Warm core and cold core rings are formed when meanders attached to these features become pinched off. Satellite fields are used by the OSCAR project in order to study these phenomena. The strength of the Kuroshio one ranges from 25 to 50 Sverdrups. Although it is not in the atmosphere, these phenomena form an Ekman spiral as a result of the Corioli
Warm core and cold core rings are formed when meanders attached to these features become pinched off. Satellite fields are used by the OSCAR project in order to study these phenomena. The strength of the Kuroshio one ranges from 25 to 50 Sverdrups. Although it is not in the atmosphere, these phenomena form an Ekman spiral as a result of the Coriolis effect, which causes them to be directed to either the right or the left of the wind. These features can be divided into surface circulation and thermohaline circulation types, and wind often causes them to rotate, creating gyres. For 10 points, name these continuous, directed flows of water.
Warm core and cold core rings are formed when meanders attached to these features become pinched off.
ocean currents