Articles | Volume 23, issue 8
https://doi.org/10.5194/acp-23-4685-2023
https://doi.org/10.5194/acp-23-4685-2023
Research article
 | 
20 Apr 2023
Research article |  | 20 Apr 2023

Turbulent structure of the Arctic boundary layer in early summer driven by stability, wind shear and cloud-top radiative cooling: ACLOUD airborne observations

Dmitry G. Chechin, Christof Lüpkes, Jörg Hartmann, André Ehrlich, and Manfred Wendisch

Viewed

Total article views: 2,051 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,525 485 41 2,051 26 28
  • HTML: 1,525
  • PDF: 485
  • XML: 41
  • Total: 2,051
  • BibTeX: 26
  • EndNote: 28
Views and downloads (calculated since 03 Jun 2022)
Cumulative views and downloads (calculated since 03 Jun 2022)

Viewed (geographical distribution)

Total article views: 2,051 (including HTML, PDF, and XML) Thereof 2,013 with geography defined and 38 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 22 Apr 2024
Download
Short summary
Clouds represent a very important component of the Arctic climate system, as they strongly reduce the amount of heat lost to space from the sea ice surface. Properties of clouds, as well as their persistence, strongly depend on the complex interaction of such small-scale properties as phase transitions, radiative transfer and turbulence. In this study we use airborne observations to learn more about the effect of clouds and radiative cooling on turbulence in comparison with other factors.
Altmetrics
Final-revised paper
Preprint