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Seasonal spatial heterogeneity of warming rates on the Tibetan Plateau over the past 30 years
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What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
inferredcites →https://doi.org/10.1002/1097-0088(20001130)20:14<1729::aid-joc556>3.0.co;2-yopenalex-snapshot
Climatic warming in the Tibetan Plateau during recent decades
inferredcites →https://doi.org/10.1002/2014jd022422openalex-snapshot
A 449 year warm season temperature reconstruction in the southeastern Tibetan Plateau and its relation to solar activity
inferredcites →https://doi.org/10.1002/joc.2388openalex-snapshot
The significant climate warming in the northern Tibetan Plateau and its possible causes
inferredcites →https://doi.org/10.1002/joc.3479openalex-snapshot
Recent ground surface warming and its effects on permafrost on the central Qinghai‐Tibet Plateau
inferredcites →https://doi.org/10.1002/joc.3781openalex-snapshot
The dramatic climate warming in the Qaidam Basin, northeastern Tibetan Plateau, during 1961–2010
inferredcites →https://doi.org/10.1007/s11442-007-0409-yopenalex-snapshot
Climate change over the Yarlung Zangbo River Basin during 1961–2005
inferredcites →https://doi.org/10.1016/j.gloplacha.2004.01.010openalex-snapshot
Mutual influence between human activities and climate change in the Tibetan Plateau during recent years
inferredcites →https://doi.org/10.1016/j.gloplacha.2013.02.010openalex-snapshot
Has the Northern Hemisphere been warming or cooling during the boreal winter of the last few decades?
inferredcites →https://doi.org/10.1029/2009gl037245openalex-snapshot
Warming in the Tibetan Plateau: Possible influences of the changes in surface water vapor
inferredcites →https://doi.org/10.1080/01621459.1968.10480934openalex-snapshot
Estimates of the Regression Coefficient Based on Kendall's Tau
inferredcites →https://doi.org/10.1175/1520-0442(1998)011<0202:pfcoas>2.0.co;2openalex-snapshot
Parameterizations for Cloud Overlapping and Shortwave Single-Scattering Properties for Use in General Circulation and Cloud Ensemble Models
inferredcites →https://doi.org/10.1175/1520-0442-12.1.159openalex-snapshot
Parameterization for Cloud Longwave Scattering for Use in Atmospheric Models
inferredcites →https://doi.org/10.1175/1520-0477(1987)068<0119:acceif>2.0.co;2openalex-snapshot
A Cirrus-Cloud Experiment: Intensive Field Observations Planned for Fire
inferredcites →https://doi.org/10.1175/2010jamc2376.1openalex-snapshot
New Techniques for the Detection and Adjustment of Shifts in Daily Precipitation Data Series
inferredcites →https://doi.org/10.1175/jam2504.1openalex-snapshot
Penalized Maximal t Test for Detecting Undocumented Mean Change in Climate Data Series
inferredcites →https://doi.org/10.1175/jcli-d-10-05000.1openalex-snapshot
Accelerated Changes of Environmental Conditions on the Tibetan Plateau Caused by Climate Change
What points at this work
Incoming claims: where this work appears in other papers’ reference lists and arguments.
inferred← citeshttps://doi.org/10.2139/ssrn.4858261openalex-extracted
Physical Parameterization Sensitivity of the Noah-Mp Land Surface Model for Hydrothermal Simulation in the Active Layer on the Qinghai-Tibet Plateau
inferred← citeshttps://doi.org/10.1002/asl.1041openalex-snapshot
Changes in snow depth under elevation‐dependent warming over the Tibetan Plateau
inferred← citeshttps://doi.org/10.1002/asl.998openalex-snapshot
Time‐dependent warming amplification over the Tibetan Plateau during the past few decades
inferred← citeshttps://doi.org/10.1002/joc.5221openalex-snapshot
Low‐frequency snow changes over the Tibetan Plateau
inferred← citeshttps://doi.org/10.1002/joc.5509openalex-snapshot
Seasonal patterns of warming amplification of high‐elevation stations across the globe
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/10.1007/s00382-016-3174-8openalex-snapshot
Two centuries temperature variations over subtropical southeast China inferred from Pinus taiwanensis Hayata tree-ring width
inferred← citeshttps://doi.org/10.1007/s00382-018-4346-5openalex-snapshot
Extremes in the magnitude of annual temperature cycle on the Tibetan Plateau over the past three centuries
inferred← citeshttps://doi.org/10.1007/s00382-019-04629-zopenalex-snapshot
Tree rings reveal hydroclimatic fingerprints of the Pacific Decadal Oscillation on the Tibetan Plateau
inferred← citeshttps://doi.org/10.1007/s00382-024-07436-3openalex-snapshot
Decline in daily maximum wind speed over the Tibetan Plateau during 1973–2020: an examination of likely causes
inferred← citeshttps://doi.org/10.1007/s00704-018-2435-3openalex-snapshot
Warming slowdown over the Tibetan plateau in recent decades
inferred← citeshttps://doi.org/10.1007/s10113-017-1163-zopenalex-snapshot
Warming over the Tibetan Plateau in the last 55 years based on area-weighted average temperature
inferred← citeshttps://doi.org/10.1007/s11069-025-07386-xopenalex-snapshot
Projected changes in average and extreme precipitation under global warming in Vietnam
inferred← citeshttps://doi.org/10.1007/s11629-024-8924-1openalex-snapshot
Evaluation of surface latent heat and sensible heat fluxes from ERA-5, GLDAS, and MODIS on different underlying surfaces in the Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.aosl.2022.100289openalex-snapshot
Drivers of elevation-dependent warming over the Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.atmosres.2021.105739openalex-snapshot
Winter vs. summer temperature variations on the southeastern Tibetan Plateau, 1718–2005 CE
inferred← citeshttps://doi.org/10.1016/j.dendro.2021.125827openalex-snapshot
Spatial and temporal differences in the response of Larix sibirica to climate change in the central Altai Mountains
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112390openalex-snapshot
A ring-width chronology from the southern slopes of the Qilian Mountains of China: A long-term context (255–2018 CE) for rapid warming over the northeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.quaint.2020.09.018openalex-snapshot
Summer mean temperature reconstruction based on tree-ring density over the past 440 years on the eastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.quaint.2022.10.015openalex-snapshot
Climatic and hydrological variations on the southwestern Tibetan Plateau during the last 30,000 years inferred from a sediment core of Lake Zabuye
inferred← citeshttps://doi.org/10.1016/j.scitotenv.2018.08.398openalex-snapshot
Spatial distribution and changes of permafrost on the Qinghai-Tibet Plateau revealed by statistical models during the period of 1980 to 2010
inferred← citeshttps://doi.org/10.1016/j.scitotenv.2021.149889openalex-snapshot
Snow cover persistence reverses the altitudinal patterns of warming above and below 5000 m on the Tibetan Plateau
inferred← citeshttps://doi.org/10.1017/jog.2019.20openalex-snapshot
Glacier mass balance over the central Nyainqentanglha Range during recent decades derived from remote-sensing data
inferred← citeshttps://doi.org/10.1029/2019gl084292openalex-snapshot
The Role of Winter Warming in Permafrost Change Over the Qinghai‐Tibet Plateau
inferred← citeshttps://doi.org/10.1029/2019jd030444openalex-snapshot
August‐September Temperature Variability on the Tibetan Plateau: Past, Present, and Future
inferred← citeshttps://doi.org/10.1029/2021jd035218openalex-snapshot
Isolating the Contributions of Seasonal Climate Warming to Permafrost Thermal Responses Over the Qinghai‐Tibet Plateau
inferred← citeshttps://doi.org/10.1029/2023jd039122openalex-snapshot
Strengthened Connections Between Arctic Sea Ice and Thermal Conditions Over the Tibetan Plateau in May After the 2000s
inferred← citeshttps://doi.org/10.1038/ncomms14008openalex-snapshot
Weakening of annual temperature cycle over the Tibetan Plateau since the 1870s
inferred← citeshttps://doi.org/10.1038/s41598-018-19431-wopenalex-snapshot
Diurnal cycle and seasonal variation of cloud cover over the Tibetan Plateau as determined from Himawari-8 new-generation geostationary satellite data
inferred← citeshttps://doi.org/10.1038/s43247-025-02443-6openalex-snapshot
Rapid ecological change outpaces climate warming in Tibetan glacier lakes
inferred← citeshttps://doi.org/10.1071/rj19027openalex-snapshot
Combined effects of grazing and climate warming drive shrub dominance on the Tibetan Plateau
inferred← citeshttps://doi.org/10.1080/10225706.2018.1426023openalex-snapshot
Tree-ring-density inferred August–September temperature variability on the eastern Tibetan Plateau for the past two centuries
inferred← citeshttps://doi.org/10.1088/1748-9326/ab5e01openalex-snapshot
Unprecedented recent late-summer warm extremes recorded in tree-ring density on the Tibetan Plateau
inferred← citeshttps://doi.org/10.1088/1748-9326/abb159openalex-snapshot
Volcanic eruptions, successive poor harvests and social resilience over southwest China during the 18–19th century
inferred← citeshttps://doi.org/10.1111/gcb.16592openalex-snapshot
Contrasting responses of peak vegetation growth to asymmetric warming: Evidences from FLUXNET and satellite observations
inferred← citeshttps://doi.org/10.1175/jcli-d-16-0359.1openalex-snapshot
Insensitivity of the Summer South Asian High Intensity to a Warming Tibetan Plateau in Modern Reanalysis Datasets
inferred← citeshttps://doi.org/10.1175/jcli-d-17-0664.1openalex-snapshot
Summer Cooling Driven by Large Volcanic Eruptions over the Tibetan Plateau
inferred← citeshttps://doi.org/10.1175/jcli-d-22-0624.1openalex-snapshot
Impacts of Atlantic Multidecadal Oscillation and Volcanic Forcing on the Late Summer Temperature of the Southern Tibetan Plateau
inferred← citeshttps://doi.org/10.1175/jhm-d-22-0152.1openalex-snapshot
Percentile-Based Relationship between Daily Precipitation and Surface Air Temperature over the Qinghai–Tibet Plateau
inferred← citeshttps://doi.org/10.3390/atmos10070416openalex-snapshot
No Significant Shift of Warming Trend over the Last Two Decades on the Mid-South of Tibetan Plateau
inferred← citeshttps://doi.org/10.3390/atmos11091016openalex-snapshot
The Response of Parameterized Orographic Gravity Waves to Rapid Warming over the Tibetan Plateau
inferred← citeshttps://doi.org/10.3390/land13101609openalex-snapshot
Dynamics of the Interaction between Freeze–Thaw Process and Surface Energy Budget on the Permafrost Region of the Qinghai-Tibet Plateau
inferred← citeshttps://doi.org/10.3390/land14020247openalex-snapshot
Physical Parameterization Sensitivity of Noah-MP for Hydrothermal Simulation Within the Active Layer on the Qinghai–Tibet Plateau
inferred← citeshttps://doi.org/10.3390/rs13020256openalex-snapshot
Spatio-Temporal Trends of Surface Energy Budget in Tibet from Satellite Remote Sensing Observations and Reanalysis Data
inferred← citeshttps://doi.org/10.3390/rs14205093openalex-snapshot
The Response of Land Surface Temperature Changes to the Vegetation Dynamics in the Yangtze River Basin
inferred← citeshttps://doi.org/10.3959/1536-1098-73.1.1openalex-snapshot
Millennium-Long Tree-Ring Chronology Reveals Megadroughts on the Southeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.5194/tc-12-103-2018openalex-snapshot
Recent glacier mass balance and area changes in the Kangri Karpo Mountains from DEMs and glacier inventories
inferred← citeshttps://doi.org/10.5814/j.issn.1674-764x.2019.04.007openalex-snapshot
Characterizing the Spatio-Temporal Dynamics and Variability in Climate Extremes Over the Tibetan Plateau during 1960–2012
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