Articles | Volume 11, issue 7
https://doi.org/10.5194/amt-11-4015-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/amt-11-4015-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Ice particle sampling from aircraft – influence of the probing position on the ice water content
Armin Afchine
Forschungszentrum Jülich, Institute of Energy and Climate Research (IEK-7), Jülich, Germany
Christian Rolf
Forschungszentrum Jülich, Institute of Energy and Climate Research (IEK-7), Jülich, Germany
Anja Costa
Forschungszentrum Jülich, Institute of Energy and Climate Research (IEK-7), Jülich, Germany
Nicole Spelten
Forschungszentrum Jülich, Institute of Energy and Climate Research (IEK-7), Jülich, Germany
Martin Riese
Forschungszentrum Jülich, Institute of Energy and Climate Research (IEK-7), Jülich, Germany
Bernhard Buchholz
Physikalisch-Technische Bundesanstalt Braunschweig, Braunschweig, Germany
Volker Ebert
Physikalisch-Technische Bundesanstalt Braunschweig, Braunschweig, Germany
Romy Heller
Deutsches Zentrum für Luft- und Raumfahrt, Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany
Stefan Kaufmann
Deutsches Zentrum für Luft- und Raumfahrt, Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany
Andreas Minikin
Deutsches Zentrum für Luft- und Raumfahrt, Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany
Christiane Voigt
Deutsches Zentrum für Luft- und Raumfahrt, Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany
Martin Zöger
Deutsches Zentrum für Luft- und Raumfahrt, Institute for Physics of the Atmosphere, Oberpfaffenhofen, Germany
Jessica Smith
Anderson Group/CCB, Harvard University, Cambridge, MA, USA
Paul Lawson
SPEC Incorporated, Boulder, CO, USA
Alexey Lykov
Department of Upper Atmospheric Layers Physics, Central Aerological Observatory (CAO), Moscow, Russia
Sergey Khaykin
LATMOS/IPSL, UVSQ Université Paris-Saclay, UPMC University Paris 06, CNRS, Guyancourt, France
Forschungszentrum Jülich, Institute of Energy and Climate Research (IEK-7), Jülich, Germany
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- Quantifying Uncertainty in Ice Particle Velocity–Dimension Relationships Using MC3E Observations A. Dzambo et al. 10.1175/JAS-D-21-0322.1
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- In situ observation of new particle formation (NPF) in the tropical tropopause layer of the 2017 Asian monsoon anticyclone – Part 2: NPF inside ice clouds R. Weigel et al. 10.5194/acp-21-13455-2021
- The dehydration carousel of stratospheric water vapor in the Asian summer monsoon anticyclone P. Konopka et al. 10.5194/acp-23-12935-2023
- A microphysics guide to cirrus – Part 2: Climatologies of clouds and humidity from observations M. Krämer et al. 10.5194/acp-20-12569-2020
- Sensitivity of convectively driven tropical tropopause cirrus properties to ice habits in high-resolution simulations F. Lamraoui et al. 10.5194/acp-23-2393-2023
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- Persistence of moist plumes from overshooting convection in the Asian monsoon anticyclone S. Khaykin et al. 10.5194/acp-22-3169-2022
- Metrology for sensor networks: metrological traceability and measurement uncertainties for air quality monitoring S. Eichstädt & O. Werhahn 10.1515/teme-2024-0042
- The Cloud Indicator: A novel algorithm for automatic detection and classification of clouds using airborne in situ observations M. Dollner et al. 10.1016/j.atmosres.2024.107504
- A comparative analysis of in situ measurements of high-altitude cirrus in the tropics F. Cairo et al. 10.5194/amt-16-4899-2023
Latest update: 22 Nov 2024
Short summary
The ice water content (IWC) of cirrus clouds is an essential parameter that determines their radiative properties and is thus important for climate simulations. Experimental investigations of IWCs measured on board research aircraft reveal that their accuracy is influenced by the sampling position. IWCs detected at the aircraft roof deviate significantly from wing, side or bottom IWCs. The reasons are deflections of the gas streamlines and ice particle trajectories behind the aircraft cockpit.
The ice water content (IWC) of cirrus clouds is an essential parameter that determines their...
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