The multisensory approach to hydrophysical measurements of the ocean surface layer

2021 ◽  
Author(s):  
Aleksei V. Ermoshkin ◽  
Mikhail B. Salin ◽  
Ivan A. Kapustin ◽  
Alexander Molkov ◽  
Nikolay A. Bogatov
Keyword(s):  
Surface Layer ◽  
Ocean Surface ◽  
Ocean Surface Layer

Methane oxidation and methane fluxes in the ocean surface layer and deep anoxic waters

Nature ◽  
1987 ◽  
Vol 327 (6119) ◽  
pp. 226-229 ◽  
Author(s):  
B. B. Ward ◽  
K. A. Kilpatrick ◽  
P. C. Novelli ◽  
M. I. Scranton
Keyword(s):  
Surface Layer ◽  
Methane Oxidation ◽  
Ocean Surface ◽  
Anoxic Waters ◽  
Methane Fluxes ◽  
Ocean Surface Layer

Two-sided turbulent boundary layer parameterizations for assessing ocean – atmosphere fluxes

2020 ◽  
Author(s):  
Florian Lemarie ◽  
Charles Pelletier ◽  
Pierre-Etienne Brilouet ◽  
Eric Blayo ◽  
Jean-Luc Redelsperger ◽  
...  
Keyword(s):  
Boundary Layer ◽  
Surface Layer ◽  
Ocean Surface ◽  
Near Surface ◽  
Surface Ocean ◽  
Turbulent Closure ◽  
Surface Fields ◽  
Ocean Surface Layer ◽  
Vertical Level ◽  
Layer Solution

<p><span>Standard </span><span>methods for determining air – sea fluxes typically rely on bulk algorithms derived from the Monin-Obukhov stability theory (MOST), </span><span>using ocean surface fields and atmosphere near-surface fields. In the context of coupled ocean – atmosphere simulations, </span><span>the </span><span>shallowest ocean vertical level is usually assimilated to </span><span>the surface, and the turbulent closure is one-sided: it aims at extrapolating atmosphere near-surface solution profiles (for wind speed, temperature and humidity) to the prescribed ocean surface values. </span><span>Assimilating near-surface ocean fields as surface ones is equivalent to considering that in the ocean surface layer, solution profiles are constant instead of also being determined by a turbulent closure. Here we introduce a method for extending existing turbulent parameterization</span><span>s</span><span> to a two-sided </span><span>context, by including the ocean surface layer and the viscous sublayers, which are also generally neglected in </span><span>standard air – sea fluxes computation. </span><span>The formalism we use for this method is derived from that of classical turbulent closure, so that our novelties can easily be implemented within existing formulations.</span> <span>Special care is taken to </span><span>ensure the smoothness of </span><span>resulting solution profiles. </span><span>We</span> <span>investigate the </span><span>impact of such two-sided bulk formulations on air - sea fluxes and </span><span>discuss further implications such as resulting bulk formulation retuning. We also present leads on incorporating </span><span>other mechanisms impacting air – sea fluxes within our framework, such as waves and radiation penetration.<br></span></p>

scholarly journals Photo-oxidation: Major sink of oxygen in the ocean surface layer

2015 ◽  
Vol 177 ◽  
pp. 472-475 ◽  
Author(s):  
W.W.C. Gieskes ◽  
R.W.P.M. Laane ◽  
P. Ruardij
Keyword(s):  
Surface Layer ◽  
Ocean Surface ◽  
Photo Oxidation ◽  
Ocean Surface Layer

scholarly journals Interannual variability of parameters of the Arctic Ocean surface layer and halocline

2020 ◽  
Vol 66 (4) ◽  
pp. 404-426
Author(s):  
E. A. Cherniavskaia ◽  
L. A. Timokhov ◽  
V. Y. Karpiy ◽  
S. Y. Malinovskiy
Keyword(s):  
Surface Layer ◽  
Arctic Ocean ◽  
Interannual Variability ◽  
Ocean Surface ◽  
The Arctic ◽  
The Arctic Ocean ◽  
Ocean Surface Layer

10Be concentration and residence time in the ocean surface layer

1979 ◽  
Vol 43 (2) ◽  
pp. 237-240 ◽  
Author(s):  
G.M. Raisbeck ◽  
F. Yiou ◽  
M. Fruneau ◽  
J.M. Loiseaux ◽  
M. Lieuvin
Keyword(s):  
Surface Layer ◽  
Residence Time ◽  
Ocean Surface ◽  
10Be Concentration ◽  
Ocean Surface Layer
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