P. Lindsay, TEMPORAL AND SPATIAL VARIATIONS IN DENSITY AND VELOCITY-FIELDS OF THEWATERS OF GARELOCH, SCOTLAND, Environmental geology, 28(4), 1996, pp. 201-212
Citations number
13
Categorie Soggetti
Water Resources","Environmental Sciences","Geosciences, Interdisciplinary
Spatial variations in the density and velocity fields have been observ
ed in the Gareloch (Scotland) during surveys in 1987-1988 and 1993-199
4. The variation of the density field has been analyzed on a variety o
f time scales from Semidiurnal to seasonal in order to quantify effect
s caused by the forcing factors of tidal mixing, freshwater input, and
wind. Initial results indicate that water density in the loch is cont
rolled (to a major degree) by the freshwater input from runoff from th
e local catchment area and from freshwater entering on the flood tide
from the Clyde Estuary. It is estimated that during winter periods the
high freshwater flows from the rivers Leven and Clyde into the Clyde
Estuary account for up to 75% of the freshwater creating the density s
tructure in the loch. Analysis of long-term dissolved oxygen data reve
als that major bottom water renewals occurred between July and January
in the years 1987-1994. Major bottom water dissolved oxygen renewals
have a general trend but during the year sporadic renewals can take pl
ace due to abnormal dry spells increasing the density of the water ent
ering from the Clyde, or consistently strong winds from the north redu
cing stratification in the loch and producing better mixed conditions.
Velocities vary spatially, with the highest velocities of up to 0.6 m
s(-1) being associated with the velocity jet effect at the constricti
on at the sill of the loch. Observed near-surface mid-loch velocities
increased as the vertical density gradients in the upper layers increa
sed. This indicates for the observed conditions that increased stratif
ication in the upper layers inhibits the entrainment rate and hence ra
te of gain of thickness of the wind-driven surface layer, resulting in
increased surface velocities for a given wind speed and direction. Th
e main flow is concentrated in the upper 10 m and velocities below 10
m are low. Observed mean spring tide surface velocities are on average
30% greater than mean neap tide surface velocities.