Diagnosis of physical and biological controls on phytoplankton distribution in the Sargasso Sea

被引:0
作者
Wang Caixia [1 ]
Malanotte-Rizzoli, Paola [2 ]
机构
[1] Ocean Univ China, Phys Oceanog Lab, Qingdao 266100, Peoples R China
[2] MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA
关键词
physical-biological coupled model; annual cycle; external forcing; bio-chemical parameter; CHLOROPHYLL MAXIMUM; MODEL; OCEAN; VARIABILITY; ATLANTIC; BERMUDA; CYCLES;
D O I
10.1007/s11802-014-1962-5
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The linkage between physical and biological processes is studied by applying a one-dimensional physical-biological coupled model to the Sargasso Sea. The physical model is the Princeton Ocean Model and the biological model is a five-component system including phytoplankton, zooplankton, nitrate, ammonium, and detritus. The coupling between the physical and biological model is accomplished through vertical mixing which is parameterized by the level 2.5 Mellor and Yamada turbulence closure scheme. The coupled model investigates the annual cycle of ecosystem production and the response to external forcing, such as heat flux, wind stress, and surface salinity, and the relative importance of physical processes in affecting the ecosystem. Sensitivity experiments are also carried out, which provide information on how the model bio-chemical parameters affect the biological system. The computed seasonal cycles compare reasonably well with the observations of the Bermuda Atlantic Time-series Study (BATS). The spring bloom of phytoplankton occurs in March and April, right after the weakening of the winter mixing and before the establishment of the summer stratification. The bloom of zooplankton occurs about two weeks after the bloom of phytoplankton. The sensitivity experiments show that zooplankton is more sensitive to the variations of biochemical parameters than phytoplankton.
引用
收藏
页码:32 / 44
页数:13
相关论文
共 31 条
[1]  
Blumberg AF., 1987, A description of a three-dimensional coastal ocean circulation model, V4, P1, DOI [10.1029/co004p0001, DOI 10.1029/CO004P0001]
[2]   The role of wind in determining the timing of the spring bloom in the Strait of Georgia [J].
Collins, A. Kathleen ;
Allen, Susan E. ;
Pawlowicz, Rich .
CANADIAN JOURNAL OF FISHERIES AND AQUATIC SCIENCES, 2009, 66 (09) :1597-1616
[3]   The response of two coupled one-dimensional mixed layer/planktonic ecosystem models to climate change in the NE subarctic Pacific Ocean [J].
Denman, KL ;
Peña, MA .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2002, 49 (24-25) :5739-5757
[4]   A new coupled, one-dimensional biological-physical model for the upper ocean: Applications to the JGOFS Bermuda Atlantic time-series study (BATS) site [J].
Doney, SC ;
Glover, DM ;
Najjar, RG .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 1996, 43 (2-3) :591-624
[5]  
EPPLEY RW, 1972, FISH B-NOAA, V70, P1063
[6]   HALF-SATURATION CONSTANTS FOR UPTAKE OF NITRATE AND AMMONIUM BY MARINE PHYTOPLANKTON [J].
EPPLEY, RW ;
ROGERS, JN ;
MCCARTHY, JJ .
LIMNOLOGY AND OCEANOGRAPHY, 1969, 14 (06) :912-&
[7]  
Esbensen SK, 1981, 29 OR STAT U CLIM RE
[8]   A NITROGEN-BASED MODEL OF PLANKTON DYNAMICS IN THE OCEANIC MIXED LAYER [J].
FASHAM, MJR ;
DUCKLOW, HW ;
MCKELVIE, SM .
JOURNAL OF MARINE RESEARCH, 1990, 48 (03) :591-639
[9]   A pelagic ecosystem model calibrated with BATS data [J].
Hurtt, GC ;
Armstrong, RA .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 1996, 43 (2-3) :653-683
[10]  
Isemer H., 1985, BUNKER CLIMATE ATLAS, V2