Upper Ocean Turbulence from High-Resolution 3D Simulations
By Patrice Klein, B. Hua, G. Lapeyre, Xavier Capet, S. L. Gentil, Hideharu Sasaki. 2008
309 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/c576617c5ed44bfabb3316afc9bc22e90baef8eb
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- Raffaele Ferrari
- James C. McWilliams
- B. Fox‐Kemper
- Robert Hallberg
- M. Molemaker
- S. Griffies
- J. Callies
- Xavier Capet
In Global and Planetary Change
- Raffaele Ferrari
- James C. McWilliams
- Robert Hallberg
- B. Fox‐Kemper
- M. Molemaker
- S. Griffies
- J. Callies
- Xavier Capet
In Oceanography
- Raffaele Ferrari
- James C. McWilliams
- B. Fox‐Kemper
- Robert Hallberg
- M. Molemaker
- S. Griffies
- J. Callies
- Xavier Capet
Citations in the corpus
- Three‐dimensional reconstruction of oceanic mesoscale currents from surface information (2008, unknown): “Indeed, very high numerical simulations with a Primitive Equation model of a nonlinear baroclinically unstable flow [Klein et al., 2008] suggest”
- Do Altimeter Wavenumber Spectra Agree with the Interior or Surface Quasigeostrophic Theory (2008, methodology): “Such relevance of the SQG theory for the upperoceanic layers has been confirmed and strengthened by high-resolution simulations using primitive equation models (Capet et al. 2008; Klein et al. 2008).”
- Physical forcing of nitrogen fixation and diazotroph community structure in the North Pacific subtropical gyre (2009, background): “In addition, submesoscale dynamics associated with ocean eddies including nonlinear Ekman transport, frontogenesis, and ageostrophic circulation all appear capable of diapycnal nutrient exchange within anticyclones [Mahadevan and Tandon, 2006; Capet et al., 2008; Klein et al., 2008; Mahadevan et al.”
- Balanced and unbalanced routes to dissipation in an equilibrated Eady flow (2010, background): “Another relevant study without a surface mixed layer (Klein et al. 2008) finds no evidence of a shear-driven frontal cross-frontal direction.”
- Statistics of vertical vorticity, divergence, and strain in a developed submesoscale turbulence field (2013, methodology): “Such an asymmetry is indeed found in high-resolution numerical simulations whenever the signature of strong submesoscale turbulence is not overshadowed by the mesoscale features [e.g., Mahadevan and Tandon, 2006; Capet et al., 2008; Klein et al., 2008].”
- A boundary-value problem for the parameterized mesoscale eddy transport (2010, result): “Recent results (e.g., Klein et al., 2008) suggest that new modes are excited when density is not uniform at the surface.”
- Mesoscale to Submesoscale Transition in the California Current System. Part II: Frontal Processes (2008, result): “In that regard, a comparison between our simulations ICC0 and ICC1 and the solution analyzed by Klein et al. (2008) at a similar grid resolution is instructive.”
- Bringing physics to life at the submesoscale (2012, background): “It is only density surfaces that remain smooth [Lapeyre et al., 2006; Klein et al., 2008].”
- Mesoscale to submesoscale transition in the California current system. Part III: Energy balance and flux (2008, background): “; Klein et al. 2008).5 Figure 9 (top) shows that the total amount of horizontal dissipation has also approximately converged by x 0.750 km; the small k values of k R dk are nearly the same for simulations ICC1 and ICC0.”
- Interpreting Energy and Tracer Spectra of Upper-Ocean Turbulence in the Submesoscale Range (1–200 km) (2013, background): “It would still be plausible to interpret the 2 2 slopes of the kinetic and potential energy spectra as signatures of surface-QG turbulence, as suggested by Klein et al. (2008).”
- Internal gravity waves from atmospheric jets and fronts (2014, background): “Such instabilities are however absent from other high-resolution simulations of upper ocean geostrophic turbulence [Klein et al., 2008], calling for further investigation.”
- Ocean Circulation Kinetic Energy: Reservoirs, Sources, and Sinks (2009, background): “This paradigm does not apply at the ocean surface, where energy appeared to cascade downscale in surface trapped modes (Klein et al., 2008).”
- Parameterization of mixed layer eddies. III: Implementation and impact in global ocean climate simulations (2010, background): “Submesoscale fronts and frontal restratification and instabilities also af- 76 fect biology (Levy et al., 1999; Spall and Richards, 2000; Mahadevan and 77 Archer, 2000; Klein and Lapeyre, 2009).”