6   Artículos

 
en línea
Nicolás Velásquez, Ricardo Mantilla, Witold Krajewski, Morgan Fonley and Felipe Quintero    
This study evaluates the potential for a newly proposed non-linear subsurface flux equation to improve the performance of the hydrological Hillslope Link Model (HLM). The equation contains parameters that are functionally related to the hillslope steepne... ver más
Revista: Hydrology    Formato: Electrónico

 
en línea
Navid Jadidoleslam, Ricardo Mantilla and Witold F. Krajewski    
The authors examine the impact of assimilating satellite-based soil moisture estimates on real-time streamflow predictions made by the distributed hydrologic model HLM. They use SMAP (Soil Moisture Active Passive) and SMOS (Soil Moisture Ocean Salinity) ... ver más
Revista: Hydrology    Formato: Electrónico

 
en línea
Pedro Campoy-López, Estefanía Pereira-Pinto, Leonardo Mantilla-Aldana and Ricardo Beiras    
The sea urchin (Paracentrotus lividus) was used to test the effects of one of the most abundant flame retardant additives for plastics, tris (1-chloro-2-propyl) phosphate (TCPP), and the synthetic hormone ethinylestradiol (EE2) on gametogenesis and gonad... ver más
Revista: Journal of Marine Science and Engineering    Formato: Electrónico

 
en línea
Morgan Fonley, Ricardo Mantilla and Rodica Curtu    
The concept of doing hydrology backwards, introduced in the literature in the last decade, relies on the possibility to invert the equations relating streamflow fluctuations at the catchment outlet to estimated hydrological forcings throughout the basin.... ver más
Revista: Hydrology    Formato: Electrónico

 
en línea
Felipe Quintero, Ricardo Mantilla, Christopher Anderson, David Claman and Witold Krajewski    
The authors explore the uncertainty implied in the estimation of changes in flood frequency due to climate change at the basins of the Cedar River and Skunk River in Iowa, United States. The study focuses on the influence of climate change on the 100-yea... ver más
Revista: Hydrology    Formato: Electrónico

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