El Niño–Global Atmospheric Oscillation as the Main Mode of Interannual Climate Variability

The interannual variability of the global mean monthly anomalies of near-surface air temperature, sea-level pressure, wind speed near the surface, amount of precipitation and total cloudiness was investigated. The amplitudes of the anomalies of these hydrometeorological characteristics between oppos...

Full description

Bibliographic Details
Published in:Atmosphere
Main Authors: Ilya V. Serykh, Dmitry M. Sonechkin
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2021
Subjects:
Online Access:https://doi.org/10.3390/atmos12111443
https://doaj.org/article/8ca38cda698e46b6ae76b00ce9f2737c
id ftdoajarticles:oai:doaj.org/article:8ca38cda698e46b6ae76b00ce9f2737c
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:8ca38cda698e46b6ae76b00ce9f2737c 2023-05-15T15:04:34+02:00 El Niño–Global Atmospheric Oscillation as the Main Mode of Interannual Climate Variability Ilya V. Serykh Dmitry M. Sonechkin 2021-11-01T00:00:00Z https://doi.org/10.3390/atmos12111443 https://doaj.org/article/8ca38cda698e46b6ae76b00ce9f2737c EN eng MDPI AG https://www.mdpi.com/2073-4433/12/11/1443 https://doaj.org/toc/2073-4433 doi:10.3390/atmos12111443 2073-4433 https://doaj.org/article/8ca38cda698e46b6ae76b00ce9f2737c Atmosphere, Vol 12, Iss 1443, p 1443 (2021) El Niño–Southern Oscillation Global Atmospheric Oscillation near-surface air temperature sea-level pressure wind speed precipitation Meteorology. Climatology QC851-999 article 2021 ftdoajarticles https://doi.org/10.3390/atmos12111443 2022-12-31T06:46:23Z The interannual variability of the global mean monthly anomalies of near-surface air temperature, sea-level pressure, wind speed near the surface, amount of precipitation and total cloudiness was investigated. The amplitudes of the anomalies of these hydrometeorological characteristics between opposite phases of the Global Atmospheric Oscillation (GAO) were calculated. The regional element of the GAO in the tropics of the Indian and Pacific Oceans is the Southern Oscillation. The results show that the oscillations of these characteristics are associated with the GAO not only in the tropical belt of the Earth but also in the middle and high latitudes, especially in the Arctic and northern Eurasia. The physical mechanism by which the transition of the GAO from the negative to the positive phase influences the weakening of the Pacific trade winds, and, as a consequence, the onset of El Niño is described. Article in Journal/Newspaper Arctic Directory of Open Access Journals: DOAJ Articles Arctic Pacific Indian Atmosphere 12 11 1443
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic El Niño–Southern Oscillation
Global Atmospheric Oscillation
near-surface air temperature
sea-level pressure
wind speed
precipitation
Meteorology. Climatology
QC851-999
spellingShingle El Niño–Southern Oscillation
Global Atmospheric Oscillation
near-surface air temperature
sea-level pressure
wind speed
precipitation
Meteorology. Climatology
QC851-999
Ilya V. Serykh
Dmitry M. Sonechkin
El Niño–Global Atmospheric Oscillation as the Main Mode of Interannual Climate Variability
topic_facet El Niño–Southern Oscillation
Global Atmospheric Oscillation
near-surface air temperature
sea-level pressure
wind speed
precipitation
Meteorology. Climatology
QC851-999
description The interannual variability of the global mean monthly anomalies of near-surface air temperature, sea-level pressure, wind speed near the surface, amount of precipitation and total cloudiness was investigated. The amplitudes of the anomalies of these hydrometeorological characteristics between opposite phases of the Global Atmospheric Oscillation (GAO) were calculated. The regional element of the GAO in the tropics of the Indian and Pacific Oceans is the Southern Oscillation. The results show that the oscillations of these characteristics are associated with the GAO not only in the tropical belt of the Earth but also in the middle and high latitudes, especially in the Arctic and northern Eurasia. The physical mechanism by which the transition of the GAO from the negative to the positive phase influences the weakening of the Pacific trade winds, and, as a consequence, the onset of El Niño is described.
format Article in Journal/Newspaper
author Ilya V. Serykh
Dmitry M. Sonechkin
author_facet Ilya V. Serykh
Dmitry M. Sonechkin
author_sort Ilya V. Serykh
title El Niño–Global Atmospheric Oscillation as the Main Mode of Interannual Climate Variability
title_short El Niño–Global Atmospheric Oscillation as the Main Mode of Interannual Climate Variability
title_full El Niño–Global Atmospheric Oscillation as the Main Mode of Interannual Climate Variability
title_fullStr El Niño–Global Atmospheric Oscillation as the Main Mode of Interannual Climate Variability
title_full_unstemmed El Niño–Global Atmospheric Oscillation as the Main Mode of Interannual Climate Variability
title_sort el niño–global atmospheric oscillation as the main mode of interannual climate variability
publisher MDPI AG
publishDate 2021
url https://doi.org/10.3390/atmos12111443
https://doaj.org/article/8ca38cda698e46b6ae76b00ce9f2737c
geographic Arctic
Pacific
Indian
geographic_facet Arctic
Pacific
Indian
genre Arctic
genre_facet Arctic
op_source Atmosphere, Vol 12, Iss 1443, p 1443 (2021)
op_relation https://www.mdpi.com/2073-4433/12/11/1443
https://doaj.org/toc/2073-4433
doi:10.3390/atmos12111443
2073-4433
https://doaj.org/article/8ca38cda698e46b6ae76b00ce9f2737c
op_doi https://doi.org/10.3390/atmos12111443
container_title Atmosphere
container_volume 12
container_issue 11
container_start_page 1443
_version_ 1766336317315088384