Seasonal and interannual variability in the distribution of nutrients and chlorophyll a across the Gulf of Alaska shelf:: 1998-2000

被引:90
作者
Childers, AR [1 ]
Whitledge, TE [1 ]
Stockwell, DA [1 ]
机构
[1] Univ Alaska, Inst Marine Sci, Fairbanks, AK 99775 USA
基金
美国国家科学基金会; 美国海洋和大气管理局;
关键词
D O I
10.1016/j.dsr2.2004.09.018
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The northern Gulf of Alaska shelf is a productive coastal region that supports several commercially important fisheries. The mechanisms supporting such high levels of productivity over this shelf, however, are not understood since it is a downwelling-dominated shelf. Furthermore, the annual nutrient cycle in this region was completely unknown prior to this research. In an effort to understand the mechanisms driving such high biological productivity, cross-shelf nutrient distributions were sampled 18 times throughout 1998, 1999 and 2000. Deep-water (> 75 m) nitrate, silicate and phosphate were positively correlated with salinity, indicating an offshore nutrient source. The average annual cycle was established, in which nitrate, silicate and phosphate responded seasonally to physical and biological processes. Ammonium concentrations were generally low and uniform (< 1.2 mu M), with occasional patches of higher concentrations. Throughout the summer months, the upper 10-20 m across shelf were depleted of nitrate, silicate and phosphate over the inner and middle shelves and depleted of nitrate and phosphate over the shelf break and slope; however, just below this nutrient-poor layer the water column was nutrient-replete. During each summer, there was an onshore flux of dense nutrient-rich bottom water onto the shelf when the downwelling relaxed. This seasonal flux created a nutrient reservoir near the bottom of the inner and middle shelves. There reservoir was eventually mixed throughout the water column during the winter months. This annual evolution may be vital to the productivity of this shelf. There was a large degree of interannual variability among the 3 years, which included El Nina, (1998) and La Nina (1999) years. Nutrient concentrations and chlorophyll were generally highest in 2000, except in May 1999, when a large eddy traveling along the continental slope greatly enhanced phytoplankton chlorophyll biomass. Daily new production estimates based on nitrate disappearance averaged over the spring. summer. season ranged from 2.46 to 6.97 mmol nitrate m(-2) day(-1). (c) 2004 Elsevier Ltd. All rights reserved.
引用
收藏
页码:193 / 216
页数:24
相关论文
共 30 条
[1]  
Chapman DC, 2000, J PHYS OCEANOGR, V30, P2941, DOI 10.1175/1520-0485(2001)031<2941:BLCOBC>2.0.CO
[2]  
2
[3]  
CHILDERS AR, 2001, THESIS U ALASKA FAIR
[4]  
Hare SR, 1999, FISHERIES, V24, P6, DOI 10.1577/1548-8446(1999)024<0006:IPR>2.0.CO
[5]  
2
[6]   Comparison of factors controlling phytoplankton productivity in the NE and NW subarctic Pacific gyres [J].
Harrison, PJ ;
Boyd, PW ;
Varela, DE ;
Takeda, S ;
Shiomoto, A ;
Odate, T .
PROGRESS IN OCEANOGRAPHY, 1999, 43 (2-4) :205-234
[7]  
Lalli C.M., 1993, BIOL OCEANOGRAPHY IN
[8]   KINETICS OF NITRATE AND AMMONIA UPTAKE BY NATURAL POPULATIONS OF MARINE PHYTOPLANKTON [J].
MACISAAC, JJ ;
DUGDALE, RC .
DEEP-SEA RESEARCH, 1969, 16 (01) :45-&
[9]  
Mantua N J., 1999, The Pacific decadal oscillation: A brief overview for non-specialists
[10]  
*NASA, 2003, TOPEX POS PRIM MISS