PHYTOPLANKTON AND THERMAL STRUCTURE IN THE UPPER OCEAN - CONSEQUENCES OF NONUNIFORMITY IN CHLOROPHYLL PROFILE

被引:183
作者
LEWIS, MR [1 ]
CULLEN, JJ [1 ]
PLATT, T [1 ]
机构
[1] FISHERIES & OCEANS CANADA, BEDFORD INST OCEANOG, MARINE ECOL LAB, DARTMOUTH B2Y 4A2, NS, CANADA
关键词
D O I
10.1029/JC088iC04p02565
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
引用
收藏
页码:2565 / 2570
页数:6
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[1]   PRODUCTION EQUATIONS IN TERMS OF CHLOROPHYLL CONCENTRATION, QUANTUM YIELD, AND UPPER LIMIT TO PRODUCTION [J].
BANNISTER, TT .
LIMNOLOGY AND OCEANOGRAPHY, 1974, 19 (01) :1-12
[2]  
BRICAUD A, 1981, LIMNOL OCEANOGR, V26, P43
[3]   THE DEEP CHLOROPHYLL MAXIMUM - COMPARING VERTICAL PROFILES OF CHLOROPHYLL-A [J].
CULLEN, JJ .
CANADIAN JOURNAL OF FISHERIES AND AQUATIC SCIENCES, 1982, 39 (05) :791-803
[4]  
CULLEN JJ, 1981, OCEANOL ACTA, V4, P23
[5]  
CULLEN JJ, 1980, THESIS U CALIF SAN D
[6]  
Denman K. L., 1973, Journal of Physical Oceanography, V3, P173, DOI 10.1175/1520-0485(1973)003<0173:ATDMOT>2.0.CO
[7]  
2
[8]   VERTICAL MICROSCALE DISTRIBUTION OF PHYTOPLANKTON IN RELATION TO THE THERMOCLINE [J].
DERENBACH, JB ;
ASTHEIMER, H ;
HANSEN, HP ;
LEACH, H .
MARINE ECOLOGY PROGRESS SERIES, 1979, 1 (03) :187-193
[9]  
DESSUREAULT JG, 1976, OCEAN ENG, V3, P99, DOI 10.1016/0029-8018(76)90038-X
[10]  
FASHAM MJR, 1982, ELECTRONICS OCEAN TE