Philippine Marginal Seas NAST/NRCP/DOST

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Marginal Seas of the Philippines:a marginal sea is a sea Status and Challengespartially enclosed by islands, archipelagos, or peninsulas, adjacent to or Cesar L Villanoy widely open to the open South China Sea Marine Science Instituteocean at the surface, West Philippine Sea and/or bounded by East UniversitySea of the Philippines submarine ridges on the Sulu Sea sea floor - Wikipedia Sulawesi Sea RTD on Philippine Marginal Seas NAST/NRCP/DOST Smaller Marginal Seas within the Archipelago San Bernardino Strait N Sibuyan Sea Sill depth 92m S Sibuyan Sea Visayan Sea Surigao Strait Camotes Sea Sill depth 52m Bohol Sea Bathymetry Philippine archipelagic basins are deep but separated by shallower topographic barriers of sills Name Max Depth Sill Depth (m) Surface Area (km2) South China Sea >5,000 2,200 3,352,500 Sulawesi Sea >5,000 1,350 430,000 Sulu Sea >5,000 520 (Panay) 287,500 350 (Sibutu) Bohol Sea 1,800 420 (Sulu) 26,150 52 (Surigao Strait) North Sibuyan 1,700 500 9,500 South Sibuyan 1,350 400 7,500 Visayan 50 Shallow sea 8,900 Camotes 800 <300 8,600 Deep water flowing over sills Temperature and oxygen profiles below 300m in the different basins Chlorophyll Forcing in the Marginal Seas Asian Monsoon Winds earth.nullschool.net Chavanne et al., 2002) Wind jets in the Verde Passage forcing local upwelling May et al, 2011 Bohol Sea Marginal Sea with significant flow from Pacific to Sulu Sea Bohol Jet and Iligan Bay Eddy Semi-enclosed nature of archipelagic basins and implications to reef connectivity Kool et al, 2011 Summary • Archipelagic marginal seas semi enclosed with topographic sills • Sills play important role in determining properties of the deep waters of basins and degree of mixing (influences productivity) • Monsoonal forcing • Funneling of wind between islands (and along boundaries of marginal seas) can produce wind jets which drives enhanced mixing and upwelling – contribution to productivity Challenges • Understanding the dynamics of marginal seas – No accurate representation of winds over the archipelagic basins – Land-sea-air interaction – orographic effects, runoff • Small time and space scales /high variability – more difficult to measure and to predict .

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