Satellite-derived UV climatology at Escudero station, Antarctic Peninsula

We have used data from the Ozone Monitoring Instrument (OMI) aboard NASA's Earth Observing System (EOS) Aura satellite over the period 2004-11 to describe the characteristics of surface ultraviolet (UV) irradiance at Escudero Station (62°12′S, 58°57′W). The station is located on King George Isl...

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Main Authors: Cordero, Raul R., Damiani, Alessandro, Seckmeyer, Gunther, Riechelmann, Stefan, Labbe, Fernando, Laroze, David, Garate, Fernanda
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge : Cambridge University Press 2013
Subjects:
EOS
Online Access:https://dx.doi.org/10.15488/2347
http://www.repo.uni-hannover.de/handle/123456789/2373
id ftdatacite:10.15488/2347
record_format openpolar
spelling ftdatacite:10.15488/2347 2023-05-15T13:58:59+02:00 Satellite-derived UV climatology at Escudero station, Antarctic Peninsula Cordero, Raul R. Damiani, Alessandro Seckmeyer, Gunther Riechelmann, Stefan Labbe, Fernando Laroze, David Garate, Fernanda 2013 https://dx.doi.org/10.15488/2347 http://www.repo.uni-hannover.de/handle/123456789/2373 en eng Cambridge : Cambridge University Press Es gilt deutsches Urheberrecht. Das Dokument darf zum eigenen Gebrauch kostenfrei genutzt, aber nicht im Internet bereitgestellt oder an Außenstehende weitergegeben werden. Dieser Beitrag ist aufgrund einer (DFG-geförderten) Allianz- bzw. Nationallizenz frei zugänglich. ozone satellite retrievals UV irradiance UV spectroradiometry words OMI climatology EOS irradiance optical depth satellite summer Antarctic Peninsula Antarctica King George Island South Shetland Islands West Antarctica Dewey Decimal Classification500 | Naturwissenschaften550 | Geowissenschaften Dewey Decimal Classification500 | Naturwissenschaften570 | Biowissenschaften, Biologie Other CreativeWork article 2013 ftdatacite https://doi.org/10.15488/2347 2021-11-05T12:55:41Z We have used data from the Ozone Monitoring Instrument (OMI) aboard NASA's Earth Observing System (EOS) Aura satellite over the period 2004-11 to describe the characteristics of surface ultraviolet (UV) irradiance at Escudero Station (62°12′S, 58°57′W). The station is located on King George Island (northern Antarctic Peninsula). Temperatures in summer are frequently above 0°C, and the surrounding ocean is typically ice-free. We found that the UV irradiance at Escudero is driven by the Antarctic ozone hole (which annually in spring leads to significant variations in the ozone) and by clouds (which are more frequent and have a larger optical depth compared with other Antarctic sites). The combined effect of ozone and clouds led to significant variations in the surface UV. The variability (taken as the standard deviation of the UV estimates retrieved from OMI) is typically greater than 30% at Escudero, but may reach values greater than 50% in spring. The consistency of OMI-derived data was checked by using ground-based spectral measurements carried out under controlled conditions in January 2011. © 2013 Antarctic Science Ltd. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica King George Island South Shetland Islands West Antarctica DataCite Metadata Store (German National Library of Science and Technology) Antarctic The Antarctic Antarctic Peninsula King George Island West Antarctica South Shetland Islands Dewey ENVELOPE(-64.320,-64.320,-65.907,-65.907) Escudero ENVELOPE(-64.817,-64.817,-67.317,-67.317) Escudero Station ENVELOPE(-58.963,-58.963,-62.201,-62.201)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic ozone
satellite retrievals
UV irradiance
UV spectroradiometry
words OMI
climatology
EOS
irradiance
optical depth
satellite
summer
Antarctic Peninsula
Antarctica
King George Island
South Shetland Islands
West Antarctica
Dewey Decimal Classification500 | Naturwissenschaften550 | Geowissenschaften
Dewey Decimal Classification500 | Naturwissenschaften570 | Biowissenschaften, Biologie
spellingShingle ozone
satellite retrievals
UV irradiance
UV spectroradiometry
words OMI
climatology
EOS
irradiance
optical depth
satellite
summer
Antarctic Peninsula
Antarctica
King George Island
South Shetland Islands
West Antarctica
Dewey Decimal Classification500 | Naturwissenschaften550 | Geowissenschaften
Dewey Decimal Classification500 | Naturwissenschaften570 | Biowissenschaften, Biologie
Cordero, Raul R.
Damiani, Alessandro
Seckmeyer, Gunther
Riechelmann, Stefan
Labbe, Fernando
Laroze, David
Garate, Fernanda
Satellite-derived UV climatology at Escudero station, Antarctic Peninsula
topic_facet ozone
satellite retrievals
UV irradiance
UV spectroradiometry
words OMI
climatology
EOS
irradiance
optical depth
satellite
summer
Antarctic Peninsula
Antarctica
King George Island
South Shetland Islands
West Antarctica
Dewey Decimal Classification500 | Naturwissenschaften550 | Geowissenschaften
Dewey Decimal Classification500 | Naturwissenschaften570 | Biowissenschaften, Biologie
description We have used data from the Ozone Monitoring Instrument (OMI) aboard NASA's Earth Observing System (EOS) Aura satellite over the period 2004-11 to describe the characteristics of surface ultraviolet (UV) irradiance at Escudero Station (62°12′S, 58°57′W). The station is located on King George Island (northern Antarctic Peninsula). Temperatures in summer are frequently above 0°C, and the surrounding ocean is typically ice-free. We found that the UV irradiance at Escudero is driven by the Antarctic ozone hole (which annually in spring leads to significant variations in the ozone) and by clouds (which are more frequent and have a larger optical depth compared with other Antarctic sites). The combined effect of ozone and clouds led to significant variations in the surface UV. The variability (taken as the standard deviation of the UV estimates retrieved from OMI) is typically greater than 30% at Escudero, but may reach values greater than 50% in spring. The consistency of OMI-derived data was checked by using ground-based spectral measurements carried out under controlled conditions in January 2011. © 2013 Antarctic Science Ltd.
format Article in Journal/Newspaper
author Cordero, Raul R.
Damiani, Alessandro
Seckmeyer, Gunther
Riechelmann, Stefan
Labbe, Fernando
Laroze, David
Garate, Fernanda
author_facet Cordero, Raul R.
Damiani, Alessandro
Seckmeyer, Gunther
Riechelmann, Stefan
Labbe, Fernando
Laroze, David
Garate, Fernanda
author_sort Cordero, Raul R.
title Satellite-derived UV climatology at Escudero station, Antarctic Peninsula
title_short Satellite-derived UV climatology at Escudero station, Antarctic Peninsula
title_full Satellite-derived UV climatology at Escudero station, Antarctic Peninsula
title_fullStr Satellite-derived UV climatology at Escudero station, Antarctic Peninsula
title_full_unstemmed Satellite-derived UV climatology at Escudero station, Antarctic Peninsula
title_sort satellite-derived uv climatology at escudero station, antarctic peninsula
publisher Cambridge : Cambridge University Press
publishDate 2013
url https://dx.doi.org/10.15488/2347
http://www.repo.uni-hannover.de/handle/123456789/2373
long_lat ENVELOPE(-64.320,-64.320,-65.907,-65.907)
ENVELOPE(-64.817,-64.817,-67.317,-67.317)
ENVELOPE(-58.963,-58.963,-62.201,-62.201)
geographic Antarctic
The Antarctic
Antarctic Peninsula
King George Island
West Antarctica
South Shetland Islands
Dewey
Escudero
Escudero Station
geographic_facet Antarctic
The Antarctic
Antarctic Peninsula
King George Island
West Antarctica
South Shetland Islands
Dewey
Escudero
Escudero Station
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
King George Island
South Shetland Islands
West Antarctica
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
King George Island
South Shetland Islands
West Antarctica
op_rights Es gilt deutsches Urheberrecht. Das Dokument darf zum eigenen Gebrauch kostenfrei genutzt, aber nicht im Internet bereitgestellt oder an Außenstehende weitergegeben werden. Dieser Beitrag ist aufgrund einer (DFG-geförderten) Allianz- bzw. Nationallizenz frei zugänglich.
op_doi https://doi.org/10.15488/2347
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