Water-table variations on a reflective ocean beach: Quogue, New York

W. L. Metcalf; H. J. Bokuniewicz; A. V. Terchunian

Water-table variations on a reflective ocean beach: Quogue, New York

W. L. Metcalf
, H. J. Bokuniewicz
, A. V. Terchunian

University of Missouri

Research output: Contribution to journal › Article › peer-review

1 Scopus citations

Abstract

The water-table elevation responded to tidal conditions. The range of variation in the water-table elevation was suppressed with distance shoreward and also reduced, apparently by the seepage of ground water into the swash zone, near the shoreline. The water-table oscillation propagated shoreward at speeds of between 7 and 20 m/hr and seemed to be substantially influenced by the continued seaward flow of fresh ground water. -from Authors

Original language	English
Pages (from-to)	61-67
Number of pages	7
Journal	Northeastern Geology and Environmental Sciences
Volume	17
Issue number	1
State	Published - 1995

Cite this

@article{8e78d6d4e74f4526aeb4744e5f0d8a74,

title = "Water-table variations on a reflective ocean beach: Quogue, New York",

abstract = "The water-table elevation responded to tidal conditions. The range of variation in the water-table elevation was suppressed with distance shoreward and also reduced, apparently by the seepage of ground water into the swash zone, near the shoreline. The water-table oscillation propagated shoreward at speeds of between 7 and 20 m/hr and seemed to be substantially influenced by the continued seaward flow of fresh ground water. -from Authors",

author = "Metcalf, \{W. L.\} and Bokuniewicz, \{H. J.\} and Terchunian, \{A. V.\}",

year = "1995",

language = "English",

volume = "17",

pages = "61--67",

journal = "Northeastern Geology and Environmental Sciences",

issn = "0194-1453",

number = "1",

}

TY - JOUR

T1 - Water-table variations on a reflective ocean beach

T2 - Quogue, New York

AU - Metcalf, W. L.

AU - Bokuniewicz, H. J.

AU - Terchunian, A. V.

PY - 1995

Y1 - 1995

N2 - The water-table elevation responded to tidal conditions. The range of variation in the water-table elevation was suppressed with distance shoreward and also reduced, apparently by the seepage of ground water into the swash zone, near the shoreline. The water-table oscillation propagated shoreward at speeds of between 7 and 20 m/hr and seemed to be substantially influenced by the continued seaward flow of fresh ground water. -from Authors

AB - The water-table elevation responded to tidal conditions. The range of variation in the water-table elevation was suppressed with distance shoreward and also reduced, apparently by the seepage of ground water into the swash zone, near the shoreline. The water-table oscillation propagated shoreward at speeds of between 7 and 20 m/hr and seemed to be substantially influenced by the continued seaward flow of fresh ground water. -from Authors

UR - https://www.scopus.com/pages/publications/0028851488

M3 - Article

AN - SCOPUS:0028851488

SN - 0194-1453

VL - 17

SP - 61

EP - 67

JO - Northeastern Geology and Environmental Sciences

JF - Northeastern Geology and Environmental Sciences

IS - 1

ER -

Water-table variations on a reflective ocean beach: Quogue, New York

Abstract

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