Snowpack runoff formation processes during rain-on-snow events

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The high-impact nature and increasing occurrence of severe weather phenomena pushes forward research on their occurrence and improving our understanding thereof. Supercell thunderstorms are the focus of much severe convective research, as they represent on ...

Near-surface mercury and ozone depletion events occur in the lowest part of the atmosphere during Arctic spring. Mercury depletion is the first step in a process that transforms long-lived elemental mercury to more reactive forms within the Arctic that are ...

Headwater streams often experience intermittent flow. Consequently, the flowing drainage network expands and contracts and the flowing drainage density (DD) varies over time. Monitoring the DD dynamics is essential to understand the processes controlling i ...

The influence of drifting and blowing snow on surface mass and energy exchange is difficult to quantify due to limitations in both measurements and models, but is still potentially very important over large areas with seasonal or perennial snow cover. We p ...

Intense snowfall sublimation was observed during a precipitation event over Davis in the Vestfold Hills, East Antarctica, from 08 to 10 January 2019. Radar observations and simulations from the Weather Research and Forecasting model revealed that orographi ...

Snowpack runoff formation processes during rain-on-snow events

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Supercell Thunderstorms in the Alpine Region - From Weather Radar Observations to Idealized Modeling

Modelling the coupled mercury-halogen-ozone cycle in the central Arctic during spring

Short-term dynamics of drainage density based on a combination of channel flow state surveys and water level measurements

Evidence of Strong Flux Underestimation by Bulk Parametrizations During Drifting and Blowing Snow

Orographic Flow Influence on Precipitation During an Atmospheric River Event at Davis, Antarctica