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The spatial distributions of downscaled ensemble mean summer PRCPTOT, SDII, R10mm and P95 changes (relative to 1986-2005) in the future are shown in Fig. 7c, d) precipitation

The above mentioned regression model was used to auto- matically derive the minimum daily rainfall needed to reach the precipitation triggering threshold at S. This calculation

The generation mechanism of terminator times in subiono- spheric VLF/LF propagation has been studied for relatively short distances (less than 2000 km), and it is found that

(1998), FAST observations in the downward auroral current region: Energetic upgoing electron beams, parallel potential drops and ion heating, Geophys. (2002), Polar observations

Here we report measurements of the splitting of teleseismic shear phases in the vicinity of the Gala´pagos hotspot, and we examine the relative contribution of asthenospheric

To place more precise constraints on the deep feeding system of Stromboli volcano and to extend the experimen- tal coverage on a magma composition representative of

On a historical time scale, this paper investigates the effect of hydroclimatic variations on the surface water salinity of Lake Tanganyika, the largest African lake and an

unsegmented fault-related anticlines; h1: growing folds in foreland basins (Pakuashan anticline, Taiwan and Chandigarh anticline, NW India); h2: fault-related folds in