Orbital and millennial northern mid-latitude westerlies over the last glacial period

The northern mid-latitude westerlies play an important role in the climate interactions between the low and high latitudes. Our understanding of the factors that control the latitudinal displacement of the westerlies remains incomplete due to insufficient climatic proxy. Here we present a latitudina...

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Published in:Climate Dynamics
Main Authors: Li, Yun, Song, Yougui, Yin, Qiuzhen, Han, Li, Wang, Yixuan
Format: Report
Language:English
Published: SPRINGER 2019
Subjects:
OSL
Online Access:http://ir.ieecas.cn/handle/361006/13533
http://ir.ieecas.cn/handle/361006/13534
https://doi.org/10.1007/s00382-019-04704-5
id ftchinacascieeca:oai:ir.ieecas.cn:361006/13534
record_format openpolar
spelling ftchinacascieeca:oai:ir.ieecas.cn:361006/13534 2023-06-11T04:12:16+02:00 Orbital and millennial northern mid-latitude westerlies over the last glacial period Li, Yun Song, Yougui Yin, Qiuzhen Han, Li Wang, Yixuan 2019-09-01 http://ir.ieecas.cn/handle/361006/13533 http://ir.ieecas.cn/handle/361006/13534 https://doi.org/10.1007/s00382-019-04704-5 英语 eng SPRINGER CLIMATE DYNAMICS http://ir.ieecas.cn/handle/361006/13533 http://ir.ieecas.cn/handle/361006/13534 doi:10.1007/s00382-019-04704-5 Orbital Millennial Northern westerlies AMOC Precession SEA REGION CLIMATE LOESS QUARTZ OSL PRECIPITATION LUMINESCENCE INSOLATION RECORD CHINA Meteorology & Atmospheric Sciences 期刊论文 2019 ftchinacascieeca https://doi.org/10.1007/s00382-019-04704-5 2023-05-08T13:24:24Z The northern mid-latitude westerlies play an important role in the climate interactions between the low and high latitudes. Our understanding of the factors that control the latitudinal displacement of the westerlies remains incomplete due to insufficient climatic proxy. Here we present a latitudinal-shift record of the westerlies in the eastern Central Asia over the past 70,000 years, on the basis of the grain size of the loess sequence from the Tacheng basin. On millennial timescale, the variation of the reconstructed westerlies resembles that of the Greenland temperature and the Atlantic meridional overturning circulation (AMOC), indicating the role of the AMOC on the westerlies. On orbital time scale, their variation is controlled by precession and insolation. Our analyses of the LOVECLIM and CCSM3 models' results show that the impact of insolation and AMOC on the latitudinal shift of the westerlies is through changing the latitudinal temperature and pressure gradients. Report Greenland Institute of Earth Environment: IEECAS OpenIR (Chinese Academy of Sciences) Greenland Climate Dynamics 53 5-6 3315 3324
institution Open Polar
collection Institute of Earth Environment: IEECAS OpenIR (Chinese Academy of Sciences)
op_collection_id ftchinacascieeca
language English
topic Orbital
Millennial
Northern westerlies
AMOC
Precession
SEA REGION
CLIMATE
LOESS
QUARTZ
OSL
PRECIPITATION
LUMINESCENCE
INSOLATION
RECORD
CHINA
Meteorology & Atmospheric Sciences
spellingShingle Orbital
Millennial
Northern westerlies
AMOC
Precession
SEA REGION
CLIMATE
LOESS
QUARTZ
OSL
PRECIPITATION
LUMINESCENCE
INSOLATION
RECORD
CHINA
Meteorology & Atmospheric Sciences
Li, Yun
Song, Yougui
Yin, Qiuzhen
Han, Li
Wang, Yixuan
Orbital and millennial northern mid-latitude westerlies over the last glacial period
topic_facet Orbital
Millennial
Northern westerlies
AMOC
Precession
SEA REGION
CLIMATE
LOESS
QUARTZ
OSL
PRECIPITATION
LUMINESCENCE
INSOLATION
RECORD
CHINA
Meteorology & Atmospheric Sciences
description The northern mid-latitude westerlies play an important role in the climate interactions between the low and high latitudes. Our understanding of the factors that control the latitudinal displacement of the westerlies remains incomplete due to insufficient climatic proxy. Here we present a latitudinal-shift record of the westerlies in the eastern Central Asia over the past 70,000 years, on the basis of the grain size of the loess sequence from the Tacheng basin. On millennial timescale, the variation of the reconstructed westerlies resembles that of the Greenland temperature and the Atlantic meridional overturning circulation (AMOC), indicating the role of the AMOC on the westerlies. On orbital time scale, their variation is controlled by precession and insolation. Our analyses of the LOVECLIM and CCSM3 models' results show that the impact of insolation and AMOC on the latitudinal shift of the westerlies is through changing the latitudinal temperature and pressure gradients.
format Report
author Li, Yun
Song, Yougui
Yin, Qiuzhen
Han, Li
Wang, Yixuan
author_facet Li, Yun
Song, Yougui
Yin, Qiuzhen
Han, Li
Wang, Yixuan
author_sort Li, Yun
title Orbital and millennial northern mid-latitude westerlies over the last glacial period
title_short Orbital and millennial northern mid-latitude westerlies over the last glacial period
title_full Orbital and millennial northern mid-latitude westerlies over the last glacial period
title_fullStr Orbital and millennial northern mid-latitude westerlies over the last glacial period
title_full_unstemmed Orbital and millennial northern mid-latitude westerlies over the last glacial period
title_sort orbital and millennial northern mid-latitude westerlies over the last glacial period
publisher SPRINGER
publishDate 2019
url http://ir.ieecas.cn/handle/361006/13533
http://ir.ieecas.cn/handle/361006/13534
https://doi.org/10.1007/s00382-019-04704-5
geographic Greenland
geographic_facet Greenland
genre Greenland
genre_facet Greenland
op_relation CLIMATE DYNAMICS
http://ir.ieecas.cn/handle/361006/13533
http://ir.ieecas.cn/handle/361006/13534
doi:10.1007/s00382-019-04704-5
op_doi https://doi.org/10.1007/s00382-019-04704-5
container_title Climate Dynamics
container_volume 53
container_issue 5-6
container_start_page 3315
op_container_end_page 3324
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