Trends and variability of cloud fraction cover in the Arctic, 1982–2009
Climatology, trends and variability of cloud fraction cover (CFC) data over the Arctic (north of 70°N), were analysed over the 1982–2009 period. Data, available from the Climate Monitoring Satellite Application Facility (CM SAF), are derived from satellite measurements by AVHRR. Climatological means...
Published in: | Theoretical and Applied Climatology |
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ftunivmodena:oai:iris.unimore.it:11380/1138905 2024-04-14T08:06:46+00:00 Trends and variability of cloud fraction cover in the Arctic, 1982–2009 BOCCOLARI, Mauro Parmiggiani, Flavio Boccolari, Mauro Parmiggiani, Flavio 2018 http://hdl.handle.net/11380/1138905 https://doi.org/10.1007/s00704-017-2125-6 http://link.springer.de/link/service/journals/00704/ eng eng info:eu-repo/semantics/altIdentifier/wos/WOS:000430539000005 volume:132 issue:3-4 firstpage:739 lastpage:749 numberofpages:11 journal:THEORETICAL AND APPLIED CLIMATOLOGY http://hdl.handle.net/11380/1138905 doi:10.1007/s00704-017-2125-6 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85017633617 http://link.springer.de/link/service/journals/00704/ info:eu-repo/semantics/closedAccess Atmospheric Science info:eu-repo/semantics/article 2018 ftunivmodena https://doi.org/10.1007/s00704-017-2125-6 2024-03-21T17:42:04Z Climatology, trends and variability of cloud fraction cover (CFC) data over the Arctic (north of 70°N), were analysed over the 1982–2009 period. Data, available from the Climate Monitoring Satellite Application Facility (CM SAF), are derived from satellite measurements by AVHRR. Climatological means confirm permanent high CFC values over the Atlantic sector during all the year and during summer over the eastern Arctic Ocean. Lower values are found in the rest of the analysed area especially over Greenland and the Canadian Archipelago, nearly continuously during all the months. These results are confirmed by CFC trends and variability. Statistically significant trends were found during all the months over the Greenland Sea, particularly during the winter season (negative, less than −5 % dec−1) and over the Beaufort Sea in spring (positive, more than +5 % dec−1). CFC variability, investigated by the Empirical Orthogonal Functions, shows a substantial “non-variability” in the Northern Atlantic Ocean. Statistically significant correlations between CFC principal components elements and both the Pacific Decadal Oscillation index and Pacific North America patterns are found. Article in Journal/Newspaper Arctic Arctic Ocean Beaufort Sea Canadian Archipelago Greenland Greenland Sea Archivio della ricerca dell'Università di Modena e Reggio Emilia (Unimore: IRIS) Arctic Arctic Ocean Greenland Pacific Theoretical and Applied Climatology 132 3-4 739 749 |
institution |
Open Polar |
collection |
Archivio della ricerca dell'Università di Modena e Reggio Emilia (Unimore: IRIS) |
op_collection_id |
ftunivmodena |
language |
English |
topic |
Atmospheric Science |
spellingShingle |
Atmospheric Science BOCCOLARI, Mauro Parmiggiani, Flavio Trends and variability of cloud fraction cover in the Arctic, 1982–2009 |
topic_facet |
Atmospheric Science |
description |
Climatology, trends and variability of cloud fraction cover (CFC) data over the Arctic (north of 70°N), were analysed over the 1982–2009 period. Data, available from the Climate Monitoring Satellite Application Facility (CM SAF), are derived from satellite measurements by AVHRR. Climatological means confirm permanent high CFC values over the Atlantic sector during all the year and during summer over the eastern Arctic Ocean. Lower values are found in the rest of the analysed area especially over Greenland and the Canadian Archipelago, nearly continuously during all the months. These results are confirmed by CFC trends and variability. Statistically significant trends were found during all the months over the Greenland Sea, particularly during the winter season (negative, less than −5 % dec−1) and over the Beaufort Sea in spring (positive, more than +5 % dec−1). CFC variability, investigated by the Empirical Orthogonal Functions, shows a substantial “non-variability” in the Northern Atlantic Ocean. Statistically significant correlations between CFC principal components elements and both the Pacific Decadal Oscillation index and Pacific North America patterns are found. |
author2 |
Boccolari, Mauro Parmiggiani, Flavio |
format |
Article in Journal/Newspaper |
author |
BOCCOLARI, Mauro Parmiggiani, Flavio |
author_facet |
BOCCOLARI, Mauro Parmiggiani, Flavio |
author_sort |
BOCCOLARI, Mauro |
title |
Trends and variability of cloud fraction cover in the Arctic, 1982–2009 |
title_short |
Trends and variability of cloud fraction cover in the Arctic, 1982–2009 |
title_full |
Trends and variability of cloud fraction cover in the Arctic, 1982–2009 |
title_fullStr |
Trends and variability of cloud fraction cover in the Arctic, 1982–2009 |
title_full_unstemmed |
Trends and variability of cloud fraction cover in the Arctic, 1982–2009 |
title_sort |
trends and variability of cloud fraction cover in the arctic, 1982–2009 |
publishDate |
2018 |
url |
http://hdl.handle.net/11380/1138905 https://doi.org/10.1007/s00704-017-2125-6 http://link.springer.de/link/service/journals/00704/ |
geographic |
Arctic Arctic Ocean Greenland Pacific |
geographic_facet |
Arctic Arctic Ocean Greenland Pacific |
genre |
Arctic Arctic Ocean Beaufort Sea Canadian Archipelago Greenland Greenland Sea |
genre_facet |
Arctic Arctic Ocean Beaufort Sea Canadian Archipelago Greenland Greenland Sea |
op_relation |
info:eu-repo/semantics/altIdentifier/wos/WOS:000430539000005 volume:132 issue:3-4 firstpage:739 lastpage:749 numberofpages:11 journal:THEORETICAL AND APPLIED CLIMATOLOGY http://hdl.handle.net/11380/1138905 doi:10.1007/s00704-017-2125-6 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85017633617 http://link.springer.de/link/service/journals/00704/ |
op_rights |
info:eu-repo/semantics/closedAccess |
op_doi |
https://doi.org/10.1007/s00704-017-2125-6 |
container_title |
Theoretical and Applied Climatology |
container_volume |
132 |
container_issue |
3-4 |
container_start_page |
739 |
op_container_end_page |
749 |
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1796303948395577344 |