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Marco Maneta   Dr.  Institute, Department or Faculty Head 
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Marco Maneta published an article in March 2018.
Top co-authors See all
Santiago Beguería

73 shared publications

Estación Experimental de Aula Dei; Consejo Superior de Investigaciones Científicas (EEAD-CSIC); Zaragoza Spain

Diego G. Miralles

57 shared publications

Laboratory of Hydrology and Water Management—Ghent University; Coupure links 653, 9000 Gent, Belgium

Chris Soulsby

32 shared publications

Northern Rivers Institute; University of Aberdeen; Aberdeen AB24 3UF UK

Fernando Domínguez-Castro

24 shared publications

Instituto Pirenaico de Ecología, Spanish National Research Council (IPE-CSIC), Campus de Aula Dei, P.O. Box 13034, E-50059 Zaragoza, Spain

Wesley W. Wallender

24 shared publications

University of California

4
Publications
41
Reads
17
Downloads
12
Citations
Publication Record
Distribution of Articles published per year 
(2011 - 2018)
Total number of journals
published in
 
3
 
Publications
Article 3 Reads 4 Citations What can we learn from multi-data calibration of a process-based ecohydrological model? Sylvain Kuppel, Doerthe Tetzlaff, Marco P. Maneta, Chris Sou... Published: 01 March 2018
Environmental Modelling & Software, doi: 10.1016/j.envsoft.2018.01.001
DOI See at publisher website
CONFERENCE-ARTICLE 29 Reads 0 Citations <strong>A proposed robust approach for calculating the Standardized Evapotranspiration Deficit Index (SEDI) at the globa... Sergio Vicente-Serrano, Diego Miralles, Fernando Dominguez-C... Published: 05 November 2017
First International Electronic Conference on the Hydrological Cycle, doi: 10.3390/CHyCle-2017-04832
DOI See at publisher website ABS Show/hide abstract

Here we propose a new methodology for calculating the Standardized Evapotranspiration Deficit Index (SEDI) at the global scale using the difference between the actual evapotranspiration (ET) and the atmospheric evaporative demand (AED). ET was estimated by the Global Land Evaporation Amsterdam Model (GLEAM) v3a. The SEDI has been proposed recently to quantify drought severity based on the difference between actual evapotranspiration (ET) and the atmospheric evaporative demand (AED). Our findings demonstrate that, regardless of the AED dataset used for calculations, a log-logistic distribution is needed in order to fit the ED time series. As such, in many regions worldwide, the SEDI is insensitive to the AED method used for calculation. The SEDI showed significant correlations with the Standardized Precipitation Evapotranspiration Index (SPEI) across a wide range of regions, particularly for short SPEI time-scales. Overall, while this work provides a robust approach for calculating spatially and temporally comparable SEDI estimates, regardless of the climate region and land surface conditions, further studies remain needed to assess the performance and the applicability of the SEDI to quantify drought severity across varying crop and natural vegetation areas.

CONFERENCE-ARTICLE 9 Reads 0 Citations <strong>Complex spatial and temporal influences of climatic drought time-scales on hydrological droughts in natural basi... Sergio Vicente-Serrano, Marina Peña-Gallardo, Jamie Hannafor... Published: 05 November 2017
First International Electronic Conference on the Hydrological Cycle, doi: 10.3390/CHyCle-2017-04835
DOI See at publisher website ABS Show/hide abstract

We have analysed the response of hydrological droughts to climatic droughts in different natural basins of United States of America. For this purpose we selected 289 complete series from an initial data set of 702 gauging stations, covering the period between 1940 and 2013. Drainage basins were obtained for each gauging station using a digital terrain model, and climate series (precipitation and the atmospheric evaporative demand) were obtained for each drainage series. A number of topographic, edaphic and remote sensing variables were quantified for each basin. A hydrological drought index (The Standardized Stream Flow Index-SSI) was obtained for each basin and the Standardized Precipitation Evapotranspiration Index (SPEI) was used as a metric of climatic drought severity. Relationship between different SPEI time scales and the SSI was quantified using Pearson’s correlations and the general patterns of response of hydrological droughts to climatic droughts were identified using a principal component analysis. In general there is a response of SSI to short SPEI time-scales but strong seasonality in this response is also found. Coherent geographic patterns were obtained from the analysis and the factors that control the different responses were analysed by means of a predictive discriminant analysis. Independent analysis for three periods (1940-1964, 1965-1989 and 1989-2013) were also performed and showed not important changes in the response of the SSI to the SPEI in the past 65 years.

Article 0 Reads 8 Citations Economic impacts of regional water scarcity in the São Francisco River Basin, Brazil: an application of a linked hydro-e... Marcelo De O. Torres, Marco Maneta, Richard Howitt, Stephen ... Published: 08 November 2011
Environment and Development Economics, doi: 10.1017/s1355770x11000362
DOI See at publisher website
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