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• W2767396600 startingPage "1589" @default.
• W2767396600 abstract "Abstract Theoretical considerations suggest that saltation dynamics is dominated by either aerodynamic entrainment or by a combination of ejection and rebound at a given time and location. Calling these two regimes “weak” and “strong” saltation, respectively, we have investigated high‐resolution snow mass flux measurements by shadowgraphy in a cold wind tunnel to determine whether these two regimes can be experimentally reproduced. In this contribution, we first suggest that aerodynamic entrainment should lead to a negative correlation in the growth rates of horizontal versus vertical mass fluxes, while for the ejection regime, a positive correlation is plausible. Based on this criterion, we find evidence of weak and strong saltation in our data. Weak saltation is characterized by smaller peaks of horizontal mass flux; however, these peaks have a higher growth rate and therefore are typically narrow. The larger peaks are associated with strong saltation, are wider, and their frequency of occurrence increases with increasing overall saltation mass flux." @default.
• W2767396600 created "2017-11-17" @default.
• W2767396600 creator A5004133465 @default.
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• W2767396600 date "2017-09-01" @default.
• W2767396600 modified "2023-10-16" @default.
• W2767396600 title "Wind tunnel observations of weak and strong snow saltation dynamics" @default.
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• W2767396600 doi "https://doi.org/10.1002/2016jf004111" @default.
• W2767396600 hasPublicationYear "2017" @default.
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