human | Q5 |
P6178 | Dimensions author ID | 01357256272.10 |
P496 | ORCID iD | 0000-0001-5098-726X |
P3829 | Publons author ID | 1378955 |
P1053 | ResearcherID | J-4779-2014 |
P1153 | Scopus author ID | 25651961100 |
P69 | educated at | Peking University | Q16952 |
P108 | employer | Peking University | Q16952 |
P734 | family name | Peng | Q842166 |
Peng | Q842166 | ||
Peng | Q842166 | ||
P106 | occupation | researcher | Q1650915 |
Q126124815 | A global map of planting years of plantations |
Q57168350 | A global yield dataset for major lignocellulosic bioenergy crops based on field measurements |
Q40203005 | A new high-resolution N2O emission inventory for China in 2008. |
Q57044488 | A representation of the phosphorus cycle for ORCHIDEE (revision 4520) |
Q114180730 | A strong mitigation scenario maintains climate neutrality of northern peatlands |
Q30742098 | A two-fold increase of carbon cycle sensitivity to tropical temperature variations |
Q101565506 | A warm summer is unlikely to stop transmission of COVID-19 naturally |
Q30754775 | Afforestation in China cools local land surface temperature |
Q48095661 | Afforestation neutralizes soil pH. |
Q56990551 | Age-Related Modulation of the Nitrogen Resorption Efficiency Response to Growth Requirements and Soil Nitrogen Availability in a Temperate Pine Plantation |
Q92284567 | Air temperature optima of vegetation productivity across global biomes |
Q57044807 | Are ecological gradients in seasonal Q10 of soil respiration explained by climate or by vegetation seasonality? |
Q40135152 | Asymmetric effects of daytime and night-time warming on Northern Hemisphere vegetation |
Q121613794 | Asymmetric influence of forest cover gain and loss on land surface temperature |
Q90630356 | Attribution of Lake Warming in Four Shallow Lakes in the Middle and Lower Yangtze River Basin |
Q36349296 | Attribution of seasonal leaf area index trends in the northern latitudes with "optimally" integrated ecosystem models |
Q114109071 | Author Correction: Gridded maps of wetlands dynamics over mid-low latitudes for 1980–2020 based on TOPMODEL |
Q57196270 | Benchmarking carbon fluxes of the ISIMIP2a biome models |
Q57160883 | Benchmarking the seasonal cycle of CO2fluxes simulated by terrestrial ecosystem models |
Q57196272 | Carbon stocks and fluxes in the high latitudes: using site-level data to evaluate Earth system models |
Q94950299 | Causes of slowing-down seasonal CO2 amplitude at Mauna Loa |
Q57196323 | Change in snow phenology and its potential feedback to temperature in the Northern Hemisphere over the last three decades |
Q57196327 | Change in winter snow depth and its impacts on vegetation in China |
Q57159641 | Climate mitigation from vegetation biophysical feedbacks during the past three decades |
Q57270686 | Climate warming from managed grasslands cancels the cooling effect of carbon sinks in sparsely grazed and natural grasslands |
Q57196294 | Combining livestock production information in a process-based vegetation model to reconstruct the history of grassland management |
Q57196296 | Decadal trends in the seasonal-cycle amplitude of terrestrial CO2 exchange resulting from the ensemble of terrestrial biosphere models |
Q90629679 | Deceleration of China's human water use and its key drivers |
Q35791154 | Declining global warming effects on the phenology of spring leaf unfolding |
Q42536595 | Declining snow cover may affect spring phenological trend on the Tibetan Plateau |
Q42164877 | Diagnosing phosphorus limitations in natural terrestrial ecosystems in carbon cycle models |
Q55033790 | Divergent hydrological response to large-scale afforestation and vegetation greening in China. |
Q57196246 | Dominant regions and drivers of the variability of the global land carbon sink across timescales |
Q60028652 | Ectomycorrhizal fungi respiration quantification and drivers in three differently-aged larch plantations |
Q60300783 | Emerging negative impact of warming on summer carbon uptake in northern ecosystems |
Q109317380 | Empirical estimates of regional carbon budgets imply reduced global soil heterotrophic respiration |
Q57196299 | Evaluating biases in simulated land surface albedo from CMIP5 global climate models |
Q57196258 | Evaluation of ORCHIDEE-MICT simulated soil moisture over China and impacts of different atmospheric forcing data |
Q58395898 | Evaluation of ORCHIDEE-MICT-simulated soil moisture over China and impacts of different atmospheric forcing data |
Q57196292 | Evaluation of air–soil temperature relationships simulated by land surface models during winter across the permafrost region |
Q57196320 | Evaluation of an improved intermediate complexity snow scheme in the ORCHIDEE land surface model |
Q37704623 | Evidence and mapping of extinction debts for global forest-dwelling reptiles, amphibians and mammals |
Q30860434 | Evidence for a weakening relationship between interannual temperature variability and northern vegetation activity |
Q47695274 | Extension of the growing season increases vegetation exposure to frost |
Q36194709 | Field warming experiments shed light on the wheat yield response to temperature in China |
Q112596699 | Future impacts of climate change on inland Ramsar wetlands |
Q57196245 | GOLUM-CNP v1.0: a data-driven modeling of carbon, nitrogen and phosphorus cycles in major terrestrial biomes |
Q57196252 | GOLUM-CNP v1.0: a data-driven modeling of carbon, nitrogen and phosphorus cycles in major terrestrial biomes |
Q38682800 | Global forest carbon uptake due to nitrogen and phosphorus deposition from 1850 to 2100. |
Q57196275 | Global land carbon sink response to temperature and precipitation varies with ENSO phase |
Q57196301 | Global patterns and climate drivers of water-use efficiency in terrestrial ecosystems deduced from satellite-based datasets and carbon cycle models |
Q31131592 | Global patterns and controls of soil organic carbon dynamics as simulated by multiple terrestrial biosphere models: Current status and future directions |
Q99710786 | Global terrestrial carbon fluxes of 1999-2019 estimated by upscaling eddy covariance data with a random forest |
Q90326123 | Global vegetation biomass production efficiency constrained by models and observations |
Q33708473 | Grassland restoration reduces water yield in the headstream region of Yangtze River |
Q56004946 | Greening of the Earth and its drivers |
Q114109102 | Gridded maps of wetlands dynamics over mid-low latitudes for 1980–2020 based on TOPMODEL |
Q57196265 | Gross and net land cover changes based on plant functional types derived from the annual ESA CCI land cover maps |
Q57196255 | Gross and net land cover changes in the main plant functional types derived from the annual ESA CCI land cover maps (1992–2015) |
Q57196257 | Gross changes in forest area shape the future carbon balance of tropical forests |
Q57196262 | Gross changes in forest area shape the future carbon balance of tropical forests |
Q57196242 | Identification of typical diurnal patterns for clear-sky climatology of surface urban heat islands |
Q57059368 | Impact of large-scale climate extremes on biospheric carbon fluxes: An intercomparison based on MsTMIP data |
Q35772145 | Impacts of Satellite-Based Snow Albedo Assimilation on Offline and Coupled Land Surface Model Simulations |
Q57196304 | Increased light-use efficiency in northern terrestrial ecosystems indicated by CO2 and greening observations |
Q57196290 | Inventory of anthropogenic methane emissions in mainland China from 1980 to 2010 |
Q57196247 | Inventory of methane emissions from livestock in China from 1980 to 2013 |
Q57160800 | Land-use and land-cover change carbon emissions between 1901 and 2012 constrained by biomass observations |
Q57196266 | Land-use and land-cover change carbon emissions between 1901 and 2012 constrained by biomass observations |
Q109932832 | Large historical carbon emissions from cultivated northern peatlands |
Q35579425 | Leaf onset in the northern hemisphere triggered by daytime temperature |
Q31134423 | Long-term linear trends mask phenological shifts |
Q121096849 | Microbial communities in terrestrial surface soils are not widely limited by carbon |
Q109932883 | Modelling northern peatland area and carbon dynamics since the Holocene with the ORCHIDEE-PEAT land surface model (SVN r5488) |
Q60028653 | Modelling northern peatlands area and carbon dynamics since the Holocene with the ORCHIDEE-PEAT land surface model (SVN r5488) |
Q57196316 | Multimodel projections and uncertainties of net ecosystem production in China over the twenty-first century |
Q57196259 | ORCHIDEE-MICT (v8.4.1), a land surface model for the high latitudes: model description and validation |
Q57196251 | ORCHIDEE-MICT-BIOENERGY: an attempt to represent the production of lignocellulosic crops for bioenergy in a global vegetation model |
Q57196253 | ORCHIDEE-MICT-BIOENERGY: an attempt to represent the production of lignocellulosic crops for bioenergy in a global vegetation model |
Q57196261 | ORCHIDEE-PEAT (revision 4596), a model for northern peatland CO2, water and energy fluxes on daily to annual scales |
Q57196254 | ORCHIDEE-PEAT (revision 4596), a model for northern peatland CO2, water, and energy fluxes on daily to annual scales |
Q124823459 | Observed changes in China’s methane emissions linked to policy drivers |
Q46306444 | On the causes of trends in the seasonal amplitude of atmospheric CO2. |
Q57196250 | Partitioning global land evapotranspiration using CMIP5 models constrained by observations |
Q36227858 | Plausible rice yield losses under future climate warming |
Q57196322 | Precipitation amount, seasonality and frequency regulate carbon cycling of a semi-arid grassland ecosystem in Inner Mongolia, China: A modeling analysis |
Q57196277 | Quantifying uncertainties of permafrost carbon–climate feedbacks |
Q57196307 | Re-evaluating the 1940s CO2 plateau |
Q57159637 | Recent Changes in Global Photosynthesis and Terrestrial Ecosystem Respiration Constrained From Multiple Observations |
Q117600034 | Recent intensification of wetland methane feedback |
Q31140267 | Reducing uncertainties in decadal variability of the global carbon budget with multiple datasets |
Q57196279 | Regional patterns of future runoff changes from Earth system models constrained by observation |
Q113855982 | Reply to: Disentangling biology from mathematical necessity in twentieth-century gymnosperm resilience trends |
Q57182098 | Representing anthropogenic gross land use change, wood harvest and forest age dynamics in a global vegetation model ORCHIDEE-MICT (r4259) |
Q57182074 | Representing anthropogenic gross land use change, wood harvest, and forest age dynamics in a global vegetation model ORCHIDEE-MICT v8.4.2 |
Q57159867 | Response to Comment on “Surface Urban Heat Island Across 419 Global Big Cities” |
Q110980159 | Retention of deposited ammonium and nitrate and its impact on the global forest carbon sink |
Q92321879 | Revisiting enteric methane emissions from domestic ruminants and their δ13CCH4 source signature |
Q57196330 | Root respiration and its relation to nutrient contents in soil and root and EVI among 8 ecosystems, northern China |
Q31031960 | Seasonal responses of terrestrial ecosystem water-use efficiency to climate change |
Q57196281 | Sensitivity of land use change emission estimates to historical land use and land cover mapping |
Q57196282 | Spatiotemporal variations in the difference between satellite-observed daily maximum land surface temperature and station-based daily maximum near-surface air temperature |
Q58413380 | Summer soil moisture regulated by precipitation frequency in China |
Q120518345 | Surface conductance for evapotranspiration of tropical forests: Calculations, variations, and controls |
Q40010461 | Surface urban heat island across 419 global big cities |
Q38642028 | Temperature increase reduces global yields of major crops in four independent estimates |
Q57196243 | Temporal response of soil organic carbon after grassland-related land-use change |
Q96431320 | Temporal trade-off between gymnosperm resistance and resilience increases forest sensitivity to extreme drought |
Q57196268 | Terrestrial ecosystem model performance in simulating productivity and its vulnerability to climate change in the northern permafrost region |
Q125848132 | The Key Role of Production Efficiency Changes in Livestock Methane Emission Mitigation |
Q31059256 | The contribution of China's emissions to global climate forcing |
Q57196285 | The effects of teleconnections on carbon fluxes of global terrestrial ecosystems |
Q33681957 | The impacts of climate change on water resources and agriculture in China |
Q30720068 | The influence of local spring temperature variance on temperature sensitivity of spring phenology |
Q56522669 | The large mean body size of mammalian herbivores explains the productivity paradox during the Last Glacial Maximum |
Q63919341 | The weakening relationship between Eurasian spring snow cover and Indian summer monsoon rainfall. |
Q57196314 | Toward “optimal” integration of terrestrial biosphere models |
Q114110185 | Trade-off between tree planting and wetland conservation in China |
Q91286975 | Tropical forest soils serve as substantial and persistent methane sinks |
Q117743612 | Vapor Pressure Deficit and Sunlight Explain Seasonality of Leaf Phenology and Photosynthesis Across Amazonian Evergreen Broadleaved Forest |
Q57160488 | Variability and quasi-decadal changes in the methane budget over the period 2000–2012 |
Q57044539 | Velocity of change in vegetation productivity over northern high latitudes |
Q57159650 | Was the extreme Northern Hemisphere greening in 2015 predictable? |
Q57044543 | Weakening temperature control on the interannual variations of spring carbon uptake across northern lands |
Q115707057 | Wetland emission and atmospheric sink changes explain methane growth in 2020 |
Q114026998 | Wetlands Cool Land Surface Temperature in Tropical Regions but Warm in Boreal Regions |
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