Abstract
Using a process-oriented modeling approach, this work explores the interaction between flow disturbances created by an isolated shelf-break canyon with coastal flows modulated by an irregular coastline such as a headland. Findings show that, on their own, both the canyon and the headland produce individual stationary barotropic topographic Rossby waves extending considerable distances >100. km) along the continental shelf. The canyon-induced wave is instrumental in the formation of stationary alternating zones of upwelling and downwelling along the shelf break. Waves created by a headland located downstream of the canyon tend to dramatically enhance the cross-shelf flow in favor of the formation of stationary coastal upwelling centers. In this case, process-individual zones of "squeezing vorticity" (negative ratio of relative vorticity to planetary vorticity) combine such as to trap previously upwelled water on the continental shelf. In contrast, headland-induced flow disturbances created upstream of the shelf-break canyon have only little impact on the cross-shelf flow. Moreover, sensitivity studies indicate that the efficiency of cross-shelf exchange critically depends on topographic parameters (in particular onshore variations of bottom slope) of the continental shelf.
Original language | English |
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Pages (from-to) | 78-88 |
Number of pages | 11 |
Journal | Continental Shelf Research |
Volume | 42 |
DOIs | |
Publication status | Published - 1 Jul 2012 |
Keywords
- Cross-shelf exchange
- Hydrodynamic modeling
- Submarine canyons
- Upwelling