Snow distribution in complex alpine terrain and its evolution in the future climate is important
in a variety of applications including hydropower, avalanche forecasting and freshwater …

Abstract Study region Central Europe Study focus Precipitation fields from reanalyses have
been widely used for hydrological applications, meteorological extreme analyses or …

Estimates of snowfall rate as derived from radar reflectivities alone are non-unique. Different
combinations of snowflake microphysical properties and particle fall speeds can conspire to …

The snow water equivalent (SWE) is a key component for understanding changes in the
cryosphere in high mountain regions. Yet, a reliable quantification at a high spatiotemporal …

An operational method for daily precipitation observation correction of aerodynamic, wetting
and evaporation errors is presented. The aerodynamic correction method used has been …

Snow and precipitation estimates in high-mountain regions typically suffer from low temporal
and spatial resolution and large uncertainties. Here, we present a two-step statistically …

A new and general approach is proposed for interpolating 6-h precipitation series over large
spatial areas. The outputs are useful for distributed hydrological modelling and studies of …

Mountain snowpack and its distribution both have intimate connections to regional
hydrology by preserving winter precipitation to sustain streamflows during the summer …

This study presents a dynamic forecast combination approach adapted to incorporate
multiple sources of precipitation. Dynamic combination serves to utilise the varying merit …

Improving estimation of snow water equivalent rate (SWER) from radar reflectivity (Ze),
known as a SWER (Ze) relationship, is a priority for NASA's Global Precipitation …