Heavy Snowfall Produced by Topographically-Induced Winds in the Snake River Plain of Eastern Idaho. Part I: Observational Analysis | Zendy

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Heavy Snowfall Produced by Topographically-Induced Winds in the Snake River Plain of Eastern Idaho. Part I: Observational Analysis

Author(s) -

Thomas A. Andretta,

Bart Geerts

Publication year - 2021

Publication title -

e-journal of severe storms meteorology

Language(s) - English

Resource type - Journals

ISSN - 1559-5404

DOI - 10.55599/ejssm.v5i3.23

Subject(s) - mesoscale meteorology , snow , geology , climatology , forcing (mathematics) , precipitation , river valley , geomorphology , meteorology , geography , archaeology

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