The NASA ACTIVATE Mission

Armin Sorooshian Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ.
Department of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ.

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Leong Wai Siu Department of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ.

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Kayley Butler Department of Civil and Environmental Engineering, University of Southern California, Los Angeles, CA.

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Michael A. Brunke Department of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ.

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Brian Cairns NASA Goddard Institute for Space Studies, New York, NY.

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Seethala Chellappan NASA Langley Research Center, Hampton, VA.
Analytical Mechanics Associates, Hampton, VA.

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Jingyi Chen Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, WA.
School of Atmospheric Physics, Nanjing University of Information Science and Technology, Nanjing, China.

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Yonghoon Choi NASA Langley Research Center, Hampton, VA.
Analytical Mechanics Associates, Hampton, VA.

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Ewan C. Crosbie NASA Langley Research Center, Hampton, VA.
Analytical Mechanics Associates, Hampton, VA.

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Lauren Cutler Department of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ.

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Joshua P. DiGangi NASA Langley Research Center, Hampton, VA.

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Glenn S. Diskin NASA Langley Research Center, Hampton, VA.

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Richard A. Ferrare NASA Langley Research Center, Hampton, VA.

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Johnathan W. Hair NASA Langley Research Center, Hampton, VA.

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Chris A. Hostetler NASA Langley Research Center, Hampton, VA.

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Simon Kirschler Institute of Atmospheric Physics, German Aerospace Center, Germany.
Institute of Atmospheric Physics, University Mainz, Germany.

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Mary M. Kleb NASA Langley Research Center, Hampton, VA.

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Xiang-Yu Li Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, WA.

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Hongyu Liu NASA Langley Research Center, Hampton, VA.
National Institute of Aerospace, Hampton, VA.

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Allison McComiskey NSF National Center for Atmospheric Research, Boulder, CO.

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Soodabeh Namdari Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ.

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David Painemal NASA Langley Research Center, Hampton, VA.
Analytical Mechanics Associates, Hampton, VA.

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Joseph S. Schlosser NASA Langley Research Center, Hampton, VA.
NASA Postdoctoral Program, NASA Langley Research Center, Hampton, VA.

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Taylor Shingler NASA Langley Research Center, Hampton, VA.

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Michael A. Shook NASA Langley Research Center, Hampton, VA.

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Sam Silva Department of Earth Sciences, University of Southern California, Los Angeles, CA.

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Kenneth Sinclair NASA Goddard Institute for Space Studies, New York, NY.
Center for Climate Systems Research, Columbia University, New York, NY.

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William L. Smith Jr. NASA Langley Research Center, Hampton, VA.

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Cassidy Soloff Department of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ.

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Snorre Stamnes NASA Langley Research Center, Hampton, VA.

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Shuaiqi Tang Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, WA.
School of Atmospheric Sciences, Nanjing University, Nanjing, China.

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Kenneth L. Thornhill NASA Langley Research Center, Hampton, VA.
Analytical Mechanics Associates, Hampton, VA.

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Florian Tornow NASA Goddard Institute for Space Studies, New York, NY.
Center for Climate Systems Research, Columbia University, New York, NY.

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George Tselioudis NASA Goddard Institute for Space Studies, New York, NY.

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Bastiaan Van Diedenhoven SRON Netherlands Institute for Space Research, Leiden, the Netherlands.

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Christiane Voigt Institute of Atmospheric Physics, German Aerospace Center, Germany.
Institute of Atmospheric Physics, University Mainz, Germany.

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Holger Vömel NSF National Center for Atmospheric Research, Boulder, CO.

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Hailong Wang Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, WA.

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Edward L. Winstead NASA Langley Research Center, Hampton, VA.
Analytical Mechanics Associates, Hampton, VA.

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Yike Xu Department of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ.

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Xubin Zeng Department of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ.

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Bo Zhang NASA Langley Research Center, Hampton, VA.
National Institute of Aerospace, Hampton, VA.

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Luke Ziemba NASA Langley Research Center, Hampton, VA.

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Paquita Zuidema Rosenstiel School of Marine, Atmospheric and Earth Science, University of Miami, Miami, FL.

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Open access

Abstract

The NASA Aerosol Cloud meTeorology Interactions oVer the western ATlantic Experiment (ACTIVATE) conducted 162 joint flights with two aircraft over the northwest Atlantic to study aerosol-cloud interactions (ACI), which represent the largest uncertainty in estimating total anthropogenic radiative forcing. The combination of a high-flying King Air and low-flying HU-25 Falcon, equipped with remote sensing and in situ instruments, characterized trace gases, aerosol particles, clouds, and meteorological variables with data collected nearly simultaneously below, within, and above marine boundary layer (MBL) clouds. Flights spanning warm and cold seasons across three years (2020-2022) provided a broad range of conditions associated with aerosol particles, cloud properties (including particle size and phase), and meteorology, ideally suited for robust ACI calculations and assessing how well models simulate a wide range of MBL clouds from stratiform to cumulus. ACTIVATE data suggest that drivers of cloud droplet number concentration (Nd), including aerosol particles and MBL dynamics, vary between winter and summer months with a stronger potential to convert aerosol particles into cloud droplets in winter. Models of varying complexity highlight some skill in simulating winter and summer cloud types, but also identify challenges that still need to be addressed such as treatment of turbulence, wet scavenging, and mesoscale organization. Remote sensing advances range from new retrieval methods for Nd, cloud phase classification, vertically-resolved aerosol and cloud condensation nuclei number concentration, and ocean surface wind speed. This work describes these scientific and technological advances along with efforts in outreach and open data science.

© 2025 American Meteorological Society. This is an Author Accepted Manuscript distributed under the terms of the default AMS reuse license. For information regarding reuse and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses).

Corresponding author address: Armin Sorooshian, Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ 85721 E-mail: armin@arizona.edu

Abstract

The NASA Aerosol Cloud meTeorology Interactions oVer the western ATlantic Experiment (ACTIVATE) conducted 162 joint flights with two aircraft over the northwest Atlantic to study aerosol-cloud interactions (ACI), which represent the largest uncertainty in estimating total anthropogenic radiative forcing. The combination of a high-flying King Air and low-flying HU-25 Falcon, equipped with remote sensing and in situ instruments, characterized trace gases, aerosol particles, clouds, and meteorological variables with data collected nearly simultaneously below, within, and above marine boundary layer (MBL) clouds. Flights spanning warm and cold seasons across three years (2020-2022) provided a broad range of conditions associated with aerosol particles, cloud properties (including particle size and phase), and meteorology, ideally suited for robust ACI calculations and assessing how well models simulate a wide range of MBL clouds from stratiform to cumulus. ACTIVATE data suggest that drivers of cloud droplet number concentration (Nd), including aerosol particles and MBL dynamics, vary between winter and summer months with a stronger potential to convert aerosol particles into cloud droplets in winter. Models of varying complexity highlight some skill in simulating winter and summer cloud types, but also identify challenges that still need to be addressed such as treatment of turbulence, wet scavenging, and mesoscale organization. Remote sensing advances range from new retrieval methods for Nd, cloud phase classification, vertically-resolved aerosol and cloud condensation nuclei number concentration, and ocean surface wind speed. This work describes these scientific and technological advances along with efforts in outreach and open data science.

© 2025 American Meteorological Society. This is an Author Accepted Manuscript distributed under the terms of the default AMS reuse license. For information regarding reuse and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses).

Corresponding author address: Armin Sorooshian, Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ 85721 E-mail: armin@arizona.edu
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