Sensitive Grain-Size Components of Last Glacial Loess on Chinese Loess Plateau and Their Response to East Asian Winter Monsoon

Chinese loess provides the most detailed terrestrial records of paleoclimate changes. We employed the grain-size components of aeolian sediments to reconstruct the history of the East Asian winter monsoon (EAWM) on the Chinese Loess Plateau (CLP). Here, using the grain-size class vs. standard deviat...

Full description

Bibliographic Details
Main Authors: Qiansuo Wang, Yougui Song, Linqiong Duan, Jinchan Li
Format: Article
Language:English
Published: MDPI AG 2023-02-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/14/2/304
_version_ 1827758693146427392
author Qiansuo Wang
Yougui Song
Linqiong Duan
Jinchan Li
author_facet Qiansuo Wang
Yougui Song
Linqiong Duan
Jinchan Li
author_sort Qiansuo Wang
collection DOAJ
description Chinese loess provides the most detailed terrestrial records of paleoclimate changes. We employed the grain-size components of aeolian sediments to reconstruct the history of the East Asian winter monsoon (EAWM) on the Chinese Loess Plateau (CLP). Here, using the grain-size class vs. standard deviation method, we extracted the environmentally sensitive grain-size components of nine last glacial loess sections. The grain-size class vs. standard deviation diagrams showed two major grain-size components (fine and coarse), which varied from section to section. Material resource distances and post-depositional pedogenesis were the main factors affecting environmentally sensitive grain-size components. The coarse grain-size components of the Yulin, Baicaoyuan, Xifeng, and Luochuan sections were influenced by the transportation distance, while we attributed the fine grain-size components of the Weinan, Shaoling, Duanjiapo, and Chaona sections to pedogenesis. At the same time, the Mianchi section’s sensitive grain-size component was also coarse, and was affected by the local circulation from the nearby Yellow River terrace. Our comparison of sensitive grain-size components and EAWM revealed that the coarse grain-size components were progressively finer along with the EAWM from the northwest to the southeast on the CLP, and they can be regarded as the most suitable proxy indicator of the EAWM on the CLP.
first_indexed 2024-03-11T09:10:02Z
format Article
id doaj.art-7b8c917dc5f54f6088ae9635b636d967
institution Directory Open Access Journal
issn 2073-4433
language English
last_indexed 2024-03-11T09:10:02Z
publishDate 2023-02-01
publisher MDPI AG
record_format Article
series Atmosphere
spelling doaj.art-7b8c917dc5f54f6088ae9635b636d9672023-11-16T19:02:58ZengMDPI AGAtmosphere2073-44332023-02-0114230410.3390/atmos14020304Sensitive Grain-Size Components of Last Glacial Loess on Chinese Loess Plateau and Their Response to East Asian Winter MonsoonQiansuo Wang0Yougui Song1Linqiong Duan2Jinchan Li3College of Land and Tourism, Luoyang Normal University, Luoyang 471934, ChinaState Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, ChinaCollege of Land and Tourism, Luoyang Normal University, Luoyang 471934, ChinaCollege of Land and Tourism, Luoyang Normal University, Luoyang 471934, ChinaChinese loess provides the most detailed terrestrial records of paleoclimate changes. We employed the grain-size components of aeolian sediments to reconstruct the history of the East Asian winter monsoon (EAWM) on the Chinese Loess Plateau (CLP). Here, using the grain-size class vs. standard deviation method, we extracted the environmentally sensitive grain-size components of nine last glacial loess sections. The grain-size class vs. standard deviation diagrams showed two major grain-size components (fine and coarse), which varied from section to section. Material resource distances and post-depositional pedogenesis were the main factors affecting environmentally sensitive grain-size components. The coarse grain-size components of the Yulin, Baicaoyuan, Xifeng, and Luochuan sections were influenced by the transportation distance, while we attributed the fine grain-size components of the Weinan, Shaoling, Duanjiapo, and Chaona sections to pedogenesis. At the same time, the Mianchi section’s sensitive grain-size component was also coarse, and was affected by the local circulation from the nearby Yellow River terrace. Our comparison of sensitive grain-size components and EAWM revealed that the coarse grain-size components were progressively finer along with the EAWM from the northwest to the southeast on the CLP, and they can be regarded as the most suitable proxy indicator of the EAWM on the CLP.https://www.mdpi.com/2073-4433/14/2/304aeoliangrain sizeatmospheric circulationlast glacial loessEast Asian winter monsoon
spellingShingle Qiansuo Wang
Yougui Song
Linqiong Duan
Jinchan Li
Sensitive Grain-Size Components of Last Glacial Loess on Chinese Loess Plateau and Their Response to East Asian Winter Monsoon
Atmosphere
aeolian
grain size
atmospheric circulation
last glacial loess
East Asian winter monsoon
title Sensitive Grain-Size Components of Last Glacial Loess on Chinese Loess Plateau and Their Response to East Asian Winter Monsoon
title_full Sensitive Grain-Size Components of Last Glacial Loess on Chinese Loess Plateau and Their Response to East Asian Winter Monsoon
title_fullStr Sensitive Grain-Size Components of Last Glacial Loess on Chinese Loess Plateau and Their Response to East Asian Winter Monsoon
title_full_unstemmed Sensitive Grain-Size Components of Last Glacial Loess on Chinese Loess Plateau and Their Response to East Asian Winter Monsoon
title_short Sensitive Grain-Size Components of Last Glacial Loess on Chinese Loess Plateau and Their Response to East Asian Winter Monsoon
title_sort sensitive grain size components of last glacial loess on chinese loess plateau and their response to east asian winter monsoon
topic aeolian
grain size
atmospheric circulation
last glacial loess
East Asian winter monsoon
url https://www.mdpi.com/2073-4433/14/2/304
work_keys_str_mv AT qiansuowang sensitivegrainsizecomponentsoflastglacialloessonchineseloessplateauandtheirresponsetoeastasianwintermonsoon
AT youguisong sensitivegrainsizecomponentsoflastglacialloessonchineseloessplateauandtheirresponsetoeastasianwintermonsoon
AT linqiongduan sensitivegrainsizecomponentsoflastglacialloessonchineseloessplateauandtheirresponsetoeastasianwintermonsoon
AT jinchanli sensitivegrainsizecomponentsoflastglacialloessonchineseloessplateauandtheirresponsetoeastasianwintermonsoon