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- W2138449338 abstract "Daily averaged salinity measurements made in the middle reach of the Delaware estuary over the past three decades indicate the presence of significant subtidal variability. The salinity signals are dominated by variabilities at seasonal to interannual timescales. For any given month of the year the interannual variability accounted for more than 80% of the total deviations from the climatological mean monthly distributions. Variability at timescales shorter than a month is relatively insignificant. The long‐term variations in salinity are closely correlated with the Delaware River discharge, with higher discharge corresponding to lower salinity and vice versa. Contrary to expectation, the long‐term variations in the axial salinity gradient appear to have a negative correlation with the river discharge, with an increase in discharge corresponding to a reduction in the axial salinity gradient and vice versa. A number of factors, including the downstream movement of the salt intrusion limit beyond the observational station, the variation in the vertical salinity structure, and the possible existence of significant lateral variability may contribute to the observed response of the axial salinity gradient to different river discharge conditions." @default.
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- W2138449338 date "1995-10-15" @default.
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- W2138449338 title "On the relationship between long‐term salinity variations and river discharge in the middle reach of the Delaware estuary" @default.
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- W2138449338 doi "https://doi.org/10.1029/95jc01406" @default.
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