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Warm core ring information


A warm core ring is a type of mesoscale eddy which forms and breaks off from an ocean current, such as the Gulf Stream or the Kuroshio Current. The ring is an independent circulatory system of warm water that can persist for several months before losing its distinctive identity.[1] Warm core rings can be detected using infrared satellites or sea height anomalies resulting from and are easily identifiable against the surrounding colder waters. In addition, warm core rings are also distinguished by their low levels of biological activity. This type of system is thought to have helped develop several hurricanes, most notably Hurricane Katrina, into significantly stronger storms due to the abundance of warmer ocean water reaching down to a significant depth,[2] which in turn fuels and intensifies the hurricane. Warm core rings are also known for affecting wildlife, having the capacity to bring wildlife from typically warm waters to areas typically dominated by cold waters.

  1. ^ "Coastal Carolina University's article on ring formation". College of Natural and Applied Sciences. Retrieved 20 April 2011.
  2. ^ Kafatos, Menas; Donglian Sun; Ritesh Gautam; Zafer Boybeyi; Ruixin Yang; Guido Cervone1 (1 September 2006). "Role of anomalous warm gulf waters in the intensification of Hurricane Katrina" (PDF). Geophysical Research Letters. 33 (17). Bibcode:2006GeoRL..3317802K. doi:10.1029/2006GL026623. S2CID 54490765. Retrieved 27 April 2011.{{cite journal}}: CS1 maint: numeric names: authors list (link)

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Warm core ring

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A warm core ring is a type of mesoscale eddy which forms and breaks off from an ocean current, such as the Gulf Stream or the Kuroshio Current. The ring...

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Kuroshio Current

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that the water in the core of a ring has a different temperature regime than the shelf waters, there are times when a warm-core ring is undergoing its spring...

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Agulhas Current

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dissipate into the larger background currents. These anticyclonic warm core rings are estimated to have a transport of 3-9 Sv each, in total injecting...

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Ring shedding

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several months and occur in most ocean basins. The separated rings can have both warm or cold cores and play a role in the thermohaline circulation, interocean...

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Cold core ring

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in diameter with depths over 5 kilometers (3.1 mi). Cold core rings are the product of warm water currents wrapping around a colder water mass as it deviates...

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Loop Current

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Hurricane Opal most definitively illustrates the deepening abilities of a warm core ring. After crossing the Yucatán Peninsula, Opal reentered the Gulf of Mexico...

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Firefly squid

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Kouichi (June 13, 2006). "Diel vertical migration of squid in the warm core ring and cold water masses in the transition region of the western North...

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Gulf Stream

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cold-core rings, which rotate cyclonically (counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere), and warm-core rings, which...

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Medieval Warm Period

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930, during a time believed to be warm enough for sailing and farming. By retrieval and isotope analysis of marine cores and from examination of mollusc...

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Global temperature record

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time period from 12,000 years ago to the present. Tree rings and measurements from ice cores can give evidence about the global temperature from 1,000-2...

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Haida Eddies

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into the lower nutrient waters of the northeast Pacific Ocean. These "warm-core rings" transport heat out to sea, supplying nutrients (particularly nitrate...

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2005 Atlantic hurricane season

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of Hurricane Katrina. This protrusion detached into a warm core ring, or a small region of warm waters to an abnormally deep depth, and began to drift...

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Climate change

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and ice cores. Around 1850 thermometer records began to provide global coverage. Between the 18th century and 1970 there was little net warming, as the...

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Hurricane Opal

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(April 27, 1999). "The Interaction between Hurricane Opal (1995) and a Warm Core Ring in the Gulf of Mexico". Monthly Weather Review. 128 (5). Miami, Florida:...

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Greta Fryxell

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Atlantic Ocean, she examined diatoms in Gulf Stream warm core rings and how the warm core rings alter the distribution of diatoms. In Antarctica, she...

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Gonatus onyx

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Kawaguchi, Kouichi (2006-06-13). "Diel vertical migration of squid in the warm core ring and cold water masses in the transition region of the western North...

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Maureen Conte

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Hatcher (1991). The biogeochemistry of particulate lipids in warm-core Gulf Stream ring systems (Thesis). OCLC 82869924. "Conte CV" (PDF). Retrieved April...

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Hurricane Catarina

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Simmonds, I. (2010). "Interactions between Hurricane Catarina (2004) and warm core rings in the South Atlantic Ocean". Journal of Geophysical Research. 115...

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Walvis Ridge

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the Agulhas rings, mesoscale warm core rings that are shed from the Agulhas Current south of the Agulhas Bank. In average, five such rings are shed each...

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Rings of Saturn

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show that the F Ring consists of one core ring and a spiral strand around it. They also show that when Prometheus encounters the ring at its apoapsis...

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Tropical cyclone

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of this fuel available. A tropical cyclone is the generic term for a warm-cored, non-frontal synoptic-scale low-pressure system over tropical or subtropical...

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Outline of oceanography

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wind Warm core ring – A type of mesoscale eddy which breaks off from a warm ocean current. The ring is an independent circulatory system of warm water...

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Saturn

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25,000 km (16,000 mi). However, measurements of Saturn's rings suggest a much more diffuse core with a mass equal to about 17 Earths and a radius equal...

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North Atlantic Aerosols and Marine Ecosystems Study

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Kunze, E. (1986). The mean and near-inertial velocity fields in a warm-core ring. Journal of physical oceanography, 16(8), 1444-1461. Talley, L. D. (2011)...

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Roman Warm Period

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Consortium 2017. A high-resolution pollen analysis of a core from Galicia concluded in 2003 that the Roman Warm Period lasted from 250 BC to AD 450 in northwestern...

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Agulhas Bank

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contribute to the shedding of an Agulhas ring. Agulhas rings are large anticyclonic eddies or warm core rings of ocean water that are pinched off the Agulhas...

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Younger Dryas

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the Greenland Summit ice core chronology, the Younger Dryas corresponds to Greenland Stadial 1 (GS-1). The preceding Allerød warm period (interstadial) is...

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Mount Takahe

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height about 200,000 years ago. Several tephra layers encountered in ice cores at Mount Waesche and Byrd Station have been attributed to Mount Takahe,...

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