TY - JOUR
AU - Schüepp, M.
AB - The paper discusses annual to decadal climate variability and change in the European Alps by utilizing the procedure of synoptic downscaling, i.e. it investigates the influence of global to continental scale synoptic structures and processes on the regional climate of the Alps. The European Alps lie to the southeast and under the right exit zone of the southwest-northeast oriented axis of the polar front jet over the North Atlantic ocean, in a transition zone between the Azores high and Icelandic low, between oceanic and continental and between Mediterranean and North Atlantic climates. Together with complex topographically induced phenomena like lee cyclogenesis, orographic precipitation, strong downslope winds and thermotopographical circulation systems, this transitional position makes climate studies in the Alps even more interesting. Only a minor correlation can be observed between global climate variability and Alpine climate. In contrast, the Alpine climate is strongly related to processes over the North Atlantic ocean and its sea ice system (e.g. it has a high correlation with the North Atlantic Oscillation and the dynamics and position of the Icelandic low), an area with a rather low climate prediction potential.
TI - Global climate change and variability and its influence on Alpine climate — concepts and observations
JF - Theoretical and Applied Climatology
DO - 10.1007/BF00865022
DA - 2004-12-06
UR - https://www.deepdyve.com/lp/springer-journals/global-climate-change-and-variability-and-its-influence-on-alpine-bh8F132FFO
SP - 221
EP - 243
VL - 58
IS - 4
DP - DeepDyve
ER -