Temporal patterns and vertical temperature gradients in micro-scale drainage flow observed using thermal imaging

  • Micro-scale cold-air flow along a gentle slope was analyzed using thermal infrared imaging (TIR), focusing exclusively on the lowermost 2 m above ground. Cold-air pulses were analyzed with regard to their vertical temperature stratification as well as flow characteristics, such as flow speed. Analyses on the transition zone between the near-surface very stable inversion layer and the less stable, warmer air above highlight turbulent situations and detrainment effects at the cold-air inversion top. Using thermal imaging in a high spatiotemporal resolution with up to 90 vertical data points and TIR pixels for 1.5 m cold-air depth, a high-precision cold-air flow analysis was realized.

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Metadaten
Author:Anja Martina GrudzielanekGND, Jan CermakGND
URN:urn:nbn:de:hbz:294-64566
DOI:https://doi.org/10.3390/atmos9120498
Parent Title (English):Atmosphere
Document Type:Article
Language:English
Date of Publication (online):2019/05/23
Date of first Publication:2018/12/14
Publishing Institution:Ruhr-Universität Bochum, Universitätsbibliothek
Tag:Open Access Fonds
micro-scale cold-air flow; nocturnal drainage flow; remote sensing; thermal infrared imaging
Volume:9
Issue:12
First Page:498-1
Last Page:498-16
Note:
Atmosphere , Bd. 9.2018, H. 12, Artikelnummer 498
Note:
Article Processing Charge funded by the Deutsche Forschungsgemeinschaft (DFG) and the Open Access Publication Fund of Ruhr-Universität Bochum.
Institutes/Facilities:Geographisches Institut
Dewey Decimal Classification:Naturwissenschaften und Mathematik / Geowissenschaften, Geologie
open_access (DINI-Set):open_access
faculties:Fakultät für Geowissenschaften
Licence (English):License LogoCreative Commons - CC BY 4.0 - Attribution 4.0 International