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Medicane Zorbas, September 2018

The evolution of Zorbas over the Ionian Sea, track uncertainty and heavy rainfall in Greece, based on ECMWF analyses.

  • 27–30 September 2018
  • Southern Ionian Sea, Peloponnese, Attica, Evia and the western Aegean
  • Historical analysis

Zorbas developed over the southern Ionian and showed tropical-like characteristics before affecting the Peloponnese and areas farther east. Its prediction carried substantial uncertainty in both track and intensity.

Analysis period26–30 September 2018
Main forecast challengeSmall changes in cyclone track
Combined hazardsWind, waves and heavy rainfall

Event timeline

  1. 27 Sep — The surface low organises over the southern Ionian Sea.
  2. 28–29 Sep — The circulation strengthens and affects southwestern Greece.
  3. 30 Sep — The system moves east, carrying rain and strong winds farther across Greece.

What happened in the atmosphere

Interaction between an upper low and the warm sea favoured a gradually more compact cyclonic structure. Surface-pressure observations and satellite imagery helped describe its actual intensity.

For small Mediterranean systems, a track shift of only a few tens of kilometres can substantially alter local gusts and rainfall. A probability distribution is therefore more useful than a single scenario.

What helps us interpret the event

  • Emphasise track uncertainty, not only the central forecast.
  • Combine satellite, surface pressure and marine wind observations.
  • The term medicane is not, by itself, a hazard category.

Historical analysis must not be used as guidance for a new event. During active severe weather, follow HNMS, Civil Protection, 112 and local authorities.

PRIMARY SOURCES

Evidence and open data

KEEP EXPLORING

Related pages

Zorbas developed over the southern Ionian and showed tropical-like characteristics before affecting the Peloponnese and areas farther east. Its prediction carried substantial uncertainty in both track and intensity. 27–30 September 2018. Interaction between an upper low and the warm sea favoured a gradually more compact cyclonic structure. Surface-pressure observations and satellite imagery helped describe its actual intensity. For small Mediterranean systems, a track shift of only a few tens of kilometres can substantially alter local gusts and rainfall. A probability distribution is therefore more useful than a single scenario.