Asymmetric impact of Atlantic Multidecadal Oscillation on El Nino and La Nina characteristics
The long-lasting cold surface conditions of North Atlantic, i.e., the negative phase of Atlantic Multidecadal Oscillation (AMO), can intensify the El Nino-Southern Oscillation through the enhanced air-sea coupling under the increased central-to-eastern tropical Pacific mean sea surface temperature....
Published in: | Geophysical Research Letters |
---|---|
Main Authors: | , , , |
Other Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union
2015
|
Subjects: | |
Online Access: | https://oasis.postech.ac.kr/handle/2014.oak/26613 https://doi.org/10.1002/2015GL064381 |
id |
ftponangunivst:oai:oasis.postech.ac.kr:2014.oak/26613 |
---|---|
record_format |
openpolar |
spelling |
ftponangunivst:oai:oasis.postech.ac.kr:2014.oak/26613 2023-05-15T17:32:21+02:00 Asymmetric impact of Atlantic Multidecadal Oscillation on El Nino and La Nina characteristics Sung, MK An, SI Kim, BM Kug, JS 환경공학부 10112320 Kug, JS 2015-06-28 https://oasis.postech.ac.kr/handle/2014.oak/26613 https://doi.org/10.1002/2015GL064381 English eng American Geophysical Union Geophysical Research Letters 42 12 4998 5004 SCI Geosciences, Multidisciplinary Geology 0094-8276 2015-OAK-0000033522 https://oasis.postech.ac.kr/handle/2014.oak/26613 doi:10.1002/2015GL064381 17842 Geophysical Research Letters, v.42, no.12, pp.4998 - 5004 000358002500044 2-s2.0-84948712212 CLIMATE VARIABILITY CIRCULATION ENSO ANOMALIES RELEVANCE ITCZ Atlantic Multidecadal Oscillation AMO El Nino La Nina asymmetry Article ART 2015 ftponangunivst https://doi.org/10.1002/2015GL064381 2022-10-20T20:17:22Z The long-lasting cold surface conditions of North Atlantic, i.e., the negative phase of Atlantic Multidecadal Oscillation (AMO), can intensify the El Nino-Southern Oscillation through the enhanced air-sea coupling under the increased central-to-eastern tropical Pacific mean sea surface temperature. However, the impact of warmer mean sea surface temperature (SST) is more efficient in the intensifying El Nino than La Nina, because of the nature of the exponential growth of atmospheric convection to SST change. Moreover, the farther eastward shift of the atmospheric convection during the negative AMO leads to the stronger El Nino due to the longer delayed negative feedback by oceanic waves. Therefore, the AMO mainly influences the El Nino intensity rather than La Nina intensity. △ 1 1 2 2 Y scie scopus Article in Journal/Newspaper North Atlantic Pohang University of Science and Technology (POSTECH): Open Access System for Information Sharing (OASIS) Pacific Geophysical Research Letters 42 12 4998 5004 |
institution |
Open Polar |
collection |
Pohang University of Science and Technology (POSTECH): Open Access System for Information Sharing (OASIS) |
op_collection_id |
ftponangunivst |
language |
English |
topic |
CLIMATE VARIABILITY CIRCULATION ENSO ANOMALIES RELEVANCE ITCZ Atlantic Multidecadal Oscillation AMO El Nino La Nina asymmetry |
spellingShingle |
CLIMATE VARIABILITY CIRCULATION ENSO ANOMALIES RELEVANCE ITCZ Atlantic Multidecadal Oscillation AMO El Nino La Nina asymmetry Sung, MK An, SI Kim, BM Kug, JS Asymmetric impact of Atlantic Multidecadal Oscillation on El Nino and La Nina characteristics |
topic_facet |
CLIMATE VARIABILITY CIRCULATION ENSO ANOMALIES RELEVANCE ITCZ Atlantic Multidecadal Oscillation AMO El Nino La Nina asymmetry |
description |
The long-lasting cold surface conditions of North Atlantic, i.e., the negative phase of Atlantic Multidecadal Oscillation (AMO), can intensify the El Nino-Southern Oscillation through the enhanced air-sea coupling under the increased central-to-eastern tropical Pacific mean sea surface temperature. However, the impact of warmer mean sea surface temperature (SST) is more efficient in the intensifying El Nino than La Nina, because of the nature of the exponential growth of atmospheric convection to SST change. Moreover, the farther eastward shift of the atmospheric convection during the negative AMO leads to the stronger El Nino due to the longer delayed negative feedback by oceanic waves. Therefore, the AMO mainly influences the El Nino intensity rather than La Nina intensity. △ 1 1 2 2 Y scie scopus |
author2 |
환경공학부 10112320 Kug, JS |
format |
Article in Journal/Newspaper |
author |
Sung, MK An, SI Kim, BM Kug, JS |
author_facet |
Sung, MK An, SI Kim, BM Kug, JS |
author_sort |
Sung, MK |
title |
Asymmetric impact of Atlantic Multidecadal Oscillation on El Nino and La Nina characteristics |
title_short |
Asymmetric impact of Atlantic Multidecadal Oscillation on El Nino and La Nina characteristics |
title_full |
Asymmetric impact of Atlantic Multidecadal Oscillation on El Nino and La Nina characteristics |
title_fullStr |
Asymmetric impact of Atlantic Multidecadal Oscillation on El Nino and La Nina characteristics |
title_full_unstemmed |
Asymmetric impact of Atlantic Multidecadal Oscillation on El Nino and La Nina characteristics |
title_sort |
asymmetric impact of atlantic multidecadal oscillation on el nino and la nina characteristics |
publisher |
American Geophysical Union |
publishDate |
2015 |
url |
https://oasis.postech.ac.kr/handle/2014.oak/26613 https://doi.org/10.1002/2015GL064381 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
Geophysical Research Letters 42 12 4998 5004 SCI Geosciences, Multidisciplinary Geology 0094-8276 2015-OAK-0000033522 https://oasis.postech.ac.kr/handle/2014.oak/26613 doi:10.1002/2015GL064381 17842 Geophysical Research Letters, v.42, no.12, pp.4998 - 5004 000358002500044 2-s2.0-84948712212 |
op_doi |
https://doi.org/10.1002/2015GL064381 |
container_title |
Geophysical Research Letters |
container_volume |
42 |
container_issue |
12 |
container_start_page |
4998 |
op_container_end_page |
5004 |
_version_ |
1766130422587064320 |