State of the climate in 2010

Several large-scale climate patterns influenced climate conditions and weather patterns across the globe during 2010. The transition from a warm El Niño phase at the beginning of the year to a cool La Niña phase by July contributed to many notable events, ranging from record wetness across much of A...

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Published in:Bulletin of the American Meteorological Society
Main Authors: Achberger, C, Ackerman, SA, Ahlstrøm, A, Alfaro, E, Allan, R, Alves, L, Amador, J, Amelie, V, Andrianjafinirina, S, Antonov, J, Arndt, D, Ashik, I, Atheru, Z, Attaher, S, Baez, J, Banzon, V, Baringer, M, Barreira, S, Barriopedro, D, Barthia, P, Beal, L, Becker, A, Behrenfeld, M, Bell, G, Belward, A
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Online Access:https://doi.org/10.1175/1520-0477-92.6.S1
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spelling ftuloxford:oai:ora.ox.ac.uk:uuid:4a468432-f5b1-4434-9fa8-d015716fb180 2024-10-06T13:42:48+00:00 State of the climate in 2010 Achberger, C Ackerman, SA Ahlstrøm, A Alfaro, E Allan, R Alves, L Amador, J Amelie, V Andrianjafinirina, S Antonov, J Arndt, D Ashik, I Atheru, Z Attaher, S Baez, J Banzon, V Baringer, M Barreira, S Barriopedro, D Barthia, P Beal, L Becker, A Behrenfeld, M Bell, G Belward, A 2016-07-28 https://doi.org/10.1175/1520-0477-92.6.S1 https://ora.ox.ac.uk/objects/uuid:4a468432-f5b1-4434-9fa8-d015716fb180 eng eng doi:10.1175/1520-0477-92.6.S1 https://ora.ox.ac.uk/objects/uuid:4a468432-f5b1-4434-9fa8-d015716fb180 https://doi.org/10.1175/1520-0477-92.6.S1 info:eu-repo/semantics/embargoedAccess Journal article 2016 ftuloxford https://doi.org/10.1175/1520-0477-92.6.S1 2024-09-06T07:47:33Z Several large-scale climate patterns influenced climate conditions and weather patterns across the globe during 2010. The transition from a warm El Niño phase at the beginning of the year to a cool La Niña phase by July contributed to many notable events, ranging from record wetness across much of Australia to historically low Eastern Pacific basin and near-record high North Atlantic basin hurricane activity. The remaining five main hurricane basins experienced below- to well-below-normal tropical cyclone activity. The negative phase of the Arctic Oscillation was a major driver of Northern Hemisphere temperature patterns during 2009/10 winter and again in late 2010. It contributed to record snowfall and unusually low temperatures over much of northern Eurasia and parts of the United States, while bringing above-normal temperatures to the high northern latitudes. The February Arctic Oscillation Index value was the most negative since records began in 1950. The 2010 average global land and ocean surface temperature was among the two warmest years on record. The Arctic continued to warm at about twice the rate of lower latitudes. The eastern and tropical Pacific Ocean cooled about 1°C from 2009 to 2010, reflecting the transition from the 2009/10 El Niño to the 2010/11 La Niña. Ocean heat fluxes contributed to warm sea surface temperature anomalies in the North Atlantic and the tropical Indian and western Pacific Oceans. Global integrals of upper ocean heat content for the past several years have reached values consistently higher than for all prior times in the record, demonstrating the dominant role of the ocean in the Earth's energy budget. Deep and abyssal waters of Antarctic origin have also trended warmer on average since the early 1990s. Lower tropospheric temperatures typically lag ENSO surface fluctuations by two to four months, thus the 2010 temperature was dominated by the warm phase El Niño conditions that occurred during the latter half of 2009 and early 2010 and was second warmest on record. The ... Article in Journal/Newspaper Antarc* Antarctic Arctic North Atlantic ORA - Oxford University Research Archive Antarctic Arctic Indian Pacific Bulletin of the American Meteorological Society 92 6 S1 S236
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description Several large-scale climate patterns influenced climate conditions and weather patterns across the globe during 2010. The transition from a warm El Niño phase at the beginning of the year to a cool La Niña phase by July contributed to many notable events, ranging from record wetness across much of Australia to historically low Eastern Pacific basin and near-record high North Atlantic basin hurricane activity. The remaining five main hurricane basins experienced below- to well-below-normal tropical cyclone activity. The negative phase of the Arctic Oscillation was a major driver of Northern Hemisphere temperature patterns during 2009/10 winter and again in late 2010. It contributed to record snowfall and unusually low temperatures over much of northern Eurasia and parts of the United States, while bringing above-normal temperatures to the high northern latitudes. The February Arctic Oscillation Index value was the most negative since records began in 1950. The 2010 average global land and ocean surface temperature was among the two warmest years on record. The Arctic continued to warm at about twice the rate of lower latitudes. The eastern and tropical Pacific Ocean cooled about 1°C from 2009 to 2010, reflecting the transition from the 2009/10 El Niño to the 2010/11 La Niña. Ocean heat fluxes contributed to warm sea surface temperature anomalies in the North Atlantic and the tropical Indian and western Pacific Oceans. Global integrals of upper ocean heat content for the past several years have reached values consistently higher than for all prior times in the record, demonstrating the dominant role of the ocean in the Earth's energy budget. Deep and abyssal waters of Antarctic origin have also trended warmer on average since the early 1990s. Lower tropospheric temperatures typically lag ENSO surface fluctuations by two to four months, thus the 2010 temperature was dominated by the warm phase El Niño conditions that occurred during the latter half of 2009 and early 2010 and was second warmest on record. The ...
format Article in Journal/Newspaper
author Achberger, C
Ackerman, SA
Ahlstrøm, A
Alfaro, E
Allan, R
Alves, L
Amador, J
Amelie, V
Andrianjafinirina, S
Antonov, J
Arndt, D
Ashik, I
Atheru, Z
Attaher, S
Baez, J
Banzon, V
Baringer, M
Barreira, S
Barriopedro, D
Barthia, P
Beal, L
Becker, A
Behrenfeld, M
Bell, G
Belward, A
spellingShingle Achberger, C
Ackerman, SA
Ahlstrøm, A
Alfaro, E
Allan, R
Alves, L
Amador, J
Amelie, V
Andrianjafinirina, S
Antonov, J
Arndt, D
Ashik, I
Atheru, Z
Attaher, S
Baez, J
Banzon, V
Baringer, M
Barreira, S
Barriopedro, D
Barthia, P
Beal, L
Becker, A
Behrenfeld, M
Bell, G
Belward, A
State of the climate in 2010
author_facet Achberger, C
Ackerman, SA
Ahlstrøm, A
Alfaro, E
Allan, R
Alves, L
Amador, J
Amelie, V
Andrianjafinirina, S
Antonov, J
Arndt, D
Ashik, I
Atheru, Z
Attaher, S
Baez, J
Banzon, V
Baringer, M
Barreira, S
Barriopedro, D
Barthia, P
Beal, L
Becker, A
Behrenfeld, M
Bell, G
Belward, A
author_sort Achberger, C
title State of the climate in 2010
title_short State of the climate in 2010
title_full State of the climate in 2010
title_fullStr State of the climate in 2010
title_full_unstemmed State of the climate in 2010
title_sort state of the climate in 2010
publishDate 2016
url https://doi.org/10.1175/1520-0477-92.6.S1
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geographic Antarctic
Arctic
Indian
Pacific
geographic_facet Antarctic
Arctic
Indian
Pacific
genre Antarc*
Antarctic
Arctic
North Atlantic
genre_facet Antarc*
Antarctic
Arctic
North Atlantic
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https://doi.org/10.1175/1520-0477-92.6.S1
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container_title Bulletin of the American Meteorological Society
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