The intertidal volume of Florida'sIndian River Lagoon

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Contributors
Publisher
Florida Academy of Sciences.
Date Issued
1992
Note

The intertidal volume of Florida's Indian River lagoon is investigated to quantify
the range of values occurring over a one-year period of time, and to determine the nature of this
temporal variability. Intertidal volumes are calculated for the lagoon as a whole, and for three
sub-basins defined by the lagoon's three inlets. A one-year simulation indicates that 38.7 x 10⁶m³
of water enters and leaves the lagoon on an average semidiurnal tidal cycle. The effective intertidal
volume, representing the net exchange, cannot be determined from the historical data base of
salinity. The range of 12.6-71.7 x 10⁶m³ is due more to diurnal inequalities than to differences
between spring and neap tide conditions. The northern part of the lagoon, with 65% of the total
surface area, contributes only 9% of the intertidal volume. The southern part of the lagoon has
18% of the surface area, but it contributes 63% of the intertidal volume. Harmonic analysis shows
that the M₂ constituent is the principal tidal constituent throughout the lagoon. In the northern
segment, semidiural constituents are damped less than diurnal constituents, and the form number
is about 1.5. Elsewhere, the form number is approximately 0.5.

Language
Type
Genre
Form
Extent
11 p.
Identifier
FA00007499
Additional Information
The intertidal volume of Florida's Indian River lagoon is investigated to quantify
the range of values occurring over a one-year period of time, and to determine the nature of this
temporal variability. Intertidal volumes are calculated for the lagoon as a whole, and for three
sub-basins defined by the lagoon's three inlets. A one-year simulation indicates that 38.7 x 10⁶m³
of water enters and leaves the lagoon on an average semidiurnal tidal cycle. The effective intertidal
volume, representing the net exchange, cannot be determined from the historical data base of
salinity. The range of 12.6-71.7 x 10⁶m³ is due more to diurnal inequalities than to differences
between spring and neap tide conditions. The northern part of the lagoon, with 65% of the total
surface area, contributes only 9% of the intertidal volume. The southern part of the lagoon has
18% of the surface area, but it contributes 63% of the intertidal volume. Harmonic analysis shows
that the M₂ constituent is the principal tidal constituent throughout the lagoon. In the northern
segment, semidiural constituents are damped less than diurnal constituents, and the form number
is about 1.5. Elsewhere, the form number is approximately 0.5.
Florida Atlantic University. Harbor Branch Oceanographic Institute contribution 906
This manuscript is an author version with the final
publication available and may be cited as: Smith, N. P. (1992). The intertidal volume of Florida's
Indian River Lagoon. Florida Scientist 55(4), 209-218.
Date Backup
1992
Date Text
1992
Date Issued (EDTF)
1992
Extension


FAU

IID
FA00007499
Person Preferred Name

Smith, Ned P.
nsmth54@fau.edu
Physical Description

pdf
11 p.
Title Plain
The intertidal volume of Florida'sIndian River Lagoon
Origin Information

1992
Florida Academy of Sciences.

Orlando, FL

Place

Orlando, FL
Title
The intertidal volume of Florida'sIndian River Lagoon
Other Title Info

The intertidal volume of Florida'sIndian River Lagoon