3 resultados para precipitation (climatology)
em Universidad de Alicante
Resumo:
As the water vapor content in the atmosphere scales with temperature, a warmer world is expected to feature an intensification of the hydrological cycle. Work to date has mainly focused on mean precipitation changes, whose connection to climatic modes is elusive at a global scale. Here we show that continental precipitation annual amplitude, which represents the annual range between minimum and maximum (monthly) rainfall, covaries with a linear combination of the Atlantic Multidecadal Oscillation and low-frequency variations in the El Niño–Southern Oscillation on a decadal to multidecadal scale with a correlation coefficient of 0.92 (P<0.01). The teleconnection is a result of changes in moisture transport in key regions. Reported trends in the annual amplitude of global precipitation in recent decades need to be assessed in light of this substantial low-frequency variability, which could mask or enhance an anthropogenic signal in hydrological cycle changes.
Resumo:
A synthetic procedure to prepare novel materials (surface-mediated fillings) based on robust hierarchical monoliths is reported. The methodology includes the deposition of a (micro- or mesoporous) silica thin film on the support followed by growth of a porous monolithic SiO2 structure. It has been demonstrated that this synthesis is viable for supports of different chemical nature with different inner diameters without shrinkage of the silica filling. The formation mechanism of the surface-mediated fillings is based on a solution/precipitation process and the anchoring of the silica filling to the deposited thin film. The interaction between the two SiO2 structures (monolith and thin film) depends on the porosity of the thin film and yields composite materials with different mechanical stability. By this procedure, capillary microreactors have been prepared and have been proved to be highly active and selective in the total and preferential oxidation of carbon monoxide (TOxCO and PrOxCO).
Resumo:
Se presenta el origen y la historia de la propuesta de un nuevo patrón de teleconexión, la Oscilación del Mediterráneo Occidental (WeMO), presentado por el autor en 2002 y aceptado internacionalmente en 2006. El índice de la WeMO, como diferencia de las presiones atmosféricas en superficie, previamente estandarizadas, de Cádiz-San Fernando y Padua, ofrece mejores correlaciones con la precipitación en la fachada oriental de la Península Ibérica que la NAO. En la actualidad medio centenar de artículos en revistas indexadas internacionalmente, de especialidades científicas diversas, no solo de Climatología, han hecho uso del nuevo patrón o lo han referenciado. Para la Península Ibérica, la WeMO es el patrón más explicativo de la precipitación torrencial desde el nordeste al sur.