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A 2,326‐year tree‐ring record of climate variability on the northeastern Qinghai‐Tibetan Plateau
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What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
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Methods of Dendrochronology
inferredcites →https://doi.org/10.1007/bf01092410openalex-snapshot
Was there a ?medieval warm period?, and if so, where and when?
inferredcites →https://doi.org/10.1016/1040-6182(96)00006-7openalex-snapshot
High resolution record of paleoclimate since the Little Ice Age from the Tibetan ice cores
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Annual climate variability in the Holocene: interpreting the message of ancient trees
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Global-scale temperature patterns and climate forcing over the past six centuries
inferredcites →https://doi.org/10.1038/scientificamerican0572-92openalex-snapshot
Tree Rings and Climate
inferredcites →https://doi.org/10.1126/science.1066208openalex-snapshot
Low-Frequency Signals in Long Tree-Ring Chronologies for Reconstructing Past Temperature Variability
inferredcites →https://doi.org/10.1126/science.284.5416.926openalex-snapshot
Seeing the Wood from the Trees
inferredcites →https://doi.org/10.1175/1520-0450(1971)010<0845:mtfstg>2.0.co;2openalex-snapshot
Multivariate Techniques for Specifying Tree-Growth and Climate Relationships and for Reconstructing Anomalies in Paleoclimate
inferredcites →https://doi.org/10.1177/095968369300300409openalex-snapshot
'Little Ice Age' summer temperature variations: their nature and relevance to recent global warming trends
inferredcites →https://doi.org/10.1177/095968369500500211openalex-snapshot
The 'segment length curse' in long tree-ring chronology development for palaeoclimatic studies
inferredcites →https://doi.org/10.1191/0959683602hl576edopenalex-snapshot
ADVANCE-10K: a European contribution towards a hemispheric dendroclimatology for the Holocene
What points at this work
Incoming claims: where this work appears in other papers’ reference lists and arguments.
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Diverse Effects of Climate Changes and Human Activities on Sedimentary Nitrogen Isotope (Δ15nsed.) in Lakes Across Different Regions of China Since the Late Holocene
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Holocene geomorphic process recorded by OSL dating of Linggo Co delta and outwash terraces from the Puruogangri area in the central Tibetan Plateau
inferred← citeshttps://doi.org/10.1002/gj.3308openalex-snapshot
High‐resolution paleoclimatic records spanning the past 30 cal ka BP inferred from Qionghai Lake sediments in south‐west China: Insights from geochemical investigations and grain‐size characteristics
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Reconstruction of a 1436‐year soil moisture and vegetation water use history based on tree‐ring widths from Qilian junipers in northeastern Qaidam Basin, northwestern China
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Tree‐ring based drought reconstruction in the central Hengduan Mountains region (China) since A.D. 1655
inferred← citeshttps://doi.org/10.1002/joc.1956openalex-snapshot
Annual temperature history in Southwest Tibet during the last 400 years recorded by tree rings
inferred← citeshttps://doi.org/10.1002/joc.2000openalex-snapshot
Temperature reconstruction from tree‐ring maximum density of Balfour spruce in eastern Tibet, China
inferred← citeshttps://doi.org/10.1002/joc.2085openalex-snapshot
Annual precipitation reconstruction since AD 775 based on tree rings from the Qilian Mountains, northwestern China
inferred← citeshttps://doi.org/10.1002/joc.2143openalex-snapshot
Rainfall history for the Hexi Corridor in the arid northwest China during the past 620 years derived from tree rings
inferred← citeshttps://doi.org/10.1002/joc.3715openalex-snapshot
Spatial patterns of moisture variations across the Tibetan Plateau during the past 700 years and their relationship with Atmospheric Oscillation modes
inferred← citeshttps://doi.org/10.1002/joc.4207openalex-snapshot
Tree‐ring‐based temperature reconstruction for the Wolong Natural Reserve, western Sichuan Plateau of China
inferred← citeshttps://doi.org/10.1002/joc.4208openalex-snapshot
An 850‐year tree‐ring‐based reconstruction of drought history in the western Qilian Mountains of northwestern China
inferred← citeshttps://doi.org/10.1002/joc.4575openalex-snapshot
Tree‐ring recorded drought variability in the northern Min Mountains of northwestern China
inferred← citeshttps://doi.org/10.1002/joc.6239openalex-snapshot
Post‐industrial late summer warming recorded in tree‐ring density in the eastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1002/joc.6733openalex-snapshot
Tree ring width‐based January–March mean minimum temperature reconstruction from Larix gmelinii in the Greater Khingan Mountains, China since AD 1765
inferred← citeshttps://doi.org/10.1002/joc.7108openalex-snapshot
Shrub‐rings used to reconstruct drought history of the central Alxa desert, northwest China
inferred← citeshttps://doi.org/10.1002/joc.8373openalex-snapshot
Long‐term evolution and non‐stationary behaviours of daily and subdaily precipitation extremes in China
inferred← citeshttps://doi.org/10.1002/joc.8591openalex-snapshot
Evolution of megadrought and pluvial events in the Qaidam Basin and Hexi Corridor, Northwest China, during the period 455–2100 CE
inferred← citeshttps://doi.org/10.1002/rcm.5034openalex-snapshot
Correlations of carbon isotope discrimination with element and ash contents in two Sabina evergreen trees in northwest China: patterns and implications
inferred← citeshttps://doi.org/10.1007/978-3-319-28977-9_17openalex-snapshot
Dendroecological Perspectives on Climate Change on the Southern Tibetan Plateau
inferred← citeshttps://doi.org/10.1007/978-3-319-61669-8_15openalex-snapshot
Hydraulic Cities, Colonial Catastrophes, and Nomadic Empires: Human-Environment Interactions in Asia
inferred← citeshttps://doi.org/10.1007/978-4-431-55540-7_6openalex-snapshot
Reconstructing Mid- to Late Holocene East Asian Monsoon Variability in the Jingpo Lake, Northeastern China
inferred← citeshttps://doi.org/10.1007/978-94-007-7817-7_3openalex-snapshot
Asian Monsoon Variability Recorded in Other Archives
inferred← citeshttps://doi.org/10.1007/bf02889758openalex-snapshot
Decadal-scale precipitation variations in arid and semiarid zones of northern China during the last 500 years
inferred← citeshttps://doi.org/10.1007/s00254-006-0421-zopenalex-snapshot
The relation of seasonal pattern in stable carbon compositions to meteorological variables in the leaves of Sabina przewalskii Kom. and Sabina chinensis (Lin.) Ant.
inferred← citeshttps://doi.org/10.1007/s00254-006-0466-zopenalex-snapshot
The variations of stable-carbon isotope ratios in Qilian juniper in northwestern China
inferred← citeshttps://doi.org/10.1007/s00334-017-0664-5openalex-snapshot
Late Holocene vegetation, climate, human and fire history of the forest-steppe-ecosystem inferred from core G2-A in the ‘Altai Tavan Bogd’ conservation area in Mongolia
inferred← citeshttps://doi.org/10.1007/s00376-007-1024-7openalex-snapshot
Temperature and precipitation changes in China during the Holocene
inferred← citeshttps://doi.org/10.1007/s00376-009-8070-2openalex-snapshot
An integrated analysis of dry-wet variability in western China for the last 4–5 centuries
inferred← citeshttps://doi.org/10.1007/s00376-009-9028-0openalex-snapshot
Drought reconstruction in the Qilian Mountains over the last two centuries and its implications for large-scale moisture patterns
inferred← citeshttps://doi.org/10.1007/s00382-004-0473-2openalex-snapshot
Annual precipitation since 515 BC reconstructed from living and fossil juniper growth of northeastern Qinghai Province, China
inferred← citeshttps://doi.org/10.1007/s00382-009-0636-2openalex-snapshot
Reconstructed droughts for the southeastern Tibetan Plateau over the past 568 years and its linkages to the Pacific and Atlantic Ocean climate variability
inferred← citeshttps://doi.org/10.1007/s00382-014-2431-yopenalex-snapshot
Millennium tree-ring reconstruction of drought variability in the eastern Qilian Mountains, northwest China
inferred← citeshttps://doi.org/10.1007/s00382-016-3433-8openalex-snapshot
Spatiotemporal drought variability of the eastern Tibetan Plateau during the last millennium
inferred← citeshttps://doi.org/10.1007/s00382-018-4244-xopenalex-snapshot
Interdecadal modulation of the Atlantic Multi-decadal Oscillation (AMO) on southwest China’s temperature over the past 250 years
inferred← citeshttps://doi.org/10.1007/s00382-021-05991-7openalex-snapshot
Evaluating cloud radiative effect from CMIP6 and two satellite datasets over the Tibetan Plateau based on CERES observation
inferred← citeshttps://doi.org/10.1007/s00382-022-06518-4openalex-snapshot
Evaluation and projections of surface air temperature over the Tibetan Plateau from CMIP6 and CMIP5: warming trend and uncertainty
inferred← citeshttps://doi.org/10.1007/s00382-023-06932-2openalex-snapshot
Little Ice Age cooling in the Western Hengduan Mountains, China: a 600-year warm-season temperature reconstruction from tree rings
inferred← citeshttps://doi.org/10.1007/s00468-007-0170-yopenalex-snapshot
Age-dependent tree-ring growth responses to climate in Qilian juniper (Sabina przewalskii Kom.)
inferred← citeshttps://doi.org/10.1007/s00468-009-0406-0openalex-snapshot
Growth variation in Abies georgei var. smithii along altitudinal gradients in the Sygera Mountains, southeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1007/s00468-011-0590-6openalex-snapshot
Age and radial growth pattern of four tree species in a subtropical forest of China
inferred← citeshttps://doi.org/10.1007/s00468-012-0757-9openalex-snapshot
Temperature variability inferred from tree-ring widths in the Dabie Mountains of subtropical central China
inferred← citeshttps://doi.org/10.1007/s00468-012-0772-xopenalex-snapshot
Individual and time-varying tree-ring growth to climate sensitivity of Pinus tabuliformis Carr. and Sabina przewalskii Kom. in the eastern Qilian Mountains, China
inferred← citeshttps://doi.org/10.1007/s00468-012-0776-6openalex-snapshot
Climate–growth analysis of Qilian juniper across an altitudinal gradient in the central Qilian Mountains, northwest China
inferred← citeshttps://doi.org/10.1007/s00468-012-0823-3openalex-snapshot
How can Populus euphratica cope with extremely dry growth conditions at 2,800 m a.s.l. on the northern Tibetan Plateau?
inferred← citeshttps://doi.org/10.1007/s00468-012-0833-1openalex-snapshot
A dendroclimatic analysis of regional moisture variation in the northeastern Tibetan Plateau during the past 150 years
inferred← citeshttps://doi.org/10.1007/s00468-013-0951-4openalex-snapshot
Tree-ring response of subtropical tree species in southeast China on regional climate and sea-surface temperature variations
inferred← citeshttps://doi.org/10.1007/s00468-014-1119-6openalex-snapshot
Age-independent climate-growth response of Chinese pine (Pinus tabulaeformis Carrière) in North China
inferred← citeshttps://doi.org/10.1007/s00468-015-1286-0openalex-snapshot
Forward modeling analyses of Qilian Juniper (Sabina przewalskii) growth in response to climate factors in different regions of the Qilian Mountains, northwestern China
inferred← citeshttps://doi.org/10.1007/s00468-015-1287-zopenalex-snapshot
Human activity impacts on the stem radial growth of Populus euphratica riparian forests in China’s Ejina Oasis, using tree-ring analysis
inferred← citeshttps://doi.org/10.1007/s00468-015-1318-9openalex-snapshot
Annual and intra-annual growth dynamics of Myricaria elegans shrubs in arid Himalaya
inferred← citeshttps://doi.org/10.1007/s00468-015-1348-3openalex-snapshot
Growth–climate relationships along an elevation gradient on a southeast-facing mountain slope in the semi-arid eastern Qaidam Basin, northeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1007/s00484-013-0757-5openalex-snapshot
Responses of tree-ring growth and crop yield to drought indices in the Shanxi province, North China
inferred← citeshttps://doi.org/10.1007/s00484-016-1297-6openalex-snapshot
Tree-ring-based reconstruction of streamflow for the Zaqu River in the Lancang River source region, China, over the past 419 years
inferred← citeshttps://doi.org/10.1007/s00484-021-02142-9openalex-snapshot
A 168-year temperature recording based on tree rings and latitude differences in temperature changes in northeast China
inferred← citeshttps://doi.org/10.1007/s00484-024-02683-9openalex-snapshot
Tree-ring based summer temperature variability since 1790 CE in the Hindu Kush region of northern Pakistan
inferred← citeshttps://doi.org/10.1007/s00704-008-0085-6openalex-snapshot
Tree-ring evidence of recent abnormal warming on the southeast Tibetan Plateau
inferred← citeshttps://doi.org/10.1007/s00704-011-0419-7openalex-snapshot
Early summer temperature reconstruction in the eastern Tibetan plateau since ad 1440 using tree-ring width of Sabina tibetica
inferred← citeshttps://doi.org/10.1007/s00704-011-0451-7openalex-snapshot
Eigen analysis of tree-ring records: Part 1, a limited representativeness of regional curve
inferred← citeshttps://doi.org/10.1007/s00704-011-0467-zopenalex-snapshot
Climatic change of inland river basin in an arid area: a case study in northern Xinjiang, China
inferred← citeshttps://doi.org/10.1007/s00704-011-0468-yopenalex-snapshot
Eigen analysis of tree-ring records: part 2, posing the eigen problem
inferred← citeshttps://doi.org/10.1007/s00704-011-0576-8openalex-snapshot
Ensemble empirical mode decomposition for tree-ring climate reconstructions
inferred← citeshttps://doi.org/10.1007/s00704-012-0725-8openalex-snapshot
Abrupt temperature changes during the last 1,500 years
inferred← citeshttps://doi.org/10.1007/s00704-013-0898-9openalex-snapshot
Frost-free season lengthening and its potential cause in the Tibetan Plateau from 1960 to 2010
inferred← citeshttps://doi.org/10.1007/s00704-016-1772-3openalex-snapshot
Reconstruction and analysis of the past five centuries of streamflow on northern slopes on Tianshan Mountains in Northern Xinjiang, China
inferred← citeshttps://doi.org/10.1007/s00704-020-03169-5openalex-snapshot
Tree ring–based minimum temperature reconstruction in the central Hengduan Mountains, China
inferred← citeshttps://doi.org/10.1007/s00704-020-03326-wopenalex-snapshot
Tree-ring-based temperature reconstruction since 1766 ce in the eastern Tianshan Mountains, arid Central Asia
inferred← citeshttps://doi.org/10.1007/s10584-006-9082-xopenalex-snapshot
The 1920S Drought Recorded by Tree Rings and Historical Documents in the Semi-Arid and Arid Areas of Northern China
inferred← citeshttps://doi.org/10.1007/s10584-006-9135-1openalex-snapshot
Tree rings and climate for the last 680 years in Wulan area of northeastern Qinghai-Tibetan Plateau
inferred← citeshttps://doi.org/10.1007/s10584-011-0111-zopenalex-snapshot
Tree-ring reconstruction of summer temperature for A.D. 1475–2003 in the central Hengduan Mountains, Northwestern Yunnan, China
inferred← citeshttps://doi.org/10.1007/s10584-015-1531-yopenalex-snapshot
Global warming-related tree growth decline and mortality on the north-eastern Tibetan plateau
inferred← citeshttps://doi.org/10.1007/s10584-016-1695-0openalex-snapshot
500-yr. precipitation variability in Southern Taihang Mountains, China, and its linkages to ENSO and PDO
inferred← citeshttps://doi.org/10.1007/s10980-011-9685-0openalex-snapshot
On the vulnerability of oasis forest to changing environmental conditions: perspectives from tree rings
inferred← citeshttps://doi.org/10.1007/s11258-006-9258-5openalex-snapshot
Species-dependent responses of juniper and spruce to increasing CO2 concentration and to climate in semi-arid and arid areas of northwestern China
inferred← citeshttps://doi.org/10.1007/s11284-017-1538-0openalex-snapshot
Divergent tree growth response to recent climate warming of Abies faxoniana at alpine treelines in east edge of Tibetan Plateau
inferred← citeshttps://doi.org/10.1007/s11430-006-0408-3openalex-snapshot
Precipitation variation in the northeastern Tibetan Plateau recorded by the tree rings since 850 AD and its relevance to the Northern Hemisphere temperature
inferred← citeshttps://doi.org/10.1007/s11430-007-0154-1openalex-snapshot
Asymmetric variability between maximum and minimum temperatures in Northeastern Tibetan Plateau: Evidence from tree rings
inferred← citeshttps://doi.org/10.1007/s11430-008-0057-9openalex-snapshot
Optically stimulated luminescence dating of aeolian sand in the Otindag dune field and Holocene climate change
inferred← citeshttps://doi.org/10.1007/s11430-008-0084-6openalex-snapshot
Tree-ring-based reconstruction of the April to September mean temperature since 1826 AD for north-central Shaanxi Province, China
inferred← citeshttps://doi.org/10.1007/s11430-009-0025-zopenalex-snapshot
Annual temperatures during the last 2485 years in the mid-eastern Tibetan Plateau inferred from tree rings
inferred← citeshttps://doi.org/10.1007/s11430-012-4374-7openalex-snapshot
Preliminary multiproxy surface air temperature field reconstruction for China over the past millennium
inferred← citeshttps://doi.org/10.1007/s11430-012-4375-6openalex-snapshot
Analysis of reconstructed annual precipitation from tree-rings for the past 500 years in the middle Qilian Mountain
inferred← citeshttps://doi.org/10.1007/s11430-015-5188-1openalex-snapshot
Response of Pinus taiwanensis growth to climate changes at its southern limit of Daiyun Mountain, mainland China Fujian Province
inferred← citeshttps://doi.org/10.1007/s11430-018-9327-1openalex-snapshot
A 1556 year-long early summer moisture reconstruction for the Hexi Corridor, Northwestern China
inferred← citeshttps://doi.org/10.1007/s11430-023-1296-9openalex-snapshot
The relationship between interannual dry/wet changes and nomadic wars in the Hexi Corridor region of China during the period 241–1912 A.D.
inferred← citeshttps://doi.org/10.1007/s11434-007-0351-5openalex-snapshot
Tree-ring based PDSI reconstruction since AD 1842 in the Ortindag Sand Land, east Inner Mongolia
inferred← citeshttps://doi.org/10.1007/s11434-008-0067-1openalex-snapshot
Pollen record and environmental evolution of Caotanhu wetland in Xinjiang since 4550 cal. a BP
inferred← citeshttps://doi.org/10.1007/s11434-008-0400-8openalex-snapshot
Millennial temperature reconstruction based on tree-ring widths of Qilian juniper from Wulan, Qinghai Province, China
inferred← citeshttps://doi.org/10.1007/s11434-009-0201-8openalex-snapshot
A 1000-year chironomid-based salinity reconstruction from varved sediments of Sugan Lake, Qaidam Basin, arid Northwest China, and its palaeoclimatic significance
inferred← citeshttps://doi.org/10.1007/s11434-010-3182-8openalex-snapshot
Temperature variability since A.D. 1837 inferred from tree-ring maximum density of Abies fabri on Gongga Mountain, China
inferred← citeshttps://doi.org/10.1007/s11434-010-3235-zopenalex-snapshot
Tree-ring-based May–July mean temperature history for Lüliang Mountains, China, since 1836
inferred← citeshttps://doi.org/10.1007/s11434-010-3237-xopenalex-snapshot
May–June mean maximum temperature change during 1360–2005 as reconstructed by tree rings of Sabina Tibetica in Zaduo, Qinghai Province
inferred← citeshttps://doi.org/10.1007/s11434-010-4215-zopenalex-snapshot
Tree ring based streamflow reconstruction for the Upper Yellow River over the past 1234 years
inferred← citeshttps://doi.org/10.1007/s11434-011-4456-5openalex-snapshot
Process-based modeling analyses of Sabina przewalskii growth response to climate factors around the northeastern Qaidam Basin
inferred← citeshttps://doi.org/10.1007/s11434-011-4706-6openalex-snapshot
Tree-ring-based annual precipitation reconstruction in Kalaqin, Inner Mongolia for the last 238 years
inferred← citeshttps://doi.org/10.1007/s11434-012-5055-9openalex-snapshot
Reconstructing mean maximum temperatures of May–August from tree-ring maximum density in North Da Hinggan Mountains, China
inferred← citeshttps://doi.org/10.1007/s11434-012-5539-7openalex-snapshot
A 457-year reconstruction of precipitation in the southeastern Qinghai-Tibet Plateau, China using tree-ring records
inferred← citeshttps://doi.org/10.1007/s11434-013-5913-0openalex-snapshot
Moisture variations over the past millennium characterized by Qaidam Basin tree-ring δ 18O
inferred← citeshttps://doi.org/10.1007/s11442-007-0175-xopenalex-snapshot
Standardization of Qilian Juniper ring-width series in the eastern margin of the Qaidam Basin
inferred← citeshttps://doi.org/10.1007/s11442-007-0293-5openalex-snapshot
January to August temperature variability since 1776 inferred from tree-ring width of Pinus tabulaeformis in Helan Mountain
inferred← citeshttps://doi.org/10.1007/s11442-008-0201-7openalex-snapshot
Reconstruction of summer temperature variation from maximum density of alpine pine during 1917–2002 for west Sichuan Plateau, China
inferred← citeshttps://doi.org/10.1007/s11442-009-0750-4openalex-snapshot
Wet-dry changes in the borderland of Shaanxi, Gansu and Ningxia from 1208 to 1369 based on historical records
inferred← citeshttps://doi.org/10.1007/s11442-015-1226-3openalex-snapshot
Which climatic factors limit radial growth of Qilian juniper at the upper treeline on the northeastern Tibetan Plateau?
inferred← citeshttps://doi.org/10.1007/s11442-016-1298-8openalex-snapshot
Integrated studies of physical geography in China: Review and prospects
inferred← citeshttps://doi.org/10.1007/s11442-016-1301-4openalex-snapshot
Recent advances on reconstruction of climate and extreme events in China for the past 2000 years
inferred← citeshttps://doi.org/10.1007/s11629-017-4425-9openalex-snapshot
Mixed signals in trends of variance in high-elevation tree ring chronologies
inferred← citeshttps://doi.org/10.1007/s11629-019-5703-5openalex-snapshot
Stability evaluation of radial growth of Picea schrenkiana in different age groups in response to climate change in the eastern Tianshan Mountains
inferred← citeshttps://doi.org/10.1007/s11676-024-01697-8openalex-snapshot
Radial growth in Qinghai spruce is most sensitive to severe drought in the Qilian Mountains of Northwest China
inferred← citeshttps://doi.org/10.1007/s11707-010-0111-8openalex-snapshot
Comparisons of drought variability between central High Asia and monsoonal Asia: Inferred from tree rings
inferred← citeshttps://doi.org/10.1007/s11707-015-0575-7openalex-snapshot
Emergence of ancient cities in relation to geopolitical circumstances and climate change during late Holocene in northeastern Tibetan Plateau, China
inferred← citeshttps://doi.org/10.1007/s11738-011-0815-8openalex-snapshot
Seasonal changes in non-structural carbohydrates and sucrose metabolism enzymes in two Sabina species
inferred← citeshttps://doi.org/10.1007/s12665-014-3519-8openalex-snapshot
Spatio-temporal process of oasification in the middle-Heihe River basin during 1368–1949 AD, China
inferred← citeshttps://doi.org/10.1007/s12665-017-6581-1openalex-snapshot
Tree-ring recorded moisture variations over the past millennium in the Hexi Corridor, northwest China
inferred← citeshttps://doi.org/10.1007/s12685-012-0057-8openalex-snapshot
Variations in discharge from the Qilian mountains, northwest China, and its effect on the agricultural communities of the Heihe basin, over the last two millennia
inferred← citeshttps://doi.org/10.1007/s40333-015-0138-5openalex-snapshot
Tree-ring-based reconstruction of temperature variability (1445–2011) for the upper reaches of the Heihe River Basin, Northwest China
inferred← citeshttps://doi.org/10.1016/j.aeolia.2013.05.002openalex-snapshot
Moisture availability over the past five centuries indicated by carbon isotopes of Tamarix taklamakanensis leaves in a nebkha profile in the Central Taklimakan Desert, NW China
inferred← citeshttps://doi.org/10.1016/j.agrformet.2018.06.011openalex-snapshot
Cambial phenology and xylogenesis of Juniperus przewalskii over a climatic gradient is influenced by both temperature and drought
inferred← citeshttps://doi.org/10.1016/j.anifeedsci.2024.116150openalex-snapshot
Effect of psychrotrophic Lactiplantibacillus plantarum L75 with exoploysaccharides-producing property on fermentation, bacterial community, and antioxidant activity of oat silage at low temperature
inferred← citeshttps://doi.org/10.1016/j.apgeochem.2013.04.004openalex-snapshot
Modern carbon burial in Lake Qinghai, China
inferred← citeshttps://doi.org/10.1016/j.catena.2019.03.036openalex-snapshot
Centennial-scale process activity in a complex landslide body in the Qilian Mountains, northeast Tibetan Plateau, China
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2022.121005openalex-snapshot
Climatic and environmental changes in the Baidunzi wetland, Northwest China, over the last 800 years inferred from glycerol dialkyl glycerol tetraethers
inferred← citeshttps://doi.org/10.1016/j.coldregions.2013.03.005openalex-snapshot
Impact of experimental warming on soil temperature and moisture of the shallow active layer of wet meadows on the Qinghai-Tibet Plateau
inferred← citeshttps://doi.org/10.1016/j.dendro.2006.10.009openalex-snapshot
A millennium-long tree-ring chronology of Sabina przewalskii on northeastern Qinghai-Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.dendro.2007.08.002openalex-snapshot
Dating of tombs in Delingha, Qinghai Province, China, on the basis of a 2332-year tree-ring juniper chronology (Sabina przewalskii Kom) (1575 BC–756 AD)
inferred← citeshttps://doi.org/10.1016/j.dendro.2009.12.002openalex-snapshot
An unstable tree-growth response to climate in two 500 year chronologies, North Eastern Qinghai-Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.dendro.2010.07.001openalex-snapshot
Summer droughts depress radial growth of Picea abies in pristine taiga of the Arkhangelsk province, northwestern Russia
inferred← citeshttps://doi.org/10.1016/j.dendro.2010.11.001openalex-snapshot
Dynamic relationships between Picea crassifolia growth and climate at upper treeline in the Qilian Mts., Northeast Tibetan Plateau, China
inferred← citeshttps://doi.org/10.1016/j.dendro.2012.07.004openalex-snapshot
Drought variations in the middle Qilian Mountains, northeast Tibetan Plateau, over the last 450 years as reconstructed from tree rings
inferred← citeshttps://doi.org/10.1016/j.dendro.2012.07.005openalex-snapshot
A simple and rapid preparation of pure cellulose confirmed by monosaccharide compositions, δ13C, yields and C%
inferred← citeshttps://doi.org/10.1016/j.dendro.2012.12.001openalex-snapshot
Growth response of Sabina tibetica to climate factors along an elevation gradient in south Tibet
inferred← citeshttps://doi.org/10.1016/j.dendro.2013.02.001openalex-snapshot
Annual precipitation variability inferred from tree-ring width chronologies in the Changling–Shoulu region, China, during AD 1853–2007
inferred← citeshttps://doi.org/10.1016/j.dendro.2014.09.001openalex-snapshot
Dendroclimatic reconstruction of autumn–winter mean minimum temperature in the eastern Tibetan Plateau since 1600 AD
inferred← citeshttps://doi.org/10.1016/j.dendro.2015.05.001openalex-snapshot
Enigmatic High-Asian tree rings: A postcard from the roof of the world (Kathmandu, Nepal)
inferred← citeshttps://doi.org/10.1016/j.dendro.2015.11.001openalex-snapshot
A 382-year reconstruction of August mean minimum temperature from tree-ring maximum latewood density on the southeastern Tibetan Plateau, China
inferred← citeshttps://doi.org/10.1016/j.dendro.2016.02.004openalex-snapshot
Universal growth modes of high-elevation conifers
inferred← citeshttps://doi.org/10.1016/j.dendro.2016.03.006openalex-snapshot
Towards improving the Central Asian dendrochronological network—New data from Tajikistan, Pamir-Alay
inferred← citeshttps://doi.org/10.1016/j.dendro.2016.05.001openalex-snapshot
Tree-ring-based reconstruction of drought variability (1792–2011) in the middle reaches of the Fen River, North China
inferred← citeshttps://doi.org/10.1016/j.dendro.2017.06.002openalex-snapshot
Historic log structures as ecological archives: A case study from eastern North America
inferred← citeshttps://doi.org/10.1016/j.dendro.2018.02.004openalex-snapshot
Climate-growth response of Chinese white pine (Pinus armandii) at different age groups in the Baiyunshan National Nature Reserve, central China
inferred← citeshttps://doi.org/10.1016/j.dendro.2018.08.004openalex-snapshot
Summer temperature variability inferred from tree-ring records in the central Hengduan Mountains, southeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.dendro.2019.04.002openalex-snapshot
A 2917-year tree-ring-based reconstruction of precipitation for the Buerhanbuda Mts., Southeastern Qaidam Basin, China
inferred← citeshttps://doi.org/10.1016/j.dendro.2020.125725openalex-snapshot
Moisture changes over the past 467 years in the central Hexi Corridor, northwestern China
inferred← citeshttps://doi.org/10.1016/j.dendro.2021.125914openalex-snapshot
Altitudinal trends in climate change result in radial growth variation of Pinus yunnanensis at an arid-hot valley of southwest China
inferred← citeshttps://doi.org/10.1016/j.dendro.2024.126202openalex-snapshot
Development of dendrochronology and its track in China since 1990 reflected by bibliometric analysis
inferred← citeshttps://doi.org/10.1016/j.earscirev.2016.03.007openalex-snapshot
Unsaturated zone hydrostratigraphies: A novel archive of past climates in dryland continental regions
inferred← citeshttps://doi.org/10.1016/j.earscirev.2019.02.012openalex-snapshot
Recent advances in dendroclimatology in China
inferred← citeshttps://doi.org/10.1016/j.earscirev.2022.104041openalex-snapshot
Asian summer monsoon variability, global teleconnections, and dynamics during the last 1,000 years
inferred← citeshttps://doi.org/10.1016/j.egyr.2020.08.024openalex-snapshot
Economic development and climate change. Which is the cause and which the effect?
inferred← citeshttps://doi.org/10.1016/j.epsl.2019.04.030openalex-snapshot
Hydroclimatic seasonality recorded by tree ring δ18O signature across a Himalayan altitudinal transect
inferred← citeshttps://doi.org/10.1016/j.foreco.2006.09.016openalex-snapshot
Topography- and species-dependent growth responses of Sabina przewalskii and Picea crassifolia to climate on the northeast Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.foreco.2009.04.017openalex-snapshot
Growth–climate responses of high-elevation conifers in the central Hengduan Mountains, southwestern China
inferred← citeshttps://doi.org/10.1016/j.foreco.2010.06.034openalex-snapshot
Divergent growth responses and increasing temperature limitation of Qinghai spruce growth along an elevation gradient at the northeast Tibet Plateau
inferred← citeshttps://doi.org/10.1016/j.gecadv.2023.100004openalex-snapshot
Assessing the past and future dynamics of the Asian summer monsoon: Insights from palaeomonsoon synthesis and CMIP6 data
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2007.10.008openalex-snapshot
Tree-ring based summer temperature reconstruction for the source region of the Yangtze River on the Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2007.12.003openalex-snapshot
Sensitive response of desert vegetation to moisture change based on a near-annual resolution pollen record from Gahai Lake in the Qaidam Basin, northwest China
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2009.07.008openalex-snapshot
Temperature changes on the Tibetan Plateau during the past 600 years inferred from ice cores and tree rings
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2010.10.013openalex-snapshot
Regional extreme climate events on the northeastern Tibetan Plateau since AD 1450 inferred from tree rings
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2011.10.009openalex-snapshot
Tree-ring based reconstruction of drought variability (1615–2009) in the Kongtong Mountain area, northern China
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2012.01.005openalex-snapshot
Reconstructed temperature for Yong'an, Fujian, Southeast China: Linkages to the Pacific Ocean climate variability
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2013.04.010openalex-snapshot
Precipitation over the past four centuries in the Dieshan Mountains as inferred from tree rings: An introduction to an HHT-based method
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2014.12.002openalex-snapshot
Drought signals in tree-ring stable oxygen isotope series of Qilian juniper from the arid northeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2016.04.010openalex-snapshot
Reconstruction of biological drought conditions during the past 2847 years in an alpine environment of the northeastern Tibetan Plateau, China, and possible linkages to solar forcing
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2019.103000openalex-snapshot
Changes in wetland salinity, human activity and wetland vegetation abundances over the past 900 years
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105477openalex-snapshot
Tree-ring records reveal intensified early-summer hot–dry coupling in the Northeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.jaridenv.2012.06.013openalex-snapshot
Dry/wet variation recorded by shrub tree-rings in the central Badain Jaran Desert of northwestern China
inferred← citeshttps://doi.org/10.1016/j.jaridenv.2013.02.011openalex-snapshot
Precipitation variability in Hulunbuir, northeastern China since 1829 AD reconstructed from tree-rings and its linkage with remote oceans
inferred← citeshttps://doi.org/10.1016/j.jaridenv.2013.12.001openalex-snapshot
Is there a link between the rise and fall of the Tuyuhun tribe (northwestern China) and climatic variations in the 4th–7th centuries AD?
inferred← citeshttps://doi.org/10.1016/j.jasrep.2017.04.008openalex-snapshot
Something old, something new, something borrowed: New insights to human-environment interaction in medieval Novgorod inferred from tree rings
inferred← citeshttps://doi.org/10.1016/j.jhydrol.2021.126836openalex-snapshot
Regional moisture sources and Indian summer monsoon (ISM) moisture transport from simultaneous monitoring of precipitation isotopes on the southeastern and northeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.jseaes.2016.03.024openalex-snapshot
Different responses of sedimentary δ15N to climatic changes and anthropogenic impacts in lakes across the Eastern margin of the Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.marmicro.2018.10.003openalex-snapshot
March SST reconstruction in the South China Sea based on Pinus massoniana tree-ring widths from Changting, Fujian, in Southeast China since 1893 CE
inferred← citeshttps://doi.org/10.1016/j.palaeo.2004.04.001openalex-snapshot
Holocene vegetation and climate of the Alashan Plateau, NW China, reconstructed from pollen data
inferred← citeshttps://doi.org/10.1016/j.palaeo.2009.02.028openalex-snapshot
A 2000 year geochemical record of palaeoclimate and hydrology derived from dune sand moisture
inferred← citeshttps://doi.org/10.1016/j.palaeo.2009.06.030openalex-snapshot
Summer monsoon precipitation variations in central China over the past 750years derived from a high-resolution absolute-dated stalagmite
inferred← citeshttps://doi.org/10.1016/j.palaeo.2010.06.017openalex-snapshot
Tree ring recorded May–August temperature variations since A.D. 1585 in the Gaoligong Mountains, southeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.palaeo.2010.08.008openalex-snapshot
A 2700-year high resolution pollen record of climate change from varved Sugan Lake in the Qaidam Basin, northeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.palaeo.2013.08.011openalex-snapshot
Reconstructed May–July mean maximum temperature since 1745AD based on tree-ring width of Pinus tabulaeformis in Qianshan Mountain, China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.01.003openalex-snapshot
Tree-ring density inferred late summer temperature variability over the past three centuries in the Gaoligong Mountains, southeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.03.003openalex-snapshot
Tree ring density-based warm-season temperature reconstruction since A.D. 1610 in the eastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.08.003openalex-snapshot
A tree-ring based reconstruction of summer relative humidity variability in eastern Mongolian Plateau and its associations with the Pacific and Indian Oceans
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.12.003openalex-snapshot
The spatial distribution of precipitation over the West Qinling region, China, AD 1470–2000
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111442openalex-snapshot
Late Holocene Temperature and Precipitation Variations in an Alpine Region of the Northeastern Tibetan Plateau and Their Response to Global Climate Change
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.112896openalex-snapshot
Climate and lake ecosystem evolution over the last millennium on the north-eastern Tibetan Plateau: Insights from stable isotope records of gastropod shells in Xing Co
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113220openalex-snapshot
Earlywood blue intensity of Picea purpurea reveals June minimum temperature variability in Eastern Tibetan Plateau since 1671CE
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113253openalex-snapshot
June–September mean temperature variability in the eastern Qinghai-Tibet Plateau over the past 225 years based on high quality tree-ring records
inferred← citeshttps://doi.org/10.1016/j.quaint.2007.10.013openalex-snapshot
Climate change over the past 2000 years in Western China
inferred← citeshttps://doi.org/10.1016/j.quaint.2007.11.020openalex-snapshot
Late Holocene climatic and environmental changes in arid central Asia
inferred← citeshttps://doi.org/10.1016/j.quaint.2010.01.020openalex-snapshot
Records of late-Holocene East Asian winter monsoon in the East China Sea: Key grain-size component of quartz versus bulk sediments
inferred← citeshttps://doi.org/10.1016/j.quaint.2012.03.033openalex-snapshot
Tree-ring derived temperature records in the central Loess Plateau, China
inferred← citeshttps://doi.org/10.1016/j.quaint.2012.03.034openalex-snapshot
A dendroclimatic reconstruction of May–June mean temperature variation in the Heng Mounatins, north China, since 1767 AD
inferred← citeshttps://doi.org/10.1016/j.quaint.2012.03.038openalex-snapshot
Spatiotemporal drought variability for central and eastern Asia over the past seven centuries derived from tree-ring based reconstructions
inferred← citeshttps://doi.org/10.1016/j.quaint.2012.03.044openalex-snapshot
Tree-ring based runoff reconstruction of the upper Fenhe River basin, North China, since 1799 AD
inferred← citeshttps://doi.org/10.1016/j.quaint.2012.03.045openalex-snapshot
Tree-ring-based precipitation reconstruction for Mt. Xinglong, China, since AD 1679
inferred← citeshttps://doi.org/10.1016/j.quaint.2012.04.011openalex-snapshot
Little Ice Age glacier fluctuations reconstructed for the southeastern Tibetan Plateau using tree rings
inferred← citeshttps://doi.org/10.1016/j.quaint.2012.04.021openalex-snapshot
Reconstructed droughts for the northeastern Tibetan Plateau since AD 1411 and its linkages to the Pacific, Indian and Atlantic Oceans
inferred← citeshttps://doi.org/10.1016/j.quaint.2012.11.011openalex-snapshot
WITHDRAWN: Groundwater recharge areas of the Continental Intercalaire aquifer-hydrogeochemical and environmental isotopes: Southern Tunisia and Algeria
inferred← citeshttps://doi.org/10.1016/j.quaint.2014.12.005openalex-snapshot
Early summer temperature changes in the southern Altai Mountains of Central Asia during the past 300 years
inferred← citeshttps://doi.org/10.1016/j.quaint.2017.05.058openalex-snapshot
Bi-decadal climate reconstruction derived from a 1200-year long pollen record from the NE Qinghai-Tibet Plateau and its implications for discussion of the late Holocene environmental dynamics
inferred← citeshttps://doi.org/10.1016/j.quaint.2018.12.016openalex-snapshot
Environmental and social factors influencing the spatiotemporal variation of archaeological sites during the historical period in the Heihe River basin, northwest China
inferred← citeshttps://doi.org/10.1016/j.quaint.2021.11.013openalex-snapshot
Aeolian sand accumulation and land desertification over the past 1,500 years as revealed by two aeolian dunes in the Beiluhe Basin on interior Qinghai-Tibet Plateau, SW China
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