Impact of PDO and AMO on interdecadal variability in extreme high temperatures in North China over the most recent 40-year period

Based on the 1979–2018 datasets of Climate Prediction Center (CPC) daily maximum air temperature, HadISST, and NCEP-DOE II reanalysis, the impact of Pacific decadal oscillation (PDO) and Atlantic multidecadal oscillation (AMO) on the interdecadal variability in extreme high temperature (EHT) in Nort...

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Veröffentlicht in:	Climate dynamics Jg. 54; H. 5-6; S. 3003 - 3020
Hauptverfasser:	Zhang, Guwei, Zeng, Gang, Li, Chun, Yang, Xiaoye
Format:	Journal Article
Sprache:	Englisch
Veröffentlicht:	Berlin/Heidelberg Springer Berlin Heidelberg 01.03.2020 Springer Springer Nature B.V
Schlagworte:	Air temperature Analysis Anomalies Anticyclones Anticyclonic circulation Atlantic Oscillation Atmospheric models Atmospheric research Atmospheric waves basins China Circulation anomalies climate Climate cycles climate models Climate prediction Climatology Cold Computer simulation data collection Earth and Environmental Science Earth Sciences Easterlies Extreme heat Extreme high temperatures Geophysics/Geodesy High temperature Interdecadal variability latitude Mathematical models Northern Hemisphere Numerical analysis Numerical simulations observational studies Oceanography Pacific Decadal Oscillation Sea surface Sea surface temperature Sea surface temperature anomalies Simulation summer Surface temperature surface water temperature Teleconnection patterns Teleconnections Temperature Temperature anomalies Variability Wave packets Wind wind direction Eastern Europe East Asia China North China Numerical simulation PDO Extreme high temperature AMO Interdecadal variation
ISSN:	0930-7575, 1432-0894
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Abstract	Based on the 1979–2018 datasets of Climate Prediction Center (CPC) daily maximum air temperature, HadISST, and NCEP-DOE II reanalysis, the impact of Pacific decadal oscillation (PDO) and Atlantic multidecadal oscillation (AMO) on the interdecadal variability in extreme high temperature (EHT) in North China (NC) is investigated through observational analysis and National Center for Atmospheric Research (NCAR) Community Atmosphere Model version 5.3 (CAM5.3) numerical simulations. The observational results show an interdecadal shift in NC’s EHT in approximately 1996 with a cold period from 1983 to 1996 and a warm period from 1997 to 2014. The summer PDO and AMO are both closely related to NC’s EHT, of which AMO dominates. From the cold to warm period, the combination of PDO and AMO changed from a positive PDO (+ PDO) phase and a negative AMO (− AMO) phase to a negative PDO (− PDO) phase and a positive AMO (+ AMO) phase. The shift in the antiphase combination of PDO and AMO plays an important role in the interdecadal transition of NC’s EHT in 1996. PDO could impact NC’s EHT through the Pacific-East Asia teleconnection pattern, and AMO could influence the NC’s EHT through an atmospheric wave train in the midlatitudes of the Northern Hemisphere. During the warm period (− PDO and + AMO), warmer sea surface temperature anomalies (SSTA) in the northern North Pacific (NP) and North Atlantic (NA) could cause anticyclonic circulation anomalies over these two basins. The anticyclonic circulations anomalies over the NP could enhance the anticyclone over NC through the Pacific-East Asian (PEA) teleconnection pattern. It could also cause an easterly wind from the NP to NC which would weaken the upper westerly over NC. The anticyclonic anomalies over the NA, which were parts of the wave train, could affect other sectors of the wave train, resulting in anticyclonic anomalies over NC. The anticyclonic anomalies over NC could strengthen the continental high and weaken the upper zonal westerly, resulting in favorable EHT conditions. During the cold period (+ PDO and − AMO), because of the same atmospheric response mechanism, a westerly wind from NC to NP and a wave train with reversed anomaly centers could be found, causing a cyclonic anomaly over NC that is not conducive to the EHT. A series of numerical simulations using CAM5.3 confirm the above observational results and show that the combination of + PDO and − AMO changing to − PDO and + AMO has a great impact on the interdecadal shift in EHT in NC in 1996. The simulations also show that both + AMO and − PDO can lead the EHT in NC individually, and the impact of AMO on the EHT in NC is dominant.
AbstractList	Based on the 1979-2018 datasets of Climate Prediction Center (CPC) daily maximum air temperature, HadISST, and NCEP-DOE II reanalysis, the impact of Pacific decadal oscillation (PDO) and Atlantic multidecadal oscillation (AMO) on the interdecadal variability in extreme high temperature (EHT) in North China (NC) is investigated through observational analysis and National Center for Atmospheric Research (NCAR) Community Atmosphere Model version 5.3 (CAM5.3) numerical simulations. The observational results show an interdecadal shift in NC's EHT in approximately 1996 with a cold period from 1983 to 1996 and a warm period from 1997 to 2014. The summer PDO and AMO are both closely related to NC's EHT, of which AMO dominates. From the cold to warm period, the combination of PDO and AMO changed from a positive PDO (+ PDO) phase and a negative AMO (- AMO) phase to a negative PDO (- PDO) phase and a positive AMO (+ AMO) phase. The shift in the antiphase combination of PDO and AMO plays an important role in the interdecadal transition of NC's EHT in 1996. PDO could impact NC's EHT through the Pacific-East Asia teleconnection pattern, and AMO could influence the NC's EHT through an atmospheric wave train in the midlatitudes of the Northern Hemisphere. During the warm period (- PDO and + AMO), warmer sea surface temperature anomalies (SSTA) in the northern North Pacific (NP) and North Atlantic (NA) could cause anticyclonic circulation anomalies over these two basins. The anticyclonic circulations anomalies over the NP could enhance the anticyclone over NC through the Pacific-East Asian (PEA) teleconnection pattern. It could also cause an easterly wind from the NP to NC which would weaken the upper westerly over NC. The anticyclonic anomalies over the NA, which were parts of the wave train, could affect other sectors of the wave train, resulting in anticyclonic anomalies over NC. The anticyclonic anomalies over NC could strengthen the continental high and weaken the upper zonal westerly, resulting in favorable EHT conditions. During the cold period (+ PDO and - AMO), because of the same atmospheric response mechanism, a westerly wind from NC to NP and a wave train with reversed anomaly centers could be found, causing a cyclonic anomaly over NC that is not conducive to the EHT. A series of numerical simulations using CAM5.3 confirm the above observational results and show that the combination of + PDO and - AMO changing to - PDO and + AMO has a great impact on the interdecadal shift in EHT in NC in 1996. The simulations also show that both + AMO and - PDO can lead the EHT in NC individually, and the impact of AMO on the EHT in NC is dominant. Based on the 1979–2018 datasets of Climate Prediction Center (CPC) daily maximum air temperature, HadISST, and NCEP-DOE II reanalysis, the impact of Pacific decadal oscillation (PDO) and Atlantic multidecadal oscillation (AMO) on the interdecadal variability in extreme high temperature (EHT) in North China (NC) is investigated through observational analysis and National Center for Atmospheric Research (NCAR) Community Atmosphere Model version 5.3 (CAM5.3) numerical simulations. The observational results show an interdecadal shift in NC’s EHT in approximately 1996 with a cold period from 1983 to 1996 and a warm period from 1997 to 2014. The summer PDO and AMO are both closely related to NC’s EHT, of which AMO dominates. From the cold to warm period, the combination of PDO and AMO changed from a positive PDO (+ PDO) phase and a negative AMO (− AMO) phase to a negative PDO (− PDO) phase and a positive AMO (+ AMO) phase. The shift in the antiphase combination of PDO and AMO plays an important role in the interdecadal transition of NC’s EHT in 1996. PDO could impact NC’s EHT through the Pacific-East Asia teleconnection pattern, and AMO could influence the NC’s EHT through an atmospheric wave train in the midlatitudes of the Northern Hemisphere. During the warm period (− PDO and + AMO), warmer sea surface temperature anomalies (SSTA) in the northern North Pacific (NP) and North Atlantic (NA) could cause anticyclonic circulation anomalies over these two basins. The anticyclonic circulations anomalies over the NP could enhance the anticyclone over NC through the Pacific-East Asian (PEA) teleconnection pattern. It could also cause an easterly wind from the NP to NC which would weaken the upper westerly over NC. The anticyclonic anomalies over the NA, which were parts of the wave train, could affect other sectors of the wave train, resulting in anticyclonic anomalies over NC. The anticyclonic anomalies over NC could strengthen the continental high and weaken the upper zonal westerly, resulting in favorable EHT conditions. During the cold period (+ PDO and − AMO), because of the same atmospheric response mechanism, a westerly wind from NC to NP and a wave train with reversed anomaly centers could be found, causing a cyclonic anomaly over NC that is not conducive to the EHT. A series of numerical simulations using CAM5.3 confirm the above observational results and show that the combination of + PDO and − AMO changing to − PDO and + AMO has a great impact on the interdecadal shift in EHT in NC in 1996. The simulations also show that both + AMO and − PDO can lead the EHT in NC individually, and the impact of AMO on the EHT in NC is dominant.
Audience	Academic
Author	Li, Chun Zhang, Guwei Yang, Xiaoye Zeng, Gang
Author_xml	– sequence: 1 givenname: Guwei orcidid: 0000-0001-8272-3007 surname: Zhang fullname: Zhang, Guwei organization: Key Laboratory of Meteorological Disaster of Ministry of Education (KLME), Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and Technology – sequence: 2 givenname: Gang surname: Zeng fullname: Zeng, Gang email: zenggang@nuist.edu.cn organization: Key Laboratory of Meteorological Disaster of Ministry of Education (KLME), Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and Technology – sequence: 3 givenname: Chun surname: Li fullname: Li, Chun organization: Physical Oceanography Laboratory and Key Laboratory of Ocean–Atmosphere Interaction and Climate in Universities of Shandong, Ocean University of China – sequence: 4 givenname: Xiaoye surname: Yang fullname: Yang, Xiaoye organization: Key Laboratory of Meteorological Disaster of Ministry of Education (KLME), Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and Technology
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Copyright	Springer-Verlag GmbH Germany, part of Springer Nature 2020 COPYRIGHT 2020 Springer Climate Dynamics is a copyright of Springer, (2020). All Rights Reserved.
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Keywords	North China Numerical simulation PDO Extreme high temperature AMO Interdecadal variation
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PublicationSubtitle	Observational, Theoretical and Computational Research on the Climate System
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PublicationYear	2020
Publisher	Springer Berlin Heidelberg Springer Springer Nature B.V
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References	HanTHeSXinHWangHRecent interdecadal shift in the relationship between Northeast China’s winter precipitation and the North Atlantic and Indian OceansClim Dyn2017503–41413142410.1007/s00382-017-3694-x XiaoDLiJSpatial and temporal characteristics of the decadal abrupt changes of global atmosphere-ocean system in the 1970sJ Geophys Res200710.1029/2007jd008956 WangYLiSLuoDSeasonal response of Asian monsoonal climate to the Atlantic Multidecadal OscillationJ Geophys Res2009114D0211210.1029/2008JD010929 McGregorGRFerroCATStephensonDBProjected changes in extreme weather and climate events in Europe. Extreme weather events and public health responses2005BerlinSpringer10.1007/3-540-28862-7_2 DuchonCELanczos filtering in one and two dimensionsJ Appl Meteorol19791881016102210.1175/1520-0450(1979)018<1016:LFIOAT>2.0.CO;2 Zhang Y, Wallace JM, Battisti DS (1997) ENSO-like interdecadal variability: 1900–1993. J Clim 10(5):1004–1020. https://doi.org/10.1175/1520-0442 BarrioPThe hot summer of 2010: redrawing the temperature record map of EuropeScience2011332602622022410.1126/science.1201224 ZhangGWZengGNiDHZhouGBDecadal shift of autumn drought in Southwest China and its possible causesChin J Atmos Sci201640231132310.3878/j.issn.1006-9895.1503.14294(in Chinese) DelworthTLMannMEObserved and simulated multi- decadal variability in the Northern hemisphereClim Dyn20001666167110.1007/s003820000075 KucharskiFBraccoAYooJHTompkinsAMFeudaleLRutiPDell’AquilaAA Gill-Matsuno-type mechanism explains the tropical Atlantic influence on African and Indian monsoon rainfallQ J R Meteorol Soc200913564056957910.1002/qj.406 Trednberth KE, Shea DJ (2006) Atlantic hurricanes and natural variability in 2005. Geol Res Lett 33(12):L12704. https://doi:10.1029/2006gl026894 DengKSongYTingMLinAWangZAn intensified mode of variability modulating the summer heat waves in eastern Europe and northern ChinaGeol Res Lett2018451136136910.1029/2018GL079836 MeehlGATebaldiCMore intense, more frequent, and longer lasting heat waves in the 21st centuryScience2004305568699499710.1126/science.1098704 XiePArkinPAGlobal precipitation: a 17-year monthly analysis based on gauge observations, satellite estimates, and numerical model outputsBull Am Meteorol Soc199778112539255810.1175/1520-0477 NapoliACrespiARagoneFMaugeriMPasqueroCVariability of orographic enhancement of precipitation in the Alpine regionSci Rep201910.1038/s41598-019-49974-5 RaynerNAParkerDEHortonEBFollandCKAlexanderLVRowellDPKentECKaplanAGlobal analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth centuryJ Geophys Res2003108D1410.1029/2002jd002670 LiRXSunJQInterdecadal variability of the large-scale extreme hot event frequency over the middle and lower reaches of the Yangtze River basin and its related atmospheric patternsAtmos Ocean Sci Lett2017111637010.1080/16742834.2017.1335580 DelworthTLZengFVecchiGAYangXZhangLZhangRThe North Atlantic Oscillation as a driver of rapid climate change in the Northern hemisphereNat Geosci2016950951210.1038/ngeo2738 SunJQPossible impact of the summer North Atlantic oscillation on extreme hot events in ChinaAtmos Ocean Sci Lett20125323123410.1080/16742834.2012.11446996 GhoshRMüllerWABaehrJBaderJImpact of observed North Atlantic multidecadal variations to European summer climate: a linear baroclinic response to surface heatingClim Dyn2017483547356310.1007/s00382-016-3283-4 ZhangRDelworthTLSimulated tropical response to a substantial weakening of the Atlantic thermohaline circulationJ Clim2005181853186010.1175/JCLI3460.1 SiDDingYOceanic forcings of the interdecadal variability in East Asian summer rainfallJ Clim201629217633764910.1175/jcli-d-15-0792.1 ZhaiPMChanges of climate extremes in ChinaClim Chang199942120321810.1023/a:1005428602279 SunJQWangHJYuanWDecadal variability of the extreme hot events in China and its associated with atmospheric circulationsClim Environ Res2011162199208(in Chinese) LeiYNGongDYZhangZYGuoDHeXZSpatial-temporal characteristics of high-temperature events in summer in eastern China and the associated atmospheric circulationGeograph Res2009283654662(in Chinese) SunJQWangHJYuanWDecadal variations of the relationship between the summer North Atlantic Oscillation and middle East Asian air temperatureJ Geophys Res2008113D1510710.1029/2007JD009626 DingTQianWHYanZWChanges in hot days and heat waves in China during 1961–2007Int J Climatol2009301452146210.1002/joc.1989 WangLXuPChenWLiuYInterdecadal variations of the silk road patternJ Clim201730249915993210.1175/jcli-d-17-0340.1 FischerEMKnuttiRAnthropogenic contribution to global occurrence of heavy-precipitation and high-temperature extremesNat Clim Chang20155656056410.1038/nclimate2617 MiaoJPWangTWangHJInterdecadal variations of the East Asian winter monsoon in CMIP5 preindustrial simulationsJ Clim201910.1175/JCLI-D-19-0148.1 SunJQRecord-breaking SST over mid-North Atlantic and extreme high temperature over the Jianghuai–Jiangnan region of China in 2013Chin Sci Bull2014593465347010.1007/s11434-014-0425-0(in Chinese) Neale RB et al (2012) Description of the NCAR community atmosphere model (CAM5.0). NCAR Tech Note NCAR/TN-486 +STR, p 274 WangYJRenFMZhangXBSpatial and temporal variations of regional high temperature events in ChinaInt J Clim201334103054306510.1002/joc.3893 XuYGaoXJShenYXuCHShiYGiorgiFA daily temperature dataset over China and its application in validating a RCM simulationAdv Atmos Sci20092676377210.1007/s00376-009-9029-z MantuaNJHareSRZhangYWallaceJMFrancisRCA Pacific Interdecadal Climate Oscillation with umpacts on Salmon productionBull Am Meteorol Soc19977861069107910.1175/1520-0477 KanamitsuMEbisuzakiWWoollenJYangSKHniloJJFiorinoMPotterGLNCEP-DOE AMIP-II reanalysis (R-2)Bull Am Meteorol Soc200210.1175/BAMS-83-11-1631 GongDYHoCHArctic Oscillation signals in the East Asian summer monsoonJ Geophys Res2003108406610.1029/2002JD002193 ZhuJHuangDQZhangYCHuangANKuangXYHuangYDecadal changes of meiyu rainfall around 1991 and its relationship with two types of ENSOJ Geophys Res Atmos20131189766977710.1002/jgrd.50779 WeiJYangHSunSQRelationship between the anomaly longitude position of subtropical high in the western Pacific and severe hot weather in North China in summerActa Meteorol Sin2004623308316(in Chinese) ChengQZhouTJMultidecadal variability of north china aridity and its relationship to PDO during 1900–2010J Clim20142731210122210.1175/jcli-d-13-00235.1 DengKSongYLinALiCHuCUnprecedented East Asian warming in spring 2018 linked to the North Atlantic tripole SST modeAtmos Ocean Sci Lett201912424625310.1080/16742834.2019.1605807 TaoPZhangYLarge-scale circulation features associated with the heat wave over Northeast China in summer 2018Atmos Ocean Sci Lett201912425426010.1080/16742834.2019.1610326 BrethertonCSWidmannMDymnikovVPWallaceJMBladéIThe effective number of spatial degrees of freedom of a time-varying fieldJ Clim1999121990200910.1175/1520-0442 GulevSKNorth Atlantic Ocean-control on surface heat flux on multidecadal timescalesNature2013499745946446710.1038/nature12268 ZhangLDelworthTLAnalysis of the characteristics and mechanisms of the Pacific decadal oscillation in a suite of coupled models from the Geophysical Fluid Dynamics LaboratoryJ Clim2015287678770110.1175/JCLI-D-14-00647.1 WuBZhouTLiTImpacts of the Pacific-Japan and circumglobal teleconnection patterns on the interdecadal variability of the East Asian Summer monsoonJ Clim20162993253327110.1175/jcli-d-15-0105.1 HuangDQDaiAGYangBYanPZhuJZhangYCContributions of different combinations of the IPO and AMO to recent changes in winter East Asian JetsJ Clim201810.1175/jcli-d-18-0218.1 WuJGaoXJA gridded daily observation dataset over China region and comparison with the other datasetsChin J Geophys2013561102111110.6038/cjg20130406(in Chinese) PlumbRAOn the three-dimensional propagation of stationary wavesJ Atmos Sci198542321722910.1175/1520-0469(1985)042<0217:OTTDPO>2.0.CO;2 WuBLinJZhouTInterdecadal circumglobal teleconnection pattern during boreal summerAtmos Sci Lett20161744645210.1002/asl.677 ZhangZQSunXGYangXQUnderstanding the interdecadal variability of East Asian summer monsoon precipitation: joint influence of three oceanic signalsJ Clim201831145485556010.1175/JCLI-D-17-0657.1 LuRYOhJHKimBJBeakHJHuangRHAssociations with the interannual variations of onset and withdrawal of the ChangmaAdv Atmos Sci20011861066108010.1002/qj.49712455204 YangHLiCYDiagnostic study of serious high temperature over South China in 2003 summerClim Environ Res20051018085(in Chinese) WangMGuQJiaXGeJAn assessment of the impact of PDO on autumn droughts in North China based on the PDSIInt J Clim2019395338535010.1002/joc.6158 LiangXZWangWCAssociation between China monsoon rainfall and tropospheric jetsQ J R Meteorol Soc19981242597262310.1002/qj.49712455204 AikenLSWestSGMultiple regression: testing and interpreting interactions1991Newbury ParkSage LiSBatesGTInfluence of the Atlantic multidecadal oscillation on the winter climate of East ChinaAdv Atmos Sci200724112613510.1007/s00376-007-0126-6 ZhuYLWangTMaJHInfluence of internal decadal variability on the summer rainfall in eastern China as simulated by CCSM4Adv Atmos Sci201633670671410.1007/s00376-016-5269-x YuanWSunJQEnhancement of the summer North Atlantic Oscillation influence on Northern Hemisphere air temperatureAdv Atmos Sci20092661209121410.1007/s00376-009-8148-x NJ Mantua (5155_CR25) 1997; 78 T Han (5155_CR15) 2017; 50 P Tao (5155_CR36) 2019; 12 RX Li (5155_CR21) 2017; 11 GW Zhang (5155_CR55) 2016; 40 TL Delworth (5155_CR6) 2016; 9 5155_CR37 S Li (5155_CR20) 2007; 24 ZQ Zhang (5155_CR56) 2018; 31 NA Rayner (5155_CR30) 2003; 108 YN Lei (5155_CR19) 2009; 28 K Deng (5155_CR8) 2019; 12 JQ Sun (5155_CR33) 2014; 59 YL Zhu (5155_CR58) 2016; 33 DQ Huang (5155_CR16) 2018 RY Lu (5155_CR23) 2001; 18 5155_CR28 P Barrio (5155_CR2) 2011; 332 B Wu (5155_CR45) 2016; 29 J Zhu (5155_CR57) 2013; 118 CE Duchon (5155_CR10) 1979; 18 CS Bretherton (5155_CR3) 1999; 12 M Kanamitsu (5155_CR17) 2002 JQ Sun (5155_CR32) 2012; 5 H Yang (5155_CR49) 2005; 10 D Xiao (5155_CR46) 2007 R Ghosh (5155_CR12) 2017; 48 EM Fischer (5155_CR11) 2015; 5 F Kucharski (5155_CR18) 2009; 135 JQ Sun (5155_CR35) 2011; 16 J Wu (5155_CR43) 2013; 56 SK Gulev (5155_CR14) 2013; 499 JQ Sun (5155_CR34) 2008; 113 5155_CR54 Q Cheng (5155_CR4) 2014; 27 GA Meehl (5155_CR27) 2004; 305 T Ding (5155_CR9) 2009; 30 A Napoli (5155_CR59) 2019 J Wei (5155_CR42) 2004; 62 DY Gong (5155_CR13) 2003; 108 W Yuan (5155_CR50) 2009; 26 RA Plumb (5155_CR29) 1985; 42 JP Miao (5155_CR60) 2019 M Wang (5155_CR41) 2019; 39 P Xie (5155_CR47) 1997; 78 YJ Wang (5155_CR39) 2013; 34 GR McGregor (5155_CR26) 2005 PM Zhai (5155_CR51) 1999; 42 B Wu (5155_CR44) 2016; 17 D Si (5155_CR31) 2016; 29 Y Wang (5155_CR38) 2009; 114 L Zhang (5155_CR53) 2015; 28 K Deng (5155_CR7) 2018; 45 XZ Liang (5155_CR22) 1998; 124 Y Xu (5155_CR48) 2009; 26 TL Delworth (5155_CR5) 2000; 16 LS Aiken (5155_CR1) 1991 L Wang (5155_CR40) 2017; 30 R Zhang (5155_CR52) 2005; 18
References_xml	– reference: KanamitsuMEbisuzakiWWoollenJYangSKHniloJJFiorinoMPotterGLNCEP-DOE AMIP-II reanalysis (R-2)Bull Am Meteorol Soc200210.1175/BAMS-83-11-1631 – reference: ZhangLDelworthTLAnalysis of the characteristics and mechanisms of the Pacific decadal oscillation in a suite of coupled models from the Geophysical Fluid Dynamics LaboratoryJ Clim2015287678770110.1175/JCLI-D-14-00647.1 – reference: ZhuJHuangDQZhangYCHuangANKuangXYHuangYDecadal changes of meiyu rainfall around 1991 and its relationship with two types of ENSOJ Geophys Res Atmos20131189766977710.1002/jgrd.50779 – reference: LuRYOhJHKimBJBeakHJHuangRHAssociations with the interannual variations of onset and withdrawal of the ChangmaAdv Atmos Sci20011861066108010.1002/qj.49712455204 – reference: WuBLinJZhouTInterdecadal circumglobal teleconnection pattern during boreal summerAtmos Sci Lett20161744645210.1002/asl.677 – reference: SiDDingYOceanic forcings of the interdecadal variability in East Asian summer rainfallJ Clim201629217633764910.1175/jcli-d-15-0792.1 – reference: DengKSongYTingMLinAWangZAn intensified mode of variability modulating the summer heat waves in eastern Europe and northern ChinaGeol Res Lett2018451136136910.1029/2018GL079836 – reference: WangYJRenFMZhangXBSpatial and temporal variations of regional high temperature events in ChinaInt J Clim201334103054306510.1002/joc.3893 – reference: XiePArkinPAGlobal precipitation: a 17-year monthly analysis based on gauge observations, satellite estimates, and numerical model outputsBull Am Meteorol Soc199778112539255810.1175/1520-0477 – reference: BarrioPThe hot summer of 2010: redrawing the temperature record map of EuropeScience2011332602622022410.1126/science.1201224 – reference: RaynerNAParkerDEHortonEBFollandCKAlexanderLVRowellDPKentECKaplanAGlobal analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth centuryJ Geophys Res2003108D1410.1029/2002jd002670 – reference: DingTQianWHYanZWChanges in hot days and heat waves in China during 1961–2007Int J Climatol2009301452146210.1002/joc.1989 – reference: WeiJYangHSunSQRelationship between the anomaly longitude position of subtropical high in the western Pacific and severe hot weather in North China in summerActa Meteorol Sin2004623308316(in Chinese) – reference: Neale RB et al (2012) Description of the NCAR community atmosphere model (CAM5.0). NCAR Tech Note NCAR/TN-486 +STR, p 274 – reference: YangHLiCYDiagnostic study of serious high temperature over South China in 2003 summerClim Environ Res20051018085(in Chinese) – reference: ZhaiPMChanges of climate extremes in ChinaClim Chang199942120321810.1023/a:1005428602279 – reference: GulevSKNorth Atlantic Ocean-control on surface heat flux on multidecadal timescalesNature2013499745946446710.1038/nature12268 – reference: DuchonCELanczos filtering in one and two dimensionsJ Appl Meteorol19791881016102210.1175/1520-0450(1979)018<1016:LFIOAT>2.0.CO;2 – reference: XiaoDLiJSpatial and temporal characteristics of the decadal abrupt changes of global atmosphere-ocean system in the 1970sJ Geophys Res200710.1029/2007jd008956 – reference: ZhangGWZengGNiDHZhouGBDecadal shift of autumn drought in Southwest China and its possible causesChin J Atmos Sci201640231132310.3878/j.issn.1006-9895.1503.14294(in Chinese) – reference: ZhangZQSunXGYangXQUnderstanding the interdecadal variability of East Asian summer monsoon precipitation: joint influence of three oceanic signalsJ Clim201831145485556010.1175/JCLI-D-17-0657.1 – reference: BrethertonCSWidmannMDymnikovVPWallaceJMBladéIThe effective number of spatial degrees of freedom of a time-varying fieldJ Clim1999121990200910.1175/1520-0442 – reference: Trednberth KE, Shea DJ (2006) Atlantic hurricanes and natural variability in 2005. 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Title	Impact of PDO and AMO on interdecadal variability in extreme high temperatures in North China over the most recent 40-year period
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