Most of the marine-weather courses I had followed focused on the movement of large weather systems: high- and low-pressure areas, fronts and troughs. These synoptic-scale features extend over hundreds or even thousands of kilometres and determine the general weather pattern. They are essential for understanding the Adriatic’s major winds, particularly the Bora, whose onset, direction and strongest zones can often be anticipated from the pressure pattern and local topography.
Yet, after arriving in the Adriatic, I soon discovered that not every dangerous weather event follows this relatively orderly pattern. The weather we actually experienced could differ sharply from the apparently moderate conditions shown on conventional wind and pressure maps. A Nevera may develop locally and intensify rapidly, producing violent gusts, abrupt wind shifts, lightning and torrential rain, even when the background wind forecast appears reassuring.