Sentence examples for snow process from inspiring English sources

Specifically, when the peaks of the distributions of daily mean temperature projected by GCMs cross the key thresholds set in the model, the GCM uncertainty, even if tiny, can be amplified by the nonlinear propagation through the snow process model.

The impact of climate change on snow water equivalent (SWE) and its uncertainty were investigated in snowy areas of subarctic and temperate climate zones in Japan by using a snow process model and climate projections derived from general circulation models (GCMs).

Also evapotranspiration and snow processes play a critical role determining, for example, before-event soil saturation.

This amplification results in large uncertainty in projections of CC impact on snow processes.

Further advances in our understanding of the snow processes in Mediterranean snow-dominated basins will be achieved by finer and more accurate representation of the climate forcing.

The greatest among-model differences in energy and moisture fluxes in these high-latitude environments occur during the spring snowmelt period, reflecting different model parameterizations of snow processes.

Further comparison of simulated results through falsification of different snow processes reveals that estimating blowing snow transport processes and sublimation loss is vital for accurate snowmelt runoff calculations in this region.

A good knowledge of the snow processes in the Mediterranean mountains is therefore a key element of water management strategies in such regions.

This study aims to compare a range of SMs in their ability at simulating snow processes under current climate, and to evaluate how they affect the assessment of the climate change-induced snow impacts at the catchment scale.

Snow processes in mid- and north-latitude basins and their interaction with runoff generation at hyperresolution (<1 km and <hourly) pose challenges in current state-of-the-art distributed hydrological models.

The results of the study revealed that the model could be successfully applicable on the basin scale to simulate river discharge and snow processes and to investigate the effect of climate change on hydrological processes.