Xiaoen Zhao , Mao Hu , Feng Chen , Shijie Wang , Tiyuan Hou
{"title":"年代际太平洋涛动驱动的太平洋Walker环流对过去500年华北季风边缘区降水变率的影响","authors":"Xiaoen Zhao , Mao Hu , Feng Chen , Shijie Wang , Tiyuan Hou","doi":"10.1016/j.gloplacha.2025.104913","DOIUrl":null,"url":null,"abstract":"<div><div>The Asian Summer Monsoon system has exerted significant impact on the ecological environment and socio-economic development of North China. Understanding the variability of monsoon precipitation and its underlying drivers in the context of anthropogenic warming necessitates the development of high-resolution precipitation reconstructions extending beyond the instrumental record. This study presents a novel tree ring network comprising 869 cores from 12 site chronologies in the North China Monsoon Marginal Region (NCMMR). A Nested Principal Component Regression model is used to reconstruct August-to-July precipitation variability from 1512 to 2021. The results indicate that, compared to the preceding five centuries, the probability of extreme high and low precipitation events increased by ∼9 % and ∼ 2 %, respectively, during the Current Warming Period (CWP, 1850–2021), with a higher long-term mean precipitation of 465.39 mm. The standard deviation and coefficient of variation for precipitation during the CWP (48.24 mm and 10.36 %, respectively) exceed those of the Historical Period (1512–1849) (36.89 mm and 8.07 %, respectively), highlighting an increase in precipitation variability over time. Analysis of global sea surface temperature patterns reveals a strong linkage between precipitation and the Interdecadal Pacific Oscillation (IPO). This is supported by a significant negative correlation between precipitation and the IPO index (<em>P</em> < 0.001), alongside the IPO's substantial contribution (25 % of explained variance) to precipitation variability. Additionally, precipitation exhibits a significant positive correlation with the Pacific Walker Circulation (PWC) index (<em>P</em> < 0.001). Climate model simulations further demonstrate that IPO-driven variations in PWC intensity regulate interdecadal precipitation variability in the NCMMR using water vapor transport anomalies.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"253 ","pages":"Article 104913"},"PeriodicalIF":4.0000,"publicationDate":"2025-06-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Impact of Pacific Walker Circulation driven by Interdecadal Pacific Oscillation on precipitation variability in the North China Monsoon Marginal Region over the past five centuries\",\"authors\":\"Xiaoen Zhao , Mao Hu , Feng Chen , Shijie Wang , Tiyuan Hou\",\"doi\":\"10.1016/j.gloplacha.2025.104913\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The Asian Summer Monsoon system has exerted significant impact on the ecological environment and socio-economic development of North China. Understanding the variability of monsoon precipitation and its underlying drivers in the context of anthropogenic warming necessitates the development of high-resolution precipitation reconstructions extending beyond the instrumental record. This study presents a novel tree ring network comprising 869 cores from 12 site chronologies in the North China Monsoon Marginal Region (NCMMR). A Nested Principal Component Regression model is used to reconstruct August-to-July precipitation variability from 1512 to 2021. The results indicate that, compared to the preceding five centuries, the probability of extreme high and low precipitation events increased by ∼9 % and ∼ 2 %, respectively, during the Current Warming Period (CWP, 1850–2021), with a higher long-term mean precipitation of 465.39 mm. The standard deviation and coefficient of variation for precipitation during the CWP (48.24 mm and 10.36 %, respectively) exceed those of the Historical Period (1512–1849) (36.89 mm and 8.07 %, respectively), highlighting an increase in precipitation variability over time. Analysis of global sea surface temperature patterns reveals a strong linkage between precipitation and the Interdecadal Pacific Oscillation (IPO). This is supported by a significant negative correlation between precipitation and the IPO index (<em>P</em> < 0.001), alongside the IPO's substantial contribution (25 % of explained variance) to precipitation variability. Additionally, precipitation exhibits a significant positive correlation with the Pacific Walker Circulation (PWC) index (<em>P</em> < 0.001). Climate model simulations further demonstrate that IPO-driven variations in PWC intensity regulate interdecadal precipitation variability in the NCMMR using water vapor transport anomalies.</div></div>\",\"PeriodicalId\":55089,\"journal\":{\"name\":\"Global and Planetary Change\",\"volume\":\"253 \",\"pages\":\"Article 104913\"},\"PeriodicalIF\":4.0000,\"publicationDate\":\"2025-06-03\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Global and Planetary Change\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S092181812500222X\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOGRAPHY, PHYSICAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Global and Planetary Change","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S092181812500222X","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
Impact of Pacific Walker Circulation driven by Interdecadal Pacific Oscillation on precipitation variability in the North China Monsoon Marginal Region over the past five centuries
The Asian Summer Monsoon system has exerted significant impact on the ecological environment and socio-economic development of North China. Understanding the variability of monsoon precipitation and its underlying drivers in the context of anthropogenic warming necessitates the development of high-resolution precipitation reconstructions extending beyond the instrumental record. This study presents a novel tree ring network comprising 869 cores from 12 site chronologies in the North China Monsoon Marginal Region (NCMMR). A Nested Principal Component Regression model is used to reconstruct August-to-July precipitation variability from 1512 to 2021. The results indicate that, compared to the preceding five centuries, the probability of extreme high and low precipitation events increased by ∼9 % and ∼ 2 %, respectively, during the Current Warming Period (CWP, 1850–2021), with a higher long-term mean precipitation of 465.39 mm. The standard deviation and coefficient of variation for precipitation during the CWP (48.24 mm and 10.36 %, respectively) exceed those of the Historical Period (1512–1849) (36.89 mm and 8.07 %, respectively), highlighting an increase in precipitation variability over time. Analysis of global sea surface temperature patterns reveals a strong linkage between precipitation and the Interdecadal Pacific Oscillation (IPO). This is supported by a significant negative correlation between precipitation and the IPO index (P < 0.001), alongside the IPO's substantial contribution (25 % of explained variance) to precipitation variability. Additionally, precipitation exhibits a significant positive correlation with the Pacific Walker Circulation (PWC) index (P < 0.001). Climate model simulations further demonstrate that IPO-driven variations in PWC intensity regulate interdecadal precipitation variability in the NCMMR using water vapor transport anomalies.
期刊介绍:
The objective of the journal Global and Planetary Change is to provide a multi-disciplinary overview of the processes taking place in the Earth System and involved in planetary change over time. The journal focuses on records of the past and current state of the earth system, and future scenarios , and their link to global environmental change. Regional or process-oriented studies are welcome if they discuss global implications. Topics include, but are not limited to, changes in the dynamics and composition of the atmosphere, oceans and cryosphere, as well as climate change, sea level variation, observations/modelling of Earth processes from deep to (near-)surface and their coupling, global ecology, biogeography and the resilience/thresholds in ecosystems.
Key criteria for the consideration of manuscripts are (a) the relevance for the global scientific community and/or (b) the wider implications for global scale problems, preferably combined with (c) having a significance beyond a single discipline. A clear focus on key processes associated with planetary scale change is strongly encouraged.
Manuscripts can be submitted as either research contributions or as a review article. Every effort should be made towards the presentation of research outcomes in an understandable way for a broad readership.