Ice cover persistence in the lower reaches of the Nemunas River has decreased during the last 150 yr. The variation in the river freeze- and break-up dates is related to climatic variables. The significance of the negative break-up trend exceeds that of the positive freeze-up trend. Low-frequency large-scale atmospheric circulation patterns such as the North Atlantic Oscillation and Arctic Oscillation (NAO/AO) appear to have more influence on the break-up date than on the freeze-up date. Different classification methods applied to the atmospheric patterns prevailing in the early freeze-up events reveal similar results; however, differences arising between classifications are attributable to non-persistent and high frequency patterns. © Inter-Research 2008.
CITATION STYLE
Stonevicius, E., Stankunavicius, G., & Kilkus, K. (2008). Ice regime dynamics in the Nemunas River, Lithuania. Climate Research, 36(1), 17–28. https://doi.org/10.3354/cr00707
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