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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doaj-44144fc3cc144469a034c28112a286142020-11-25T00:03:31ZengMDPI AGAtmosphere2073-44332019-02-011029210.3390/atmos10020092atmos10020092Changes in Global Blocking Character in Recent DecadesAnthony R. Lupo0Andrew D. Jensen1Igor I. Mokhov2Alexander V. Timazhev3Timothy Eichler4Bahtiyar Efe5Atmospheric Science Program, School of Natural Resources, University of Missouri, Columbia, MO 65211, USADepartment of Mathematics and Meteorology, Northland College, Ashland, WI 54806, USAA.M. Obukhov Institute of Atmospheric Physics, Russian Academy of Science, 3 Pyzhevsky, Moscow 119017, RussiaA.M. Obukhov Institute of Atmospheric Physics, Russian Academy of Science, 3 Pyzhevsky, Moscow 119017, RussiaDepartment of Geosciences, University of Arkansas, Fayetteville, AR 72701, USAAtmospheric Science Program, School of Natural Resources, University of Missouri, Columbia, MO 65211, USAA 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.https://www.mdpi.com/2073-4433/10/2/92blockingENSOclimate changeinterdecadal variabilityPacific Decadal OscillationNorth Atlantic OscillationAtlantic Multidecadal Oscillation |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Anthony R. Lupo Andrew D. Jensen Igor I. Mokhov Alexander V. Timazhev Timothy Eichler Bahtiyar Efe |
spellingShingle |
Anthony R. Lupo Andrew D. Jensen Igor I. Mokhov Alexander V. Timazhev Timothy Eichler Bahtiyar Efe Changes in Global Blocking Character in Recent Decades Atmosphere blocking ENSO climate change interdecadal variability Pacific Decadal Oscillation North Atlantic Oscillation Atlantic Multidecadal Oscillation |
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 |
MDPI AG |
series |
Atmosphere |
issn |
2073-4433 |
publishDate |
2019-02-01 |
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. |
topic |
blocking ENSO climate change interdecadal variability Pacific Decadal Oscillation North Atlantic Oscillation Atlantic Multidecadal Oscillation |
url |
https://www.mdpi.com/2073-4433/10/2/92 |
work_keys_str_mv |
AT anthonyrlupo changesinglobalblockingcharacterinrecentdecades AT andrewdjensen changesinglobalblockingcharacterinrecentdecades AT igorimokhov changesinglobalblockingcharacterinrecentdecades AT alexandervtimazhev changesinglobalblockingcharacterinrecentdecades AT timothyeichler changesinglobalblockingcharacterinrecentdecades AT bahtiyarefe changesinglobalblockingcharacterinrecentdecades |
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