Figure 4
From: Alarming coastal vulnerability of the deltaic and sandy beaches of North Africa
(A) Temporal evolution of the flooding events in the Medjerda River and (C) Nile catchments, for the last century; (B) Marine storms occurrence from 1980 to 2020 in the WBGT and (D) Nile Delta. Statistical data are collected in the stations of Tunis Carthage (Tunisia) and Cairo (Egypt). The significant wave height was established from the data of the historical records along the Tunisian46 and the Nile Delta Coasts56.
