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Using WRF to Model Temperature During Stable Boundary Layer Conditions on the Finnmarksvidda Plateau, Northern Norway

Autor: Lillegraven, Bjørn Gilje

Publikováno v: Lillegraven, Bjørn Gilje. Using WRF to Model Temperature During Stable Boundary Layer Conditions on the Finnmarksvidda Plateau, Northern Norway. Master thesis, University of Oslo, 2020

Externí odkaz: http://hdl.handle.net/10852/79739
https://www.duo.uio.no/bitstream/handle/10852/79739/1/Lillegraven_BG_Master_2020.pdf

The Large eddy Observatory, Voitsumra Experiment 2019 (LOVE19) with high-resolution, spatially distributed observations of air temperature, wind speed, and wind direction from fiber-optic distributed sensing, towers, and ground-based remote sensing

Autor: Karl Lapo, Anita Freundorfer, Antonia Fritz, Johann Schneider, Johannes Olesch, Wolfgang Babel, Christoph K. Thomas

The weak-wind stable boundary layer (wwSBL) is poorly described by theory and breaks basic assumptions necessary for observations of turbulence. Understanding the wwSBL requires distributed observations capable of separating between sub-mesoscales an

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2a207c08bfde40b86685792f081c3ea9

From Dutch Short-Lived to Antarctic Long-Lived Stable Boundary Layers

Autor: van der Linden, S.J.A.

Stable boundary layers (SBLs) are a common aspect of the earth’s atmosphere and are characterized by a stable density stratification in which the temperature increases with height. This typically occurs during the night, resulting in a short-lived

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a9fcb337d0b9596fad20ebb514d2641f

Regime occupation and transition information obtained from observable meteorological state variables in the stably stratified nocturnal boundary layer

Autor: Abraham, Carsten

The stably stratified nocturnal boundary layer (SBL) can be classified into two distinct regimes: one with moderate to strong winds, weak stratification and mechanically sustained turbulence (wSBL) and the other one with moderate to weak wind conditi

Externí odkaz: https://dspace.library.uvic.ca//handle/1828/10511