A02: Tethered balloon-borne energy budget measurements in the cloudy central Arctic
PIs: Holger Siebert, Manfred Wendisch
Tethered balloon–borne measurements of atmospheric vertical profiles (up to one–kilometer altitude) of turbulent energy fluxes (sensible and latent heat), radiative energy fluxes, and turbulent fluxes of momentum are proposed. The observations will investigate the influence of macrophysical (cloud base height and temperature and geometric thickness, cloud cover) and microphysical (effective radius) properties of Arctic low–level clouds on (i) the profiles of fluxes (both, turbulent and radiative), (ii) the respective radiative forcing, and (iii) the related net warming/cooling of the near–surface air temperature. Three new sensor packages for balloon–borne measurements of turbulence, cloud and aerosol microphysical properties, and radiation quantities will be developed, extensively tested and deployed from an ice–floe camp during the cruise of Research Vessel (RV) Polarstern in early summer (May to June) 2017. The tethered balloon–borne in–situ observations are closely coordinated with the flux measurements of the two projects A01 (ship–based) and A03 (aircraft–borne).
Hypothesis: Cloud macrophysical and microphysical properties notably influence (i) the profiles of turbulent and radiative energy fluxes, (ii) the cloud radiative forcing at the surface, and (iii) the net warming/cooling of the near–surface air temperature in the cloudy ABL in the Arctic.
- How do profiles of turbulent and radiative fluxes differ for typical ABL structures, and for different cloud macrophysical and microphysical properties?
- How strongly do different aerosol loads influence the energy fluxes in the cloudy ABL?
- To what extend does evapourative and radiative cooling at cloud top affect the stability of the ABL?
- How closely linked are the surface radiative forcing (and the related cooling/warming) due to the clouds and cloud macrophysical and microphysical properties?
Role within (AC)³
- Ground site in Cluster A, microphysics closure in Cluster B and D
- Radiation budget in Cluster C, process understanding in E and A-D
Prof. Dr. Manfred Wendisch
University of Leipzig
Leipzig Institute for Meteorology (LIM)
Wendisch, M., A. Macke, A. Ehrlich, C. Lüpkes, M. Mech, D. Chechin, K. Dethloff, C. Barrientos, H. Bozem, M. Brückner, H.-C. Clemen, S. Crewell, T. Donth, R. Dupuy, C. Dusny, K. Ebell, U. Egerer, R. Engelmann, C. Engler, O. Eppers, M. Gehrmann, X. Gong, M. Gottschalk, C. Gourbeyre, H. Griesche, J. Hartmann, M. Hartmann, B. Heinold, A. Herber, H. Herrmann, G. Heygster, P. Hoor, S. Jafariserajehlou, E. Jäkel, E. Järvinen, O. Jourdan, U. Kästner, S. Kecorius, E.M. Knudsen, F. Köllner, J. Kretzschmar, L. Lelli, D. Leroy, M. Maturilli, L. Mei, S. Mertes, G. Mioche, R. Neuber, M. Nicolaus, T. Nomokonova, J. Notholt, M. Palm, M. van Pinxteren, J. Quaas, P. Richter, E. Ruiz-Donoso, M. Schäfer, K. Schmieder, M. Schnaiter, J. Schneider, A. Schwarzenböck, P. Seifert, M.D. Shupe, H. Siebert, G. Spreen, J. Stapf, F. Stratmann, T. Vogl, A. Welti, H. Wex, A. Wiedensohler, M. Zanatta, S. Zeppenfeld, 2018: The Arctic Cloud Puzzle: Using ACLOUD/PASCAL Multi-Platform Observations to Unravel the Role of Clouds and Aerosol Particles in Arctic Amplification, accepted by Bull. Amer. Meteor. Soc., doi:10.1175/BAMS-D-18-0072.1, in press