NASA Logo

NTRS

NTRS - NASA Technical Reports Server

Advisory – Planned Maintenance: On Monday, July 15 at 9 PM Eastern the STI Compliance and Distribution Services will be performing planned maintenance on the STI Repository (NTRS) for approximately one hour. During this time users will not be able to access the STI Repository (NTRS).

Back to Results
Vertical structure of biomass burning aerosol transported over the southeast Atlantic OceanBiomass burning in southwestern Africa produces smoke plumes that are transported over the Atlantic Ocean and overlie vast regions of stratocumulus clouds. This aerosol layer contributes to direct and indirect radiative forcing of the atmosphere in this region particularly during the months of August, September, and October. There was a multi-year international campaign to study this aerosol and its interactions with clouds. Here, we report on the evolution of aerosol distributions and properties as measured by the airborne high spectral resolution lidar (HSRL-2) during the ORACLES (Observations of Aerosols above Clouds and their intEractionS) campaign in September 2016. The NASA Langley HSRL-2 instrument was flown on the NASA ER-2 aircraft for several days in September 2016. Data were aggregated at two pairs of 2° × 2° grid boxes to examine the evolution of the vertical profile of aerosol properties during transport over the ocean. Results showed that the structure of the profile of aerosol extinction and microphysical properties is maintained over a 1 to 2 d timescale. In the 3–5 km altitude range, 95 % of the aerosol extinction was contributed by particles in the 0.05–0.50 µm radius size range with the aerosol in this size range having an average effective radius of 0.16 µm. This indicates that there is essentially no scavenging or dry deposition at these altitudes. Moreover, there is very little day-to-day variation in these properties, such that time sampling as happens in such campaigns may be representative of longer periods such as monthly means. Below 3 km, there is considerable mixing with larger aerosol, most likely continental source near land. Furthermore, these measurements indicated that there was often a distinct gap between the bottom of the aerosol layer and cloud tops at the selected locations as evidenced by a layer of several hundred meters that contained relatively low aerosol extinction values above the clouds.
Document ID
20220011479
Acquisition Source
Langley Research Center
Document Type
Accepted Manuscript (Version with final changes)
Authors
Harshvardhan Harshvardhan ORCID
(Purdue University West Lafayette West Lafayette, Indiana, United States)
Richard Ferrare
(Langley Research Center Hampton, Virginia, United States)
Sharon Burton
(Langley Research Center Hampton, Virginia, United States)
Johnathan Hair
(Langley Research Center Hampton, Virginia, United States)
Chris Hostetler
(Langley Research Center Hampton, Virginia, United States)
David Harper
(Langley Research Center Hampton, Virginia, United States)
Anthony Cook
(Langley Research Center Hampton, Virginia, United States)
Marta Fenn
(Science Systems and Applications (United States) Lanham, Maryland, United States)
Amy Jo Scarino
(Science Systems and Applications (United States) Lanham, Maryland, United States)
Eduard Chemyakin
(Science Systems and Applications (United States) Lanham, Maryland, United States)
Detlef Müller ORCID
(University of Hertfordshire Hatfield, United Kingdom)
Date Acquired
July 29, 2022
Publication Date
August 3, 2022
Publication Information
Publication: Atmospheric Chemistry and Physics
Publisher: European Geosciences Union / Copernicus Publications
Volume: 22
Issue: 15
Issue Publication Date: August 1, 2022
ISSN: 1680-7316
e-ISSN: 1680-7324
Subject Category
Meteorology And Climatology
Earth Resources And Remote Sensing
Funding Number(s)
WBS: 281945.02.80.01.44
CONTRACT_GRANT: NNL16AA05C
CONTRACT_GRANT: EVS-2 13-EVS2-13-0028
Distribution Limits
Public
Copyright
Use by or on behalf of the US Gov. Permitted.
Keywords
lidar
aerosol
biomass burning
No Preview Available