The NCAA Division I Men's Basketball Tournament Final Four appearances by coach is a list that highlights coaches who have led their teams to the Final Four, which is the semi-final round of the tournament. While I cannot provide a complete up-to-date list, I can mention some of the notable coaches with multiple Final Four appearances as of my last update in October 2023.

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.

Biogeography is the study of the geographic distribution of living organisms, both plants and animals, across different regions of the world and the factors that influence these distributions. It combines aspects of biology, ecology, geography, and geology to understand how species and ecosystems are distributed in space and time. Key aspects of biogeography include: 1. **Species Distribution**: Understanding where different species are found and the ecological and evolutionary reasons behind these patterns.

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.

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.

A marine heatwave is a prolonged period of unusually high sea surface temperatures in a specific region of the ocean. These temperature anomalies can significantly affect marine ecosystems, weather patterns, and human activities. Marine heatwaves can be caused by various factors, including: 1. **Climate Change**: Rising global temperatures contribute to higher sea surface temperatures, leading to more frequent and intense marine heatwaves. 2. **Ocean Currents**: Changes in ocean circulation patterns can lead to localized warming.

A mid-ocean ridge is an underwater mountain range that is a key feature of the Earth's ocean floors. It is formed by the process of seafloor spreading, where tectonic plates move apart and magma from the mantle rises to create new oceanic crust. This process occurs at divergent plate boundaries, where two tectonic plates are moving away from each other.

Hydrothermal circulation refers to the movement of water that is heated by geological processes within the Earth's crust, particularly in areas of volcanic activity or along mid-ocean ridges. This process plays a crucial role in the thermal and chemical dynamics of the Earth's crust and ocean floor. Here's how hydrothermal circulation typically works: 1. **Heat Source**: The circulation is usually driven by heat from magma or hot rocks below the Earth's surface. This heat causes water in the surrounding rock to become heated.

The Oxygen Minimum Zone (OMZ) refers to a region of the ocean that has significantly reduced concentrations of dissolved oxygen compared to surrounding areas. These zones are typically found in the deeper waters of the ocean, often between about 200 meters and 1,000 meters in depth, although the specific depth can vary depending on the location and oceanographic conditions.

The Interdecadal Pacific Oscillation (IPO) is a long-term climate variability pattern in the Pacific Ocean that can influence climatic conditions across the globe. It is characterized by fluctuations in sea surface temperatures (SST) and atmospheric pressure across the Pacific Ocean on interdecadal timescales, typically spanning several decades. The IPO can switch between phases, similar to the El Niño Southern Oscillation (ENSO), but with much longer cycles.

The Kaikō ROV (Remotely Operated Vehicle) is a specialized underwater robot used for deep-sea exploration and research. Developed by the Japan Agency for Marine-Earth Science and Technology (JAMSTEC), the Kaikō ROV is notable for its design and capabilities, enabling it to operate at extreme depths of up to several thousand meters in the ocean.

La Niña is a climatic phenomenon that is part of the El Niño-Southern Oscillation (ENSO) cycle. It is characterized by the cooling of sea surface temperatures in the central and eastern Pacific Ocean, particularly near the equator. This phenomenon typically occurs every few years and can last for several months to years.

Lagrangian Ocean Analysis is a method used in oceanography to study and understand ocean dynamics, currents, and the movement of particles or fluid parcels within the ocean. The term "Lagrangian" refers to a perspective in fluid dynamics that focuses on the motion of individual particles as they move through the fluid, rather than looking at fixed points in space (which is called a Eulerian perspective).

Longshore drift, also known as littoral drift, is a geological process that involves the movement of sediment along the coast by wave action. It occurs when waves approach the shore at an angle, carrying sand and pebbles up the beach. As the waves break and recede, gravity pulls the sediment back down the slope of the beach in a direct line, resulting in a zigzag pattern of movement along the coastline.

The lunitidal interval is the time difference between the local high tide and the local mean noon, which is calculated based on the lunar cycle. It represents the period it takes for the tide to peak after the moon is directly overhead or underfoot. This interval varies depending on the position of the moon, the geographical location, and local factors affecting tides, such as the shape of the coastline and the depth of the water.

Monterey Canyon is a prominent underwater canyon located off the coast of central California, near the city of Monterey. It is one of the largest marine canyons on the North American continental shelf and extends approximately 95 miles (153 kilometers) in length and up to 2.5 miles (4 kilometers) in depth. The canyon is part of the larger Monterey Bay National Marine Sanctuary.