The June 2013 flood in the Canadian Rockies featured rain‐on‐snow (ROS) runoff
generation at alpine elevations that contributed to the high streamflows observed during the …

Shifts in winter temperature and precipitation patterns can profoundly affect snow
accumulation and melt regimes. These shifts have varying impacts on local to large-scale …

It is becoming increasingly popular to reintroduce beaver to streams with the hopes of
restoring riparian ecosystem function or reducing some of the hydrological impacts of …

The choice of proper input data and suitable calibration schemes is challenging in the
hydrological modeling of higher-latitude watersheds with their unique hydro-climatic …

Abstract From 19 to 22 June 2013, intense rainfall and concurrent snowmelt led to
devastating floods in the Canadian Rockies, foothills and downstream areas of southern …

A devastating flood struck Southern Alberta in late June 2013, with much of its streamflow
generation in the Front Ranges of the Rocky Mountains, west of Calgary. To better …

Using a sub-selection of regional climate models at 0.11°(≈≈ 12 km) grid resolution from
the EURO-CORDEX ensemble, we investigate how the spatial extent of areas associated …

The freezing level in the free troposphere often intercepts the terrain of the world's major
mountain ranges, creating a rain–snow limit. In this work, we use the free tropospheric …

Abstract The mountain headwater Bow River at Banff, Alberta, Canada, was subject to a
large flood in June 2013, over which considerable debate has ensued regarding its …

Abstract The Canadian Rockies are a triple-continental divide, whose high mountains are
drained by major snow-fed and rain-fed rivers flowing to the Pacific, Atlantic, and Arctic …