Sentence examples for shelf current from inspiring English sources

The genetic structure of A. polyacanthus was consistent with these cross shelf current patterns.

The model predicts a "shelf current", shown in Figure 2C, similar to that observed by DeFelice et al. (Rodriguez-Menchaca et al,. 2012).

At smaller spatial scales this inflow generates complex continental shelf current patterns modulated by winds, tides and local reef matrix densities [ 65].

Moreover the molecular stent hypothesis does not account for the dependence of the "shelf current" on external Na+ (Rodriguez-Menchaca et al., 2012), which is expected if amphetamines act by being transported into the cell, a Na+-dependent process.

Utilizing the earliest hatch date and the earliest and latest settlement dates for each cohort, near-reef water temperature, chlorophyll a concentration, wind speed, alongshore and cross-shelf current velocity data, and all otolith-derived ELHTs (i.e. larval growth, PLD, size-at-settlement, juvenile growth) were averaged over the larval and juvenile periods separately.

Penelope Green's article "Lisa Occhipinti Empties the Shelves" (Currents, April 28) highlights the work of a bookbinder and author who creates "haunted stacks of decayed, burned and water-soaked books" as fine art and decorating pieces.

In both cases, cross-shelf currents control sediment distribution and accumulation, not location or amount of primary eolian input.

During the present-day high stand, the main flows, resulting from the interaction between alongshore and cross-shelf currents had a downbasin depositional behavior and resulted in the complete healing, or partial backfilling of the slope channels.

Such cross-shelf currents differ among regions and are predominantly weaker and flow in an onshore direction in the northern region, are stronger and flow in an offshore direction in the central and southern regions of the GBR [ 65].

In contrast, and considering its present local distribution and estimated node ages, the ancestor of Marosatherina most likely colonized western Sulawesi by dispersal from the Sahul Shelf, the current distribution of Pseudomugil and Melanotaeniidae.

The shelf-edge current (water depth of 200 3000 m) was stronger in fall and weaker in spring.