Comparison of the Arctic upper-air temperatures from radiosonde and radio occultation observations
Air temperature is one of the most important parameters used for monitoring Arctic climate change. The Constellation Observing System for Meteorology, Ionosphere, and Climate and Formosa Satellite mission 3 (COSMIC/FORMOSAT-3) radio occultation (RO) "wet" temperature product (i.e., "w...
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ftcopernicus:oai:publications.copernicus.org:amtd53677 2023-05-15T14:36:27+02:00 Comparison of the Arctic upper-air temperatures from radiosonde and radio occultation observations Chang, Liang Guo, Lixin Feng, Guiping Wu, Xuerui Gao, Guoping 2018-08-10 application/pdf https://doi.org/10.5194/amt-2016-232 https://amt.copernicus.org/preprints/amt-2016-232/ eng eng doi:10.5194/amt-2016-232 https://amt.copernicus.org/preprints/amt-2016-232/ eISSN: 1867-8548 Text 2018 ftcopernicus https://doi.org/10.5194/amt-2016-232 2020-07-20T16:24:05Z Air temperature is one of the most important parameters used for monitoring Arctic climate change. The Constellation Observing System for Meteorology, Ionosphere, and Climate and Formosa Satellite mission 3 (COSMIC/FORMOSAT-3) radio occultation (RO) "wet" temperature product (i.e., "wetPrf") was introduced to analyze the Arctic air temperature profiles at 925–200 hPa in 2007–2012. The "wet" temperatures were further compared with radiosonde (RS) observations. Results from the spatially and temporally synchronized RS and COSMIC observations showed that their temperatures were matched well with each other, especially at 400 hPa. Comparisons of seasonal temperatures and anomalies from COSMIC and homogenized RS observations suggested the limited number of COSMIC observations during the spatial matchup may be insufficient to describe the small-scale spatial structure of temperature variations. Furthermore, comparisons of seasonal temperature anomalies from RS and 5 × 5 degree gridded COSMIC observations at 400 hPa during the sea ice minimum (SIM) of 2007 and 2012 were also made. Results revealed that the widely covered COSMIC observations can provide more details than RS observations in describing the Arctic temperature variations. Therefore, despite COSMIC observations being unsuitable to describe the Arctic temperatures in the lowest level, they provide a complementary data source to study the Arctic upper-air temperature variations and related climate change. Text Arctic Climate change Sea ice Copernicus Publications: E-Journals Arctic |
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Copernicus Publications: E-Journals |
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ftcopernicus |
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English |
description |
Air temperature is one of the most important parameters used for monitoring Arctic climate change. The Constellation Observing System for Meteorology, Ionosphere, and Climate and Formosa Satellite mission 3 (COSMIC/FORMOSAT-3) radio occultation (RO) "wet" temperature product (i.e., "wetPrf") was introduced to analyze the Arctic air temperature profiles at 925–200 hPa in 2007–2012. The "wet" temperatures were further compared with radiosonde (RS) observations. Results from the spatially and temporally synchronized RS and COSMIC observations showed that their temperatures were matched well with each other, especially at 400 hPa. Comparisons of seasonal temperatures and anomalies from COSMIC and homogenized RS observations suggested the limited number of COSMIC observations during the spatial matchup may be insufficient to describe the small-scale spatial structure of temperature variations. Furthermore, comparisons of seasonal temperature anomalies from RS and 5 × 5 degree gridded COSMIC observations at 400 hPa during the sea ice minimum (SIM) of 2007 and 2012 were also made. Results revealed that the widely covered COSMIC observations can provide more details than RS observations in describing the Arctic temperature variations. Therefore, despite COSMIC observations being unsuitable to describe the Arctic temperatures in the lowest level, they provide a complementary data source to study the Arctic upper-air temperature variations and related climate change. |
format |
Text |
author |
Chang, Liang Guo, Lixin Feng, Guiping Wu, Xuerui Gao, Guoping |
spellingShingle |
Chang, Liang Guo, Lixin Feng, Guiping Wu, Xuerui Gao, Guoping Comparison of the Arctic upper-air temperatures from radiosonde and radio occultation observations |
author_facet |
Chang, Liang Guo, Lixin Feng, Guiping Wu, Xuerui Gao, Guoping |
author_sort |
Chang, Liang |
title |
Comparison of the Arctic upper-air temperatures from radiosonde and radio occultation observations |
title_short |
Comparison of the Arctic upper-air temperatures from radiosonde and radio occultation observations |
title_full |
Comparison of the Arctic upper-air temperatures from radiosonde and radio occultation observations |
title_fullStr |
Comparison of the Arctic upper-air temperatures from radiosonde and radio occultation observations |
title_full_unstemmed |
Comparison of the Arctic upper-air temperatures from radiosonde and radio occultation observations |
title_sort |
comparison of the arctic upper-air temperatures from radiosonde and radio occultation observations |
publishDate |
2018 |
url |
https://doi.org/10.5194/amt-2016-232 https://amt.copernicus.org/preprints/amt-2016-232/ |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change Sea ice |
genre_facet |
Arctic Climate change Sea ice |
op_source |
eISSN: 1867-8548 |
op_relation |
doi:10.5194/amt-2016-232 https://amt.copernicus.org/preprints/amt-2016-232/ |
op_doi |
https://doi.org/10.5194/amt-2016-232 |
_version_ |
1766309062891274240 |