Cyclones and earthquakes
By Riwan KERGUILLEC et Dominique SELLIER
L’Atlas Bleu / Exploring
cyclone, earthquake, oceanic fronts, vulnerability
The article highlights the physical characteristics and formation mechanisms of tropical cyclones and earthquakes on a global scale. Two maps provide visualization of the concentration zones for each of these phenomena and demonstrate the very high level of exposure of the planet’s oceanic fronts.
Tropical cyclones are large-scale seasonal weather phenomena (gusts of up to 118 km/h) that count as one of the hazards specific to coastal fronts due to the factors that dictate their behaviour and movement. They are formed at latitudes of between 8° and 30° in one of the six main tropical cyclone basins, above warm oceans (>26°C), therefore, mainly in summer and autumn. They then travel towards coastal areas due to the deflection caused by the Coriolis effect. Given that cyclones are located where the continent meets the ocean and lose power as they move over land due to reduced evaporation, oceanic coastal fronts and islands are seasonally exposed to their direct (high winds, heavy rain, flooding, storm surges) or indirect (landslides) effects.
Earthquakes are caused by a strain between two lithospheric plates and are accompanied by a sudden release of energy deep below and at the earth’s surface. Oceanic crust formation at oceanic ridges and its destruction at oceanic trenches are two major global tectonic phenomena that involve extreme mechanical stress, thus leading to high seismic activity. A survey of earthquakes over the last 20 years in countries with oceanic coastal fronts has clearly shown that there are zones of high seismic activity at active plate margins (the Ring of Fire in the Pacific). Earthquakes are therefore one of the most frequent and destructive risks faced by these coastal fronts.
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