Jm. Jaeger et al., LATERAL TRANSPORT OF SETTLING PARTICLES IN THE ROSS SEA AND IMPLICATIONS FOR THE FATE OF BIOGENIC MATERIAL, J GEO RES-O, 101(C8), 1996, pp. 18479-18488
The Ross Sea, Antarctica, with its high rates of primary productivity
and biogenic accumulation, provides an important location to test the
validity of a one-dimensional particle-settling model. As part of an i
nterdisciplinary field project performed from 1990 to 1992 to examine
cycling and accumulation of biogenic matter in the Ross Sea, water-col
umn particulate and current data were collected at three sites. At eac
h of the sites, a current meter and sediment trap were placed 240 m be
low the water surface, and a similar set of instruments was located 40
m above the seabed. The moorings were deployed for 1- to 2-years dura
tion. The current-meter records showed that the speed of flow in the s
outhwestern Ross Sea is relatively slow (< 20 cm s(-1)) and current di
rection is highly variable. Currents in the south-central Ross Sea hav
e moderate speeds (< 40 cm s(-1)) and less directional variability. Th
e northwestern Ross Sea has the strongest flows (> 50 cm s(-1)) and le
ast variability in direction. To examine the validity of a one-dimensi
onal approximation for fluxes of biogenic material, two models were de
veloped to determine the net displacement of particles settling throug
h the water column. Current-meter data and particle-settling character
istics were incorporated in both models. One model produced a time-var
ying, linearly interpolated current field between the moorings in whic
h particle advection was evaluated, The second model used time-average
d progressive-vector plots to estimate lateral particle advection, Res
ults show that particles are displaced the least at the southwestern s
ite (<20 km), moderate distances at the south-central site (<50 km), a
nd the greatest at the northwestern site (>50 km), The pattern in disp
lacement trends correlates well with observed sediment types and accum
ulation rates at each site, A one-dimensional model for the settling o
f biogenic material is most applicable at the southwestern site and le
ast applicable at the northwestern site.