Analysis of drought conditions and their effects on Lake Trasimeno (Central Italy) levels

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dc.contributor.author Valigi, Daniela
dc.contributor.author Luque Espinar, Juan Antonio
dc.contributor.author Di Matteo, Lucio
dc.contributor.author Cambi, Constanza
dc.contributor.author Pardo Iguzquiza, Eulogio
dc.contributor.author Rossi, Mauro
dc.date.accessioned 2020-09-21T09:47:11Z
dc.date.available 2020-09-21T09:47:11Z
dc.date.issued 2016-08-16
dc.identifier.citation Acque Sotterranee - Italian Journal of Groundwater, 2016, 17-215, 39-47 es_ES
dc.identifier.issn 2280-6458.
dc.identifier.uri http://hdl.handle.net/20.500.12468/361
dc.description.abstract An analysis of drought conditions on the Lake Trasimeno area (Umbria, Central Italy) and of their influence on the lake levels is presented. Lake Trasimeno is one of the largest Italian lakes, and its economic and environmental importance is very high. The analysis of temperature data (1963-2014) shows that annual temperature is increasing – in accordance with what is known for Central Italy and the Mediterranean area – with a significant gradient of about 0.023°C/ year. No significant annual and seasonal rainfall trends were observed over the Lake Trasimeno catchment. The power spectrum analysis of rainfall and lake level fluctuations shows that both periodograms have high statistical confidence levels (>99%) for annual and semi-annual cycles. The annual cycles of the periodogram of lake level fluctuations show a higher statistical confidence level than semi-annual cycles. Some other cycles such as the El-Niño Southern oscillation, North Atlantic oscillation, and solar activity are highlighted, with significance levels lower than that of annual and semi-annual cycles. The standardized precipitation (SPI) and standardized reconnaissance drought indices, at different time scales, show that frequency and duration of extreme and severe droughts have increased in the last 25 years. A significant relationship between 12-month SPI and 12-month standardized lake levels fluctuations was obtained for the 1989-2014 period, indicating that SPI12 can be a useful indicator to represent drought severity for systems such as the Lake Trasimeno by considering lake level fluctuations rather than lake levels. es_ES
dc.description.sponsorship Dipartimento di Fisica e Geologia, Università degli Studi di Perugia, Italia es_ES
dc.description.sponsorship Unidad de Granada, Instituto Geológico y Minero de España, España es_ES
dc.description.sponsorship Istituto di Ricerca per la Protezione Idrogeologica, Consiglio Nazionale delle Ricerche, Italia es_ES
dc.language.iso en es_ES
dc.publisher Associazione Acque Sotterranee es_ES
dc.rights Acceso abierto es_ES
dc.subject Lake Trasimeno es_ES
dc.subject lake levels es_ES
dc.subject climate indices es_ES
dc.subject drought es_ES
dc.subject power spectral analysis es_ES
dc.title Analysis of drought conditions and their effects on Lake Trasimeno (Central Italy) levels es_ES
dc.type Postprint es_ES
dc.relation.publisherversion https://www.acquesotterranee.net/index.php/acque/article/view/215 es_ES
dc.identifier.doi https://doi.org/10.7343/as-2016-215 es_ES
dc.coverage.spatialStudy Lago Trasimeno, Umbria, Italia es_ES


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