Causation and effect
It is caused by canalisation of the air-current along the northern edge of the Alps, during high-pressure conditions in northern or eastern Europe respectively. Towards western Swiss Plateau, the Bise is pressed between the Jura mountains and Pre-Alps whereby it strengthens and mostly climaxes on the western shore of Lake Geneva. In summer, the Bise wind causes rather dry and sunny weather whereas in winter, it frequently forms low stratus clouds over the Swiss Plateau by strengthening the inversion layer.
The strength of the Bise wind can be determined by the analysis of the air pressure difference (in hectopascal [hPa]) between Geneva and Güttingen in canton of Thurgau. The Bise arises as soon as the air pressure in Güttingen (TG) is higher than in Geneva. The greater this air pressure difference, the stronger the Bise blows through the Swiss Plateau. In case of an inverted air pressure difference (low air pressure in Güttingen (TG) and high air pressure in Geneva), the opposite of Bise occurs: The wind blows from southwest through the Swiss Plateau.
Use and Etymology
- "Bisendiagramm". Appenzell, Switzerland: MeteoGroup Schweiz AG. Retrieved 2018-02-25.
- "La bise va se calmer après une journée chaotique, mais plusieurs écoles vont rester fermées" (in French). Geneva: RTS Radio Télévision Suisse. 17 January 2017. Retrieved 2018-02-25.
- Fredrika Bremer, Two Years in Switzerland and Italy, Hurst and Blackett 1861, p.258
- The Century: A Popular Quarterly by Making of America Project, The Century Co. 1909, p.463
- Mary Shelley, The Last Man, vol. 3 ch. 8.
- W. R. Trumble; A. Stevenson, eds.,Shorter Oxford Dictionary, Oxford University Press 2002
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