Seasonal upper-layer T-S structure in the Gulf of St. Lawrence during the ice-free months

Citation
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
ISSN journal
09670645 → ACNP
Volume
47
Issue
3-4
Year of publication
2000
Pages
385 - 413
Database
ISI
SICI code
0967-0645(2000)47:3-4<385:SUTSIT>2.0.ZU;2-2
Abstract
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..