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Bringing physics to life at the submesoscale
by
Lévy, Marina
, Franks, Peter J. S.
, Rivière, Pascal
, Ferrari, Raffaele
, Martin, Adrian P.
in
Earth Sciences
/ Earth, ocean, space
/ ecosystems
/ Eddies
/ Environmental Sciences
/ Euphotic zone
/ Exact sciences and technology
/ Fluid dynamics
/ Fluid flow
/ fronts
/ Horizontal
/ Internal waves
/ Marine
/ Nonlinear dynamics
/ Oceanic turbulence
/ Oceanography
/ Oceans
/ Organic carbon
/ phytoplankton
/ Primary production
/ Sampling
/ Sciences of the Universe
/ submesoscale
/ Turbulence
/ Turbulent flow
/ Upper ocean
2012
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Bringing physics to life at the submesoscale
by
Lévy, Marina
, Franks, Peter J. S.
, Rivière, Pascal
, Ferrari, Raffaele
, Martin, Adrian P.
in
Earth Sciences
/ Earth, ocean, space
/ ecosystems
/ Eddies
/ Environmental Sciences
/ Euphotic zone
/ Exact sciences and technology
/ Fluid dynamics
/ Fluid flow
/ fronts
/ Horizontal
/ Internal waves
/ Marine
/ Nonlinear dynamics
/ Oceanic turbulence
/ Oceanography
/ Oceans
/ Organic carbon
/ phytoplankton
/ Primary production
/ Sampling
/ Sciences of the Universe
/ submesoscale
/ Turbulence
/ Turbulent flow
/ Upper ocean
2012
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Do you wish to request the book?
Bringing physics to life at the submesoscale
by
Lévy, Marina
, Franks, Peter J. S.
, Rivière, Pascal
, Ferrari, Raffaele
, Martin, Adrian P.
in
Earth Sciences
/ Earth, ocean, space
/ ecosystems
/ Eddies
/ Environmental Sciences
/ Euphotic zone
/ Exact sciences and technology
/ Fluid dynamics
/ Fluid flow
/ fronts
/ Horizontal
/ Internal waves
/ Marine
/ Nonlinear dynamics
/ Oceanic turbulence
/ Oceanography
/ Oceans
/ Organic carbon
/ phytoplankton
/ Primary production
/ Sampling
/ Sciences of the Universe
/ submesoscale
/ Turbulence
/ Turbulent flow
/ Upper ocean
2012
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Journal Article
Bringing physics to life at the submesoscale
2012
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Overview
A common dynamical paradigm is that turbulence in the upper ocean is dominated by three classes of motion: mesoscale geostrophic eddies, internal waves and microscale three‐dimensional turbulence. Close to the ocean surface, however, a fourth class of turbulent motion is important: submesoscale frontal dynamics. These have a horizontal scale of O(1–10) km, a vertical scale of O(100) m, and a time scale of O(1) day. Here we review the physical‐chemical‐biological dynamics of submesoscale features, and discuss strategies for sampling them. Submesoscale fronts arise dynamically through nonlinear instabilities of the mesoscale currents. They are ephemeral, lasting only a few days after they are formed. Strong submesoscale vertical velocities can drive episodic nutrient pulses to the euphotic zone, and subduct organic carbon into the ocean's interior. The reduction of vertical mixing at submesoscale fronts can locally increase the mean time that photosynthetic organisms spend in the well‐lit euphotic layer and promote primary production. Horizontal stirring can create intense patchiness in planktonic species. Submesoscale dynamics therefore can change not only primary and export production, but also the structure and the functioning of the planktonic ecosystem. Because of their short time and space scales, sampling of submesoscale features requires new technologies and approaches. This paper presents a critical overview of current knowledge to focus attention and hopefully interest on the pressing scientific questions concerning these dynamics.
Key Points
Submesoscale physics control ecology locally, but also feedback to basin scales
Strong gradients in community structure are created at the submesoscale
Despite recent innovations, sampling the submesoscale remains a major challenge
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