Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

The Stokes drift in ocean surface drift prediction

View through CrossRef
<p>Ocean surface drift forecasts are essential for numerous applications. It is a central asset in search and rescue and oil spill response operations, but it is also used for predicting the transport of pelagic eggs, larvae and detritus or other organisms and solutes, for evaluating ecological isolation of marine species, for tracking plastic debris, and for environmental planning and management. The accuracy of surface drift forecasts depends to a large extent on the quality of ocean current, wind and waves forecasts, but also on the drift model used. The standard Eulerian leeway drift model used in most operational systems considers near-surface currents provided by the top grid cell of the ocean circulation model and a correction term proportional to the near-surface wind. Such formulation assumes that the 'wind correction term' accounts for many processes including windage, unresolved ocean current vertical shear, and wave-induced drift. However, the latter two processes are not necessarily linearly related to the local wind velocity. We propose three other drift models that attempt to account for the unresolved near-surface current shear by extrapolating the near-surface currents to the surface assuming Ekman dynamics. Among them two models consider explicitly the Stokes drift, one without and the other with a wind correction term. We assess the performance of the drift models using observations from drifting buoys deployed in the Estuary and Gulf of St. Lawrence, Canada. Drift model inputs are obtained from regional atmospheric, ocean circulation, and spectral wave models. The performance of these drift models is evaluated based on a number of error metrics (e.g. speed, direction, separation distance between the observed and simulated positions) and skill scores determined at different lead times ranging from 3h to 72h. Results show that extrapolating the top-layer ocean model currents to the surface assuming Ekman dynamics for the ageostrophic currents, and adding the Stokes drift predicted by a spectral wave model, leads to the best drift forecast skills without the need to include a wind correction term.</p>
Title: The Stokes drift in ocean surface drift prediction
Description:
<p>Ocean surface drift forecasts are essential for numerous applications.
It is a central asset in search and rescue and oil spill response operations, but it is also used for predicting the transport of pelagic eggs, larvae and detritus or other organisms and solutes, for evaluating ecological isolation of marine species, for tracking plastic debris, and for environmental planning and management.
The accuracy of surface drift forecasts depends to a large extent on the quality of ocean current, wind and waves forecasts, but also on the drift model used.
The standard Eulerian leeway drift model used in most operational systems considers near-surface currents provided by the top grid cell of the ocean circulation model and a correction term proportional to the near-surface wind.
Such formulation assumes that the 'wind correction term' accounts for many processes including windage, unresolved ocean current vertical shear, and wave-induced drift.
However, the latter two processes are not necessarily linearly related to the local wind velocity.
We propose three other drift models that attempt to account for the unresolved near-surface current shear by extrapolating the near-surface currents to the surface assuming Ekman dynamics.
Among them two models consider explicitly the Stokes drift, one without and the other with a wind correction term.
We assess the performance of the drift models using observations from drifting buoys deployed in the Estuary and Gulf of St.
Lawrence, Canada.
Drift model inputs are obtained from regional atmospheric, ocean circulation, and spectral wave models.
The performance of these drift models is evaluated based on a number of error metrics (e.
g.
speed, direction, separation distance between the observed and simulated positions) and skill scores determined at different lead times ranging from 3h to 72h.
Results show that extrapolating the top-layer ocean model currents to the surface assuming Ekman dynamics for the ageostrophic currents, and adding the Stokes drift predicted by a spectral wave model, leads to the best drift forecast skills without the need to include a wind correction term.
</p>.

Related Results

Access impact of observations
Access impact of observations
The accuracy of the Copernicus Marine Environment and Monitoring Service (CMEMS) ocean analysis and forecasts highly depend on the availability and quality of observations to be as...
Assessing the potential composition of Europa’s subsurface ocean from water-rock interactions.
Assessing the potential composition of Europa’s subsurface ocean from water-rock interactions.
<p><strong>Introduction:</strong> Constraining the composition of Europa’s ocean is critical to understanding whether it cou...
Environmental History of Oceanic Noise Pollution
Environmental History of Oceanic Noise Pollution
The concept of “ocean noise” precedes the concept of “ocean noise pollution” by about half a century. Those seeking a body of scholarly literature on ocean noise as an environmenta...
A new sea ice state dependent parameterization for the free drift of sea ice
A new sea ice state dependent parameterization for the free drift of sea ice
Abstract. Free drift estimates of sea ice motion are necessary to produce a seamless observational record combining buoy and satellite-derived sea ice motion vectors. We develop a ...
Closing the Ocean Science Gap: Empowering Africa towards Ocean Innovation and Global Ocean-Based Solutions
Closing the Ocean Science Gap: Empowering Africa towards Ocean Innovation and Global Ocean-Based Solutions
The global ocean science community faces critical inequities that hinder Africa’s participation in research and innovation, resulting in limited African contributions to ocean-base...
Role of Ocean Memory in Subpolar North Atlantic Decadal Variability
Role of Ocean Memory in Subpolar North Atlantic Decadal Variability
The decadal variability in the subpolar North Atlantic Ocean heat content is significantly influenced by the atmosphere. The impact of seasonal-annual atmospheric perturbations las...
Thermochemical modelling of the ocean composition of Enceladus from ocean floor to outer space
Thermochemical modelling of the ocean composition of Enceladus from ocean floor to outer space
<p>Enceladus, an icy moon of Saturn, is a potentially habitable environment. Its South Polar Region hosts active plumes that eject material from the subsurface into s...
Convergence de méthodes numériques pour la mécanique des fluides : équation de Navier-Stokes stochastique et ses variantes
Convergence de méthodes numériques pour la mécanique des fluides : équation de Navier-Stokes stochastique et ses variantes
Convergence of numerical methods in fluid mechanics : The stochastic Navier-Stokes equation and its variants Bien que le développement et l'évolution des méthodes n...

Back to Top