RT Journal Article
T1 The state of climate in NW Iberia
A1 Barriopedro Cepero, David
A1 Álvarez, I.
A1 Gómez Gesteira, M.
A1 Gimeno, L.
A1 Taboada, J. J.
A1 Lorenzo, M. N.
A1 Castro, M. de
A1 Nieto, R.
A1 Crespo, A. J. C.
A1 Ramos, A. M.
A1 Iglesias, I.
A1 Gómez Gesteira, J. L.
A1 Santo, F. E.
A1 Trigo, I. F.
AB Since 1974, there has been a significant increasing trend in land and sea surface temperatures of 0.5 and 0.24 degrees C decade(-1), respectively, in the NW Iberian Peninsula. Over the same period, annual precipitation does not show any trend, although some tendencies have been detected at seasonal scales. A significant positive trend, on average of 2 cm decade(-1), was also observed in sea level rise from 1943 onwards. Ekman transport perpendicular to the coast (upwelling index) showed a decrease from 1975 to 2008 at both annual and seasonal scales. In addition, the flow of the Mino River (the main river in the area) has also decreased at a mean rate of 18 m(3) s(-1) decade(-1) since 1970. At a synoptic scale, winter cyclone frequency and winter and spring blocking activity have decreased since the 1950s, which may partially explain the winter precipitation decline and the winter and spring temperature increases. These changes in synoptic systems are also in agreement with reported trends in the dominant variability modes of atmospheric circulation affecting NW Iberia, particularly a pronounced positive trend in the North Atlantic Oscillation from the 1970s to the 1990s.
PB Inter-Research
SN 0936-577X
YR 2011
FD 2011
LK https://hdl.handle.net/20.500.14352/44107
UL https://hdl.handle.net/20.500.14352/44107
LA eng
NO This work is supported by the Ministerio de Ciencia e Innovación under the FEDER-funded project CTM2007-62546-C03-03/MAR and under the projects CGL 2009-09143 and INCITE09383278PR.
NO Ministerio de Ciencia e Innovacion (MICINN)
DS Docta Complutense
RD 10 abr 2025