The quality of data from the National Science Foundation's UV Monitoring Network for Polar Regions

The U.S. National Science Foundation’s network for monitoring UV radiation in polar regions is now in its 15th year of operation. During this period, the deployed SUV-100 spectroradiometers have repeatedly been modified, and data processing methods have been changed. These modifications have continu...

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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.559.8269
http://uv.biospherical.com/presentations/SPIE_conference_China 2002.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.559.8269 2023-05-15T13:37:45+02:00 The quality of data from the National Science Foundation's UV Monitoring Network for Polar Regions The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.559.8269 http://uv.biospherical.com/presentations/SPIE_conference_China 2002.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.559.8269 http://uv.biospherical.com/presentations/SPIE_conference_China 2002.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://uv.biospherical.com/presentations/SPIE_conference_China 2002.pdf Solar ultraviolet radiation Antarctica QA/QC cosine correction text ftciteseerx 2016-01-08T11:57:04Z The U.S. National Science Foundation’s network for monitoring UV radiation in polar regions is now in its 15th year of operation. During this period, the deployed SUV-100 spectroradiometers have repeatedly been modified, and data processing methods have been changed. These modifications have continuously improved the quality of published data, but have also introduced step-changes into the data set. For example, a change of the wavelength calibration method in 1997 has improved the wavelength accuracy to ±0.04 nm (±1σ), but also lead to a step of 2-4 % in published biological dose rates. In order to best assess long-term changes in UV at network locations, it is desirable to remove these steps and to homogenize the data set. This publication discusses possible ways to accomplish these objectives, with special emphasis on absolute calibration, wavelength accuracy, and the cosine error. To date, published data are not corrected for the instruments ’ cosine errors. Such corrections are not straightforward, as older data are affected by an azimuth asymmetry of the irradiance collector, which was not constant over the years. A new method to correct the errors for both clear and cloudy sky conditions was developed, and is described here. Results indicate that dose rates published prior to the year 2000 are low by 2-5%, and exhibit a variation with the Sun’s azimuth angle. By modifying the instruments ’ irradiance collectors in 2000, the azimuth asymmetry was virtually eliminated, however, the modification also lead to a step-change of about 3 % in published data. The ability of the new correction algorithm to Text Antarc* Antarctica Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic Solar ultraviolet radiation
Antarctica
QA/QC
cosine correction
spellingShingle Solar ultraviolet radiation
Antarctica
QA/QC
cosine correction
The quality of data from the National Science Foundation's UV Monitoring Network for Polar Regions
topic_facet Solar ultraviolet radiation
Antarctica
QA/QC
cosine correction
description The U.S. National Science Foundation’s network for monitoring UV radiation in polar regions is now in its 15th year of operation. During this period, the deployed SUV-100 spectroradiometers have repeatedly been modified, and data processing methods have been changed. These modifications have continuously improved the quality of published data, but have also introduced step-changes into the data set. For example, a change of the wavelength calibration method in 1997 has improved the wavelength accuracy to ±0.04 nm (±1σ), but also lead to a step of 2-4 % in published biological dose rates. In order to best assess long-term changes in UV at network locations, it is desirable to remove these steps and to homogenize the data set. This publication discusses possible ways to accomplish these objectives, with special emphasis on absolute calibration, wavelength accuracy, and the cosine error. To date, published data are not corrected for the instruments ’ cosine errors. Such corrections are not straightforward, as older data are affected by an azimuth asymmetry of the irradiance collector, which was not constant over the years. A new method to correct the errors for both clear and cloudy sky conditions was developed, and is described here. Results indicate that dose rates published prior to the year 2000 are low by 2-5%, and exhibit a variation with the Sun’s azimuth angle. By modifying the instruments ’ irradiance collectors in 2000, the azimuth asymmetry was virtually eliminated, however, the modification also lead to a step-change of about 3 % in published data. The ability of the new correction algorithm to
author2 The Pennsylvania State University CiteSeerX Archives
format Text
title The quality of data from the National Science Foundation's UV Monitoring Network for Polar Regions
title_short The quality of data from the National Science Foundation's UV Monitoring Network for Polar Regions
title_full The quality of data from the National Science Foundation's UV Monitoring Network for Polar Regions
title_fullStr The quality of data from the National Science Foundation's UV Monitoring Network for Polar Regions
title_full_unstemmed The quality of data from the National Science Foundation's UV Monitoring Network for Polar Regions
title_sort quality of data from the national science foundation's uv monitoring network for polar regions
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.559.8269
http://uv.biospherical.com/presentations/SPIE_conference_China 2002.pdf
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genre_facet Antarc*
Antarctica
op_source http://uv.biospherical.com/presentations/SPIE_conference_China 2002.pdf
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http://uv.biospherical.com/presentations/SPIE_conference_China 2002.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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