- Industry: Education
- Number of terms: 34386
- Number of blossaries: 0
- Company Profile:
Founded in 1876, Texas A&M University is a U.S. public and comprehensive university offering a wide variety of academic programs far beyond its original label of agricultural and mechanical trainings. It is one of the few institutions holding triple federal designations as a land-, sea- and ...
The hypothetical air temperature in calm conditions that would cause the same heat flux from the skin as occurs for the true winds and the true air temperature.
Industry:Earth science
The hypothetical tide which would exist if the ocean responded instantly to the tide producing forces and formed an equilibrium surface. The effects of friction, inertia, and the irregular distribution of land masses are ignored.
Industry:Earth science
The intensification of the western limb of an oceanic circulation gyre. This is inevitable given a rotating earth, a meridional boundary, and a zonal wind stress pattern that reverses direction at some latitude as was shown using a simple dynamical model in the classic paper of Stommel (1948). Common features of such currents include their flowing as swift narrow streams along the western continental rise of ocean basins, their extension to great depth well below the thermocline, and their separation from the coast at some point and continuation into the open ocean as narrow jets that develop instabilities along their paths. The most well-known western boundary currents are the Gulf Stream and the Kuroshio Current.
Industry:Earth science
The interface between seasonal sea ice and open water. This is not a clear–cut boundary but a complex belt with distinct characteristics. The MIZ may be up to 100–200 km wide, with the poleward parat comprising broken ice in the early stages of melting. The geographic location of the outer edge can vary over relatively short time scales due to compaction and release caused by variations in wind stress.
Industry:Earth science
The interface between the atmosphere and the ocean. This was proposed, along with the adjectival form navifacial, in Montgomery (1969).
Industry:Earth science
The interval between the transit of the moon over a meridian and the time of strength of ebb of the following tide.
Industry:Earth science
The large amplitude motion of the energy–containing eddies in the oceans and the atmosphere.
Industry:Earth science
The latitude of the mean annual position of the equatorial trough. This is located at about 5° N rather than on the geographical equator.
Industry:Earth science
The layer of water below the thermocline in a fresh water lake, as opposed to the epilimnion.
Industry:Earth science
The level in the ocean below which the solution rate of calcium carbonate exceeds its deposition rate. This is also called the carbonate compensation depth.
Industry:Earth science
