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The Regional Ocean Modeling System (ROMS) is a free-surface, terrain-following, primitive equations ocean model widely used by the scientific community for a diverse range of applications. The operational Northeast Atlantic (NEATL) model is an implementation of the ROMS model...
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Data on the offshore geologic intrusive bodies around Ireland. An intrusion is liquid rock that forms under Earth's surface. Magma from under the surface is slowly pushed up from deep within the earth into any cracks or spaces it can find, sometimes pushing existing country...
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Location of marine basin divisions in the North Atlantic around Ireland. A geological basin is a large low-lying area. It is often below sea level. There are five designated basins and each basin represents a large submarine depression of a generally circular, elliptical or...
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EnvironmentSeasonal density driven transport from the Irish Offshore Strategic Environmental Assessment (IOSEA).
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This dataset contains a GIS vector polyline of 11,770 2D seismic survey lines undertaken in seas around Ireland. Data includes contractor, line, survey Id, company, survey area name, project code and prefix details. A 2D survey typically contains numerous lines acquired...
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Tectonic elements in the Bay of Biscay.
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Low water mass movement of ocean currents from the Irish Offshore Strategic Environmental Assessment (IOSEA 5) publication. Large masses of moving water are called currents. In the oceans there are major surface currents, subsurface currents, and tidal currents. This data is a...
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An ocean current is a continuous, directed movement of seawater generated by forces acting upon this mean flow, such as breaking waves, wind, the Coriolis effect, cabbeling, and temperature and salinity differences, while tides are caused by the gravitational pull of the Sun...
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EnvironmentWestern Irish Sea gyre data was provided by Petroleum Affairs Division. This data was created as part of the Irish Offshore Strategic Environmental Assessment (IOSEA). A gyre in oceanography is any large system of rotating ocean currents, particularly those involved with large...
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An ocean current is a continuous, directed movement of seawater generated by forces acting upon this mean flow, such as breaking waves, wind, the Coriolis effect, cabbeling, and temperature and salinity differences, while tides are caused by the gravitational pull of the Sun...
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EnergyLicensing rounds awarded by the Petroleum Affairs Division (PAD) in the Irish Atlantic Margin. The 2015 licensing round includes three regions. The Irish Atlantic Margin geographic coverage includes foreshore and offshore waters in what is known as the Currently Designated...
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In oceanography, a front is a boundary between two distinct water masses. The water masses are defined by moving in different directions, i.e. on one side of the front the water is generally moving in one way, and on the other side of the front, the water is moving in another....
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Data on the offshore volcanic geologic ridges near Ireland in the West European Basin. A ridge is a geological feature consisting of a chain of mountains or hills that form a continuous elevated crest for some distance. Ridges are usually termed hills or mountains as well,...
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Offshore volcanic geologic faults in the North Atlantic Ocean.
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Upper water mass movement of ocean currents from the Irish Offshore Strategic Environmental Assessment (IOSEA 5). Large masses of moving water are called currents. In the oceans there are major surface currents, subsurface currents, and tidal currents. This data represents an...
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Data on the offshore geologic igneous features in the North Atlantic Ocean near Ireland. Igneous rock (derived from the Latin word ignis meaning fire) is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rock is formed through the cooling...
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EnvironmentAn ocean current is a continuous, directed movement of seawater generated by forces acting upon this mean flow, such as breaking waves, wind, the Coriolis effect, cabbeling, and temperature and salinity differences, while tides are caused by the gravitational pull of the Sun...
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