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• W2100967560 abstract "Abstract Vast regions of the northern hemisphere are exposed to snowfall and seasonal frost. This has large effects on spatiotemporal distribution of infiltration and groundwater recharge processes as well as on the fate of pollutants. Therefore, snow and frost need to be central inherent elements of risk assessment and management schemes. However, snow and frost are often neglected or treated summarily or in a simplistic way by groundwater modellers. Snow deposition is uneven, and the snow is likely to sublimate, be redistributed and partly melt during the winter influencing the mass and spatial distribution of snow storage available for infiltration, the presence of ice layers within and under the snowpack and, therefore, also the spatial distribution of depths and permeability of the soil frost. In steep terrain, snowmelt may travel downhill tens of metres in hours along snow layers. The permeability of frozen soil is mainly influenced by soil type, its water and organic matter content, and the timing of the first snow in relation to the timing of sub‐zero temperatures. The aim with this paper is to review the literature on snow and frost processes, modelling approaches with the purpose to visualize and emphasize the need to include these processes when modelling, managing and predicting groundwater recharge for areas exposed to seasonal snow and frost. Copyright © 2015 John Wiley & Sons, Ltd." @default.
• W2100967560 created "2016-06-24" @default.
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• W2100967560 date "2015-11-21" @default.
• W2100967560 modified "2023-10-06" @default.
• W2100967560 title "Snow and frost: implications for spatiotemporal infiltration patterns - a review" @default.
• W2100967560 cites W1484724709 @default.
• W2100967560 cites W1486307680 @default.
• W2100967560 cites W1515459346 @default.
• W2100967560 cites W1537336040 @default.
• W2100967560 cites W1576810658 @default.
• W2100967560 cites W1579933083 @default.
• W2100967560 cites W1597050087 @default.
• W2100967560 cites W1630591977 @default.
• W2100967560 cites W1748672491 @default.
• W2100967560 cites W1764309586 @default.
• W2100967560 cites W1814839012 @default.
• W2100967560 cites W1953586934 @default.
• W2100967560 cites W1964888512 @default.
• W2100967560 cites W1967409546 @default.
• W2100967560 cites W1967709917 @default.
• W2100967560 cites W1968277074 @default.
• W2100967560 cites W1968294159 @default.
• W2100967560 cites W1969056482 @default.
• W2100967560 cites W1971036806 @default.
• W2100967560 cites W1971330928 @default.
• W2100967560 cites W1971367924 @default.
• W2100967560 cites W1972066109 @default.
• W2100967560 cites W1973962400 @default.
• W2100967560 cites W1977220632 @default.
• W2100967560 cites W1977952008 @default.
• W2100967560 cites W1980845324 @default.
• W2100967560 cites W1981595366 @default.
• W2100967560 cites W1983140832 @default.
• W2100967560 cites W1985553137 @default.
• W2100967560 cites W1986383808 @default.
• W2100967560 cites W1986804812 @default.
• W2100967560 cites W1987996171 @default.
• W2100967560 cites W1988944681 @default.
• W2100967560 cites W1989503949 @default.
• W2100967560 cites W1989810095 @default.
• W2100967560 cites W1990069749 @default.
• W2100967560 cites W1993388356 @default.
• W2100967560 cites W1993707994 @default.
• W2100967560 cites W1994937457 @default.
• W2100967560 cites W1996665266 @default.
• W2100967560 cites W1996924361 @default.
• W2100967560 cites W2002557602 @default.
• W2100967560 cites W2004492229 @default.
• W2100967560 cites W2004853040 @default.
• W2100967560 cites W2005534109 @default.
• W2100967560 cites W2006870385 @default.
• W2100967560 cites W2007620536 @default.
• W2100967560 cites W2010640501 @default.
• W2100967560 cites W2011718085 @default.
• W2100967560 cites W2011946406 @default.
• W2100967560 cites W2013319974 @default.
• W2100967560 cites W2013643853 @default.
• W2100967560 cites W2014227089 @default.
• W2100967560 cites W2015789373 @default.
• W2100967560 cites W2016917133 @default.
• W2100967560 cites W2017793249 @default.
• W2100967560 cites W2019053085 @default.
• W2100967560 cites W2020922488 @default.
• W2100967560 cites W2021394130 @default.
• W2100967560 cites W2021436787 @default.
• W2100967560 cites W2023225965 @default.
• W2100967560 cites W2023615150 @default.
• W2100967560 cites W2024212243 @default.
• W2100967560 cites W2024621358 @default.
• W2100967560 cites W2024960235 @default.
• W2100967560 cites W2026722268 @default.
• W2100967560 cites W2027717752 @default.
• W2100967560 cites W2028999185 @default.
• W2100967560 cites W2029297029 @default.
• W2100967560 cites W2032076634 @default.
• W2100967560 cites W2032718082 @default.
• W2100967560 cites W2033780566 @default.
• W2100967560 cites W2033918267 @default.
• W2100967560 cites W2036666629 @default.
• W2100967560 cites W2036773355 @default.
• W2100967560 cites W2036902133 @default.
• W2100967560 cites W2040919723 @default.
• W2100967560 cites W2042881507 @default.
• W2100967560 cites W2042950605 @default.
• W2100967560 cites W2043623819 @default.
• W2100967560 cites W2044765007 @default.
• W2100967560 cites W2045545316 @default.
• W2100967560 cites W2046209139 @default.
• W2100967560 cites W2047622094 @default.
• W2100967560 cites W2048224617 @default.
• W2100967560 cites W2050857380 @default.
• W2100967560 cites W2051575490 @default.

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