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Paleoclimatic changes and modulation of East Asian summer monsoon by high-latitude forcing over the last 130,000 years as revealed by independently dated loess-paleosol sequences on the NE Tibetan Plateau

ClimatologyMeteorologyEngineeringSummer MonsoonNe Tibetan PlateauHigh-latitude ForcingEast Asian LanguagesLast 130,000PaleoclimatologyEarth ScienceTibetan PlateauClimate Dynamics