Rg. Bell et al., CHARACTERIZATION OF PHYSICAL ENVIRONMENTAL-FACTORS ON AN INTERTIDAL SANDFLAT, MANUKAU HARBOR, NEW-ZEALAND, Journal of experimental marine biology and ecology, 216(1-2), 1997, pp. 11-31
Physical environmental factors, including sediment characteristics, in
undation time, tidal currents and wind waves, likely to influence the
structure of the benthic community at meso-scales (1-100 m) were chara
cterised for a sandflat off Wiroa Island (Manukau Harbour, New Zealand
). In a 500x250 m study site, sediment characteristics and bed topogra
phy were mostly homogenous apart from patches of low-relief ridges and
runnels. Field measurements and hydrodynamic modelling portray a comp
lex picture of sediment or particulate transport on the intertidal fla
t, involving interactions between the larger scale tidal processes and
the smaller scale wave dynamics (1-4 s; 1-15 m). Peak tidal currents
in isolation are incapable of eroding bottom sediments, but in combina
tion with near-bed orbital currents generated by only very small wind
waves, sediment transport can be initiated. Work done on the bed integ
rated over an entire tidal cycle by prevailing wind waves is greatest
on the elevated and flatter slopes of the study site, where waves shoa
l over a wider surf zone and water depths remain shallow enough for wa
ve-orbital currents to disturb the bed. The study also provided physic
al descriptors quantifying static and hydrodynamic (tidal and wave) fa
ctors which were used in companion studies on ecological spatial model
ling of bivalve distributions and micro-scale sediment reworking and t
ransport. (C) 1997 Elsevier Science B.V.