Reconciling Lagrangian Diffusivity and Effective Diffusivity in Contour-Based CoordinatesSource: Journal of Physical Oceanography:;2019:;volume 049:;issue 006::page 1521DOI: 10.1175/JPO-D-18-0251.1Publisher: American Meteorological Society
Abstract: AbstractThe present study reconciles theoretical differences between the Lagrangian diffusivity and effective diffusivity in a transformed spatial coordinate based on the contours of a quasi-conservative tracer. In the transformed coordinate, any adiabatic stirring effect, such as shear-induced dispersion, is naturally isolated from diabatic cross-contour motions. Therefore, Lagrangian particle motions in the transformed coordinate obey a transformed zeroth-order stochastic (i.e., random walk) model with the diffusivity replaced by the effective diffusivity. Such a stochastic model becomes the theoretical foundation on which both diffusivities are exactly unified. In the absence of small-scale diffusion, particles do not disperse at all in the transformed contour coordinate. Besides, the corresponding Lagrangian autocorrelation becomes a delta function and is thus free from pronounced overshoot and negative lobe at short time lags that may be induced by either Rossby waves or mesoscale eddies; that is, particles decorrelate immediately and Lagrangian diffusivity is already asymptotic no matter how small the time lag is. The resulting instantaneous Lagrangian spreading rate is thus conceptually identical to the effective diffusivity that only measures the instantaneous irreversible mixing. In these regards, the present study provides a new look at particle dispersion in contour-based coordinates.
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contributor author | Qian, Yu-Kun | |
contributor author | Peng, Shiqiu | |
contributor author | Liang, Chang-Xia | |
date accessioned | 2019-10-05T06:48:22Z | |
date available | 2019-10-05T06:48:22Z | |
date copyright | 4/8/2019 12:00:00 AM | |
date issued | 2019 | |
identifier other | JPO-D-18-0251.1.pdf | |
identifier uri | http://yetl.yabesh.ir/yetl1/handle/yetl/4263472 | |
description abstract | AbstractThe present study reconciles theoretical differences between the Lagrangian diffusivity and effective diffusivity in a transformed spatial coordinate based on the contours of a quasi-conservative tracer. In the transformed coordinate, any adiabatic stirring effect, such as shear-induced dispersion, is naturally isolated from diabatic cross-contour motions. Therefore, Lagrangian particle motions in the transformed coordinate obey a transformed zeroth-order stochastic (i.e., random walk) model with the diffusivity replaced by the effective diffusivity. Such a stochastic model becomes the theoretical foundation on which both diffusivities are exactly unified. In the absence of small-scale diffusion, particles do not disperse at all in the transformed contour coordinate. Besides, the corresponding Lagrangian autocorrelation becomes a delta function and is thus free from pronounced overshoot and negative lobe at short time lags that may be induced by either Rossby waves or mesoscale eddies; that is, particles decorrelate immediately and Lagrangian diffusivity is already asymptotic no matter how small the time lag is. The resulting instantaneous Lagrangian spreading rate is thus conceptually identical to the effective diffusivity that only measures the instantaneous irreversible mixing. In these regards, the present study provides a new look at particle dispersion in contour-based coordinates. | |
publisher | American Meteorological Society | |
title | Reconciling Lagrangian Diffusivity and Effective Diffusivity in Contour-Based Coordinates | |
type | Journal Paper | |
journal volume | 49 | |
journal issue | 6 | |
journal title | Journal of Physical Oceanography | |
identifier doi | 10.1175/JPO-D-18-0251.1 | |
journal fristpage | 1521 | |
journal lastpage | 1539 | |
tree | Journal of Physical Oceanography:;2019:;volume 049:;issue 006 | |
contenttype | Fulltext |