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- W1972477588 abstract "Low salinity plumes have been observed to emanate from the southwestern corner of Onslow Bay, North Carolina near Cape Fear and to extend northeasterly towards Cape Lookout. The length of these plumes is 100–120 km, roughly two-thirds the southwest to northeast extent of the Bay. They influence as much as 20% of the surface area of the Bay with fresh-water volumes ranging from 0·69 to 0·86 km3. This corresponds to at least 15% of the freshwater volume of the entire Bay. The freshwater flux as the plumes cross Frying Pan Shoals ranges from 2·25×102 to 4·05×102 m3 s−1. These plumes dominated the surface salinity structure over the inner half of the shelf in Onslow Bay during 14–15 July and 21–23 July 1976. In addition, a southwesterly flow of waters from Raleigh Bay into Onslow Bay was also observed during the same period. Both flows appear to result from wind-induced circulation." @default.
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- W1972477588 date "1980-07-01" @default.
- W1972477588 modified "2023-10-14" @default.
- W1972477588 title "Summertime advection of low salinity surface waters into Onslow Bay" @default.
- W1972477588 cites W2045736058 @default.
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- W1972477588 doi "https://doi.org/10.1016/s0302-3524(80)80030-2" @default.
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