Changes in Global Blocking Character in Recent Decades

A global blocking climatology published by this group for events that occurred during the late 20th century examined a comprehensive list of characteristics that included block intensity (BI). In addition to confirming the results of other published climatologies, they found that Northern Hemisphere...

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Published in:Atmosphere
Main Authors: Anthony R. Lupo, Andrew D. Jensen, Igor I. Mokhov, Alexander V. Timazhev, Timothy Eichler, Bahtiyar Efe
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2019
Subjects:
Online Access:https://doi.org/10.3390/atmos10020092
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spelling ftmdpi:oai:mdpi.com:/2073-4433/10/2/92/ 2023-08-20T04:08:26+02:00 Changes in Global Blocking Character in Recent Decades Anthony R. Lupo Andrew D. Jensen Igor I. Mokhov Alexander V. Timazhev Timothy Eichler Bahtiyar Efe agris 2019-02-21 application/pdf https://doi.org/10.3390/atmos10020092 EN eng Multidisciplinary Digital Publishing Institute Meteorology https://dx.doi.org/10.3390/atmos10020092 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 10; Issue 2; Pages: 92 blocking ENSO climate change interdecadal variability Pacific Decadal Oscillation North Atlantic Oscillation Atlantic Multidecadal Oscillation Text 2019 ftmdpi https://doi.org/10.3390/atmos10020092 2023-07-31T22:03:43Z A global blocking climatology published by this group for events that occurred during the late 20th century examined a comprehensive list of characteristics that included block intensity (BI). In addition to confirming the results of other published climatologies, they found that Northern Hemisphere (NH) blocking events (1968–1998) were stronger than Southern Hemisphere (SH) blocks and winter events are stronger than summer events in both hemispheres. This work also examined the interannual variability of blocking as related to El Niño and Southern Oscillation (ENSO). Since the late 20th century, there is evidence that the occurrence of blocking has increased globally. A comparison of blocking characteristics since 1998 (1998–2018 NH; 2000–2018 SH) shows that the number of blocking events and their duration have increased significantly in both hemispheres. The blocking BI has decreased by about six percent in the NH, but there was little change in the BI for the SH events. Additionally, there is little or no change in the primary genesis regions of blocking. An examination of variability related to ENSO reveals that the NH interannual-scale variations found in the earlier work has reversed in the early 21st century. This could either be the result of interdecadal variability or a change in the climate. Interdecadal variations are examined as well. Text North Atlantic North Atlantic oscillation MDPI Open Access Publishing Pacific Atmosphere 10 2 92
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic blocking
ENSO
climate change
interdecadal variability
Pacific Decadal Oscillation
North Atlantic Oscillation
Atlantic Multidecadal Oscillation
spellingShingle blocking
ENSO
climate change
interdecadal variability
Pacific Decadal Oscillation
North Atlantic Oscillation
Atlantic Multidecadal Oscillation
Anthony R. Lupo
Andrew D. Jensen
Igor I. Mokhov
Alexander V. Timazhev
Timothy Eichler
Bahtiyar Efe
Changes in Global Blocking Character in Recent Decades
topic_facet blocking
ENSO
climate change
interdecadal variability
Pacific Decadal Oscillation
North Atlantic Oscillation
Atlantic Multidecadal Oscillation
description A global blocking climatology published by this group for events that occurred during the late 20th century examined a comprehensive list of characteristics that included block intensity (BI). In addition to confirming the results of other published climatologies, they found that Northern Hemisphere (NH) blocking events (1968–1998) were stronger than Southern Hemisphere (SH) blocks and winter events are stronger than summer events in both hemispheres. This work also examined the interannual variability of blocking as related to El Niño and Southern Oscillation (ENSO). Since the late 20th century, there is evidence that the occurrence of blocking has increased globally. A comparison of blocking characteristics since 1998 (1998–2018 NH; 2000–2018 SH) shows that the number of blocking events and their duration have increased significantly in both hemispheres. The blocking BI has decreased by about six percent in the NH, but there was little change in the BI for the SH events. Additionally, there is little or no change in the primary genesis regions of blocking. An examination of variability related to ENSO reveals that the NH interannual-scale variations found in the earlier work has reversed in the early 21st century. This could either be the result of interdecadal variability or a change in the climate. Interdecadal variations are examined as well.
format Text
author Anthony R. Lupo
Andrew D. Jensen
Igor I. Mokhov
Alexander V. Timazhev
Timothy Eichler
Bahtiyar Efe
author_facet Anthony R. Lupo
Andrew D. Jensen
Igor I. Mokhov
Alexander V. Timazhev
Timothy Eichler
Bahtiyar Efe
author_sort Anthony R. Lupo
title Changes in Global Blocking Character in Recent Decades
title_short Changes in Global Blocking Character in Recent Decades
title_full Changes in Global Blocking Character in Recent Decades
title_fullStr Changes in Global Blocking Character in Recent Decades
title_full_unstemmed Changes in Global Blocking Character in Recent Decades
title_sort changes in global blocking character in recent decades
publisher Multidisciplinary Digital Publishing Institute
publishDate 2019
url https://doi.org/10.3390/atmos10020092
op_coverage agris
geographic Pacific
geographic_facet Pacific
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Atmosphere; Volume 10; Issue 2; Pages: 92
op_relation Meteorology
https://dx.doi.org/10.3390/atmos10020092
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos10020092
container_title Atmosphere
container_volume 10
container_issue 2
container_start_page 92
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