S2P3-R (v1.0): a framework for efficient regional modelling of physical and biological structures and processes in shelf seas

被引:10
作者
Marsh, R. [1 ]
Hickman, A. E. [1 ]
Sharples, J. [2 ,3 ]
机构
[1] Univ Southampton, Natl Oceanog Ctr, Southampton, Hants, England
[2] Univ Liverpool, Sch Environm Sci, Liverpool L69 3BX, Merseyside, England
[3] Natl Oceanog Ctr, Liverpool L3 5DA, Merseyside, England
基金
英国自然环境研究理事会;
关键词
CHLOROPHYLL-A CONCENTRATION; EAST CHINA SEA; CELTIC SEA; NORTH-SEA; EUROPEAN-SHELF; SPRING BLOOM; SST DATA; PHYTOPLANKTON; OCEAN; FRONTS;
D O I
10.5194/gmd-8-3163-2015
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
An established one-dimensional (1-D) model of Shelf Sea Physics and Primary Production (S2P3) is adapted for flexible use in selected regional settings over selected periods of time. This Regional adaptation of S2P3, the S2P3-R framework (v1.0), can be efficiently used to investigate physical and biological phenomena in shelf seas that are strongly controlled by vertical processes. These include spring blooms that follow the onset of stratification, tidal mixing fronts that seasonally develop at boundaries between mixed and stratified water, and sub-surface chlorophyll maxima that persist throughout summer. While not representing 3-D processes, S2P3-R reveals the horizontal variation of the key 1-D (vertical) processes. S2P3-R should therefore only be used in regions where horizontal processes - including mean flows, eddy fluxes and internal tides - are known to exert a weak influence in comparison with vertical processes. In such cases, S2P3-R may be used as a highly versatile research tool, alongside more complex and computationally expensive models. In undergraduate oceanography modules and research projects, the model serves as an effective practical tool for linking theory and field observations. Three different regional configurations of S2P3-R are described, illustrating a range of diagnostics, evaluated where practical with observations. The model can be forced with daily meteorological variables for any selected year in the reanalysis era (1948 onwards). Example simulations illustrate the considerable extent of synoptic-to-interannual variability in the physics and biology of shelf seas. In discussion, the present limitations of S2P3-R are emphasised, and future developments are outlined.
引用
收藏
页码:3163 / 3178
页数:16
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