强明瑞
近期热点
资料介绍
个人简历
教育背景1992.9-1996.7山西师范大学,本科/学士,地理学1996.9-1999.7中国科学院兰州沙漠研究所,研究生/硕士,自然地理学1999.9-2002.12兰州大学,研究生/博士,自然地理学工作经历2003.7-2005.9北京师范大学资源学院,地理学博士后工作站2005.9-2008.5兰州大学资源环境学院,副教授2008.5-2018.7兰州大学资源环境学院,教授2018.7—华南师范大学地理科学学院,教授2008.9-2009.9德国波茨坦地球科学中心(GFZ),访问学者科研项目国家重点研发计划“全球变化及应对”重点专项项目“全新世亚洲季风变异与干旱环境及其驱动机制”课题二,2017YFA0603402,亚洲干旱区气候变化及突变事件,2017/7-2022/7,581万元,在研,课题负责人国家自然科学基金面上项目,41671190,北疆泥炭沉积记录的全新世大气粉尘变化,2017/01-2020/12,75万元(直接经费),在研,主持国家自然科学基金面上项目,41271219,青藏高原东北部更尕海沉积记录的全新世湖泊水位与气候变化,2013/01-2016/12,80万元,已结题,主持高等学校博士学科点专项科研基金(博导类),20130211110035,共和盆地更尕海现代沉水植物成因碳酸盐稳定同位素变化及其气候意义,2014/1-2016/12,12万元,已结题,主持国家自然科学基金面上项目,40671192,柴达木盆地湖泊沉积记录的全新世尘暴序列与粉尘释放历史,2007/1-2009/12,38万元,已结题,主持国家自然科学基金青年基金项目,40301051,全新世青藏高原北缘苏干湖沉积记录的尘暴事件演化历史,2004/1-2006/12,30万元,已结题,主持中国博士后科学基金项目,2003034109,2ka以来贺兰山东西两侧湖泊沉积记录的气候变化,2004/1-2005/12,1万元,已结题,主持教育部“新世纪优秀人才支持计划”,NCET-07-0395,2008/1-2010/12,50万元,已结题,主持国家重大科学研究计划项目,2012CB956102,湖泊与湿地生态系统对全球变化的响应及生态恢复对策研究(课题二),2012/1-2016/12,84.97万元,已结题,骨干成员国家重点基础研究发展计划项目(“973”项目),2011CB403301,黄河上游沙漠宽谷段风沙水沙过程与调控机理(课题一),2011/1-2015/12,43万元,已结题,骨干成员国家自然科学基金创新群体项目,40421101、40721061,青藏高原和中东亚干旱区环境变化与地表过程研究,2005/1-2013/12,26万元,已结题,骨干成员国家自然科学基金重点项目,40830105,世界各地黄土磁化率与古气候不同关系机制以及古气候重建问题系统研究,2009/1-2012/12,10万元,已结题,骨干成员国家自然科学基金面上项目,40301050,苏干湖微层沉积记录与青藏高原北部全新世气候变化研究,2004/1-2006/12,30万元,已结题,参加研究领域
环境变化近期论文
Li,Y.,Qiang,M.R.*,Jin,Y.X.,Liu,L.,Zhou,A.F.,Zhang,J.W.,2018.InfluenceofaquaticplantphotosynthesisonthereservoireffectofGenggahaiLake,northeasternQinghai-TibetanPlateau.Radiocarbon,60,561-569.QiangM.R.*,SongL.,JinY.X.,LiY.,LiuL.,ZhangJ.W.,ZhaoY.,ChenF.H.,2017.A16-kaoxygen-isotoperecordfromGenggahaiLakeonthenortheasternQinghai-TibetanPlateau:Hydroclimaticevolutionandchangesinatmosphericcirculation.QuaternaryScienceReviews162,72-87.QiangM.R.*,JinY.X.,Liu,X.X.,SongL.,LiH.,LiF.S.,ChenF.H.,2016.LatePleistoceneandHoloceneaeoliansedimentationinGongheBasin,northeasternQinghai-TibetanPlateau:Variability,processes,andclimaticimplications.QuaternaryScienceReviews132,57-73.LiY.,QiangM.R.*,Zhang,J.W.,HuangX.Z.,ZhouA.F.,ChenJ.H.,WangG.G.,ZhaoY.,2017.Hydroclimaticchangesoverthepast900yearsdocumentedbythesedimentsofTiewaikeLake,AltaiMountains,northwesternChina.QuaternaryInternational452,91-101.QiangM.R.*,LiuY.Y.,JinY.X.,SongL.,HuangX.T.,ChenF.H.,2014.HolocenerecordofeolianactivityfromGenggahaiLake,northeasternQinghai-TibetanPlateau,China.GeophysicalResearchLetters41,589-595.QiangM.R.*,ChenF.H.,SongL.,LiuX.X.,LiM.Z.,WangQ.,2013.LateQuaternaryaeolianactivityinGongheBasin,northeasternQinghai-TibetanPlateau,China.QuaternaryResearch79,403-412.QiangM.R.*,SongL.,ChenF.H.,LiM.Z.,LiuX.X.,WangQ.,2013.A16-kalake-levelrecordinferredfrommacrofossilsinasedimentcorefromGenggahaiLake,northeasternQinghai–TibetanPlateau(China).JournalofPaleolimnology49,575-590.SongL.*,QiangM.R.*,LangL.L.,LiuX.X.,WangQ.,LiM.Z.,2012.ChangesinpalaeoproductivityofGenggahaiLakeoverthepast16kaintheGongheBasin,northeasternQinghai-TibetanPlateau.ChineseScienceBulletin57,2595-2605.QiangM.R.*,ChenF.H.,WangZ.T.,NiuG.M.,SongL.,2010.AeoliandepositsatthesoutheasternmarginoftheTenggerDesert(China):ImplicationsforsurfacewindstrengthintheAsiandustsourceareaoverthepast20,000years.Palaeogeography,Palaeoclimatology,Palaeoecology286,66-80.QiangM.*,LangL.,WangZ.,2010.Dofine-grainedcomponentsofloessindicatewesterlies:InsightsfromobservationsofduststormdepositsatLenghu(QaidamBasin,China).JournalofAridEnvironments74,1232-1239.QiangM.R.*,ChenF.H.,ZhangJ.W.,ZuR.P.,JinM.,ZhouA.F.,XiaoS.,2007.GrainsizeinsedimentsfromLakeSugan:apossiblelinkagetoduststormeventsatthenorthernmarginoftheQinghai–TibetanPlateau.EnvironmentalGeology51(7),1229-1238.QiangM.R.*,ChenF.H.,ZhouA.F.,XiaoS.,ZhangJ.W.,WangZ.T.,2007.ImpactsofwindvelocityonsandanddustdepositionduringduststormasinferredfromaseriesofobservationsinthenortheasternQinghai–TibetanPlateau,China.PowderTechnology175,82-89.QiangM.R.*,ChenF.H.*,ZhangJ.W.,GaoS.Y.,ZhouA.F.,2005.ClimaticchangesdocumentedbystableisotopesofsedimentarycarbonateinLakeSugan,northeasternTibetanPlateauofChina,since2kaBP.ChineseScienceBulletin,50(17),1930-1939.QiangM.R.*,LiS.,GaoS.Y.,2004.EvidenceforabruptclimaticchangesonthenorthwesternmarginoftheEastAsianmonsoonduringthelastDeglaciation.ChineseGeographicalScience14(2),117-121.ChenF.H.,QiangM.R.,ZhouA.F.,XiaoS.,ChenJ.H.,SunD.H.,2013.A2000-yearduststormrecordfromLakeSuganinthedustsourceareaofaridChina.JournalofGeophysicalResearch(Atmospheres)118,2149-2160.RaoZ.G.,QiangM.R.,JiaG.D.,LiY.X.,DanD.,ChenF.H.,2016.A15kalakewaterdeltaDrecordfromGenggahaiLake,northeasternTibetanPlateau,anditspaleoclimaticsignificance.OrganicGeochemistry97,5-16.ZhangJ.W.,MaX.Y.,QiangM.R.,HuangX.Z.,LiS.,GuoX.Y.,HendersonA.C.G.,HolmesJ.A.,ChenF.H.,2016.Developinginorganiccarbon-basedradiocarbonchronologiesforHolocenelakesedimentsinaridNWChina.QuaternaryScienceReviews144,66-82.RaoZ.G.,JiaG.D.,QiangM.R.,ZhaoY.,2014.Assessmentofthedifferencebetweenmid-andlongchaincompoundspecificdeltaDn-alkanesvaluesinlacustrinesedimentsasapaleoclimaticindicator.OrganicGeochemistry76,104-117.ChenF.H.,QiangM.R.,FengZ.D.,WangH.B.,BloemendalJ.,2003.StableEastAsianmonsoonclimateduringthelastinterglacial(Eemian)indicatedbypaleosolS1inthewesternpartoftheChineseLoessPlateau.GlobalandPlanetaryChange36(3),171-179.GaoS.Y.,LuR.J.,QiangM.R.,HasiE.,ZhangD.S.,ChenY.,XiaH.,2005.Reconstructionofprecipitationinthelast140yearsfromtreeringatsouthmarginoftheTenggerDesert,China.ChineseScienceBulletin50(21),2487-2492ZhouA.F.,ChenF.H.,QiangM.R.,YangM.L.,ZhangJ.W.,2007.Thediscoveryofannuallylaminatedsediments(varves)fromshallowSuganLakeininlandaridChinaandtheirpaleoclimaticsignificance.ScienceinChina(DSeries)50(8),1218-1224.ZuR.P.,XueX.,QiangM.R.,YangB.,QuJ.J.,ZhangK.C.,2008.Characteristicsofnear-surfacewindregimesintheTaklimakanDesert,China.Geomorphology96,39–47.SchettlerG.,RomerR.L.,QiangM.R.,PlessenB.,DulskiP.,2009.Size-dependentgeochemicalsignaturesofHoloceneloessdepositsfromtheHexiCorridor(China).JournalofAsianEarthSciences35,103-136.ZhangD.J.,DongG.H.,WangH.,RenX.Y.,HaP.P.,QiangM.R.,Chen,F.H.,2016.HistoryandpossiblemechanismsofprehistorichumanmigrationtotheTibetanPlateau,ScienceChina(EarthSciences),59(9),1765-1778.LiG.Q.,RaoZ.G.,DuanY.W.,XiaD.S.,WangL.B.,MadsenD.B.,JiaJ.,WeiH.T.,QiangM.R.,ChenJ.H.,ChenF.H.,2016.Paleoenvironmentalchangesrecordedinaluminescencedatedloess/paleosolsequencefromtheTianshanMountains,aridcentralAsia,sincethePenultimateGlaciation,EarthandPlanetaryScienceLetters,448:1-12.LuR.J.,GaoS.Y.,WangY.J.,MaY.Z.,QiangM.R.,ZhangD.S.,2013.Tree-ringbaseddroughtreconstructionatthenorthwesternmarginofmonsoonregionofChinasince1862.QuaternaryInternational283,93-97.ZuR.P.,GaoQ.Z.,QuJ.J.,QiangM.R.,2003.EnvironmentalChangesofoasesatsouthmarginofTarimBasin,China.EnvironmentalGeology44,639-644.HolmesJ.A.,ZhangJ.W.,ChenF.C.,QiangM.R.,2007.Paleoclimaticimplicationsofan850-yearoxygen-isotoperecordfromthenorthernTibetanPlateau.GeophysicalResearchLetters34,L23403,doi:10.1029/2007GL032228.WangZ.T.,ZhangJ.W.,ZhangQ.H.,QiangM.R.,ChenF.H.,LingY.Q.,2008.BarchansofMinqin:Sedimenttransport.Geomorphology96,233–238.ZhangJ.W.,HolmesJ.A.,ChenF.H.,QiangM.R.,ZhouA.F.,ChenS.,2009.An850-yearostracod-shelltrace-elementrecordfromSuganLake,northernTibetanPlateau,China:Implicationsforinterpretingtheshellchemistryinhigh-Mg/Cawaters.QuaternaryInternational194,119–133.ZhangJ.W.,ChenF.H.,HolmesJ.A.,LiH.,GuoX.Y,WangJ.L.,LiS.,LüY.B.,ZhaoY.,QiangM.R.,2011.HolocenemonsoonclimatedocumentedbyoxygenandcarbonisotopesfromlakesedimentsandpeatbogsinChina:areviewandsynthesis.QuaternaryScienceReviews30,1973-1987.RaoZ.G.,ZhuZ.Y.,JiaG.D.,ChenF.H.,BartonL.,ZhangJ.W.,QiangM.R.,2010.RelationshipbetweenclimaticconditionsandtherelativeabundanceofmodernC-3andC-4plantsinthreeregionsaroundtheNorthPacific.ChineseScienceBulletin55,1931-1936.ZhouA.F.,ChenF.H.,WangZ.L.,YangM.L.,QiangM.R.,ZhangJ.W.,2009.Temporalchangeofradiocarbonreservoireffectinsuganlake,northwestchinaduringthelateHolocene,Radiocarbon51,529-535.WangX.M.,XiaoH.L.,LiJ.C.,QiangM.R.,SuZ.Z.,2008.NebkhadevelopmentanditsrelationshiptoenvironmentalchangeintheAlaxaPlateau,China.EnvironmentalGeology56,359-365.RaoZ.G.,ZhuZ.Y.,WangS.P.,JiaG.D.,QiangM.R.,WuY.,2009.CPIvaluesofterrestrialhigherplant-derivedlong-chainn-alkanes:apotentialpaleoclimaticproxy.FrontierofEarthScienceinChina2009,3(3),266-272.RashkiA.,KaskaoutisD.G.,RautenbachC.J.deW.,ErikssonP.G.,QiangM.R.,GuptaP.,2012.DuststormsandtheirhorizontaldustloadingintheSistanregion,Iran.AeolianResearch5,51-62.#强明瑞*,陈发虎*,张家武,高尚玉,周爱锋.2ka来苏干湖沉积碳酸盐稳定同位素记录的气候变化.科学通报,2005,50(13):1385-1393.强明瑞*,陈发虎,周爱锋,肖舜,张家武,金明,2006.苏干湖沉积物粒度组成记录尘暴事件的初步研究.第四纪研究26(6),915-922.强明瑞*,鲁瑞洁,张家武,肖舜,陈发虎,2006.柴达木盆地苏干湖表层沉积与尘暴事件——元素示踪的初步结果.湖泊科学18(6),590-596.强明瑞*,陈发虎,高尚玉,2004.苏干湖沉积碳酸盐稳定同位素古气候意义的初步研究.第四纪研究24(5),598-599.强明瑞*,肖舜,张家武,陈发虎,2007.柴达木盆地北部风速对尘暴事件降尘的影响.中国沙漠27(2),290-295.强明瑞*,李森,金明,陈发虎,2000.60ka来腾格里沙漠东南缘风成沉积与沙漠演化.中国沙漠20(3),256-259.李森,强明瑞,李保生,高尚玉,2004.末次冰消期东亚季风区西北缘气候快速变化事件.地质论评50(1),106-112.宋磊,强明瑞*,牛光明,郎丽丽,2009.柴达木盆地苏干湖沉积元素特征与大风尘暴事件.海洋地质与第四纪地质29(1),95-102.肖舜,陈发虎,强明瑞,张家武,周爱锋,孙东怀,2007.青海苏干湖表层沉积物粒度分布模式与大气粉尘记录.地理学报62(11),1153-1164.鲁瑞洁,夏虹,强明瑞,张登山,2008.近130a来毛乌素沙漠北部泊江海子湖泊沉积记录的气候环境变化.中国沙漠28(1),44-49.牛光明,强明瑞*,宋磊,郎丽丽,王立强.2010.5000a来柴达木盆地东南缘风成沉积记录的冬季风演化.中国沙漠30(4),1031-1039.宋磊,强明瑞*,2010.更尕海现代碎屑物质粒度组成空间分异及其输入过程.第四纪研究30(6):1199-1208.#宋磊*,强明瑞*,郎丽丽,刘星星,王亲,李明治,2012.16kaBP共和盆地更尕海湖泊生产力演化历史.科学通报57(19),1763-1774.李渊,强明瑞*,王刚刚,李丰山,刘英英,金彦香,李昊,金明,2015.晚冰期以来共和盆地更尕海碎屑物质输入过程与气候变化.第四纪研究35(1),160-171.金彦香,强明瑞*,刘英英,李渊,李昊,李丰山,2015.共和盆地更尕海现代水环境与碳酸盐碳氧同位素组成变化.科学通报60(9),847-856.周爱锋,强明瑞,张家武,陈发虎,钟艳霞,陈建徽,肖舜,2008.苏干湖沉积物纹层计年和210Pb,137Cs测年对比.兰州大学学报(自然科学版)44(6),15-18.#周爱锋,陈发虎,强明瑞,杨美临,张家武,2007.内陆干旱区柴达木盆地苏干湖年纹层的发现及其意义.中国科学(D辑,地球科学)37(7),941-948.#高尚玉,鲁瑞洁,强明瑞,哈斯,张登山,陈原,夏虹,2006.140年来腾格里沙漠南缘树木年轮记录的降水量变化.科学通报51(3),326-331.#饶志国,朱照宇,贾国东,陈发虎,BartonLoukas,张家武,强明瑞,2010.环北太平洋地区现代植被中C3/C4植物相对丰度与气候条件关系研究.科学通报55(12),1134-1140.宋磊,强明瑞*,金彦香,徐军强,李渊,2013.青藏高原东北部更尕海沉积软体动物壳体同位素初步研究.地球环境学报4(1),1183-1190.强明瑞,李森,侯甬坚,2010.西藏土地沙漠化形成时代与过程.见:李森等著,西藏土地沙漠化及其防治.北京:科学出版社,pp52-76. 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