Antarctic network of lamp-calibrated multichannel radiometers for continuous ozone and uv radiation data

Three NILU-UV multichannel radiometers have been installed in 1999 at the Argentinian sites of Ushuaia (54S), Marambio (64S) and Belgrano-II (77S) in order to continuously monitor UV radiation, photosynthetically active radiation and total ozone. The measurements were established by INM, Spain in co...

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Main Authors: Redondas, A., Torres, C., Meinander, O., Lakkala, K., García, R., Cuevas, E., Ochoa, H., Deferrari, G., Díaz, S.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/acpd-8-3383-2008
https://www.atmos-chem-phys-discuss.net/acpd-2007-0654/
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spelling ftcopernicus:oai:publications.copernicus.org:acpd5061 2023-05-15T13:45:55+02:00 Antarctic network of lamp-calibrated multichannel radiometers for continuous ozone and uv radiation data Redondas, A. Torres, C. Meinander, O. Lakkala, K. García, R. Cuevas, E. Ochoa, H. Deferrari, G. Díaz, S. 2018-08-09 application/pdf https://doi.org/10.5194/acpd-8-3383-2008 https://www.atmos-chem-phys-discuss.net/acpd-2007-0654/ eng eng doi:10.5194/acpd-8-3383-2008 https://www.atmos-chem-phys-discuss.net/acpd-2007-0654/ eISSN: 1680-7324 Text 2018 ftcopernicus https://doi.org/10.5194/acpd-8-3383-2008 2019-12-24T09:58:23Z Three NILU-UV multichannel radiometers have been installed in 1999 at the Argentinian sites of Ushuaia (54S), Marambio (64S) and Belgrano-II (77S) in order to continuously monitor UV radiation, photosynthetically active radiation and total ozone. The measurements were established by INM, Spain in collaboration with FMI, Finland, DNA-IAA, Argentina and CADIC, Argentina to observe and characterize the spatial and temporal evolution of ozone and ultraviolet radiation in the Antarctic region. Special attention has been given to the quality control and quality assurance of the measurements under harsh climatological conditions. The ozone and UV time series of 2000–2006 were calibrated using a polynomial fit for lamp measurements performed every second week all year round. The gaps in these data are minimal, with almost no data missing, and the data products are available from http://www.polarvortex.org in near real time. The data products include the erythemally-weighted UV, UVB and UVA radiation, photosynthetically active radiation (PAR), total ozone (O 3 ) and a cloud parameter (CLT). For UV data, dose rates as well as daily doses are available; from these the maximum measured UV indices (UVI), during 2000–2006, were 12.0, 9.7 and 8.1 at Ushuaia, Marambio and Belgrano-II, respectively. Text Antarc* Antarctic Copernicus Publications: E-Journals Antarctic Argentina Belgrano ENVELOPE(-64.967,-64.967,-65.150,-65.150) Belgrano II ENVELOPE(-34.617,-34.617,-77.867,-77.867) Marambio ENVELOPE(-56.750,-56.750,-64.283,-64.283) The Antarctic Ushuaia ENVELOPE(-40.000,-40.000,-82.167,-82.167)
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Three NILU-UV multichannel radiometers have been installed in 1999 at the Argentinian sites of Ushuaia (54S), Marambio (64S) and Belgrano-II (77S) in order to continuously monitor UV radiation, photosynthetically active radiation and total ozone. The measurements were established by INM, Spain in collaboration with FMI, Finland, DNA-IAA, Argentina and CADIC, Argentina to observe and characterize the spatial and temporal evolution of ozone and ultraviolet radiation in the Antarctic region. Special attention has been given to the quality control and quality assurance of the measurements under harsh climatological conditions. The ozone and UV time series of 2000–2006 were calibrated using a polynomial fit for lamp measurements performed every second week all year round. The gaps in these data are minimal, with almost no data missing, and the data products are available from http://www.polarvortex.org in near real time. The data products include the erythemally-weighted UV, UVB and UVA radiation, photosynthetically active radiation (PAR), total ozone (O 3 ) and a cloud parameter (CLT). For UV data, dose rates as well as daily doses are available; from these the maximum measured UV indices (UVI), during 2000–2006, were 12.0, 9.7 and 8.1 at Ushuaia, Marambio and Belgrano-II, respectively.
format Text
author Redondas, A.
Torres, C.
Meinander, O.
Lakkala, K.
García, R.
Cuevas, E.
Ochoa, H.
Deferrari, G.
Díaz, S.
spellingShingle Redondas, A.
Torres, C.
Meinander, O.
Lakkala, K.
García, R.
Cuevas, E.
Ochoa, H.
Deferrari, G.
Díaz, S.
Antarctic network of lamp-calibrated multichannel radiometers for continuous ozone and uv radiation data
author_facet Redondas, A.
Torres, C.
Meinander, O.
Lakkala, K.
García, R.
Cuevas, E.
Ochoa, H.
Deferrari, G.
Díaz, S.
author_sort Redondas, A.
title Antarctic network of lamp-calibrated multichannel radiometers for continuous ozone and uv radiation data
title_short Antarctic network of lamp-calibrated multichannel radiometers for continuous ozone and uv radiation data
title_full Antarctic network of lamp-calibrated multichannel radiometers for continuous ozone and uv radiation data
title_fullStr Antarctic network of lamp-calibrated multichannel radiometers for continuous ozone and uv radiation data
title_full_unstemmed Antarctic network of lamp-calibrated multichannel radiometers for continuous ozone and uv radiation data
title_sort antarctic network of lamp-calibrated multichannel radiometers for continuous ozone and uv radiation data
publishDate 2018
url https://doi.org/10.5194/acpd-8-3383-2008
https://www.atmos-chem-phys-discuss.net/acpd-2007-0654/
long_lat ENVELOPE(-64.967,-64.967,-65.150,-65.150)
ENVELOPE(-34.617,-34.617,-77.867,-77.867)
ENVELOPE(-56.750,-56.750,-64.283,-64.283)
ENVELOPE(-40.000,-40.000,-82.167,-82.167)
geographic Antarctic
Argentina
Belgrano
Belgrano II
Marambio
The Antarctic
Ushuaia
geographic_facet Antarctic
Argentina
Belgrano
Belgrano II
Marambio
The Antarctic
Ushuaia
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source eISSN: 1680-7324
op_relation doi:10.5194/acpd-8-3383-2008
https://www.atmos-chem-phys-discuss.net/acpd-2007-0654/
op_doi https://doi.org/10.5194/acpd-8-3383-2008
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