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dc.contributor.authorKrogh, Sebastian A.
dc.contributor.authorBroxton, Patrick D.
dc.contributor.authorManley, Patricia N.
dc.contributor.authorHarpold, Adrian A.
dc.date.accessioned2020-06-11T19:50:35Z
dc.date.available2020-06-11T19:50:35Z
dc.date.issued2020-03-20
dc.identifier.citationKrogh SA, Broxton PD, Manley PN and Harpold AA (2020) Using Process Based Snow Modeling and Lidar to Predict the Effects of Forest Thinning on the Northern Sierra Nevada Snowpack. Front. For. Glob. Change 3:21. doi: 10.3389/ffgc.2020.00021en_US
dc.identifier.issn2624-893X
dc.identifier.doi10.3389/ffgc.2020.00021
dc.identifier.urihttp://hdl.handle.net/10150/641563
dc.description.abstractReductions in snow accumulation and melt in headwater basins are increasing the water stress on forest ecosystems across the western US. Forest thinning has the potential to reduce water stress by decreasing sublimation losses from canopy interception; however, it can also increase snowpack exposure to sun and wind. We used the high-resolution (1 m) energy and mass balance Snow Physics and Lidar Mapping (SnowPALM) model to investigate the effect of two virtual forest thinning scenarios on the snowpack of two adjacent watersheds (54 km(2) total) in the Lake Tahoe Basin, California, where forest thinning is being planned. SnowPALM realistically represents small-scale snow-forest interactions to simulate the impact of virtual thinning experiments in which trees <10 and <20 m are removed. In general, thinning results in an overall increase in peak snow water equivalent and snowmelt. Areas around sheltered tree clusters have the largest increases of snowmelt due to decreases of canopy sublimation, while more open and exposed areas show a small decrease due to increases in snowpack sublimation. At the 30-m forest stand scale, existing forest structure controls the efficacy of thinning, where forest stands with mean leaf area index (LAI) >3 m(2)/m(2) and 5-15-m tall show the largest increases in snow accumulation (up to 450 mm) and melt volume (up to 650 mm). Despite the role of tree- and stand-scale thinning on snowmelt, macroscale effects were limited to slightly larger increases in melt volumes at mid to low elevation slopes (<2,300 masl) and south facing areas per unit of LAI removed. A decision support tool using machine learning (random forest) was developed to synthesize SnowPALM results, and was applied to neighboring watersheds. These results will inform ongoing forest management practices in California, and improve our understanding of the effects of snow-forest interactions at scales relevant to water management.en_US
dc.language.isoenen_US
dc.publisherFRONTIERS MEDIA SAen_US
dc.rights© 2020 Krogh, Broxton, Manley and Harpold. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY).en_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_US
dc.subjectsnow hydrologyen_US
dc.subjectmodelingen_US
dc.subjectlidaren_US
dc.subjectforesten_US
dc.subjectforest managementen_US
dc.subjectrestorationen_US
dc.titleUsing Process Based Snow Modeling and Lidar to Predict the Effects of Forest Thinning on the Northern Sierra Nevada Snowpacken_US
dc.typeArticleen_US
dc.identifier.eissn2624-893X
dc.contributor.departmentUniv Arizona, Sch Nat Resources & Environmen_US
dc.identifier.journalFRONTIERS IN FORESTS AND GLOBAL CHANGEen_US
dc.description.noteOpen access journalen_US
dc.description.collectioninformationThis item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.en_US
dc.eprint.versionFinal published versionen_US
dc.source.journaltitleFrontiers in Forests and Global Change
dc.source.volume3
refterms.dateFOA2020-06-11T19:50:36Z


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© 2020 Krogh, Broxton, Manley and Harpold. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY).
Except where otherwise noted, this item's license is described as © 2020 Krogh, Broxton, Manley and Harpold. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY).