P. Doyon et Rg. Ingram, Seasonal upper-layer T-S structure in the Gulf of St. Lawrence during the ice-free months, DEEP-SEA II, 47(3-4), 2000, pp. 385-413
Citations number
51
Categorie Soggetti
Aquatic Sciences","Earth Sciences
Journal title
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY
A 75-year hydrographic data set was analyzed to determine the monthly mean
vertical fields of temperature (T) and salinity (S) for 15 sub-regions of t
he Gulf of St. Lawrence (GSL). Objective fields of sea-surface temperature
(SST), salinity and chlorophyll-a (Chl a) also were computed and compared w
ith similar climatologies. Use of recent satellite-derived data enhanced ob
servational coverage of SST and Chi a. These interpolated fields reproduced
several known physical surface characteristics of the GSL with a very smal
l relative interpolation error. The surface heat budget was computed over t
he entire GSL for the 7 ice-free months (May-November incl.) by using SST m
aps in combination with atmospheric fields and satellite-derived monthly av
eraged cloud cover data. Monthly means of mixed-layer depth, upperlayer hea
t content and upper-layer stratification were obtained for 15 sub-regions o
f the GSL. Simple 1D calculations (heat transfer, mixed-layer deepening rat
es, stratification change rates, heat storage rates) were used to study the
seasonal evolution of the upper-layer thermohaline structure. It was obser
ved that the upper-layer could be relatively well modeled in most areas by
considering only the vertical processes. (C) 1999 Elsevier Science Ltd. All
rights reserved..