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

被引:16
作者
Doyon, P [1 ]
Ingram, RG
机构
[1] McGill Univ, Dept Atmospher & Ocean Sci, Montreal, PQ H3A 2K6, Canada
[2] CRIM, Montreal, PQ H3A 1B9, Canada
[3] Univ British Columbia, St Johns Coll, Vancouver, BC V6T 1Z4, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
D O I
10.1016/S0967-0645(99)00112-5
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
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 the Gulf of St. Lawrence (GSL). Objective fields of sea-surface temperature (SST), salinity and chlorophyll-a (Chl a) also were computed and compared with similar climatologies. Use of recent satellite-derived data enhanced observational coverage of SST and Chi a. These interpolated fields reproduced several known physical surface characteristics of the GSL with a very small relative interpolation error. The surface heat budget was computed over the entire GSL for the 7 ice-free months (May-November incl.) by using SST maps in combination with atmospheric fields and satellite-derived monthly averaged cloud cover data. Monthly means of mixed-layer depth, upperlayer heat content and upper-layer stratification were obtained for 15 sub-regions of the GSL. Simple 1D calculations (heat transfer, mixed-layer deepening rates, stratification change rates, heat storage rates) were used to study the seasonal evolution of the upper-layer thermohaline structure. It was observed 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..
引用
收藏
页码:385 / 413
页数:29
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