{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1361137044217569408.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2007wr006545"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2007WR006545"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2007WR006545"}}],"dc:title":[{"@value":"Inhomogeneous precipitation distribution and snow transport in steep terrain"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The inhomogeneous snow distribution found in alpine terrain is the result of wind and precipitation interacting with the (snow) surface over topography. We introduce and explain preferential deposition of precipitation as the deposition process without erosion of previously deposited snow and thus in absence of saltation. A numerical model is developed, describing the relevant processes of saltation, suspension, and preferential deposition. The model uses high‐resolution wind fields calculated with a meteorological model, ARPS. The model is used to simulate a 120 h snow storm period over a steep alpine ridge, for which snow distribution measurements are available. The comparison to measurements shows that the model captures the larger‐scale snow distribution patterns and predicts the total additional lee slope loading well. However, the spatial resolution of 25 m is still insufficient to capture the smaller‐scale deposition features observed. The model suggests that the snow distribution on the ridge scale is primarily caused by preferential deposition and that this result is not sensitive to model parameters such as turbulent diffusivity, drift threshold, or concentration in the saltation layer.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380294643738216076","@type":"Researcher","foaf:name":[{"@value":"M. Lehning"}],"jpcoar:affiliationName":[{"@value":"WSL, Swiss Federal Institute for Snow and Avalanche Research SLF Davos  Davos Switzerland"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044217569408","@type":"Researcher","foaf:name":[{"@value":"H. Löwe"}],"jpcoar:affiliationName":[{"@value":"WSL, Swiss Federal Institute for Snow and Avalanche Research SLF Davos  Davos Switzerland"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044217569411","@type":"Researcher","foaf:name":[{"@value":"M. Ryser"}],"jpcoar:affiliationName":[{"@value":"WSL, Swiss Federal Institute for Snow and Avalanche Research SLF Davos  Davos Switzerland"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044217569409","@type":"Researcher","foaf:name":[{"@value":"N. Raderschall"}],"jpcoar:affiliationName":[{"@value":"WSL, Swiss Federal Institute for Snow and Avalanche Research SLF Davos  Davos Switzerland"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00431397"},{"@type":"EISSN","@value":"19447973"}],"prism:publicationName":[{"@value":"Water Resources Research"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2008-07","prism:volume":"44","prism:number":"7","prism:startingPage":"W07404"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2007WR006545"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2007WR006545"}],"createdAt":"2008-07-02","modifiedAt":"2023-10-12","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360285707321269760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Development of a system for predicting snow distribution in built-up environments: Combining a mesoscale meteorological model and a CFD model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306904386045184","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Field-based investigation of snow-drift flux increases in blowing snow and application to mapping of short-term visibility reduction using mesoscale meteorological simulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763099255424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Case Study of Blowing Snow Potential Diagnosis with Dynamical Downscaling"},{"@value":"Case study of drifting snow potential diagnosis with dynamical downscaling"}]},{"@id":"https://cir.nii.ac.jp/crid/1390287629001084032","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Recent studies on numerical simulation of snow redistribution caused by blowing snow"},{"@language":"ja","@value":"吹雪による積雪再配分の数値シミュレーションに関する最近の研究"},{"@language":"ja-Kana","@value":"フブキ ニ ヨル セキセツ サイハイブン ノ スウチ シミュレーション ニ カンスル サイキン ノ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390854882571725568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Calculation of Snowdrift Distribution over Complex Topography to Improve the Accuracy of Snow Avalanche Warning Systems"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317037089664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Development of a snowdrift model with the lattice Boltzmann method"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2007wr006545"},{"@type":"CROSSREF","@value":"10.2151/sola.2019-007_references_DOI_HOsUGE7TMhZ7qAoo5wokbtJXmyg"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00449-0_references_DOI_HOsUGE7TMhZ7qAoo5wokbtJXmyg"},{"@type":"CROSSREF","@value":"10.1016/j.jweia.2024.105989_references_DOI_HOsUGE7TMhZ7qAoo5wokbtJXmyg"},{"@type":"CROSSREF","@value":"10.5331/seppyo.71.2_83_references_DOI_HOsUGE7TMhZ7qAoo5wokbtJXmyg"},{"@type":"CROSSREF","@value":"10.1016/j.jweia.2010.12.004_references_DOI_HOsUGE7TMhZ7qAoo5wokbtJXmyg"},{"@type":"CROSSREF","@value":"10.2151/sola.2022-012_references_DOI_HOsUGE7TMhZ7qAoo5wokbtJXmyg"}]}