Snow processes, such as refreezing of meltwater and cold content dynamics (i.e. warming and cooling of the snowpack), are poorly understood in the Himalaya. A new study, led by Emmy Stigter, presents new insights on which snow processes play a key role in the energy and mass balance of the seasonal snowpack at high altitude. Based on in-situ meteorological and snow observations at two high-altitude locations, we show that refreezing of meltwater and cold content dynamics have a considerable influence on the snowpack mass and energy balance.
In situ data-driven calculations showed that more than 30%
of seasonal snow meltwater refreezes. This estimate is supported by field
observations. Field observations of the snowpack revealed several ice layers
within the snowpack, which confirms the occurrence of meltwater refreezing
within the snowpack.
A continuous time series of the snowpack temperature revealed
that approximately 21% of the positive incoming energy is used to warm up the
snowpack. The warming stage before actual melt is an indicator that simplistic
snow melt models do not suffice as cold content dynamics are generally not
accounted for in these models.
Our study improves the understanding of snow processes that are relevant for more accurate modeling of the snowpack in this region. It also demonstrates that refreezing of meltwater and cold content dynamics should be included in future (hydrologic) modelling studies.
Stigter, E.E., Steiner, J.F., Koch, I., Saloranta, T.M., Kirkham, J.D., Immerzeel, W.W., 2021. Energy and mass balance dynamics of the seasonal snowpack at two high-altitude sites in the Himalaya. Cold Regions Science and Technology 183, 103233. https://doi.org/10.1016/j.coldregions.2021.103233
The post High-altitude snow dynamics appeared first on Mountain Hydrology.