Inland water bodies in Chile can locally increase rainfall intensity

► We evaluated possible effects of water bodies on rainfall intensity. ► We considered different climates for our study. ► We considered return periods of 5 and 100years. ► We compared locations near and away from water reservoirs. ► Our results indicate strong influences of water bodies on dryer cl...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Journal of hydrology (Amsterdam) 2013-02, Vol.481, p.56-63
Hauptverfasser: Pizarro, Roberto, Garcia-Chevesich, Pablo, Valdes, Rodrigo, Dominguez, Francina, Hossain, Faisal, Ffolliott, Peter, Olivares, Claudio, Morales, Carolina, Balocchi, Francisco, Bro, Per
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:► We evaluated possible effects of water bodies on rainfall intensity. ► We considered different climates for our study. ► We considered return periods of 5 and 100years. ► We compared locations near and away from water reservoirs. ► Our results indicate strong influences of water bodies on dryer climates. Analysis of precipitation observations from Chile indicated that man-made water reservoirs might be affecting the intensity of extreme precipitation events. Fifty rain gauges were used to evaluate rainfall intensities under different climates, using the Gumbel method (T=5 and 100years) and average maximum recorded rainfall intensities to construct IDF curves for each station. A spatial analysis of the stations was undertaken to establish graphical relationships on documented maximum annual rainfall intensities for 1h and those obtained by the Gumbel method as a function of latitude, longitude, elevation, and the distance from water bodies. The Mann–Whitney U test was applied with an error of 5%. Values obtained from stations located close to water bodies were compared to those located away from them. The results show significant changes in dryer climates.
ISSN:0022-1694
1879-2707
DOI:10.1016/j.jhydrol.2012.12.012