Horizontal variability of aerosol optical depth observed during the ARCTAS airborne experiment

We present statistics on the horizontal variability of aerosol optical depth (AOD) directly measured from the NASA P-3 aircraft. Our measurements during two contrasting phases (in Alaska and Canada) of the ARCTAS mission arguably constrain the variability in most aerosol environments common over the...

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Main Authors: Y. Shinozuka, J. Redemann
Format: Article
Language:English
Published: Copernicus Publications 2011-08-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/11/8489/2011/acp-11-8489-2011.pdf
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author Y. Shinozuka
J. Redemann
author_facet Y. Shinozuka
J. Redemann
author_sort Y. Shinozuka
collection DOAJ
description We present statistics on the horizontal variability of aerosol optical depth (AOD) directly measured from the NASA P-3 aircraft. Our measurements during two contrasting phases (in Alaska and Canada) of the ARCTAS mission arguably constrain the variability in most aerosol environments common over the globe. In the Canada phase, which features local emissions, 499 nm AOD has a median relative standard deviation (std<sub>rel, med</sub>) of 19 % and 9 % and an autocorrelation (<i>r</i>) of 0.37 and 0.71 over 20 km and 6 km horizontal segments, respectively. In the Alaska phase, which features long-range transport, the variability is considerably lower (std<sub>rel, med</sub> = 3 %, <i>r</i> = 0.92 even over 35.2 km). Compared to the magnitude of AOD, its wavelength dependence varies less in the Canada phase, more in the Alaska phase. We translate these findings from straight-line flight tracks into grid boxes and points, to help interpretation and design of satellite remote sensing, suborbital observations and transport modeling.
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spelling doaj.art-f1e06e02557640a4b033a9ac52f542ad2022-12-22T00:18:06ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242011-08-0111168489849510.5194/acp-11-8489-2011Horizontal variability of aerosol optical depth observed during the ARCTAS airborne experimentY. ShinozukaJ. RedemannWe present statistics on the horizontal variability of aerosol optical depth (AOD) directly measured from the NASA P-3 aircraft. Our measurements during two contrasting phases (in Alaska and Canada) of the ARCTAS mission arguably constrain the variability in most aerosol environments common over the globe. In the Canada phase, which features local emissions, 499 nm AOD has a median relative standard deviation (std<sub>rel, med</sub>) of 19 % and 9 % and an autocorrelation (<i>r</i>) of 0.37 and 0.71 over 20 km and 6 km horizontal segments, respectively. In the Alaska phase, which features long-range transport, the variability is considerably lower (std<sub>rel, med</sub> = 3 %, <i>r</i> = 0.92 even over 35.2 km). Compared to the magnitude of AOD, its wavelength dependence varies less in the Canada phase, more in the Alaska phase. We translate these findings from straight-line flight tracks into grid boxes and points, to help interpretation and design of satellite remote sensing, suborbital observations and transport modeling.http://www.atmos-chem-phys.net/11/8489/2011/acp-11-8489-2011.pdf
spellingShingle Y. Shinozuka
J. Redemann
Horizontal variability of aerosol optical depth observed during the ARCTAS airborne experiment
Atmospheric Chemistry and Physics
title Horizontal variability of aerosol optical depth observed during the ARCTAS airborne experiment
title_full Horizontal variability of aerosol optical depth observed during the ARCTAS airborne experiment
title_fullStr Horizontal variability of aerosol optical depth observed during the ARCTAS airborne experiment
title_full_unstemmed Horizontal variability of aerosol optical depth observed during the ARCTAS airborne experiment
title_short Horizontal variability of aerosol optical depth observed during the ARCTAS airborne experiment
title_sort horizontal variability of aerosol optical depth observed during the arctas airborne experiment
url http://www.atmos-chem-phys.net/11/8489/2011/acp-11-8489-2011.pdf
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