Minimum aerosol layer detection sensitivities and their subsequent impacts on aerosol optical thickness retrievals in CALIPSO level 2 data products
Due to instrument sensitivities and algorithm detection limits, level 2 (L2) Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) 532 nm aerosol extinction profile retrievals are often populated with retrieval fill values (RFVs), which indicate the absence of detectable levels of aerosol wit...
Main Authors: | , , , , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2018-01-01
|
Series: | Atmospheric Measurement Techniques |
Online Access: | https://www.atmos-meas-tech.net/11/499/2018/amt-11-499-2018.pdf |
id |
doaj-c9c6d643d6a944cc9235a964239df3a9 |
---|---|
record_format |
Article |
spelling |
doaj-c9c6d643d6a944cc9235a964239df3a92020-11-24T22:33:44ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482018-01-011149951410.5194/amt-11-499-2018Minimum aerosol layer detection sensitivities and their subsequent impacts on aerosol optical thickness retrievals in CALIPSO level 2 data productsT. D. Toth0J. R. Campbell1J. S. Reid2J. L. Tackett3M. A. Vaughan4J. Zhang5J. W. Marquis6Dept. of Atmospheric Sciences, University of North Dakota, Grand Forks, ND, USAAerosol and Radiation Sciences Section, Marine Meteorology Division, Naval Research Laboratory, Monterey, CA, USAAerosol and Radiation Sciences Section, Marine Meteorology Division, Naval Research Laboratory, Monterey, CA, USAScience Systems and Applications, Inc., Hampton, VA, USANASA Langley Research Center, Hampton, VA, USADept. of Atmospheric Sciences, University of North Dakota, Grand Forks, ND, USADept. of Atmospheric Sciences, University of North Dakota, Grand Forks, ND, USADue to instrument sensitivities and algorithm detection limits, level 2 (L2) Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) 532 nm aerosol extinction profile retrievals are often populated with retrieval fill values (RFVs), which indicate the absence of detectable levels of aerosol within the profile. In this study, using 4 years (2007–2008 and 2010–2011) of CALIOP version 3 L2 aerosol data, the occurrence frequency of daytime CALIOP profiles containing all RFVs (all-RFV profiles) is studied. In the CALIOP data products, the aerosol optical thickness (AOT) of any all-RFV profile is reported as being zero, which may introduce a bias in CALIOP-based AOT climatologies. For this study, we derive revised estimates of AOT for all-RFV profiles using collocated Moderate Resolution Imaging Spectroradiometer (MODIS) Dark Target (DT) and, where available, AErosol RObotic NEtwork (AERONET) data. Globally, all-RFV profiles comprise roughly 71 % of all daytime CALIOP L2 aerosol profiles (i.e., including completely attenuated profiles), accounting for nearly half (45 %) of all daytime cloud-free L2 aerosol profiles. The mean collocated MODIS DT (AERONET) 550 nm AOT is found to be near 0.06 (0.08) for CALIOP all-RFV profiles. We further estimate a global mean aerosol extinction profile, a so-called <q>noise floor</q>, for CALIOP all-RFV profiles. The global mean CALIOP AOT is then recomputed by replacing RFV values with the derived noise-floor values for both all-RFV and non-all-RFV profiles. This process yields an improvement in the agreement of CALIOP and MODIS over-ocean AOT.https://www.atmos-meas-tech.net/11/499/2018/amt-11-499-2018.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
T. D. Toth J. R. Campbell J. S. Reid J. L. Tackett M. A. Vaughan J. Zhang J. W. Marquis |
spellingShingle |
T. D. Toth J. R. Campbell J. S. Reid J. L. Tackett M. A. Vaughan J. Zhang J. W. Marquis Minimum aerosol layer detection sensitivities and their subsequent impacts on aerosol optical thickness retrievals in CALIPSO level 2 data products Atmospheric Measurement Techniques |
author_facet |
T. D. Toth J. R. Campbell J. S. Reid J. L. Tackett M. A. Vaughan J. Zhang J. W. Marquis |
author_sort |
T. D. Toth |
title |
Minimum aerosol layer detection sensitivities and their subsequent impacts on aerosol optical thickness retrievals in CALIPSO level 2 data products |
title_short |
Minimum aerosol layer detection sensitivities and their subsequent impacts on aerosol optical thickness retrievals in CALIPSO level 2 data products |
title_full |
Minimum aerosol layer detection sensitivities and their subsequent impacts on aerosol optical thickness retrievals in CALIPSO level 2 data products |
title_fullStr |
Minimum aerosol layer detection sensitivities and their subsequent impacts on aerosol optical thickness retrievals in CALIPSO level 2 data products |
title_full_unstemmed |
Minimum aerosol layer detection sensitivities and their subsequent impacts on aerosol optical thickness retrievals in CALIPSO level 2 data products |
title_sort |
minimum aerosol layer detection sensitivities and their subsequent impacts on aerosol optical thickness retrievals in calipso level 2 data products |
publisher |
Copernicus Publications |
series |
Atmospheric Measurement Techniques |
issn |
1867-1381 1867-8548 |
publishDate |
2018-01-01 |
description |
Due to instrument sensitivities and algorithm detection limits, level 2 (L2)
Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) 532 nm aerosol
extinction profile retrievals are often populated with retrieval fill values
(RFVs), which indicate the absence of detectable levels of aerosol within
the profile. In this study, using 4 years (2007–2008 and 2010–2011) of
CALIOP version 3 L2 aerosol data, the occurrence frequency of daytime CALIOP
profiles containing all RFVs (all-RFV profiles) is studied. In the CALIOP
data products, the aerosol optical thickness (AOT) of any all-RFV profile is
reported as being zero, which may introduce a bias in CALIOP-based AOT
climatologies. For this study, we derive revised estimates of AOT for
all-RFV profiles using collocated Moderate Resolution Imaging
Spectroradiometer (MODIS) Dark Target (DT) and, where available, AErosol RObotic NEtwork (AERONET) data. Globally, all-RFV profiles comprise roughly
71 % of all daytime CALIOP L2 aerosol profiles (i.e., including completely
attenuated profiles), accounting for nearly half (45 %) of all daytime cloud-free L2 aerosol profiles. The mean collocated MODIS DT (AERONET) 550 nm AOT is found to be near 0.06 (0.08) for CALIOP all-RFV profiles. We
further estimate a global mean aerosol extinction profile, a so-called
<q>noise floor</q>, for CALIOP all-RFV profiles. The global mean CALIOP AOT is
then recomputed by replacing RFV values with the derived noise-floor values
for both all-RFV and non-all-RFV profiles. This process yields an
improvement in the agreement of CALIOP and MODIS over-ocean AOT. |
url |
https://www.atmos-meas-tech.net/11/499/2018/amt-11-499-2018.pdf |
work_keys_str_mv |
AT tdtoth minimumaerosollayerdetectionsensitivitiesandtheirsubsequentimpactsonaerosolopticalthicknessretrievalsincalipsolevel2dataproducts AT jrcampbell minimumaerosollayerdetectionsensitivitiesandtheirsubsequentimpactsonaerosolopticalthicknessretrievalsincalipsolevel2dataproducts AT jsreid minimumaerosollayerdetectionsensitivitiesandtheirsubsequentimpactsonaerosolopticalthicknessretrievalsincalipsolevel2dataproducts AT jltackett minimumaerosollayerdetectionsensitivitiesandtheirsubsequentimpactsonaerosolopticalthicknessretrievalsincalipsolevel2dataproducts AT mavaughan minimumaerosollayerdetectionsensitivitiesandtheirsubsequentimpactsonaerosolopticalthicknessretrievalsincalipsolevel2dataproducts AT jzhang minimumaerosollayerdetectionsensitivitiesandtheirsubsequentimpactsonaerosolopticalthicknessretrievalsincalipsolevel2dataproducts AT jwmarquis minimumaerosollayerdetectionsensitivitiesandtheirsubsequentimpactsonaerosolopticalthicknessretrievalsincalipsolevel2dataproducts |
_version_ |
1725729560385814528 |