Reply to comment by Behzad Ataie-Ashtiani on: Effects of tidal fluctuations on mixing and spreading in coastal aquifers Homogeneous case

María Pool; Vincent E.A. Post; Craig T. Simmons

doi:10.1002/2015WR017111

Reply to comment by Behzad Ataie-Ashtiani on: Effects of tidal fluctuations on mixing and spreading in coastal aquifers Homogeneous case

María Pool, Vincent E.A. Post, Craig T. Simmons

College of Science and Engineering

Research output: Contribution to journal › Comment/debate

1 Citation (Scopus)

Abstract

We would like to thank Prof. Behzad Ataie‐Ashtiani for his explanatory comment on our paper [Ataie‐Ashtiani, 2015]. He notes that in confined aquifers with a vertical seaside boundary, a tidal overheight does not develop. This is in contrast to an unconfined aquifer for which a tidal overheight may develop when the tidal amplitude is significant relative to the saturated thickness, in particular in the presences of a sloping land surface. As Prof. Ataie‐Ashtiani points out, the absence of a tidal overheight in the case of a confined aquifer makes that the difference in the model outcomes for a specified head and a specified flux at the inland boundary will be less pronounced than for an unconfined aquifer.

Original language	English
Pages (from-to)	4859-4860
Number of pages	2
Journal	Water Resources Research
Volume	51
Issue number	6
DOIs	https://doi.org/10.1002/2015WR017111
Publication status	Published - 1 Jun 2015

Keywords

mixing-spreading of the transition zone
spatial moments
tidal oscillations

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title = "Reply to comment by Behzad Ataie-Ashtiani on: Effects of tidal fluctuations on mixing and spreading in coastal aquifers Homogeneous case",

abstract = "We would like to thank Prof. Behzad Ataie‐Ashtiani for his explanatory comment on our paper [Ataie‐Ashtiani, 2015]. He notes that in confined aquifers with a vertical seaside boundary, a tidal overheight does not develop. This is in contrast to an unconfined aquifer for which a tidal overheight may develop when the tidal amplitude is significant relative to the saturated thickness, in particular in the presences of a sloping land surface. As Prof. Ataie‐Ashtiani points out, the absence of a tidal overheight in the case of a confined aquifer makes that the difference in the model outcomes for a specified head and a specified flux at the inland boundary will be less pronounced than for an unconfined aquifer. ",

keywords = "mixing-spreading of the transition zone, spatial moments, tidal oscillations",

author = "Mar{\'i}a Pool and Post, {Vincent E.A.} and Simmons, {Craig T.}",

year = "2015",

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doi = "10.1002/2015WR017111",

language = "English",

volume = "51",

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journal = "Water Resources Research",

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TY - JOUR

T1 - Reply to comment by Behzad Ataie-Ashtiani on

T2 - Effects of tidal fluctuations on mixing and spreading in coastal aquifers Homogeneous case

AU - Pool, María

AU - Post, Vincent E.A.

AU - Simmons, Craig T.

PY - 2015/6/1

Y1 - 2015/6/1

N2 - We would like to thank Prof. Behzad Ataie‐Ashtiani for his explanatory comment on our paper [Ataie‐Ashtiani, 2015]. He notes that in confined aquifers with a vertical seaside boundary, a tidal overheight does not develop. This is in contrast to an unconfined aquifer for which a tidal overheight may develop when the tidal amplitude is significant relative to the saturated thickness, in particular in the presences of a sloping land surface. As Prof. Ataie‐Ashtiani points out, the absence of a tidal overheight in the case of a confined aquifer makes that the difference in the model outcomes for a specified head and a specified flux at the inland boundary will be less pronounced than for an unconfined aquifer.

AB - We would like to thank Prof. Behzad Ataie‐Ashtiani for his explanatory comment on our paper [Ataie‐Ashtiani, 2015]. He notes that in confined aquifers with a vertical seaside boundary, a tidal overheight does not develop. This is in contrast to an unconfined aquifer for which a tidal overheight may develop when the tidal amplitude is significant relative to the saturated thickness, in particular in the presences of a sloping land surface. As Prof. Ataie‐Ashtiani points out, the absence of a tidal overheight in the case of a confined aquifer makes that the difference in the model outcomes for a specified head and a specified flux at the inland boundary will be less pronounced than for an unconfined aquifer.

KW - mixing-spreading of the transition zone

KW - spatial moments

KW - tidal oscillations

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DO - 10.1002/2015WR017111

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JO - Water Resources Research

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SN - 0043-1397

IS - 6

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Reply to comment by Behzad Ataie-Ashtiani on: Effects of tidal fluctuations on mixing and spreading in coastal aquifers Homogeneous case

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Keywords

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