Abstract
Observations on a micro-structure scale were obtained of a radar bright band. The most important interpretations of the observations indicate: (1) Snow pellet aggregation occurs above and in the upper band levels, (2) Thermodynamically, the band is identified by an isothermal layer and a thin unstable layer (2.30°C/100 meters) near the band base.
DOI: https://doi.org/10.3402/tellusa.v16i4.8987 | Journal eISSN: 3035-9554
Language: English
Page range: 518 - 522
Published on: Jan 1, 2012
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 2012 Edward N. Brown, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.