Fig. 2: Analogues Analysis for the 1966 Acqua Alta event in Venice. | npj Climate and Atmospheric Science

Fig. 2: Analogues Analysis for the 1966 Acqua Alta event in Venice.

From: Attributing Venice Acqua Alta events to a changing climate and evaluating the efficacy of MoSE adaptation strategy

Fig. 2

6-hourly mean sea-level pressure, slp (a), 2-meter temperatures, t2m (e), total precipitation accumulated over 24 h, pr (i), maximum Scirocco wind component over 24 h, w (m), centered at the time of the event. Average of the 17 analogues found for the counterfactual [1950-1979] (b) and factual [1993-2022] (c) periods and corresponding 2-meter temperatures (f, g), total precipitation (j, k) and Scirocco wind speed (n, o). Δslp (d), Δt2m (h), Δpr (l) and Δw (p) between factual and counterfactual periods: coloured-filled areas refer to significant anomalies with respect to the bootstrap procedure (significance is defined as exceeding the 95th percentile in the bootstrap distribution).

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