The influence of seasonally frozen ground (SFG) on water, energy, and solute fluxes is
important in cold climate regions. The hydrological role of permafrost is now being actively …

Flood is one of the most devastating natural hazards and is responsible for sizeable social-
economic losses and substantial fatalities. Flood events with diverse behavior …

Impacts of climatic variations and human activities on water discharge in the lower streams
of dammed rivers have been widely studied due to the rich water resources and hydropower …

The continuing warming of the climate system is reducing snow cover depth and duration
worldwide. Changes in snow cover can significantly affect the soil microclimate and the …

Studies have shown that the effects of freeze–thaw action on soil structure have become
more frequent and intense with the global warming, in turn, affects the dynamic processes of …

In mid-high latitude areas, seasonal freeze–thaw cycles generate significant effects on pore
structure of soils, and in turn, affect soil mechanical properties and soil erosion processes …

In midlatitude seasonally frozen areas, the freeze–thaw cycle affects the movement of soil
water, which increases the uncertainty in salt transport and aggravates the risk of soil …

Abstract Changes in soil pores and aggregate stability due to freeze-thaw cycles (FTCs) are
important causes of increased soil erosion during snowmelt. Soil erosion causes spatial …

In seasonal frozen soil areas, much meltwater is formed during the thawing period, which
easily causes snowmelt floods and waterlogging disasters. The meltwater simultaneously …

The movement of nitrate to surface water bodies during snow accumulation and melting has
been extensively studied, but there are only limited studies on the influence of snow …