Institute of Atmospheric Physics – Lidar Department, Deutsches Zentrum für Luft- und Raumfahrt, Oberpfaffenhofen, Germany
Christian Lemmerz
Institute of Atmospheric Physics – Lidar Department, Deutsches Zentrum für Luft- und Raumfahrt, Oberpfaffenhofen, Germany
Publisher's note: Benjamin Witschas and Christian Lemmerz were added as co-authors to this paper on 20 October 2023. They originally contributed to the manuscript but were missing in the author list upon publication.
Viewed
Total article views: 3,315 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
2,509
708
98
3,315
106
160
HTML: 2,509
PDF: 708
XML: 98
Total: 3,315
BibTeX: 106
EndNote: 160
Views and downloads (calculated since 14 Feb 2022)
Cumulative views and downloads
(calculated since 14 Feb 2022)
Total article views: 2,723 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
2,169
479
75
2,723
91
145
HTML: 2,169
PDF: 479
XML: 75
Total: 2,723
BibTeX: 91
EndNote: 145
Views and downloads (calculated since 08 Jun 2022)
Cumulative views and downloads
(calculated since 08 Jun 2022)
Total article views: 592 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
340
229
23
592
15
15
HTML: 340
PDF: 229
XML: 23
Total: 592
BibTeX: 15
EndNote: 15
Views and downloads (calculated since 14 Feb 2022)
Cumulative views and downloads
(calculated since 14 Feb 2022)
Viewed (geographical distribution)
Total article views: 3,315 (including HTML, PDF, and XML)
Thereof 3,315 with geography defined
and 0 with unknown origin.
Total article views: 2,723 (including HTML, PDF, and XML)
Thereof 2,722 with geography defined
and 1 with unknown origin.
Total article views: 592 (including HTML, PDF, and XML)
Thereof 592 with geography defined
and 0 with unknown origin.
Wind measurements from the mixed layer to cloud tops are scarce, causing a lack of knowledge on wind mixing between and within these layers. We use airborne observations of wind profiles and local wind at high frequency to study wind transport in cloud fields. A case with thick clouds had its maximum transport in the cloud layer, caused by eddies > 700 m, which was not expected from turbulence theory. In other cases large eddies undid transport of smaller eddies resulting in no net transport.
Wind measurements from the mixed layer to cloud tops are scarce, causing a lack of knowledge on...
