Seasonal snow cover is the largest single component of the cryosphere in areal extent,
covering an average of 46 million square km of Earth's surface (31% of the land area) each …

The temporal evolution of seasonal snow cover and its spatial variability in environments
such as mountains, prairies or polar regions is strongly influenced by the interactions …

" Across diverse disciplines, the term resilience is appearing more and more often. However,
while each discipline has developed theory and models to explain the resilience of the …

ERA5-Land (ERA5L) is a reanalysis product derived by running the land component of
ERA5 at increased resolution. This study evaluates its soil temperature in permafrost regions …

Cold regions involve hydrological processes that are not often addressed appropriately in
hydrological models. The Cold Regions Hydrological Modelling platform (CRHM) was …

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 …

This paper reviews measurement techniques and corresponding devices used to determine
the physical properties of the seasonal snowpack from distances close to the ground …

After a programme of integrated field and modelling research, hydrological processes of
considerable uncertainty such as snow redistribution by wind, snow interception …

This paper evaluates the use of field data on the spatial variability of snow water equivalent
(SWE) to guide the design of distributed snow models. An extensive reanalysis of results …

This second edition brings this definitive book completely up to date with the many advances
in our understanding of Arctic climate since the first edition was published in 2005. The book …