The strait has a width that varies from ∼40 to ∼100 km and as such the wind field is typically ageostrophic and controlled by the pressure gradient in the along-strait direction. Here we use weather station data from the region as well as two reanalyses and an operational analysis with nominal horizontal resolutions that vary from ∼30 to ∼2.5 km to characterize the wind field in the vicinity of the strait.
However, its remote location has limited our knowledge of the winds along the strait. The winds that blow along the strait play an important role in modulating ice and water exports from the Arctic Ocean as well as in helping to establish the Arctic's largest and most productive polynya that forms at its southern terminus. Through the process of chemosynthesis, bacteria provide energy and nutrients to vent species without the need for sunlight.Nares Strait is the long and narrow strait bounded by steep topography that connects the Arctic Ocean's Lincoln Sea to the North Atlantic's Baffin Bay. The conversion of mineral-rich hydrothermal fluid into energy is a key aspect of these unique ecosystems. The ability of vent organisms to survive and thrive in such extreme pressures and temperatures and in the presence of toxic mineral plumes is fascinating. The study of hydrothermal vent ecosystems continues to redefine our understanding of the requirements for life. They appear to shimmer because of differences in water temperatures or bubble because of the presence of gases, like carbon dioxide. Vents with even cooler, weaker flows are often called seeps. Compared to black smokers, white smokers usually emit cooler plumes and form smaller chimneys. The plumes of white smokers are lightly colored and rich in barium, calcium, and silicon. Black smokers emit the hottest, darkest plumes, which are high in sulfur content and form chimneys up to 18 stories tall, or 55 meters (180 feet). Hydrothermal vent structures are characterized by different physical and chemical factors, including the minerals, temperatures, and flow levels of their plumes. As the vent minerals cool and solidify into mineral deposits, they form different types of hydrothermal vent structures. The hot, mineral-rich waters then exit the oceanic crust and mix with the cool seawater above. As pressure builds and the seawater warms, it begins to dissolve minerals and rise toward the surface of the crust. Seawater circulates deep in the ocean’s crust and becomes superheated by hot magma. Along mid-ocean ridges where tectonic plates spread apart, magma rises and cools to form new crust and volcanic mountain chains. Hydrothermal vents are like geysers, or hot springs, on the ocean floor. Scientists later realized that bacteria were converting the toxic vent minerals into usable forms of energy through a process called chemosynthesis, providing food for other vent organisms. Despite the extreme temperatures and pressures, toxic minerals, and lack of sunlight that characterized the deep-sea vent ecosystem, the species living there were thriving.
They also realized that an entirely unique ecosystem, including hundreds of new species, existed around the vents. The scientists had made a fascinating discovery-deep-sea hydrothermal vents.
They wondered how deep-ocean temperatures could change so drastically-from near freezing to 400 ☌ (750 ☏)-in such a short distance.
SEA OF ROSES 1977 SERIES
In 1977, scientists exploring the Galápagos Rift along the mid-ocean ridge in the eastern Pacific noticed a series of temperature spikes in their data.
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