Zur Erforschung der polaren troposphärischen Grundschicht vor dem Zweiten Internationalen Polarjahr 1932/1933
In the period between the two polar years 1882/83 and 1932/33, the classical captive and sounding balloon ascent methods developed at aerological observatories were also employed in the polar regions. It was only in the period leading up to the second Polar Year that radiosonde ascents and aircraft...
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ftleibnizopen:oai:oai.leibnizopen.de:8BhCiIcBdbrxVwz6swSU 2023-06-06T11:47:31+02:00 Zur Erforschung der polaren troposphärischen Grundschicht vor dem Zweiten Internationalen Polarjahr 1932/1933 Bernhardt, Karl-Heinz 2008 https://nbn-resolving.org/urn:nbn:de:0168-ssoar-65948-0 https://www.ssoar.info/ssoar/handle/document/65948 unknown Deposit Licence - Keine Weiterverbreitung, keine Bearbeitung Deposit Licence - No Redistribution, No Modifications Deutsches Schiffahrtsarchiv, 31 (2008), S. 434-448. ISSN 0343-3668 Geschichte Naturwissenschaften Technik(wissenschaften) angewandte Wissenschaften History Natural Science and Engineering Applied Sciences Zeitschriftenartikel journal article 2008 ftleibnizopen 2023-04-16T23:28:57Z In the period between the two polar years 1882/83 and 1932/33, the classical captive and sounding balloon ascent methods developed at aerological observatories were also employed in the polar regions. It was only in the period leading up to the second Polar Year that radiosonde ascents and aircraft sounding came into use as new methods of aerological research. In the North Polar region, vertical temperature, humidity and wind profiles in the boundary layer were developed overseas (Arthur Berson, Hermann Elias, Hugo Hergesell) and in Greenland (Max Robitzsch, Alfred Wegener and others) during the early decades of the twentieth century with the aid of kite, captive and sounding balloon ascents. Here special attention was paid to cloud and inversion layers as well as to the catabatic wind then described for the first time. Various types of boundary layers, among them the extreme stratification conditions during the polar night, were also found by George Clarke Simpson and Erich Barkow in the Antarctic. Barkow’s micrometeorological measurements, including the registration of turbulent temperature fluctuations, are worthy of particular mention. begutachtet (peer reviewed) Veröffentlichungsversion peer reviewed Published Version Article in Journal/Newspaper Antarc* Antarctic Greenland polar night LeibnizOpen (The Leibniz Association) Antarctic Barkow ENVELOPE(-63.000,-63.000,-73.367,-73.367) Greenland The Antarctic |
institution |
Open Polar |
collection |
LeibnizOpen (The Leibniz Association) |
op_collection_id |
ftleibnizopen |
language |
unknown |
topic |
Geschichte Naturwissenschaften Technik(wissenschaften) angewandte Wissenschaften History Natural Science and Engineering Applied Sciences |
spellingShingle |
Geschichte Naturwissenschaften Technik(wissenschaften) angewandte Wissenschaften History Natural Science and Engineering Applied Sciences Bernhardt, Karl-Heinz Zur Erforschung der polaren troposphärischen Grundschicht vor dem Zweiten Internationalen Polarjahr 1932/1933 |
topic_facet |
Geschichte Naturwissenschaften Technik(wissenschaften) angewandte Wissenschaften History Natural Science and Engineering Applied Sciences |
description |
In the period between the two polar years 1882/83 and 1932/33, the classical captive and sounding balloon ascent methods developed at aerological observatories were also employed in the polar regions. It was only in the period leading up to the second Polar Year that radiosonde ascents and aircraft sounding came into use as new methods of aerological research. In the North Polar region, vertical temperature, humidity and wind profiles in the boundary layer were developed overseas (Arthur Berson, Hermann Elias, Hugo Hergesell) and in Greenland (Max Robitzsch, Alfred Wegener and others) during the early decades of the twentieth century with the aid of kite, captive and sounding balloon ascents. Here special attention was paid to cloud and inversion layers as well as to the catabatic wind then described for the first time. Various types of boundary layers, among them the extreme stratification conditions during the polar night, were also found by George Clarke Simpson and Erich Barkow in the Antarctic. Barkow’s micrometeorological measurements, including the registration of turbulent temperature fluctuations, are worthy of particular mention. begutachtet (peer reviewed) Veröffentlichungsversion peer reviewed Published Version |
format |
Article in Journal/Newspaper |
author |
Bernhardt, Karl-Heinz |
author_facet |
Bernhardt, Karl-Heinz |
author_sort |
Bernhardt, Karl-Heinz |
title |
Zur Erforschung der polaren troposphärischen Grundschicht vor dem Zweiten Internationalen Polarjahr 1932/1933 |
title_short |
Zur Erforschung der polaren troposphärischen Grundschicht vor dem Zweiten Internationalen Polarjahr 1932/1933 |
title_full |
Zur Erforschung der polaren troposphärischen Grundschicht vor dem Zweiten Internationalen Polarjahr 1932/1933 |
title_fullStr |
Zur Erforschung der polaren troposphärischen Grundschicht vor dem Zweiten Internationalen Polarjahr 1932/1933 |
title_full_unstemmed |
Zur Erforschung der polaren troposphärischen Grundschicht vor dem Zweiten Internationalen Polarjahr 1932/1933 |
title_sort |
zur erforschung der polaren troposphärischen grundschicht vor dem zweiten internationalen polarjahr 1932/1933 |
publishDate |
2008 |
url |
https://nbn-resolving.org/urn:nbn:de:0168-ssoar-65948-0 https://www.ssoar.info/ssoar/handle/document/65948 |
long_lat |
ENVELOPE(-63.000,-63.000,-73.367,-73.367) |
geographic |
Antarctic Barkow Greenland The Antarctic |
geographic_facet |
Antarctic Barkow Greenland The Antarctic |
genre |
Antarc* Antarctic Greenland polar night |
genre_facet |
Antarc* Antarctic Greenland polar night |
op_source |
Deutsches Schiffahrtsarchiv, 31 (2008), S. 434-448. ISSN 0343-3668 |
op_rights |
Deposit Licence - Keine Weiterverbreitung, keine Bearbeitung Deposit Licence - No Redistribution, No Modifications |
_version_ |
1767952982757867520 |