Electrical Current-Assisted Reaction Crucibles Technique

Bochkanov, Fedor Yu.; Karpenkov, D.; Fomin, Vladislav E.; Kvashnin, Alexander G.; Tukmakova, Anastasiya S.; Кулеш, Н. А.; Kurichenko, Vladislav

doi:10.2139/ssrn.4284409

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Horizontal Vertical and Temporal Averages And Integrals1

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2023

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“…where Ψ; Φ are computed by coarse-graining each field as a scalar (66,67). Computational details of the Helmholtz decomposition, which uses the ALGLIB package (80), can be found in the Supplemental Materials.…”

Section: Horizontal Vertical and Temporal Averages And Integralsmentioning

confidence: 99%

Global cascade of kinetic energy in the ocean and the atmospheric imprint

Storer,

Buzzicotti,

Khatri

et al. 2023

Sci. Adv.

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Here, we present an estimate for the ocean's global scale transfer of kinetic energy (KE), across scales from 10 to 40,000 km. Oceanic KE transfer between gyre scales and mesoscales is induced by the atmosphere’s Hadley, Ferrel, and polar cells, and the intertropical convergence zone induces an intense downscale KE transfer. Upscale transfer peaks at 300 gigawatts across mesoscales of 120 km in size, roughly one-third the energy input by winds into the oceanic general circulation. Nearly three quarters of this “cascade” occurs south of 15°S and penetrates almost the entire water column. The mesoscale cascade has a self-similar seasonal cycle with characteristic lag time of ≈27 days per octave of length scales; transfer across 50 km peaks in spring, while transfer across 500 km peaks in summer. KE of those mesoscales follows the same cycle but peaks ≈40 days after the peak cascade, suggesting that energy transferred across a scale is primarily deposited at a scale four times larger.

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Section: Horizontal Vertical and Temporal Averages And Integralsmentioning

confidence: 99%