Coupled 3D physical and biological modelling of the mesoscale variability observed in North-East Atlantic in spring 1997: biological processes

被引:32
作者
Popova, EE
Lozano, CJ
Srokosz, MA
Fasham, MJR
Haley, PJ
Robinson, AR
机构
[1] Southampton Oceanog Ctr, Southampton SO14 3ZH, Hants, England
[2] Harvard Univ, Dept Earth & Planetary Sci, Div Appl Sci, Cambridge, MA 02138 USA
基金
英国自然环境研究理事会;
关键词
modelling; ecosystems; mesoscale processes; data assimilation;
D O I
10.1016/S0967-0637(02)00091-2
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
A limited area, eddy resolving coupled physical and biological model and data assimilation are used to reproduce and analyse the ecosystem variability observed in the North-East Atlantic in April-May 1997 on Discovery cruise 227. The ecosystem was in a post-bloom grazing controlled regime. The combination of the deep mixing in the upper layer during the cruise and a deeper than average winter convection led to high-nutrient-low-chlorophyll type conditions, which are unusual for this location. These conditions and lack of strong mesoscale physical features led to low spatial variability of phyto- and zooplankton yet strong sensitivity to the variations in the vertical mixing (storm event). Modelling results show that plankton patchiness formation under these conditions was dominated by biological mechanisms (mainly predator-prey oscillations). Furthermore, this mechanism, together with mixing and stirring, are responsible in this order for the observed scales and variability of patchiness from homogeneous low winter concentrations of phyto- and zooplankton. (C) 2002 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:1741 / 1768
页数:28
相关论文
共 42 条
[1]  
Anderson J, 2000, SHEFF PACK TECHNOL, V1, P47
[2]   Size-fractionated primary production and nitrogen uptake during a North Atlantic phytoplankton bloom: implications for carbon export estimates [J].
Bury, SJ ;
Boyd, PW ;
Preston, T ;
Savidge, G ;
Owens, NJP .
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS, 2001, 48 (03) :689-720
[3]  
Carter E. F., 1987, Journal of Atmospheric and Oceanic Technology, V4, P49, DOI 10.1175/1520-0426(1987)004<0049:AMFTEO>2.0.CO
[4]  
2
[5]   An empirical model of the phytoplankton chlorophyll:carbon ratio - The conversion factor between productivity and growth rate [J].
Cloern, JE ;
Grenz, C ;
VidergarLucas, L .
LIMNOLOGY AND OCEANOGRAPHY, 1995, 40 (07) :1313-1321
[6]  
CONKRIGHT M, 1994, WORLD OCEAN ATLAS 19, V1
[7]  
desBaar H. J. W., 2000, CHANGING OCEAN CARBO, P61
[8]   CONTINUOUS ASSIMILATION IN AN OPEN DOMAIN OF THE NORTHEAST ATLANTIC .1. METHODOLOGY AND APPLICATION TO ATHENA-88 [J].
DOMBROWSKY, E ;
DEMEY, P .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1992, 97 (C6) :9719-9731
[9]   INTRODUCTION TO THE JGOFS NORTH-ATLANTIC BLOOM EXPERIMENT [J].
DUCKLOW, HW ;
HARRIS, RP .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 1993, 40 (1-2) :1-8
[10]   The role of higher predation in plankton population models [J].
Edwards, AM ;
Yool, A .
JOURNAL OF PLANKTON RESEARCH, 2000, 22 (06) :1085-1112