Meteorological forcing of coastal waters by the inverse barometer effect

File
Contributors
Publisher
Elsevier Ltd.
Date Issued
1979
Note

Water level and surface pressure data from the northeastern and northwestern Gulf of Mexico are used to investigate the water level response to meteorological forcing by the inverse barometer effect. Statistically significant coherence-squared values are computed for variations in cross-Gulf surface pressure and water level differences over time scales on the order of 2 to 6 days.

Language
Type
Genre
Extent
9 p.
Identifier
3172952
Additional Information
Water level and surface pressure data from the northeastern and northwestern Gulf of Mexico are used to investigate the water level response to meteorological forcing by the inverse barometer effect. Statistically significant coherence-squared values are computed for variations in cross-Gulf surface pressure and water level differences over time scales on the order of 2 to 6 days.
This manuscript is an author version with the final publication available at http://www.sciencedirect.com/science/journal/03023524 and may be cited as: Smith, N. P. (1979). Meteorological forcing of coastal waters by the inverse barometer effect. Estuarine and Coastal Marine Science, 8(2), 149-156. doi:10.1016/0302-3524(79)90070-7
Florida Atlantic University. Harbor Branch Oceanographic Institute contribution #124.
Date Backup
1979
Date Text
1979
DOI
10.1016/0302-3524(79)90070-7
Date Issued (EDTF)
1979
Extension


FAU
FAU
admin_unit="FAU01", ingest_id="ing10123", creator="creator:BCHANG", creation_date="2011-08-02 16:25:10", modified_by="super:FAUDIG", modification_date="2014-02-11 11:03:49"

IID
FADT3172952
Issuance
single unit
Person Preferred Name

Smith, Ned P.

creator

nsmth54@fau.edu
Physical Description

pdf
9 p.
Title Plain
Meteorological forcing of coastal waters by the inverse barometer effect
Origin Information

Elsevier Ltd.
1979
single unit
Title
Meteorological forcing of coastal waters by the inverse barometer effect
Other Title Info

Meteorological forcing of coastal waters by the inverse barometer effect