Process contribution to the time-varying residual circulation in tidally dominated estuarine environments
Brown, Jennifer ORCID: https://orcid.org/0000-0002-3894-4651; Bolanos-Sanchez, Rodolfo; Souza, Alejandro. 2014 Process contribution to the time-varying residual circulation in tidally dominated estuarine environments. Estuaries and Coasts, 37 (5). 1041-1057. https://doi.org/10.1007/s12237-013-9745-6
Before downloading, please read NORA policies.
|
Text
Dee_residual_current.pdf Download (2MB) | Preview |
|
|
Text (Open Access paper)
art%3A10.1007%2Fs12237-013-9745-6.pdf - Published Version Available under License Creative Commons Attribution. Download (6MB) | Preview |
Abstract/Summary
In tide dominated environments residual circulation is the comparatively weak net flow in addition to the oscillatory tidal current. Understanding the 3D structure of this circulation is of importance for coastal management as it impacts the net (longer-term and event-scale) transport of suspended particles and the advection of tracer quantities. The Dee Estuary, northwest Britain, is used to understand which physical processes have an important contribution to the time-varying residual circulation. Model simulations are used to extract the time-varying contributions of tidal, riverine (baroclinicity and discharge), meteorological, external and wave processes, along with their interactions. Under hypertidal conditions strong semi-diurnal interaction within the residual makes it difficult to clearly see the affect of a process without filtering. An approach to separate the residual into the isolated process contribution and the contribution due to interaction is described. Applying this method to two hypertidal estuarine channels, one tide-dominant and one baroclinic-dominant, reveals that process interaction can be as important as the sub-tidal residual process contributions themselves. The time-variation of the residual circulation highlights the impact of different physical process components at the event-scale of tidal conditions (neap and spring cycles) and offshore storms (wind, wave and surge influence). This gives insight into short-term deviation from the typical estuarine residual. Both channels are found to react differently to the same local conditions, with different short-term change in process dominance during events of high and low energy.
Item Type: | Publication - Article |
---|---|
Digital Object Identifier (DOI): | https://doi.org/10.1007/s12237-013-9745-6 |
Programmes: | NOC Programmes > Marine Physics and Ocean Climate |
Additional Keywords: | Dee Estuary, Tide surge stratification, POLCOMS–GOTM–WAM, Coastal management, Residual circulation, Hypertidal interaction |
NORA Subject Terms: | Marine Sciences |
Date made live: | 10 Feb 2014 13:27 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/504185 |
Actions (login required)
View Item |
Document Downloads
Downloads for past 30 days
Downloads per month over past year