Terrestrial hydrology is central to the Arctic system and its freshwater circulation. Water
transport and water constituents vary, however, across a very diverse geography. In this …

A Lagrangian snow‐evolution model (SnowModel‐LG) was used to produce daily, pan‐
Arctic, snow‐on‐sea‐ice, snow property distributions on a 25× 25‐km grid, from 1 August …

Tundra dominates two‐thirds of the unglaciated, terrestrial Arctic. Although this region has
experienced rapid and widespread changes in vegetation phenology and productivity over …

The characteristics of an aboveground cosmic‐ray neutron sensor (CRNS) are evaluated for
monitoring a mountain snowpack in the Austrian Alps from March 2014 to June 2016 …

Northern European countries such as Finland are highly sensitive to variability and changes
in snowfall and snow cover. Intense snowfall may cause severe problems for traffic and …

Snow water equivalent (SWE) measurements of seasonal snowpack are crucial in many
research fields. Yet accurate measurements at a high temporal resolution are difficult to …

Snow depth is one of the key physical parameters for understanding land surface energy
balance, soil thermal regime, water cycle, and assessing water resources from local …

For wildlife inhabiting snowy environments, snow properties such as onset date, depth,
strength, and distribution can influence many aspects of ecology, including movement …

Snowpack distribution in Arctic and alpine landscapes often occurs in repeating, year‐to‐
year patterns due to local topographic, weather, and vegetation characteristics. Previous …

Arctic coastal watersheds, though rarely monitored, are expected to have increased runoff,
as climate models predict more precipitation in the Arctic. This study provides a synthesis of …