4.5 Article

Geo-Hydrological Events and Temporal Trends in CAPE and TCWV over the Main Cities Facing the Mediterranean Sea in the Period 1979-2018

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ATMOSPHERE
卷 13, 期 1, 页码 -

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MDPI
DOI: 10.3390/atmos13010089

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flood; flash flood; Mediterranean Sea; CAPE; TCWV; geo-hydrological event; temporal trend; Hurst exponent

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The Mediterranean region is a meeting point between Europe, Africa, and the Middle East. It experiences high meteorological variability, resulting in frequent intensive precipitation events. This research analyzes precipitation-related events and their increasing trend in the Mediterranean region, linking it to two meteorological variables associated with high-intensity precipitation events.
The Mediterranean region is regarded as the meeting point between Europe, Africa and the Middle East. Due to favourable climatic conditions, many civilizations have flourished here. Approximately, about half a billion people live in the Mediterranean region, which provides a key passage for trading between Europe and Asia. Belonging to the middle latitude zone, this region experiences high meteorological variability that is mostly induced by contrasting hot and cold air masses that generally come from the west. Due to such phenomenon, this region is subject to frequent intensive precipitation events. Besides, in this complex physiographic and orographic region, human activities have contributed to enhance the geo-hydrologic risk. Further, in terms of climate change, the Mediterranean is a hot spot, probably exposing it to future damaging events. In this framework, this research focuses on the analysis of precipitation related events recorded in the EM-DAT disasters database for the period 1979-2018. An increasing trend emerges in both event records and related deaths. Then a possible linkage with two meteorological variables was investigated. Significant trends were studied for CAPE (Convective Available Potential Energy) and TCWV (Total Column Water Vapor) data, as monthly means in 100 km(2) cells for 18 major cities facing the Mediterranean Sea. The Mann-Kendall trend test, Sen's slope estimation and the Hurst exponent estimation for the investigation of persistency in time series were applied. The research provides new evidence and quantification for the increasing trend of climate related disasters at the Mediterranean scale: recorded events in 1999-2018 are about four times the ones in 1979-1998. Besides, it relates this rise with the trend of two meteorological variables associated with high intensity precipitation events, which shows a statistically significative increasing trend in many of the analysed cities facing the Mediterranean Sea.

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