http://www.cnr.it/ontology/cnr/individuo/prodotto/ID137679
Seasonal rainfall trends and teleconnections in Calabria (Contributo in volume (capitolo o saggio))
- Type
- Label
- Seasonal rainfall trends and teleconnections in Calabria (Contributo in volume (capitolo o saggio)) (literal)
- Anno
- 2010-01-01T00:00:00+01:00 (literal)
- Alternative label
Caloiero T.; Coscarelli R.; Ferrari E.; Mancini M. (2010)
Seasonal rainfall trends and teleconnections in Calabria
Nuova Bios, Cosenza (Italia) in Analyses and images of hydrological extremes in Mediterranean environments, 2010
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Caloiero T.; Coscarelli R.; Ferrari E.; Mancini M. (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#citta
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#titoloVolume
- Analyses and images of hydrological extremes in Mediterranean environments (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- CNR; Università della Calabria; Politecnico di Milano (literal)
- Titolo
- Seasonal rainfall trends and teleconnections in Calabria (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#inCollana
- Analyses and images of hydrological extremes in Mediterranean environments (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#isbn
- 978-88-97181-00-2 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#curatoriVolume
- Ferrari E.; Versace P. (literal)
- Abstract
- The following work presents a trend analysis of seasonal precipitation observed in a region of Southern Italy (Calabria) through the Mann-Kendall non-parametric test and a correlation analysis between rainfalls aggregated at different time scales and two global circulation indexes, the North Atlantic Oscillation Index (NAOI) and the Mediterranean Oscillation Index (MOI). The results show a general negative trend in precipitation, with the exception of summer season, and links of the NAOI with autumn and winter rainfalls, observed in the north-western part of Calabria, and of the MOI with winter precipitation, revealing a more uniform distribution throughout the region. (literal)
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