Green-up dates in the Tibetan Plateau have continuously advanced from 1982 to 2011.
about
Vegetation Changes in the Permafrost Regions of the Qinghai-Tibetan Plateau from 1982-2012: Different Responses Related to Geographical Locations and Vegetation Types in High-Altitude AreasHistorical Records of Mercury Stable Isotopes in Sediments of Tibetan LakesClimatic change controls productivity variation in global grasslandsComplex responses of spring vegetation growth to climate in a moisture-limited alpine meadow.Light-intensity grazing improves alpine meadow productivity and adaption to climate change on the Tibetan Plateau.Large-scale variations in the vegetation growing season and annual cycle of atmospheric CO2 at high northern latitudes from 1950 to 2011.Phenological response of tundra plants to background climate variation tested using the International Tundra Experiment.Consistent response of vegetation dynamics to recent climate change in tropical mountain regions.Assessing phenological change and climatic control of alpine grasslands in the Tibetan Plateau with MODIS time series.Cold truths: how winter drives responses of terrestrial organisms to climate change.Field evidence for earlier leaf-out dates in alpine grassland on the eastern Tibetan Plateau from 1990 to 2006.Radial growth of two dominant montane conifer tree species in response to climate change in North-Central ChinaChanges in autumn vegetation dormancy onset date and the climate controls across temperate ecosystems in China from 1982 to 2010.Determining the relative importance of climatic drivers on spring phenology in grassland ecosystems of semi-arid areas.Greater deciduous shrub abundance extends tundra peak season and increases modeled net CO2 uptake.Temperature and snowfall trigger alpine vegetation green-up on the world's roof.Change in the Green-Up Dates for Quercus mongolica in Northeast China and Its Climate-Driven Mechanism from 1962 to 2012.Biophysical regulation of carbon fluxes over an alpine meadow ecosystem in the eastern Tibetan Plateau.Interannual variations in spring phenology and their response to climate change across the Tibetan Plateau from 1982 to 2013.Strong impacts of daily minimum temperature on the green-up date and summer greenness of the Tibetan Plateau.Temporal Trends and Spatial Variability of Vegetation Phenology over the Northern Hemisphere during 1982-2012.Greater phenological sensitivity on the higher Tibetan Plateau: new insights from weekly 5 km EVI2 datasets.Environmental Humidity Regulates Effects of Experimental Warming on Vegetation Index and Biomass Production in an Alpine Meadow of the Northern Tibet.New perspective on spring vegetation phenology and global climate change based on Tibetan Plateau tree-ring data.The impacts of climate change and human activities on biogeochemical cycles on the Qinghai-Tibetan Plateau.The response of aboveground net primary productivity of desert vegetation to rainfall pulse in the temperate desert region of northwest China.Earlier-season vegetation has greater temperature sensitivity of spring phenology in northern hemisphere.Leaf unfolding of Tibetan alpine meadows captures the arrival of monsoon rainfallAn increase in the biogenic aerosol concentration as a contributing factor to the recent wetting trend in Tibetan Plateau.Changes in flowering functional group affect responses of community phenological sequences to temperature change.Productivity responses of desert vegetation to precipitation patterns across a rainfall gradient.Trends toward an earlier peak of the growing season in Northern Hemisphere mid-latitudes.Growing season carries stronger contributions to albedo dynamics on the Tibetan plateauReply to Wang et al.: Snow cover and air temperature affect the rate of changes in spring phenology in the Tibetan PlateauDeclining snow cover may affect spring phenological trend on the Tibetan Plateau.Reply to Shen et al. No evidence to show nongrowing season NDVI affects spring phenology trend in the Tibetan Plateau over the last decade.No evidence of continuously advanced green-up dates in the Tibetan Plateau over the last decade.A global moderate resolution dataset of gross primary production of vegetation for 2000-2016.Grazing exclusion by fencing non-linearly restored the degraded alpine grasslands on the Tibetan Plateau.Influences of population pressure change on vegetation greenness in China's mountainous areas.
P2860
Q28469383-00C94C24-EF96-4051-A229-0525D564C803Q28602357-761D027D-CC23-4E0E-8C86-81ADD59691DFQ30383416-4368EABB-75E1-4F61-B437-6B6A9B73FFCCQ30385491-EA941DF8-F6E1-400F-941B-6EDDE85EAC5CQ30387134-94DF2C25-4A47-472A-A347-2F502764BB64Q30643674-0A3FF2A7-693E-4ACE-BBD5-EFBD46516955Q30654173-6A1EFE3E-84E9-4734-8EEA-87439BFD25DCQ30662765-4A3D469D-E6BE-4667-AF12-94881D2B0366Q30788937-1151CBB2-CC14-427A-B763-A74C0A7CFA1DQ30797840-68F7C03C-B6C9-4735-A8C2-29B23881B608Q30841061-F37872B6-2F34-40C2-A383-DA4915B3B36AQ30869353-E2FCDED3-98A8-46C1-8C63-87E02614EF3DQ30872278-76C5E0D8-0A71-45EE-B9E2-BB7B3B454C63Q30876002-3A9D941D-B7D2-48C6-A595-E162FFBFC815Q30882615-861EF94D-3DC0-4C05-B8ED-F3E1886DD176Q30938774-06BDF590-050A-4701-89D6-C0D84C188138Q30975968-AB420DEC-C690-4889-BAD6-CE1C0CE464F5Q31004297-50C43393-1A10-42E2-9E3B-7A4641455E9FQ31051895-1C8D5829-3A59-4EC5-A962-42E1CB8B1788Q31082883-FDE1541D-513F-427C-9A02-A903B2A99888Q31106484-DDC3FE5D-977E-4D3C-B8D6-DB06611D30C2Q31139195-42BFA38A-20DE-4944-88E7-639C5AD373C6Q31140218-87624157-B624-42B1-9F09-2B464B548718Q33886931-6E6AE7D2-5E74-41F8-8B90-5611763779BEQ34762371-D6C6CEA2-FFE6-4024-9C53-155134E7BDCEQ34982762-BED7DB76-0400-4670-A734-7F442D79C2C7Q35088562-31E1A479-28FE-4595-994E-39180F1F3B30Q35917440-77B6CA85-98CA-46F4-BAF6-F4B2FAE4494FQ36100098-E840787F-A140-4F16-A8C6-0EC3B70BD851Q36226796-B8AC2D1B-EED7-4ADC-B9E8-58A14B68D990Q39051519-FC41E69F-DF3A-43A2-884D-9C3CC29875EFQ39608354-68F3AFCC-F52C-499C-B453-6E67CE27A6B3Q41501054-3F3A96CB-4B75-4A23-A21B-23F26C71C7F0Q42536572-6C2B0B1F-DFB4-477A-92CD-5D0E708F8AFEQ42536595-010E1191-7DA9-4DB7-B9A0-0065B4BFE0DCQ43111170-51C2056D-F28B-44FB-9A05-31B91A2414F4Q43111181-982FD484-A6E7-422A-BF36-F054BCFD859AQ43299339-8CF2E493-8C18-46F3-A64A-A164D4CABAF8Q46218192-F547C75B-3DFC-433A-BFDF-640F898622B9Q47161738-B2E8A220-CD56-461D-8F03-87AA364A5495
P2860
Green-up dates in the Tibetan Plateau have continuously advanced from 1982 to 2011.
description
2013 nî lūn-bûn
@nan
2013年の論文
@ja
2013年論文
@yue
2013年論文
@zh-hant
2013年論文
@zh-hk
2013年論文
@zh-mo
2013年論文
@zh-tw
2013年论文
@wuu
2013年论文
@zh
2013年论文
@zh-cn
name
Green-up dates in the Tibetan Plateau have continuously advanced from 1982 to 2011.
@ast
Green-up dates in the Tibetan Plateau have continuously advanced from 1982 to 2011.
@en
type
label
Green-up dates in the Tibetan Plateau have continuously advanced from 1982 to 2011.
@ast
Green-up dates in the Tibetan Plateau have continuously advanced from 1982 to 2011.
@en
prefLabel
Green-up dates in the Tibetan Plateau have continuously advanced from 1982 to 2011.
@ast
Green-up dates in the Tibetan Plateau have continuously advanced from 1982 to 2011.
@en
P2093
P2860
P356
P1476
Green-up dates in the Tibetan Plateau have continuously advanced from 1982 to 2011.
@en
P2093
Geli Zhang
Jinwei Dong
Xiangming Xiao
Yangjian Zhang
P2860
P304
P356
10.1073/PNAS.1210423110
P407
P577
2013-02-25T00:00:00Z