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

696 shared publications

National School of Public Health, Carlos III Institute of Health, Avda. Monforte de Lemos, 5, 28029 Madrid, Spain

Antonio Ramos

270 shared publications

Centro de Ciências e Tecnologias Nucleares (C2TN), Instituto Superior Técnico, Universidade de Lisboa. Estrada Nacional 10 (km 139.7), 2695-066 Bobadela LRS, Portugal

Cecilia Brunetti

209 shared publications

Tree and Timber Institute, National Research Council of Italy (CNR-IVALSA), Via Madonna del Piano 10, 50019 Firenze, Italy

Pedro M. A. Miranda

209 shared publications

Instituto Dom Luiz, Faculdade de Ciências, University of Lisbon, 1749-016 Lisbon, Portugal

M.C. Freitas

197 shared publications

Instituto Dom Luiz, Faculdade de Ciências da Universidade de Lisboa, Campo Grande, 1749-016 Lisbon, Portugal

62
Publications
19
Reads
0
Downloads
522
Citations
Publication Record
Distribution of Articles published per year 
(1970 - 2017)
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 9 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 1 Read 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 3 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 3 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