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Please use this identifier to cite or link to this item:
http://hdl.handle.net/10174/8371
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Title: | Western Mediterranean precipitation over the last 300 years from instrumental observations |
Authors: | Camuffo, D. Bertolin, C. Diodato, N. Cocheo, C. Barriendos, M. Dominguez-Castro, F. Garnier, E. Alcoforado, M.J. Nunes, M.F. |
Editors: | Oppenheinmer, Michael Yohe, Gary |
Keywords: | climate change history of climate historical instrumental observations history of science |
Issue Date: | 21-Mar-2013 |
Publisher: | Michael Oppenheimer / Gary Yohe; Springer |
Citation: | Camuffo,D & Bertoni,C. & Diodato,N. & Cocheo, C.& Barriendos, M. & Dominguez-Castro, F. & Garnier,E. &, Alcoforado, M.J. & Nunes, M.F., Western Mediterranean precipitation over the last
300 years from instrumental observations, Climatic Change (2013) 117:85–101. |
Abstract: | The paper reports the results of the analysis of the 14 longest precipitation
instrumental series, covering the last 300 years, that have been recovered in six subareas
of the Western Mediterranean basin, i.e., Portugal, Northern and Southern Spain, Southern
France, Northern and Southern Italy. This study extends back by one century our knowledge
about the instrumental precipitation over theWestern Mediterranean, and by two centuries in
some specific subareas. All the time series show repeated swings. No specific trends have been found over the whole period, except in a few cases, but with modest time changes and
sometimes having opposite tendency. The same can be said for the most recent decades
although with some more marked departures from the average. The correlation between the
various Mediterranean subareas is generally not significant, or almost uncorrelated. The
Wavelet Spectral Analysis applied to the precipitation identifies only a minor 56-year cycle
in autumn, i.e., the same return period that has been found in literature for the Sea Surface
Temperature over North Atlantic. A comparison with a gridded dataset reconstruction based on
mixed multiproxy and instrumental observations, shows that the grid reconstruction is in good
agreement with the observed data for the period after 1900, less for the previous period. |
URI: | http://hdl.handle.net/10174/8371 |
ISSN: | 0165-0009 |
Type: | article |
Appears in Collections: | CEHFC - Publicações - Artigos em Revistas Internacionais Com Arbitragem Científica
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