Thermal and haline variability over the central Bering Sea shelf: Seasonal and interannual perspectives

被引:56
作者
Danielson, S. [1 ]
Eisner, L. [2 ]
Weingartner, T. [1 ]
Aagaard, K. [3 ]
机构
[1] Univ Alaska Fairbanks, Inst Marine Sci, Sch Fisheries & Ocean Sci, Fairbanks, AK 99775 USA
[2] Natl Marine Fisheries Serv, NOAA, Alaska Fisheries Sci Ctr, Ted Stevens Marine Res Inst, Juneau, AK USA
[3] Univ Washington, Appl Phys Lab, Polar Sci Ctr, Seattle, WA 98105 USA
基金
美国国家科学基金会;
关键词
Bering Sea; Seasonal variability; Interannual variability; Temperature; Salinity; Ekman transport; ALEUTIAN LOW; FRESH-WATER; HEAT FLUXES; ICE; ECOSYSTEM; PACIFIC; EDGE; FLOW; PRODUCTIVITY; CLIMATOLOGY;
D O I
10.1016/j.csr.2010.12.010
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
We examine multi-year conductivity-temperature-depth (CTD) data to better understand temperature and salinity variability over the central Bering Sea shelf. Particular consideration is given to observations made annually from 2002 to 2007 between August and October, although other seasons and years are also considered. Vertical and horizontal correlation maps show that near-surface and near-bottom salinity anomalies tend to fluctuate in phase across the central shelf, but that temperature anomalies are vertically coherent only in the weakly or unstratified inner-shelf waters. We formulate heat content (HC) and freshwater content (FWC) budgets based on the CTD observations, direct estimates of external fluxes (surface heat fluxes, ice melt, precipitation (P), evaporation (E) and river discharge), and indirect estimates of advective contributions. Ice melt, P - E, river discharge, and along-isobath advection are sufficient to account for the mean spring-to-fall increase in FWC, while summer surface heat fluxes are primarily responsible for the mean seasonal increase in HC, although interannual variability in the HC at the end of summer appears related to variability in the along-isobath advection during the summer months. On the other hand, FWC anomalies at the end of summer are significantly correlated with the mean wind direction and cross-isobath Ekman transport averaged over the previous winter. Consistent with the latter finding, salinities exhibit a weak but significant inverse correlation between the coastal and mid-shelf waters. The cross-shelf transport likely has significant effect on nutrient fluxes and other processes important to the functioning of the shelf ecosystem. Both the summer and winter advection fields appear to result from the seasonal mean position and strength of the Aleutian Low. We find that interannual thermal and haline variability over the central Bering Sea shelf are largely uncoupled. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:539 / 554
页数:16
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