Modelling the ecosystem dynamics of the Barents Sea including the marginal ice zone II. Carbon flux and interannual variability

被引:149
作者
Wassmann, P [1 ]
Slagstad, D
Riser, CW
Reigstad, M
机构
[1] Univ Tromso, Norwegian Coll Fishery Sci, N-9037 Tromso, Norway
[2] SINTEF, Fisheries & Aquaculture, N-7465 Trondheim, Norway
关键词
3D modelling; carbon flux; marginal ice zone; interannual variability; Barents Sea;
D O I
10.1016/j.jmarsys.2005.05.006
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
An upgraded and revised physically-biologically coupled, nested 3D model with 4 km grid size is applied to investigate the seasonal carbon flux and its interannual variability. The model is validated using field data from the years for which the carbon flux was modelled, focussing on its precision in space and tune, the adequacy of the validation data, suspended biomass and vertical export. The model appears to reproduce the space and time ( 1 week and 10 nautical miles) distribution of suspended biomass well, but it underestimates vertical export of carbon at depth. The modelled primary production ranges from 79 to 118 g C m(-2) year(-1) (average 93 g C m(-2) year(-1)) between 4 different years with higher variability in the ice-covered Arctic ( +/- 26%) than in the Atlantic ( +/- 7%) section. Meteorological forcing has a strong impact on the vertical stratification of the regions dominated by Atlantic water and this results in significant differences in seasonal variability in primary production. The spatially integrated primary production in the Barents Sea is 42-49% greater during warm years than the production during the coolest and most icecovered year. (c) 2005 Elsevier B.V. All rights reserved.
引用
收藏
页码:1 / 24
页数:24
相关论文
共 60 条
[1]   A STUDY OF THE CLIMATIC SYSTEM IN THE BARENTS SEA [J].
ADLANDSVIK, B ;
LOENG, H .
POLAR RESEARCH, 1991, 10 (01) :45-49
[2]   Vertical flux of phytoplankton and particulate biogenic matter in the marginal ice zone of the Barents Sea in May 1993 [J].
Andreassen, IJ ;
Wassmann, P .
MARINE ECOLOGY PROGRESS SERIES, 1998, 170 :1-14
[3]   Seasonal and spatial changes in biomass, structure, and development progress of the zooplankton community in the Barents Sea [J].
Arashkevich, E ;
Wassmann, P ;
Pasternak, A ;
Riser, CW .
JOURNAL OF MARINE SYSTEMS, 2002, 38 (1-2) :125-145
[4]   The contribution of microzooplankton to the diet of mesozooplankton in an upwelling filament off the north west coast of Spain [J].
Batten, SD ;
Fileman, ES ;
Halvorsen, E .
PROGRESS IN OCEANOGRAPHY, 2001, 51 (2-4) :385-398
[5]   A SIMPLE, SOLAR SPECTRAL MODEL FOR DIRECT-NORMAL AND DIFFUSE HORIZONTAL IRRADIANCE [J].
BIRD, RE .
SOLAR ENERGY, 1984, 32 (04) :461-471
[6]  
CADEE GC, 1992, POLAR BIOL, V12, P75
[7]   Seasonal dynamics of phytoplankton and Calanus finmarchicus in the North Sea as revealed by a coupled one-dimensional model [J].
Carlotti, F ;
Radach, G .
LIMNOLOGY AND OCEANOGRAPHY, 1996, 41 (03) :522-539
[8]   Calibration of sediment traps and particulate organic carbon export using 234Th in the Barents Sea [J].
Coppola, L ;
Roy-Barman, M ;
Wassmann, P ;
Mulsow, S ;
Jeandel, C .
MARINE CHEMISTRY, 2002, 80 (01) :11-26
[9]   The importance of advection on production of Calanus finmarchicus in the Atlantic part of the Barents Sea [J].
Edvardsen, A ;
Tande, KS ;
Slagstad, D .
SARSIA, 2003, 88 (04) :261-273
[10]   Physical and ecological processes in the marginal ice zone of the northern Barents Sea during the summer melt period [J].
Falk-Petersen, S ;
Hop, H ;
Budgell, WP ;
Hegseth, EN ;
Korsnes, R ;
Loyning, TB ;
Orbæk, JB ;
Kawamura, T ;
Shirasawa, K .
JOURNAL OF MARINE SYSTEMS, 2000, 27 (1-3) :131-159