Contrasting aerosol refractive index and hygroscopicity in the inflow and outflow of deep convective storms: Analysis of airborne data from DC3

Sorooshian, Armin; Shingler, T.; Crosbie, E.; Barth, M. C.; Homeyer, C. R.; Campuzano‐Jost, P.; Day, D. A.; Jimenez, J. L.; Thornhill, K. L.; Ziemba, L. D.; Blake, D. R.; Fried, A.

doi:10.1002/2017jd026638

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Contrasting aerosol refractive index and hygroscopicity in the inflow and outflow of deep convective storms: Analysis of airborne data from DC3

2017
By Sorooshian, Armin ; Shingler, T. ; Crosbie, E. ; ...
Source: Journal of Geophysical Research: Atmospheres, 122(8), 4565-4577

[PDF-787.99 KB]

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Journal Title:

Journal of Geophysical Research: Atmospheres
Personal Author:

Sorooshian, Armin ; Shingler, T. ; Crosbie, E. ; Barth, M. C. ; Homeyer, C. R. ; ... More +

Sorooshian, Armin ; Shingler, T. ; Crosbie, E. ; Barth, M. C. ; Homeyer, C. R. ; Campuzano‐Jost, P. ; Day, D. A. ; Jimenez, J. L. ; Thornhill, K. L. ; Ziemba, L. D. ; Blake, D. R. ; Fried, A. Less -
NOAA Program & Office:

NESDIS (National Environmental Satellite, Data, and Information Service) ; CIRES (Cooperative Institute for Research in Environmental Sciences) ; NCEI (National Centers for Environmental Information)

NESDIS (National Environmental Satellite, Data, and Information Service) ; CIRES (Cooperative Institute for Research in Environmental Sciences) ; NCEI (National Centers for Environmental Information) Less -
Description:

We examine three case studies during the Deep Convective Clouds and Chemistry (DC3) ﬁeld experiment when storm in ﬂow and out ﬂow air were sampled for aerosol subsaturated hygroscopicity and the real part of refractive index ( n) with a Differential Aerosol Sizing and Hygroscopicity Probe (DASH-SP) on the NASA DC-8. Relative to in ﬂow aerosol particles, out ﬂow particles were more hygroscopic (by 0.03 based on the estimated κparameter) in one of the three storms examined. Two of three “control ”ﬂights with no storm convection reveal higher κvalues, albeit by only 0.02, at high altitude ( >8 km) versus <4 km. Entrainment modeling shows that measured κvalues in the out ﬂow of the three storm ﬂights are higher
Keywords:

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Atmospheric Science Earth And Planetary Sciences (miscellaneous) Geophysics Space And Planetary Science
Source:

Journal of Geophysical Research: Atmospheres, 122(8), 4565-4577
DOI:

https://doi.org/10.1002/2017jd026638
ISSN:

2169-897X;2169-8996;
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PDF
Publisher:

American Geophysical Union (AGU)
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Journal Article
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urn:sha256:443eb12475e3da4442af5c52599a2293f5df235bdeffc9f5168236de0ededb09
Download URL:

https://repository.library.noaa.gov/view/noaa/54739/noaa_54739_DS1.pdf
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