2007
DOI: 10.1016/j.pocean.2007.07.001
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A review of the shelf-slope circulation along Australia’s southern shelves: Cape Leeuwin to Portland

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Cited by 200 publications
(232 citation statements)
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“…The extent and influence of currents and water masses vary seasonally and inter-annually in Bass Strait [11]. In accordance with previous oceanographic works at this region, our areas of influence highlighted eastward influence during autumn and winter, whereas areas of influences grow westward during summer [17,39]. This spatio-temporal variability is integrated in our dynamic scale by constructing areas of influence on a monthly basis.…”
Section: Discussionsupporting
confidence: 89%
“…The extent and influence of currents and water masses vary seasonally and inter-annually in Bass Strait [11]. In accordance with previous oceanographic works at this region, our areas of influence highlighted eastward influence during autumn and winter, whereas areas of influences grow westward during summer [17,39]. This spatio-temporal variability is integrated in our dynamic scale by constructing areas of influence on a monthly basis.…”
Section: Discussionsupporting
confidence: 89%
“…Water bodies that may enter the strait are the Subantarctic Surface Water (SASW) from the south, South Australian Current (SAC) from the northwest and East Australian Current (EAC) from the northeast (Newell 1961). Most current flow is eastward and enhanced by the predominantly westerly winds across southern Australia (Blackman et al 1987, Middleton & Bye 2007.…”
Section: Resale or Republication Not Permitted Without Written Consenmentioning
confidence: 99%
“…Inter-annual variability in Bass Strait water temperature and productivity may be influenced by broad-scale events, including the ENSO in the western Pacific Ocean (Kidson & Renwick 2002, Middleton & Bye 2007. ENSO cycles influence the relative strength of the Leeuwin Current, causing variability in ocean productivity and species' movements (Pearce & Phillips 1988, Wilson et al 2001.…”
Section: Resale or Republication Not Permitted Without Written Consenmentioning
confidence: 99%
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“…In the austral summer the locations of two westward flows rather than one off the southern coast, i.e., a coastal current and the Flinders Current, have been depicted in Fig. 2 of Middleton and Bye (2007). Middleton and Cirano (2002) have shown that a positive wind stress curl on the southern coast can generate the westward Flinders Current, which has been observed to lie off the continental slope as a subsurface current which can reach the surface.…”
Section: Wind Forcing Over a Flat Bottommentioning
confidence: 99%