Publication | Closed Access

Late Holocene relative humidity history on the southeastern Tibetan plateau inferred from a tree-ring δ 18 O record: Recent decrease and conditions during the last 1500 years

ClimatologyHoloceneEngineeringGeomorphologyGeographyDendrochronologyTibetan PlateauGeochronologyPaleoclimatologyEarth ScienceTree-ring δ 18Southeastern Tibetan PlateauO Record