Margaret Goud Collins

International Institute for Applied Systems Analysis

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Jean‐Yves Collot

Institut de Recherche pour le Développement

Maria Ask

Uppsala University

Jonathan B. Martin

University of Florida

Stefan Menger

Halliburton (United Kingdom)

Pamela Reid

University of North Carolina Wilmington

Thomas Scott Staerker

Florida State University

Jose Ignacio Martinez-Rodriguez

Pierrick Roperch

Université de Rennes

Terrence M. Quinn

The University of Texas at Austin

John N. Leonard

Manchester Royal Infirmary

Cooperative Institutions

International Institute for Applied Systems Analysis

Centre National de la Recherche Scientifique

Scripps Institution of Oceanography

Woods Hole Oceanographic Institution

University of California System

Institut de Recherche pour le Développement

University of Texas Institute for Geophysics

Texas A&M University

University of New Caledonia

University of California, San Diego

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International Organizations and Biodiversity

Elsevier eBooks (2013)

Margaret Goud Collins

10.1016/b978-0-12-384719-5.00395-6

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Citations (3)

The Coupling between Harbor Seiches at Palawan Island and Sulu Sea Internal Solitons*

Journal of Physical Oceanography (1998)

Graham S. Giese David Chapman Margaret Goud Collins Rolu Encarnacion Gil S. Jacinto

Between 1989 and 1991 the authors made observations that confirm and elucidate the coupling between harbor seiches at Puerto Princesa on Palawan Island in the Philippines and tide-generated internal solitons in the Sulu Sea. Published tidal current predictions for Basilan Strait in the Sulu Archipeligo were used to produce an index to the daily ebb tidal flows near Pearl Bank where the solitons originate. The coherence between predicted maximum ebb tidal current speed and observed seiche activity was 0.60 and the phase lag between the two quantities closely matched published estimates of the time required for solitons to cross the Sulu Sea. Arrival of the Sulu Sea waves immediately offshore of Puerto Princesa in the form of internal bores corresponded in time to the initiation of harbor seiche activity. A more precise estimate of soliton travel time was determined from the time difference between predicted maximum ebb current and the initiation of seiche activity, and it was found to have a remarkably regular seasonal pattern, which can be largely explained by seasonal variations in Sulu Sea temperature and salinity stratification. Therefore, the timing of seiche events at Puerto Princesa can be forecast based on Sulu Archipeligo tide predictions and soliton travel time. In general, the fortnightly pattern of seiche magnitude follows that of tidal current predictions, but day-to-day deviations are common. Seiche magnitude varies seasonally with generally low activity during the winter (northeast) monsoon and usually maximum activity late in the summer (southwest) monsoon.

Seiche

Internal tide

10.1175/1520-0485(1998)028<2418:tcbhsa>2.0.co;2

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Citations (17)

ODP Leg 134, Hole 831B - Well Logging Data

Zenodo (CERN European Organization for Nuclear Research) (2020)

Jean‐Yves Collot H. Gary Greene Laura B. Stokking Kazumi Akimoto Maria Ask

Logging data are measurements of physical properties of the formation surrounding a borehole, acquired in situ after completion of coring (wireline logging) or during drilling (Logging-While-Drilling, LWD). The range of data (resistivity, gamma radiation, velocity, density, borehole images,…) in any hole depends on the scientific objectives and operational constraints.

10.5281/zenodo.3942396

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ODP Leg 134, Hole 832B - Well Logging Data

Zenodo (CERN European Organization for Nuclear Research) (2020)

Jean‐Yves Collot H. Gary Greene Laura B. Stokking Kazumi Akimoto Maria Ask

10.5281/zenodo.3942398

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Citations (0)

ODP Leg 134, Hole 831B - Well Logging Data

Zenodo (CERN European Organization for Nuclear Research) (2020)

Jean‐Yves Collot H. Gary Greene Laura B. Stokking Kazumi Akimoto Maria Ask