TY - JOUR
T1 - Observations of aerosol, cloud, turbulence, and radiation properties at the top of the Marine Boundary Layer over the Eastern North Atlantic Ocean
AU - Siebert, Holger
AU - Szodry, Kai Erik
AU - Egerer, Ulrike
AU - Wehner, Birgit
AU - Henning, Silvia
AU - Chevalier, Karine
AU - Lückerath, Janine
AU - Welz, Oliver
AU - Weinhold, Kay
AU - Lauermann, Felix
AU - Gottschalk, Matthias
AU - Ehrlich, André
AU - Wendisch, Manfred
AU - Fialho, Paulo
AU - Roberts, Greg
AU - Allwayin, Nithin
AU - Schum, Simeon
AU - Shaw, Raymond A.
AU - Mazzoleni, Claudio
AU - Mazzoleni, Lynn
AU - Nowak, Jakub L.
AU - Malinowski, Szymon P.
AU - Karpinska, Katarzyna
AU - Kumala, Wojciech
AU - Czyzewska, Dominika
AU - Luke, Edward P.
AU - Kollias, Pavlos
AU - Wood, Robert
AU - Mellado, Juan Pedro
N1 - Publisher Copyright:
©2021 American Meteorological Society
PY - 2021/1
Y1 - 2021/1
N2 - We report on the Azores Stratocumulus Measurements of Radiation, Turbulence and Aerosols (ACORES) campaign, which took place around Graciosa and Pico Islands/Azores in July 2017. The main objective was to investigate the vertical distribution of aerosol particles, stratocumulus microphysical and radiative properties, and turbulence parameters in the eastern North Atlantic. The vertical exchange of mass, momentum, and energy between the free troposphere (FT) and the cloudy marine boundary layer (MBL) was explored over a range of scales from sub-meters to kilometers. To cover these spatial scales with appropriate measurements, helicopter-borne observations with unprecedented high resolution were realized using the Airborne Cloud Turbulence Observation System (ACTOS) and Spectral Modular Airborne Radiation Measurement System–Helicopter-Borne Observations (SMART-HELIOS) instrumental payloads. The helicopter-borne observations were combined with ground-based aerosol measurements collected at two continuously running field stations on Pico Mountain (2,225 m above sea level, in the FT), and at the Atmospheric Radiation Measurement (ARM) station on Graciosa (at sea level). First findings from the ACORES observations we are discussing in the paper are as follows: (i) we have observed a high variability of the turbulent cloud-top structure on horizontal scales below 100 m with local temperature gradients of up to 4 K over less than 1 m vertical distance, (ii) we have collected strictly collocated radiation measurements supporting the relevance of small-scale processes by revealing significant inhomogeneities in cloud-top brightness temperature to scales well below 100 m, and (iii) we have concluded that aerosol properties are completely different in the MBL and FT with often-complex stratification and frequently observed burst-like new particle formation.
AB - We report on the Azores Stratocumulus Measurements of Radiation, Turbulence and Aerosols (ACORES) campaign, which took place around Graciosa and Pico Islands/Azores in July 2017. The main objective was to investigate the vertical distribution of aerosol particles, stratocumulus microphysical and radiative properties, and turbulence parameters in the eastern North Atlantic. The vertical exchange of mass, momentum, and energy between the free troposphere (FT) and the cloudy marine boundary layer (MBL) was explored over a range of scales from sub-meters to kilometers. To cover these spatial scales with appropriate measurements, helicopter-borne observations with unprecedented high resolution were realized using the Airborne Cloud Turbulence Observation System (ACTOS) and Spectral Modular Airborne Radiation Measurement System–Helicopter-Borne Observations (SMART-HELIOS) instrumental payloads. The helicopter-borne observations were combined with ground-based aerosol measurements collected at two continuously running field stations on Pico Mountain (2,225 m above sea level, in the FT), and at the Atmospheric Radiation Measurement (ARM) station on Graciosa (at sea level). First findings from the ACORES observations we are discussing in the paper are as follows: (i) we have observed a high variability of the turbulent cloud-top structure on horizontal scales below 100 m with local temperature gradients of up to 4 K over less than 1 m vertical distance, (ii) we have collected strictly collocated radiation measurements supporting the relevance of small-scale processes by revealing significant inhomogeneities in cloud-top brightness temperature to scales well below 100 m, and (iii) we have concluded that aerosol properties are completely different in the MBL and FT with often-complex stratification and frequently observed burst-like new particle formation.
KW - Aerosols
KW - Aircraft observations
KW - Cloud radiative effects
KW - Small scale processes
UR - https://www.scopus.com/pages/publications/85101325167
U2 - 10.1175/BAMS-D-19-0191.1
DO - 10.1175/BAMS-D-19-0191.1
M3 - Article
AN - SCOPUS:85101325167
SN - 0003-0007
VL - 102
SP - E123-E147
JO - Bulletin of the American Meteorological Society
JF - Bulletin of the American Meteorological Society
IS - 1
ER -