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Regionality and seasonality of submesoscale and mesoscale turbulence in the North Pacific Ocean ArchiMer
Sasaki, Hideharu; Klein, Patrice; Sasai, Yoshikazu; Qiu, Bo.
The kinetic energy (KE) seasonality has been revealed by satellite altimeters in many oceanic regions. Question about the mechanisms that trigger this seasonality is still challenging. We address this question through the comparison of two numerical simulations. The first one, with a 1/10° horizontal grid spacing, 54 vertical levels, represents dynamics of physical scales larger than 50 km. The second one, with a 1/30° grid spacing, 100 vertical levels, takes into account the dynamics of physical scales down to 16 km. Comparison clearly emphasizes in the whole North Pacific Ocean, not only a significant KE increase by a factor up to three, but also the emergence of seasonal variability when the scale range 16–50 km (called submesoscales in this study) is...
Tipo: Text Palavras-chave: Submesoscale turbulence; Scale interactions; Mixed-layer instability; High-resolution simulations; North Pacific.
Ano: 2017 URL: http://archimer.ifremer.fr/doc/00392/50347/51110.pdf
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Seasonal Mesoscale and Submesoscale Eddy Variability along the North Pacific Subtropical Countercurrent ArchiMer
Qiu, Bo; Chen, Shuiming; Klein, Patrice; Sasaki, Hideharu; Sasai, Yoshikazu.
Located at the center of the western North Pacific Subtropical Gyre, the Subtropical Countercurrent (STCC) is not only abundant in mesoscale eddies, but also exhibits prominent submesoscale eddy features. Output from a 1/30 degrees high-resolution OGCM simulation and a gridded satellite altimetry product are analyzed to contrast the seasonal STCC variability in the mesoscale versus submesoscale ranges. Resolving the eddy scales of >150 km, the altimetry product reveals that the STCC eddy kinetic energy and rms vorticity have a seasonal maximum in May and April, respectively, a weak positive vorticity skewness without seasonal dependence, and an inverse (forward) kinetic energy cascade for wavelengths larger (shorter) than 250 km. In contrast, the...
Tipo: Text Palavras-chave: Circulation/ Dynamics; Eddies; Instability; Mesoscale processes; Observational techniques and algorithms; Altimetry; Models and modeling; Ocean models; Variability; Seasonal variability.
Ano: 2014 URL: http://archimer.ifremer.fr/doc/00245/35588/34142.pdf
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Impact of oceanic-scale interactions on the seasonal modulation of ocean dynamics by the atmosphere ArchiMer
Sasaki, Hideharu; Klein, Patrice; Qiu, Bo; Sasai, Yoshikazu.
Ocean eddies (with a size of 100-300 km), ubiquitous in satellite observations, are known to represent about 80% of the total ocean kinetic energy. Recent studies have pointed out the unexpected role of smaller oceanic structures (with 1-50 km scales) in generating and sustaining these eddies. The interpretation proposed so far invokes the internal instability resulting from the large-scale interaction between upper and interior oceanic layers. Here we show, using a new high-resolution simulation of the realistic North Pacific Ocean, that ocean eddies are instead sustained by a different process that involves small-scale mixed-layer instabilities set up by large-scale atmospheric forcing in winter. This leads to a seasonal evolution of the eddy kinetic...
Tipo: Text Palavras-chave: Earth sciences; Oceanography.
Ano: 2014 URL: http://archimer.ifremer.fr/doc/00250/36098/34642.pdf
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Interannual to Decadal Variations of Submesoscale Motions around the North Pacific Subtropical Countercurrent ArchiMer
Sasaki, Hideharu; Qiu, Bo; Klein, Patrice; Sasai, Yoshikazu; Nonaka, Masami.
The outputs from a submesoscale permitting hindcast simulation from 1990 to 2016 are used to investigate the interannual to decadal variations of submesoscale motions. The region we focus on is the subtropical Northwestern Pacific including the subtropical countercurrent. The submesoscale kinetic energy (KE) is characterized by strong interannual and decadal variability, displaying larger magnitudes in 1996, 2003, and 2015, and smaller magnitudes in 1999, 2009, 2010, and 2016. These variations are partially explained by those of the available potential energy (APE) release at submesoscale driven by mixed layer instability in winter. Indeed, this APE release depends on the mixed layer depth and horizontal buoyancy gradient, both of them modulated with the...
Tipo: Text Palavras-chave: Submesoscale motion; Interannual to decadal variations; Mixed layer instability; North Pacific Subtropical Countercurrent.
Ano: 2020 URL: https://archimer.ifremer.fr/doc/00641/75287/75641.pdf
Registros recuperados: 4
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