Articles | Volume 19, issue 7
https://doi.org/10.5194/acp-19-4933-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-19-4933-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
12 Apr 2019
Research article |
| 12 Apr 2019
| 12 Apr 2019
Estimations of global shortwave direct aerosol radiative effects above opaque water clouds using a combination of A-Train satellite sensors
Meloë S. Kacenelenbogen
CORRESPONDING AUTHOR
NASA Ames Research Center, Moffett Field, CA, USA
Mark A. Vaughan
NASA
Langley Research Center, Hampton, VA, USA
Jens Redemann
University of Oklahoma,
120 David L. Boren Blvd., Suite 5900, Norman, OK, USA
Stuart A. Young
Science
Systems and Applications, Inc., Hampton, VA, USA
Zhaoyan Liu
NASA
Langley Research Center, Hampton, VA, USA
Science
Systems and Applications, Inc., Hampton, VA, USA
Yongxiang Hu
NASA
Langley Research Center, Hampton, VA, USA
Ali H. Omar
NASA
Langley Research Center, Hampton, VA, USA
Samuel LeBlanc
Bay
Area Environmental Research Institute, Sonoma, CA, USA
Yohei Shinozuka
Bay
Area Environmental Research Institute, Sonoma, CA, USA
John Livingston
Bay
Area Environmental Research Institute, Sonoma, CA, USA
Qin Zhang
Bay
Area Environmental Research Institute, Sonoma, CA, USA
Kathleen A. Powell
NASA
Langley Research Center, Hampton, VA, USA
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- Validation and diurnal variation evaluation of MERRA-2 multiple aerosol properties on a global scale X. Su et al. 10.1016/j.atmosenv.2023.120019
- Retrieving UV–Vis spectral single-scattering albedo of absorbing aerosols above clouds from synergy of ORACLES airborne and A-train sensors H. Jethva et al. 10.5194/amt-17-2335-2024
- A novel simplified method for surface albedo together with a look-up table to get an 18-year assessment of surface aerosol direct radiative effect in Central and East China Y. Shi et al. 10.1016/j.atmosenv.2020.117858
- Satellite-based analysis of top of atmosphere shortwave radiative forcing trend induced by biomass burning aerosols over South-Eastern Atlantic C. Jouan & G. Myhre 10.1038/s41612-024-00631-3
- Spatiotemporal Heterogeneity of Aerosol and Cloud Properties Over the Southeast Atlantic: An Observational Analysis I. Chang et al. 10.1029/2020GL091469
- Intercomparison of biomass burning aerosol optical properties from in situ and remote-sensing instruments in ORACLES-2016 K. Pistone et al. 10.5194/acp-19-9181-2019
- Three-Dimensional Distributions of the Direct Effect of anExtended and Intense Dust Aerosol Episode (16–18 June 2016) over the Mediterranean Basin on Regional Shortwave Radiation, Atmospheric Thermal Structure, and Dynamics M. Gavrouzou et al. 10.3390/app13126878
- Improved simulations of biomass burning aerosol optical properties and lifetimes in the NASA GEOS Model during the ORACLES-I campaign S. Das et al. 10.5194/acp-24-4421-2024
- Estimating aerosol emission from SPEXone on the NASA PACE mission using an ensemble Kalman smoother: observing system simulation experiments (OSSEs) A. Tsikerdekis et al. 10.5194/gmd-15-3253-2022
- Satellite inference of water vapour and above-cloud aerosol combined effect on radiative budget and cloud-top processes in the southeastern Atlantic Ocean L. Deaconu et al. 10.5194/acp-19-11613-2019
- Impact of smoke and non-smoke aerosols on radiation and low-level clouds over the southeast Atlantic from co-located satellite observations A. Baró Pérez et al. 10.5194/acp-21-6053-2021
- Global Clear-Sky Aerosol Speciated Direct Radiative Effects over 40 Years (1980–2019) M. Korras-Carraca et al. 10.3390/atmos12101254
- Radiative forcing of climate change from the Copernicus reanalysis of atmospheric composition N. Bellouin et al. 10.5194/essd-12-1649-2020
- Impact of biomass burning aerosols (BBA) on the tropical African climate in an ocean–atmosphere–aerosol coupled climate model M. Mallet et al. 10.5194/acp-24-12509-2024
- An overview of the ORACLES (ObseRvations of Aerosols above CLouds and their intEractionS) project: aerosol–cloud–radiation interactions in the southeast Atlantic basin J. Redemann et al. 10.5194/acp-21-1507-2021
- AEROCOM and AEROSAT AAOD and SSA study – Part 1: Evaluation and intercomparison of satellite measurements N. Schutgens et al. 10.5194/acp-21-6895-2021
- Two decades observing smoke above clouds in the south-eastern Atlantic Ocean: Deep Blue algorithm updates and validation with ORACLES field campaign data A. Sayer et al. 10.5194/amt-12-3595-2019
- Bounding Global Aerosol Radiative Forcing of Climate Change N. Bellouin et al. 10.1029/2019RG000660
- The Influence of Elevated Smoke Layers on Stratocumulus Clouds Over the SE Atlantic in the NASA Goddard Earth Observing System (GEOS) Model S. Das et al. 10.1029/2019JD031209
- Aerosol direct radiative effect over clouds from a synergy of Ozone Monitoring Instrument (OMI) and Moderate Resolution Imaging Spectroradiometer (MODIS) reflectances M. de Graaf et al. 10.5194/amt-12-5119-2019
- Climate models generally underrepresent the warming by Central Africa biomass-burning aerosols over the Southeast Atlantic M. Mallet et al. 10.1126/sciadv.abg9998
- Sensitivity of global direct aerosol shortwave radiative forcing to uncertainties in aerosol optical properties J. Elsey et al. 10.5194/acp-24-4065-2024
- On the differences in the vertical distribution of modeled aerosol optical depth over the southeastern Atlantic I. Chang et al. 10.5194/acp-23-4283-2023
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- Aerosol Direct Radiative Effect Sensitivity Analysis T. Thorsen et al. 10.1175/JCLI-D-19-0669.1
Latest update: 20 Nov 2024
Short summary
Significant efforts are required to estimate the direct radiative effects of aerosols above clouds (DAREcloudy). We have used a combination of passive and active A-Train satellite sensors and derive mainly positive global and regional DAREcloudy values (e.g., global seasonal values between 0.13 and 0.26 W m-2). Despite differences in methods and sensors, the DAREcloudy values in this study are generally higher than previously reported. We discuss the primary reasons for these higher estimates.
Significant efforts are required to estimate the direct radiative effects of aerosols above...
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