Description
Meteorological background
On 3 November, air pressure over the Adriatic began to drop as the influence of an anticyclone from northeastern Europe weakened, due to an approaching surface cyclone from the western Mediterranean. This cyclone was linked to an upper-level trough with a closed low positioned slightly to the west. By 4 November, the cyclone affected the Adriatic, with its center moving over the northern Adriatic, causing a pressure drop to 995 hPa before continuing northeast. Meanwhile, the anticyclone to the east created a pronounced pressure gradient over the Adriatic. This set the stage for SE winds on 3 November, which gradually intensified. By the morning of 4 November, the winds reached strong to gale-force levels, shifting to SW in the afternoon as the cyclone moved northeast.
Sea-level evolution
On 4 November 1966, at 12:00 UTC, the sea level in Bakar reached 94 cm above the long-term average, followed by a second peak of 92 cm at 20:00 UTC. The first peak occurred after the daily tidal maximum, with synoptic component still building up, and tide contributing 9 cm. In contrast, the evening peak coincided with synoptic component’s maximum, while the tide, in a negative phase, contributed -19 cm. Synoptic component was an isolated storm-surge event with no pre-existing seiches. Storm surge was driven by a strong, sustained Sirocco wind blowing along the Adriatic for over a day, accumulating water into the basin’s closed end. It contributed 48 cm to the first peak and 63 cm to the second.
The remaining sea-level rise resulted from processes acting on other time scales (refer to Figure 1 in the Introduction for detailed explanations). Local processes contributed 3 cm to the first peak and 15 cm to the second, long-period sea-level variability added 14 cm, and mean sea-level changes accounted for 20 cm.
The first peak was the result of a combination of all contributing processes, while the second peak was primarily driven by a significant synoptic component, along with positive contributions from all other processes except the tide.
Useful links:
La cronaca dell’ Aqua “granda”
Le acque alte eccezionali