Zur Überwachung der Höhenlage der 0°-Grenze in der Atmosphäre anhand von Radarbeobachtungen
By: G. Malkowski
Abstract
The observation of precipitation clouds by means of a RHI-radar set allows the control of the actual height of the freezing level without the use of radiosonde measurements. Warmings and coolings of the lower and middle troposphere layers caused by airmass changes are thereby detected faster than by use of the regular radiosonde ascents, which are often available only twice a day.
DOI: https://doi.org/10.3402/tellusa.v19i3.9814 | Journal eISSN: 3035-9554
Language: English
Page range: 462 - 466
Submitted on: Jul 18, 1966
Published on: Jan 1, 1967
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1967 G. Malkowski, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.