Please login first
Ricardo Trigo      
Timeline See timeline
Ricardo Trigo published an article in July 2017.
Top co-authors See all
Shilong Piao

157 shared publications

Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China

M. Vázquez

147 shared publications

Kantonsspital Aarau

Filippo Giorgi

145 shared publications

The Abdus Salam International Center for Theoretical Physics, Trieste, Italy

J Díaz

143 shared publications

Instituto de Física Corpuscular (IFIC), CSIC & Universitat de València, Calle Catedrático José Beltrán, 2, 46980 Paterna, Valencia, Spain

Michael E. Mann

130 shared publications

Department of Meteorology; Pennsylvania State University; University Park Pennsylvania USA

62
Publications
10
Reads
0
Downloads
795
Citations
Publication Record
Distribution of Articles published per year 
(1970 - 2017)
Total number of journals
published in
 
38
 
Publications See all
Article 2 Reads 1 Citation Saharan dust intrusions in Spain: Health impacts and associated synoptic conditions Julio Díaz, Cristina Linares, Rocío Carmona, Ana Russo, Cris... Published: 01 July 2017
Environmental Research, doi: 10.1016/j.envres.2017.03.047
DOI See at publisher website
PubMed View at PubMed
Article 0 Reads 6 Citations The deadliest storm of the 20th century striking Portugal: Flood impacts and atmospheric circulation Ricardo M. Trigo, Catarina Ramos, Susana S. Pereira, Alexand... Published: 01 October 2016
Journal of Hydrology, doi: 10.1016/j.jhydrol.2015.10.036
DOI See at publisher website
Article 0 Reads 7 Citations Land degradation assessment over Iberia during 1982-2012 C.M. Gouveia, P. Páscoa, Ana Russo, R.M. Trigo, Célia Gouvei... Published: 27 June 2016
Cuadernos de Investigación Geográfica, doi: 10.18172/cig.2945
DOI See at publisher website
Article 0 Reads 1 Citation A thermodynamically based model for actual evapotranspiration of an extensive grass field close to FAO reference, suitab... H.A.R. De Bruin, I.F. Trigo, F. C. Bosveld, J.F. Meirink Published: 01 May 2016
Journal of Hydrometeorology, doi: 10.1175/jhm-d-15-0006.1
DOI See at publisher website
Article 2 Reads 10 Citations Responses of European precipitation distributions and regimes to different blocking locations Pedro M. Sousa, Ricardo M. Trigo, David Barriopedro, Pedro M... Published: 25 April 2016
Climate Dynamics, doi: 10.1007/s00382-016-3132-5
DOI See at publisher website
Article 2 Reads 9 Citations Atmospheric rivers moisture sources from a Lagrangian perspective Alexandre M. Ramos, Raquel Nieto, Ricardo Tomé, Luis Gimeno,... Published: 22 April 2016
Earth System Dynamics, doi: 10.5194/esd-7-371-2016
DOI See at publisher website
ABS Show/hide abstract
An automated atmospheric river (AR) detection algorithm is used for the North Atlantic Ocean basin, allowing the identification of the major ARs affecting western European coasts between 1979 and 2012 over the winter half-year (October to March). The entire western coast of Europe was divided into five domains, namely the Iberian Peninsula (9.75°W, 36–43.75°N), France (4.5°W, 43.75–50°N), UK (4.5°W, 50–59°N), southern Scandinavia and the Netherlands (5.25°E, 50–59°N), and northern Scandinavia (5.25°E, 59–70°N). Following the identification of the main ARs that made landfall in western Europe, a Lagrangian analysis was then applied in order to identify the main areas where the moisture uptake was anomalous and contributed to the ARs reaching each domain. The Lagrangian data set used was obtained from the FLEXPART (FLEXible PARTicle dispersion) model global simulation from 1979 to 2012 and was forced by ERA-Interim reanalysis on a 1° latitude–longitude grid. The results show that, in general, for all regions considered, the major climatological areas for the anomalous moisture uptake extend along the subtropical North Atlantic, from the Florida Peninsula (northward of 20°N) to each sink region, with the nearest coast to each sink region always appearing as a local maximum. In addition, during AR events the Atlantic subtropical source is reinforced and displaced, with a slight northward movement of the sources found when the sink region is positioned at higher latitudes. In conclusion, the results confirm not only the anomalous advection of moisture linked to ARs from subtropical ocean areas but also the existence of a tropical source, together with midlatitude anomaly sources at some locations closer to AR landfalls.
Top