In Chapter 5 of this book, it is shown that the formation of ice on the surface of a lake (‘ice-on’) and its thawing and ultimate disappearance (‘ice-off’) are complex phenomena governed by mechanisms that involve many interacting meteorological (and some non-meteorological) forcing factors. Linking ice phenology – the timing of ice-on and ice-off – to climatic forcing might therefore be expected to be a difficult task. This task, however, is simplified considerably by the fact that air temperature is the dominant variable driving ice phenology (Williams, 1971; Ruosteenoja, 1986; Vavrus et al., 1996; Williams and Stefan, 2006), and is also correlated to some extent with other relevant meteorological driving variables such as solar radiation, relative humidity and snowfall.
CITATION STYLE
Livingstone, D. M., Adrian, R., Blenckner, T., George, G., & Weyhenmeyer, G. A. (2010). Lake Ice Phenology. In The Impact of Climate Change on European Lakes (pp. 51–61). Springer Netherlands. https://doi.org/10.1007/978-90-481-2945-4_4
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