"The European mountain cryosphere: a review of its current state, trends, and future challenges"
Martin Beniston et al , 2018
https://archive-ouverte.unige.ch/unige:103006/ATTACHMENT01Abstract:
"The mountain cryosphere of mainland Europe is
recognized to have important impacts on a range of environmental
processes. In this paper, we provide an overview on
the current knowledge on snow, glacier, and permafrost processes,
as well as their past, current, and future evolution.
We additionally provide an assessment of current cryosphere
research in Europe and point to the different domains requiring
further research. Emphasis is given to our understanding
of climate–cryosphere interactions, cryosphere controls
on physical and biological mountain systems, and related
impacts. By the end of the century, Europe’s mountain
cryosphere will have changed to an extent that will impact the
landscape, the hydrological regimes, the water resources, and
the infrastructure. The impacts will not remain confined to
the mountain area but also affect the downstream lowlands,
entailing a wide range of socioeconomical consequences. European
mountains will have a completely different visual appearance,
in which low- and mid-range-altitude glaciers will
have disappeared and even large valley glaciers will have experienced
significant retreat and mass loss. Due to increased
air temperatures and related shifts from solid to liquid precipitation,
seasonal snow lines will be found at much higher
altitudes, and the snow season will be much shorter than today.
These changes in snow and ice melt will cause a shift
in the timing of discharge maxima, as well as a transition of
runoff regimes from glacial to nival and from nival to pluvial.
This will entail significant impacts on the seasonality of
high-altitude water availability, with consequences for water
storage and management in reservoirs for drinking water,
irrigation, and hydropower production. Whereas an upward
shift of the tree line and expansion of vegetation can
be expected into current periglacial areas, the disappearance
of permafrost at lower altitudes and its warming at higher
elevations will likely result in mass movements and process
chains beyond historical experience. Future cryospheric research
has the responsibility not only to foster awareness of
these expected changes and to develop targeted strategies to
precisely quantify their magnitude and rate of occurrence but
also to help in the development of approaches to adapt to
these changes and to mitigate their consequences. Major joint
efforts are required in the domain of cryospheric monitoring,
which will require coordination in terms of data availability
and quality. In particular, we recognize the quantification
of high-altitude precipitation as a key source of uncertainty
in projections of future changes. Improvements in numerical
modeling and a better understanding of process chains affecting
high-altitude mass movements are the two further fields
that – in our view – future cryospheric research should focus
on."
extract from the conclusion:
"Within a few decades, these impacts will have a bearing on ecosystems and
the services provided by them and on a number of economic
sectors, including hydropower, agriculture, and tourism. The
management of natural hazards will equally be affected, and
a need for adaptation to climate change will arise.
"