 nm CDOM absorption ratio (E2 : E3), and Chl a all indicated spatial and temporal signals in the quantity and composition of organic matter in the SML and SSW. This prompts us to hypothesise that spatiotemporal variation in R660 and its relationship with SA is a consequence of compositional differences in the surfactant fraction of the SML DOM pool that warrants further investigation.

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