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Open cells can decrease the mixing of free-tropospheric biomass burning aerosol into the south-east Atlantic boundary layer

Ultra-clean and smoky marine boundary layers frequently occur in the same season over the southeast Atlantic

Modeling the smoky troposphere of the southeast Atlantic: a comparison to ORACLES airborne observations from September of 2016

Shinozuka, Y., et al. (2019), Modeling the smoky troposphere of the southeast Atlantic: a comparison to ORACLES airborne observations from September of 2016, Atmos. Chem. Phys. Discuss., doi: https://doi.org/10.5194/acp-2019-678 (submitted).

Above Cloud Aerosol Optical Depth from airborne observations in the South-East Atlantic

LeBlanc, S., et al. (2019), Above Cloud Aerosol Optical Depth from airborne observations in the South-East Atlantic, doi: https://doi.org/10.5194/acp-2019-43 (submitted).

Above-Cloud Aerosol Radiative Effects based on ORACLES 2016 and ORACLES 2017 Aircraft Experiments

Biomass Burning Aerosol as a Modulator of Droplet Number in the Southeast Atlantic Region

Low-level liquid cloud properties during ORACLES retrieved using airborne polarimetric measurements and a neural network algorithm

Comparison of Optimal Estimation HDO/H2O Retrievals from AIRS with ORACLES measurements

Herman, R. L., et al. (2019), Comparison of Optimal Estimation HDO/H2O Retrievals from AIRS with ORACLES measurements, doi:https://doi.org/10.5194/amt-2019-195 (submitted).

The Observed Structure and Precipitation Characteristics of Southeast Atlantic Stratocumulus from Airborne Radar during ORACLES 2016-17

Dzambo, A., et al. (2019), The Observed Structure and Precipitation Characteristics of Southeast Atlantic Stratocumulus from Airborne Radar during ORACLES 2016-17, J. Appl. Meteor. Climat., 58, 2197-2215, doi:https://doi.org/10.1175/JAMC-D-19-0032.1.

ORACLES - P-3 Orion - WFF 09/24/16 Science Report

This was a coastal flight, going farther north (to 8 S) than any other ORACLES 2016 flight. We went along 11 E to sample an intense young plume forecast by WRF. We did find the plume, and this flight will be very useful for aerosol properties in the FT. The MBL was complicated by the presence of 2 or 3 layers of cloud, and we encountered intermediate-level clouds high in the plume. These complicate the radiation measurements as well as the FT/MBL exchange.

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