Landscape and climate change interactions are considerably interrelated in mountainous areas, where unsuitable or discontinuous surface meteorological variables constitute an impediment to the generation of homogeneous ecological and hydrological data and may hinder long-term environmental studies. To facilitate snow days’ reconstructions, we developed a non-linear multivariate regression model (NLMRM) estimating snow days per year (SDY) in a focus area, the northern Swiss Pre-Alpine Region (SPAR). The model was calibrated and assessed by using measured SDY data and other climatic variables in the period 1931-2006 were used to calibrate and asses the model, which is then used to estimate SDY (for a longer period earlier than 1931. The extended SDY series (1836-2017) showed a significant decrease of SDY passing shifting from about 36 days yr-1 in 1836-1943 to 29.9 days yr-1 in 1944-2017, on average. This indicates that, while warming is the major factor driving the snow cover SDY decrease recently observed in the study area, in a century-long perspective other processes related to local precipitation and large-scale climatic patterns emerge from our century-long perspective as important drivers of snow cover SDY variability in the Swiss pre-alpine region.
Reconstruction of snow days based on monthly climate indicators in the Swiss pre-alpine region
Simona Fratianni;
2020-01-01
Abstract
Landscape and climate change interactions are considerably interrelated in mountainous areas, where unsuitable or discontinuous surface meteorological variables constitute an impediment to the generation of homogeneous ecological and hydrological data and may hinder long-term environmental studies. To facilitate snow days’ reconstructions, we developed a non-linear multivariate regression model (NLMRM) estimating snow days per year (SDY) in a focus area, the northern Swiss Pre-Alpine Region (SPAR). The model was calibrated and assessed by using measured SDY data and other climatic variables in the period 1931-2006 were used to calibrate and asses the model, which is then used to estimate SDY (for a longer period earlier than 1931. The extended SDY series (1836-2017) showed a significant decrease of SDY passing shifting from about 36 days yr-1 in 1836-1943 to 29.9 days yr-1 in 1944-2017, on average. This indicates that, while warming is the major factor driving the snow cover SDY decrease recently observed in the study area, in a century-long perspective other processes related to local precipitation and large-scale climatic patterns emerge from our century-long perspective as important drivers of snow cover SDY variability in the Swiss pre-alpine region.File | Dimensione | Formato | |
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