Zobrazeno 1 - 10
of 993
pro vyhledávání: '"R. MOTT"'
Publikováno v:
The Cryosphere, Vol 18, Pp 4315-4333 (2024)
Mountain snowpack forecasting relies on accurate mass and energy input information in relation to the snowpack. For this reason, coupled snow–atmosphere models, which downscale input fields to the snow model using atmospheric physics, have been dev
Externí odkaz:
https://doaj.org/article/5f12c0cc1d7f43b1966d2fe8120cad39
Publikováno v:
The Cryosphere, Vol 18, Pp 3533-3557 (2024)
Snow hydrological regimes in mountainous catchments are strongly influenced by snowpack heterogeneity resulting from wind- and gravity-induced redistribution processes, requiring them to be modelled at hectometre and finer resolutions. This study pre
Externí odkaz:
https://doaj.org/article/daa0a82a241e4c1fb40cce84d7c925f8
Publikováno v:
Geoscientific Model Development, Vol 16, Pp 5049-5068 (2023)
High-resolution (< 1 km) atmospheric modeling is increasingly used to study precipitation distributions in complex terrain and cryosphere–atmospheric processes. While this approach has yielded insightful results, studies over annual timescales or a
Externí odkaz:
https://doaj.org/article/bd25c6c9db7d44d9a44d9495cb34943f
Publikováno v:
The Cryosphere, Vol 14, Pp 4699-4718 (2020)
Multi-scale interactions between the glacier surface, the overlying atmosphere, and the surrounding alpine terrain are highly complex and force temporally and spatially variable local glacier energy fluxes and melt rates. A comprehensive measurement
Externí odkaz:
https://doaj.org/article/c17bf0467e6143faaef659f786a748fb
Publikováno v:
The Cryosphere, Vol 13, Pp 1247-1265 (2019)
The mass balance of very small glaciers is often governed by anomalous snow accumulation, winter precipitation being multiplied by snow redistribution processes (gravitationally or wind driven), or suppressed snow ablation driven by micrometeorologic
Externí odkaz:
https://doaj.org/article/1f05802554824768811808e554494730
Autor:
F. Gerber, N. Besic, V. Sharma, R. Mott, M. Daniels, M. Gabella, A. Berne, U. Germann, M. Lehning
Publikováno v:
The Cryosphere, Vol 12, Pp 3137-3160 (2018)
Snow distribution in complex alpine terrain and its evolution in the future climate is important in a variety of applications including hydropower, avalanche forecasting and freshwater resources. However, it is still challenging to quantitatively
Externí odkaz:
https://doaj.org/article/c62693c36f624f6ea243f8c1b1e161ef
Publikováno v:
The Cryosphere, Vol 10, Iss 1, Pp 445-458 (2016)
The longevity of perennial snowfields is not fully understood, but it is known that strong atmospheric stability and thus boundary-layer decoupling limit the amount of (sensible and latent) heat that can be transmitted from the atmosphere to the snow
Externí odkaz:
https://doaj.org/article/3b70857cdfe24d859764f60310552651
Publikováno v:
The Cryosphere, Vol 5, Iss 4, Pp 1083-1098 (2011)
Mountain snow covers typically become patchy over the course of a melting season. The snow pattern during melt is mainly governed by the end of winter snow depth distribution and the local energy balance. The objective of this study is to investigate
Externí odkaz:
https://doaj.org/article/8533889a458147e7ac3eab3fc52d2a00
Publikováno v:
The Cryosphere, Vol 4, Iss 4, Pp 545-559 (2010)
Mountain snow-cover is normally heterogeneously distributed due to wind and precipitation interacting with the snow cover on various scales. The aim of this study was to investigate snow deposition and wind-induced snow-transport processes on differe
Externí odkaz:
https://doaj.org/article/3897dcb7aecf42b2bab8fcfeac8e5c6c
Publikováno v:
The Cryosphere, Vol 4, Iss 2, Pp 215-225 (2010)
The spatio-temporal variability of the mountain snow cover determines the avalanche danger, snow water storage, permafrost distribution and the local distribution of fauna and flora. Using a new type of terrestrial laser scanner, which is particularl
Externí odkaz:
https://doaj.org/article/7c5b29428b5f419bb646318b1d1fb832