Original scientific paper UDC 551.465 Occurrence of the Istrian Coastal Countercurrent in 2000, a year with a mucilage event

late June–early July. Remarkably, previous investigations indicated that re-current occurrences of intense ICCC coincided with mucilage and/or anoxia events in the region. In fact, already during late winter, when a sea heat gain was relatively intense, a significant transversal transport of freshened waters of Po origin occurred. Lower salinity and warmer water pool, which might be the core of an anticyclonic gyre in the northeastern Adriatic, was present also during spring and summer. This indicates the establishment of a pronounced closed circulation system in the area