Eddy saturation and eddy compensation are concepts primarily associated with the study of oceanic and atmospheric dynamics, particularly in the context of how large-scale flow patterns interact with smaller-scale eddies. ### Eddy Saturation **Eddy saturation** refers to a state in which the response of the oceanic or atmospheric circulation to changes in forcing (such as temperature, wind patterns, or other climatic influences) becomes limited by the presence of eddies.
An Ekman current meter is an instrument used to measure the velocity of ocean currents. It operates based on the principles of the Ekman layer, which is a thin layer of water in the ocean affected by wind and the Coriolis effect, leading to complex flow patterns. The Ekman current meter typically consists of a series of rotating blades or fins attached to a rotating shaft.
El Niño is a climate phenomenon characterized by the periodic warming of sea surface temperatures in the central and eastern tropical Pacific Ocean. This warming typically occurs every two to seven years and can last for several months to a couple of years. El Niño is one part of the larger El Niño-Southern Oscillation (ENSO) cycle, which includes its opposite phase, La Niña, where sea surface temperatures are cooler than average.
The El Niño–Southern Oscillation (ENSO) is a climate pattern that describes the periodic fluctuations in sea surface temperatures and atmospheric conditions in the central and eastern tropical Pacific Ocean. ENSO has three phases: 1. **El Niño**: This phase is characterized by warmer-than-average sea surface temperatures in the central and eastern Pacific. It tends to occur every 2 to 7 years and can last several months to a couple of years.
Eratosthenes Seamount is an underwater mountain located in the eastern Mediterranean Sea, off the coast of Cyprus. It is named after the ancient Greek mathematician and astronomer Eratosthenes, who is known for calculating the Earth's circumference. The seamount is part of the Eratosthenes Plateau, which is a large geological structure characterized by its complex geological history and unique bathymetry.
The European Conference on Underwater Acoustics (ECUA) is a significant scientific conference focused on the field of underwater acoustics and its various applications. It serves as a platform for researchers, engineers, and practitioners from around the world to discuss the latest developments, research findings, technologies, and methodologies related to underwater acoustics.
The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a scientific initiative designed to provide a long-term observatory for the study of the deep-sea environment and the water column. EMSO aims to gather and share high-quality, real-time data on various marine phenomena, including physical, chemical, and biological processes occurring in deeper ocean waters.
The Faroe-Bank Channel overflow refers to a significant oceanographic phenomenon occurring in the North Atlantic Ocean, specifically involving the movement of dense water from the Nordic Seas into the Atlantic. The Faroe-Bank Channel is a deep underwater trench located between the Faroe Islands and the Scottish coast.
A "flaw lead" typically refers to a potential sales opportunity or a prospect that has been identified as having issues or needs that your product or service could address. In a sales context, "lead" generally means a potential customer, while "flaw" might indicate specific problems, pain points, or deficiencies that the lead is experiencing. In essence, a flaw lead is a more targeted type of lead because it highlights a specific issue that your business can solve.
The term "Florida Platform" can refer to different concepts depending on the context. Here are a couple of possible interpretations: 1. **Political Context**: In U.S. politics, particularly in the context of the Democratic Party, the "Florida Platform" may refer to a set of policy positions or a political agenda that reflects the interests and needs of Florida citizens.
Fram Strait is a body of water located between Greenland to the west and the Svalbard archipelago to the east. It connects the Arctic Ocean to the Greenland Sea and serves as a critical passage for sea ice movement, ocean currents, and marine life in the region. The strait is named after the Norwegian polar ship Fram, which was used in polar exploration.
The "Friendly Floatees" spill refers to a maritime incident that occurred in 1992 when a shipping container filled with thousands of plastic bath toys, including rubber ducks, frogs, and turtles, fell overboard from a cargo ship in the Pacific Ocean. Specifically, this incident happened when the ship, the *Ever Laurel*, encountered rough seas in the north Pacific, causing the container to break loose and spill its contents into the ocean.
In oceanography, a "front" refers to a boundary or transition zone between two different water masses that have distinct physical properties, such as temperature, salinity, or density. These differences can lead to variations in water characteristics and can significantly influence marine ecosystems, weather patterns, and ocean circulation. There are several types of fronts in oceanography: 1. **Temperature Fronts**: These occur where there is a sharp change in water temperature, often associated with currents or upwelling zones.
The Gas Hydrate Stability Zone (GHSZ) is a region in the geological environment where gas hydrates can form and remain stable. Gas hydrates are crystalline structures made up of water and gas molecules, typically methane, that form under specific temperature and pressure conditions. The stability of gas hydrates is primarily influenced by three factors: 1. **Pressure**: Gas hydrates are stable at high pressures.
The Geochemical Ocean Sections Study (GEOSECS) is a significant scientific initiative aimed at understanding the chemical composition and properties of the ocean and how they relate to global biogeochemical cycles. Conducted from the mid-1970s to the early 1980s, GEOSECS focused on collecting and analyzing oceanographic data to investigate various aspects of the ocean's chemistry, including the distribution of nutrients, trace elements, and isotopes.
Geophysical fluid dynamics (GFD) is a branch of fluid dynamics that focuses on the behavior of fluids in the Earth's atmosphere and oceans, as well as in other planetary environments. It combines principles from fluid mechanics, geophysics, and applied mathematics to study the motion of large-scale fluid systems influenced by the Earth's rotation, gravity, and other geophysical forces.
Glacio-geological databases are specialized collections of geological and glaciological data that focus on the study of glaciers, ice sheets, and their interactions with the Earth's geology. These databases may include a wide range of information, such as: 1. **Geological Mapping**: Data on rock types, mineral compositions, and geological structures in regions affected by glacial processes.
The Global Ocean Data Analysis Project (GLODAP) is a collaborative scientific initiative aimed at collecting, processing, and distributing high-quality oceanographic data related to the carbon cycle and biogeochemistry of the world's oceans. The project focuses on the analysis and synthesis of data from various oceanographic research cruises, particularly those that measure essential variables such as nutrients, carbon dioxide, oxygen, and other tracers relevant to ocean health and climate change.
The Gulf Trough, also known as the Gulf of Mexico Trough or Gulf Trough system, is a geological feature in the Gulf of Mexico area. It represents a significant structural depression or an area of subsidence, primarily formed by tectonic processes, sediment deposition, and erosion over millions of years. The Gulf Trough is part of the larger Gulf of Mexico basin and plays a vital role in the region's geology, marine ecology, and hydrocarbon deposits.
A "Guyot" refers to a specific type of underwater geological feature that is characterized by a flat-topped mountain or hill, typically found on the ocean floor. These formations are submerged and often have steep sides, with their flat tops corresponding to sea level at some point in geological history. Guyots are formed from volcanic activity and represent the eroded remnants of once-active volcanoes that have subsided due to tectonic activity.