An interdecadal climate dipole between Northeast Asia and Antarctica over the past five centuries

Keyan Fang, Deliang Chen, Zhengtang Guo, Yan Zhao, David Frank, Maosheng He, Feifei Zhou, Feng Shi, Heikki Seppä, Peng Zhang, Raphael Neukom

Tutkimustuotos: ArtikkelijulkaisuArtikkeliTieteellinenvertaisarvioitu

Kuvaus

Climate models emphasize the need to investigate inter-hemispheric climatic interactions. However, these models often underestimate the inter-hemispheric differences in climate change. With the wide application of reanalysis data since 1948, we identified a dipole pattern between the geopotential heights (GPHs) in Northeast Asia and Antarctica on the interdecadal scale in boreal summer. This Northeast Asia/Antarctica (NAA) dipole pattern is not conspicuous on the interannual scale, probably in that the interannual inter-hemispheric climate interaction is masked by strong interannual signals in the tropics associated with the El Nino-Southern Oscillation (ENSO). Unfortunately, the instrumental records are not sufficiently long-lasting to detect the interdecadal variability of the NAA. We thus reconstructed GPHs since 1565, making using the proxy records mostly from tree rings in Northeast Asia and ice cores from Antarctica. The strength of the NAA is time-varying and it is most conspicuous in the eighteenth century and after the late twentieth century. The strength of the NAA matches well with the variations of the solar radiation and tends to increase in along with its enhancement. In boreal summer, enhanced heating associated with high solar radiation in the Northern Hemisphere drives more air masses from the South to the North. This inter-hemispheric interaction is particularly strong in East Asia as a result of the Asian summer monsoon. Northeast Asia and Antarctica appear to be the key regions responsible for inter-hemispheric interactions on the interdecadal scale in boreal summer since they are respectively located at the front and the end of this inter-hemispheric trajectory.

Alkuperäiskielienglanti
LehtiClimate dynamics : observational, theoretical and computational research on the climate system
Vuosikerta52
Numero1-2
Sivut765–775
Sivumäärä11
ISSN0930-7575
DOI - pysyväislinkit
TilaJulkaistu - tammikuuta 2019
OKM-julkaisutyyppiA1 Alkuperäisartikkeli tieteellisessä aikakauslehdessä, vertaisarvioitu

Tieteenalat

  • 1171 Geotieteet

Lainaa tätä

Fang, Keyan ; Chen, Deliang ; Guo, Zhengtang ; Zhao, Yan ; Frank, David ; He, Maosheng ; Zhou, Feifei ; Shi, Feng ; Seppä, Heikki ; Zhang, Peng ; Neukom, Raphael. / An interdecadal climate dipole between Northeast Asia and Antarctica over the past five centuries. Julkaisussa: Climate dynamics : observational, theoretical and computational research on the climate system. 2019 ; Vuosikerta 52, Nro 1-2. Sivut 765–775.
@article{871afbbb3f9246798205ca2218a398d8,
title = "An interdecadal climate dipole between Northeast Asia and Antarctica over the past five centuries",
abstract = "Climate models emphasize the need to investigate inter-hemispheric climatic interactions. However, these models often underestimate the inter-hemispheric differences in climate change. With the wide application of reanalysis data since 1948, we identified a dipole pattern between the geopotential heights (GPHs) in Northeast Asia and Antarctica on the interdecadal scale in boreal summer. This Northeast Asia/Antarctica (NAA) dipole pattern is not conspicuous on the interannual scale, probably in that the interannual inter-hemispheric climate interaction is masked by strong interannual signals in the tropics associated with the El Nino-Southern Oscillation (ENSO). Unfortunately, the instrumental records are not sufficiently long-lasting to detect the interdecadal variability of the NAA. We thus reconstructed GPHs since 1565, making using the proxy records mostly from tree rings in Northeast Asia and ice cores from Antarctica. The strength of the NAA is time-varying and it is most conspicuous in the eighteenth century and after the late twentieth century. The strength of the NAA matches well with the variations of the solar radiation and tends to increase in along with its enhancement. In boreal summer, enhanced heating associated with high solar radiation in the Northern Hemisphere drives more air masses from the South to the North. This inter-hemispheric interaction is particularly strong in East Asia as a result of the Asian summer monsoon. Northeast Asia and Antarctica appear to be the key regions responsible for inter-hemispheric interactions on the interdecadal scale in boreal summer since they are respectively located at the front and the end of this inter-hemispheric trajectory.",
keywords = "1171 Geosciences, Interdecadal climate change, Asian summer monsoon, Climate reconstruction, Northeast Asia, Antarctica, SUMMER MONSOON, TEMPERATURE VARIABILITY, PART I, LAST, TELECONNECTION, OSCILLATION, REANALYSIS",
author = "Keyan Fang and Deliang Chen and Zhengtang Guo and Yan Zhao and David Frank and Maosheng He and Feifei Zhou and Feng Shi and Heikki Sepp{\"a} and Peng Zhang and Raphael Neukom",
year = "2019",
month = "1",
doi = "10.1007/s00382-018-4161-z",
language = "English",
volume = "52",
pages = "765–775",
journal = "Climate dynamics : observational, theoretical and computational research on the climate system",
issn = "0930-7575",
publisher = "Springer",
number = "1-2",

}

An interdecadal climate dipole between Northeast Asia and Antarctica over the past five centuries. / Fang, Keyan; Chen, Deliang; Guo, Zhengtang; Zhao, Yan; Frank, David; He, Maosheng; Zhou, Feifei; Shi, Feng; Seppä, Heikki; Zhang, Peng; Neukom, Raphael.

julkaisussa: Climate dynamics : observational, theoretical and computational research on the climate system, Vuosikerta 52, Nro 1-2, 01.2019, s. 765–775.

Tutkimustuotos: ArtikkelijulkaisuArtikkeliTieteellinenvertaisarvioitu

TY - JOUR

T1 - An interdecadal climate dipole between Northeast Asia and Antarctica over the past five centuries

AU - Fang, Keyan

AU - Chen, Deliang

AU - Guo, Zhengtang

AU - Zhao, Yan

AU - Frank, David

AU - He, Maosheng

AU - Zhou, Feifei

AU - Shi, Feng

AU - Seppä, Heikki

AU - Zhang, Peng

AU - Neukom, Raphael

PY - 2019/1

Y1 - 2019/1

N2 - Climate models emphasize the need to investigate inter-hemispheric climatic interactions. However, these models often underestimate the inter-hemispheric differences in climate change. With the wide application of reanalysis data since 1948, we identified a dipole pattern between the geopotential heights (GPHs) in Northeast Asia and Antarctica on the interdecadal scale in boreal summer. This Northeast Asia/Antarctica (NAA) dipole pattern is not conspicuous on the interannual scale, probably in that the interannual inter-hemispheric climate interaction is masked by strong interannual signals in the tropics associated with the El Nino-Southern Oscillation (ENSO). Unfortunately, the instrumental records are not sufficiently long-lasting to detect the interdecadal variability of the NAA. We thus reconstructed GPHs since 1565, making using the proxy records mostly from tree rings in Northeast Asia and ice cores from Antarctica. The strength of the NAA is time-varying and it is most conspicuous in the eighteenth century and after the late twentieth century. The strength of the NAA matches well with the variations of the solar radiation and tends to increase in along with its enhancement. In boreal summer, enhanced heating associated with high solar radiation in the Northern Hemisphere drives more air masses from the South to the North. This inter-hemispheric interaction is particularly strong in East Asia as a result of the Asian summer monsoon. Northeast Asia and Antarctica appear to be the key regions responsible for inter-hemispheric interactions on the interdecadal scale in boreal summer since they are respectively located at the front and the end of this inter-hemispheric trajectory.

AB - Climate models emphasize the need to investigate inter-hemispheric climatic interactions. However, these models often underestimate the inter-hemispheric differences in climate change. With the wide application of reanalysis data since 1948, we identified a dipole pattern between the geopotential heights (GPHs) in Northeast Asia and Antarctica on the interdecadal scale in boreal summer. This Northeast Asia/Antarctica (NAA) dipole pattern is not conspicuous on the interannual scale, probably in that the interannual inter-hemispheric climate interaction is masked by strong interannual signals in the tropics associated with the El Nino-Southern Oscillation (ENSO). Unfortunately, the instrumental records are not sufficiently long-lasting to detect the interdecadal variability of the NAA. We thus reconstructed GPHs since 1565, making using the proxy records mostly from tree rings in Northeast Asia and ice cores from Antarctica. The strength of the NAA is time-varying and it is most conspicuous in the eighteenth century and after the late twentieth century. The strength of the NAA matches well with the variations of the solar radiation and tends to increase in along with its enhancement. In boreal summer, enhanced heating associated with high solar radiation in the Northern Hemisphere drives more air masses from the South to the North. This inter-hemispheric interaction is particularly strong in East Asia as a result of the Asian summer monsoon. Northeast Asia and Antarctica appear to be the key regions responsible for inter-hemispheric interactions on the interdecadal scale in boreal summer since they are respectively located at the front and the end of this inter-hemispheric trajectory.

KW - 1171 Geosciences

KW - Interdecadal climate change

KW - Asian summer monsoon

KW - Climate reconstruction

KW - Northeast Asia

KW - Antarctica

KW - SUMMER MONSOON

KW - TEMPERATURE VARIABILITY

KW - PART I

KW - LAST

KW - TELECONNECTION

KW - OSCILLATION

KW - REANALYSIS

U2 - 10.1007/s00382-018-4161-z

DO - 10.1007/s00382-018-4161-z

M3 - Article

VL - 52

SP - 765

EP - 775

JO - Climate dynamics : observational, theoretical and computational research on the climate system

JF - Climate dynamics : observational, theoretical and computational research on the climate system

SN - 0930-7575

IS - 1-2

ER -