How Long Is Too Long? Variogram Analysis of AERONET Data to Aid Aerosol Validation and Intercomparison Studies
Abstract Geophysical data sets derived from satellite sensors, ground/airborne instrumentation, and computational models are often compared against each other. A common example is the validation of satellite aerosol optical depth (AOD) retrievals against measurements from Aerosol Robotic Network (AE...
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ftdoajarticles:oai:doaj.org/article:7ea57009360040c4b41071c99e87af5f 2023-05-15T13:06:38+02:00 How Long Is Too Long? Variogram Analysis of AERONET Data to Aid Aerosol Validation and Intercomparison Studies Andrew M. Sayer 2020-09-01T00:00:00Z https://doi.org/10.1029/2020EA001290 https://doaj.org/article/7ea57009360040c4b41071c99e87af5f EN eng American Geophysical Union (AGU) https://doi.org/10.1029/2020EA001290 https://doaj.org/toc/2333-5084 2333-5084 doi:10.1029/2020EA001290 https://doaj.org/article/7ea57009360040c4b41071c99e87af5f Earth and Space Science, Vol 7, Iss 9, Pp n/a-n/a (2020) aerosol variogram validation time series AERONET Astronomy QB1-991 Geology QE1-996.5 article 2020 ftdoajarticles https://doi.org/10.1029/2020EA001290 2022-12-31T10:21:06Z Abstract Geophysical data sets derived from satellite sensors, ground/airborne instrumentation, and computational models are often compared against each other. A common example is the validation of satellite aerosol optical depth (AOD) retrievals against measurements from Aerosol Robotic Network (AERONET) Sun photometers. Spatiotemporal mismatch between data set sampling means that uncaptured variation in the underlying geophysical field introduces apparent disagreement into such comparisons, known as representation or collocation matchup uncertainty. This study uses variogram analysis of AERONET data to estimate temporal mismatch uncertainties and decorrelation time scales for the global AERONET record. As well as total AOD, the fine‐ and coarse‐mode AODs, Ångström Exponent (AE), and fine‐mode fraction (FMF) of AOD are analyzed. Globally, a time difference of 30 min typically induces from 0.011–0.035 variation in AOD. For total, fine, and coarse AODs the typical time to decorrelation is around 2–10 days. For AE and FMF it is 3–33 days; that is, aerosol systems often persist significantly longer than individual events in them. Biomass burning regions tend to show the largest and fastest subdaily AOD variability and also longest times to decorrelation. Some sites show significant season‐to‐season variations in behavior. These results can be used to inform site‐specific time collocation thresholds for aerosol validation analyses and account for temporal variation when estimating data set uncertainty. They also have implications for comparisons between different satellite products or models, data aggregation, and time series analyses. Results are provided on a site‐by‐site basis to facilitate use by other researchers. Article in Journal/Newspaper Aerosol Robotic Network Directory of Open Access Journals: DOAJ Articles Earth and Space Science 7 9 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
aerosol variogram validation time series AERONET Astronomy QB1-991 Geology QE1-996.5 |
spellingShingle |
aerosol variogram validation time series AERONET Astronomy QB1-991 Geology QE1-996.5 Andrew M. Sayer How Long Is Too Long? Variogram Analysis of AERONET Data to Aid Aerosol Validation and Intercomparison Studies |
topic_facet |
aerosol variogram validation time series AERONET Astronomy QB1-991 Geology QE1-996.5 |
description |
Abstract Geophysical data sets derived from satellite sensors, ground/airborne instrumentation, and computational models are often compared against each other. A common example is the validation of satellite aerosol optical depth (AOD) retrievals against measurements from Aerosol Robotic Network (AERONET) Sun photometers. Spatiotemporal mismatch between data set sampling means that uncaptured variation in the underlying geophysical field introduces apparent disagreement into such comparisons, known as representation or collocation matchup uncertainty. This study uses variogram analysis of AERONET data to estimate temporal mismatch uncertainties and decorrelation time scales for the global AERONET record. As well as total AOD, the fine‐ and coarse‐mode AODs, Ångström Exponent (AE), and fine‐mode fraction (FMF) of AOD are analyzed. Globally, a time difference of 30 min typically induces from 0.011–0.035 variation in AOD. For total, fine, and coarse AODs the typical time to decorrelation is around 2–10 days. For AE and FMF it is 3–33 days; that is, aerosol systems often persist significantly longer than individual events in them. Biomass burning regions tend to show the largest and fastest subdaily AOD variability and also longest times to decorrelation. Some sites show significant season‐to‐season variations in behavior. These results can be used to inform site‐specific time collocation thresholds for aerosol validation analyses and account for temporal variation when estimating data set uncertainty. They also have implications for comparisons between different satellite products or models, data aggregation, and time series analyses. Results are provided on a site‐by‐site basis to facilitate use by other researchers. |
format |
Article in Journal/Newspaper |
author |
Andrew M. Sayer |
author_facet |
Andrew M. Sayer |
author_sort |
Andrew M. Sayer |
title |
How Long Is Too Long? Variogram Analysis of AERONET Data to Aid Aerosol Validation and Intercomparison Studies |
title_short |
How Long Is Too Long? Variogram Analysis of AERONET Data to Aid Aerosol Validation and Intercomparison Studies |
title_full |
How Long Is Too Long? Variogram Analysis of AERONET Data to Aid Aerosol Validation and Intercomparison Studies |
title_fullStr |
How Long Is Too Long? Variogram Analysis of AERONET Data to Aid Aerosol Validation and Intercomparison Studies |
title_full_unstemmed |
How Long Is Too Long? Variogram Analysis of AERONET Data to Aid Aerosol Validation and Intercomparison Studies |
title_sort |
how long is too long? variogram analysis of aeronet data to aid aerosol validation and intercomparison studies |
publisher |
American Geophysical Union (AGU) |
publishDate |
2020 |
url |
https://doi.org/10.1029/2020EA001290 https://doaj.org/article/7ea57009360040c4b41071c99e87af5f |
genre |
Aerosol Robotic Network |
genre_facet |
Aerosol Robotic Network |
op_source |
Earth and Space Science, Vol 7, Iss 9, Pp n/a-n/a (2020) |
op_relation |
https://doi.org/10.1029/2020EA001290 https://doaj.org/toc/2333-5084 2333-5084 doi:10.1029/2020EA001290 https://doaj.org/article/7ea57009360040c4b41071c99e87af5f |
op_doi |
https://doi.org/10.1029/2020EA001290 |
container_title |
Earth and Space Science |
container_volume |
7 |
container_issue |
9 |
_version_ |
1766014324172652544 |