Downward Longwave Irradiance at the Thule High Arctic Atmospheric Observatory (THAAO_DLI) ... : THAAO_DLI ...
Measurements of downward shortwave (SW) and longwave (LW) irradiances started in 2009 with the installation of one pyranometer and one pyrgeometer on the roof of building 1971 (about 5 m agl). Different models of instruments have been operated: Eppley PSP and Kipp&Zonen CMP21 pyranometers for SW...
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Agenzia Nazionale per le nuove tecnologie, l’energia e lo sviluppo economico sostenibile (ENEA)
2022
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Online Access: | https://dx.doi.org/10.13127/thaao/dli https://www.thuleatmos-it.it/dataaccess/DLI |
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ftdatacite:10.13127/thaao/dli 2023-08-27T04:07:35+02:00 Downward Longwave Irradiance at the Thule High Arctic Atmospheric Observatory (THAAO_DLI) ... : THAAO_DLI ... Meloni, Daniela Di Sarra, Alcide Di Iorio, Tatiana Pace, Giandomenico Muscari, Giovanni Iaccarino, Antonio Calì Quaglia, Filippo 2022 text/plain text/tab-separated-values https://dx.doi.org/10.13127/thaao/dli https://www.thuleatmos-it.it/dataaccess/DLI en eng Agenzia Nazionale per le nuove tecnologie, l’energia e lo sviluppo economico sostenibile (ENEA) https://dx.doi.org/10.1007/s00382-011-1280-1 https://dx.doi.org/10.4401/ag-6382 https://dx.doi.org/10.13127/thaao/dli_macmap CC BY 4.0 https://creativecommons.org/licenses/by/4.0 climate change Arctic amplification surface radiative balance cloud radiative effect dataset Downward Longwave Irradiances measured at the ground at the THAAO since 2009 Dataset 2022 ftdatacite https://doi.org/10.13127/thaao/dli10.1007/s00382-011-1280-110.4401/ag-638210.13127/thaao/dli_macmap 2023-08-07T14:24:23Z Measurements of downward shortwave (SW) and longwave (LW) irradiances started in 2009 with the installation of one pyranometer and one pyrgeometer on the roof of building 1971 (about 5 m agl). Different models of instruments have been operated: Eppley PSP and Kipp&Zonen CMP21 pyranometers for SW irradiance, and Eppley PIR and Kipp&Zonen CGR4 pyrgeometers for LW irradiance. See https://www.thuleatmos-it.it/instruments/radiometers for additional details. Radiometers are ventilated to prevent ice/dew formation on their domes. Data are recorded with a 30 second time step and are used to calculate hourly means and standard deviations. Corrections are applied to SW measurements in order to remove the thermal offset and to take into account the cosine response of each pyranometer. SW and LW irradiance measurements from Kipp&Zonen models are obtained accounting for the dependance of the radiometers’ sensitivity on temperature. Regular calibrations allow our team to monitor changes of the sensitivity with ... Dataset Arctic Climate change DataCite Metadata Store (German National Library of Science and Technology) Arctic |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
climate change Arctic amplification surface radiative balance cloud radiative effect |
spellingShingle |
climate change Arctic amplification surface radiative balance cloud radiative effect Meloni, Daniela Di Sarra, Alcide Di Iorio, Tatiana Pace, Giandomenico Muscari, Giovanni Iaccarino, Antonio Calì Quaglia, Filippo Downward Longwave Irradiance at the Thule High Arctic Atmospheric Observatory (THAAO_DLI) ... : THAAO_DLI ... |
topic_facet |
climate change Arctic amplification surface radiative balance cloud radiative effect |
description |
Measurements of downward shortwave (SW) and longwave (LW) irradiances started in 2009 with the installation of one pyranometer and one pyrgeometer on the roof of building 1971 (about 5 m agl). Different models of instruments have been operated: Eppley PSP and Kipp&Zonen CMP21 pyranometers for SW irradiance, and Eppley PIR and Kipp&Zonen CGR4 pyrgeometers for LW irradiance. See https://www.thuleatmos-it.it/instruments/radiometers for additional details. Radiometers are ventilated to prevent ice/dew formation on their domes. Data are recorded with a 30 second time step and are used to calculate hourly means and standard deviations. Corrections are applied to SW measurements in order to remove the thermal offset and to take into account the cosine response of each pyranometer. SW and LW irradiance measurements from Kipp&Zonen models are obtained accounting for the dependance of the radiometers’ sensitivity on temperature. Regular calibrations allow our team to monitor changes of the sensitivity with ... |
format |
Dataset |
author |
Meloni, Daniela Di Sarra, Alcide Di Iorio, Tatiana Pace, Giandomenico Muscari, Giovanni Iaccarino, Antonio Calì Quaglia, Filippo |
author_facet |
Meloni, Daniela Di Sarra, Alcide Di Iorio, Tatiana Pace, Giandomenico Muscari, Giovanni Iaccarino, Antonio Calì Quaglia, Filippo |
author_sort |
Meloni, Daniela |
title |
Downward Longwave Irradiance at the Thule High Arctic Atmospheric Observatory (THAAO_DLI) ... : THAAO_DLI ... |
title_short |
Downward Longwave Irradiance at the Thule High Arctic Atmospheric Observatory (THAAO_DLI) ... : THAAO_DLI ... |
title_full |
Downward Longwave Irradiance at the Thule High Arctic Atmospheric Observatory (THAAO_DLI) ... : THAAO_DLI ... |
title_fullStr |
Downward Longwave Irradiance at the Thule High Arctic Atmospheric Observatory (THAAO_DLI) ... : THAAO_DLI ... |
title_full_unstemmed |
Downward Longwave Irradiance at the Thule High Arctic Atmospheric Observatory (THAAO_DLI) ... : THAAO_DLI ... |
title_sort |
downward longwave irradiance at the thule high arctic atmospheric observatory (thaao_dli) ... : thaao_dli ... |
publisher |
Agenzia Nazionale per le nuove tecnologie, l’energia e lo sviluppo economico sostenibile (ENEA) |
publishDate |
2022 |
url |
https://dx.doi.org/10.13127/thaao/dli https://www.thuleatmos-it.it/dataaccess/DLI |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change |
genre_facet |
Arctic Climate change |
op_relation |
https://dx.doi.org/10.1007/s00382-011-1280-1 https://dx.doi.org/10.4401/ag-6382 https://dx.doi.org/10.13127/thaao/dli_macmap |
op_rights |
CC BY 4.0 https://creativecommons.org/licenses/by/4.0 |
op_doi |
https://doi.org/10.13127/thaao/dli10.1007/s00382-011-1280-110.4401/ag-638210.13127/thaao/dli_macmap |
_version_ |
1775348342065201152 |