Physical oceanographic processes affecting larval transport around and through North Carolina inlets
Physical oceanographic processes affecting larval transport around and through North Carolina inlets
复制标题
影响幼虫在北卡罗来纳州入口周围和通过北卡罗来纳州入口运输的物理海洋学过程
DOI:
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发表时间:
1985
期刊:
影响因子:
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通讯作者:
G. Janowitz
中科院分区:
文献类型:
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作者:
L. Pietrafesa;G. Janowitz
Atlantic Spot, Flounder, Croaker and Menhaden all spawn in shelf waters of North Carolina during late fall to early winter. The juveniles use estuaries such as Pamlico Sound and the Cape Fear River as nurseries during their first winter and spring. Previous studies of recruitment into the estuaries through barrier island inlets or estarine mouths assume that the pre and post metamorphosed larvae enter the estuaries at the bottom of the water column and move upstream thereafter. The mechanisms were presumed tidal. The Pamlico Sound has several inlets, Oregon, Hatteras and ocracroke, through which larvae can enter not only during flood stages of the tide but also in the presence of favorable oceanic to estuary sea level pressure gradients. The Cape Fear River has a strong semi-diurnal tidal flow both flood and ebb and also responds vigorously to one-sided divergences and convergences at its mouth. Flow, looking out of the mouth, is in at the left and out on the right. The conclusions are that, in addition to flooding tides, non-local forcing at the estuary mouths can effect transport of larval fish through the estuary mouths, throughout the entire water column.