Over 70% of the surface of Earth is ocean, comprising highly diverse marine and coastal ecosystems. These ecosystems provide a wide range of essential ecosystem services that support human societies, including our health and economies.

The information provided in the map below remains incomplete in some places of the world. The Ocean+ team is always looking to update these maps as soon as new data becomes available. If we are missing any information for your location, please contact us at oceanplus@unep-wcmc.org.


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Experience ultimate comfort in our brand-new Premier Sunrise Ocean Plus room. Enjoy stunning panoramic ocean views and the lush greenery of Manuel Antonio National Park from your private balcony.

The infinity of oceans in your bathroom: Ocean Plus. Ocean Plus Series creates unique atmosphere in bathrooms with its plain chicness. The environmentally-friendly series that attracts attention with its functionality besides its flawless design carries the ocean breeze to the bathrooms.

Ocans is the culmination of two years of planning, four years of filming, which included 70 expeditions to 54 shooting locations. The film banks on the beauty of the oceans (plus the skill of the crew and some fancy equipment) to convince viewers that ocean conservation is paramount. Not surprisingly, the technique works, say the critics.

We develop a spectral inversion method for mass redistribution on the Earth's surface given geodetic measurements of the solid Earth's geometrical shape, using the elastic load Love numbers. First, spectral coefficients are geodetically estimated to some degree. Spatial inversion then finds the continental surface mass distribution that would force geographic variations in relative sea level such that it is self-consistent with an equipotential top surface and the deformed ocean bottom surface and such that the total (ocean plus continental mass) load has the same estimated spectral coefficients. Applying this theory, we calculate the contribution of seasonal interhemispheric (degree 1) mass transfer to variation in global mean sea level and nonsteric static ocean topography, using published GPS results for seasonal degree-1 surface loading from the global IGS network. Our inversion yields ocean-continent mass exchange with annual amplitude (2.92  0.14)  1015 kg and maximum ocean mass on 25 August 3 days. After correction for the annual variation in global mean vertical deformation of the ocean floor (0.4 mm amplitude), we find geocentric sea level has an amplitude of 7.6  0.4 mm, consistent with TOPEX-Poseidon results (minus steric effects). The seasonal variation in sea level at a point strongly depends on location ranging from 3 to 19 mm, the largest being around Antarctica in mid-August. Seasonal gradients in static topography have amplitudes of up to 10 mm over 5000 km, which may be misinterpreted as dynamic topography. Peak continental loads occur at high latitudes in late winter at the water-equivalent level of 100-200 mm.

The first projects undertaken arise from those in which NOAA and institute investigators have ongoing interactions and collaborations. As the institute moves forward, the goal is for the CINAR scientists to work closely with NOAA investigators to plan future projects and programs, and to work together to find funding for the work. Examples include studies of climate-related ocean acidification (a worrisome result of excess carbon dioxide in the atmosphere) and marine spatial planning (similar to land use planning, but focused on specific marine habitats or systems).

Another expected major activity is developing and deploying arrays of underwater vehicles and instruments needed to continuously monitor the ocean as part of the growing ocean observatory network. Central to these efforts will be arrays of meteorological and hydrographic sensors deployed in the equatorial Pacific and other areas far from the northeastern U.S., but where measurements are needed to understand global climate processes that ultimately affect this region and its valuable fisheries and ecosystems. e24fc04721

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