Yuting Yang

ORCID: 0000-0002-4573-1929
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About
Contact & Profiles
Research Areas
  • Plant Water Relations and Carbon Dynamics
  • Hydrology and Watershed Management Studies
  • Climate variability and models
  • Cryospheric studies and observations
  • Flood Risk Assessment and Management
  • Hydrology and Drought Analysis
  • Meteorological Phenomena and Simulations
  • Climate change and permafrost
  • Atmospheric and Environmental Gas Dynamics
  • Soil and Unsaturated Flow
  • Ecology and Vegetation Dynamics Studies
  • Soil erosion and sediment transport
  • Tree-ring climate responses
  • Arctic and Antarctic ice dynamics
  • Remote Sensing in Agriculture
  • Plant responses to elevated CO2
  • Forest ecology and management
  • Geophysics and Gravity Measurements
  • Hydrological Forecasting Using AI
  • Peatlands and Wetlands Ecology
  • Landslides and related hazards
  • Coastal wetland ecosystem dynamics
  • Geology and Paleoclimatology Research
  • Land Use and Ecosystem Services
  • Solar Radiation and Photovoltaics

Tsinghua University
2014-2025

Peking University
2023-2025

Ministry of Water Resources of the People's Republic of China
2023-2025

Institute of Optics and Electronics, Chinese Academy of Sciences
2025

Chinese Academy of Sciences
2020-2025

University of Chinese Academy of Sciences
2016-2025

Northwest University
2024

China Agricultural University
2012-2024

Lanzhou Jiaotong University
2023-2024

Sichuan Normal University
2024

Abstract Understanding hydrological effects of ecological restoration (ER) is fundamental to develop effective measures guiding future ER and adapt climate change in China's Loess Plateau (LP). Streamflow ( Q ) an important indicator processes that represents the combined climatic land surface conditions. Here 14 catchments located LP were chosen explore response different driving factors during period 1961–2009 by using elasticity decomposition methods based on Budyko framework. Our results...

10.1002/2014wr016589 article EN Water Resources Research 2015-07-22

Earlier vegetation greening under climate change raises evapotranspiration and thus lowers spring soil moisture, yet the extent magnitude of this water deficit persistence into following summer remain elusive. We provide observational evidence that increased foliage cover over Northern Hemisphere, during 1982-2011, triggers an additional moisture is further carried summer. Climate model simulations independently support attribute driving process to be larger increases in than precipitation....

10.1126/sciadv.aax0255 article EN cc-by-nc Science Advances 2020-01-03

Abstract Drought is an intermittent disturbance of the water cycle that profoundly affects terrestrial carbon cycle. However, response coupled and cycles to drought underlying mechanisms remain unclear. Here we provide first global synthesis effect on ecosystem use efficiency (WUE = gross primary production (GPP)/evapotranspiration (ET)). Using two observational WUE datasets (i.e., eddy-covariance measurements at 95 sites (526 site-years) gridded diagnostic modelling based existing...

10.1038/srep23284 article EN cc-by Scientific Reports 2016-03-17

Plant rooting depth (Zr) is a key parameter in hydrological and biogeochemical models, yet the global spatial distribution of Zr largely unknown due to difficulties its direct measurement. Additionally, observations are usually only representative single plant or several plants, which can differ greatly from effective over modeling unit (e.g., catchment grid-box). Here, we provide parameterization an analytical model that balances marginal carbon cost benefit deeper roots, produce...

10.1002/2016wr019392 article EN Water Resources Research 2016-10-01

Abstract This review examines the role of atmospheric evaporative demand (AED) in drought. AED is a complex concept and here we discuss possible definitions, subsequent metrics to measure estimate AED, different physical drivers that control it. The influence on meteorological, environmental/agricultural hydrological droughts discussed, stressing important spatial differences related climatological conditions. Likewise, drought has implications regarding how consider their attempts quantify...

10.1002/wcc.632 article EN Wiley Interdisciplinary Reviews Climate Change 2019-12-19

Soil organic carbon (SOC) stored in permafrost across the high-latitude/altitude Northern Hemisphere represents an important potential source under future warming. Here, we provide a comprehensive investigation on spatiotemporal dynamics of SOC over high-altitude Tibetan Plateau (TP), which has received less attention compared with circum-Arctic region. The region covers ~42% entire TP and contains ~37.21 Pg perennially frozen at baseline period (2006-2015). With continuous warming, active...

10.1126/sciadv.aaz3513 article EN cc-by-nc Science Advances 2020-05-06

Abstract Afforestation and deforestation as human disturbances to vegetation have profound impacts on ecohydrological processes influencing both water carbon cycles ecosystem sustainability. Since 1999, large‐scale revegetation activities such “Grain‐to‐Green Program” been implemented across China's Loess Plateau. However, negative consequences, including streamflow decline soil drying emerged. Here we estimate the equilibrium cover over Plateau based an model assess balance under actual...

10.1002/2017jg004038 article EN Journal of Geophysical Research Biogeosciences 2018-02-23

Abstract Vegetation phenology is a sensitive indicator of the dynamic response terrestrial ecosystems to climate change. In this study, spatiotemporal pattern vegetation dormancy onset date ( DOD ) and its controls over temperate China were examined by analysing satellite‐derived normalized difference index concurrent data from 1982 2010. Results show that preseason (May through October) air temperature primary climatic control spatial across China, whereas cumulative precipitation...

10.1111/gcb.12778 article EN Global Change Biology 2014-11-28

Leaf area index (LAI) is increasing throughout the globe, implying Earth greening. Global modeling studies support this contention, yet satellite observations and model simulations have never been directly compared. Here, for first time, a coupled land–climate was used to quantify potential impact of satellite-observed greening over past 30 years on terrestrial water cycle. The global LAI enhancement 8% between early 1980s 2010s modeled caused increases 12.0 ± 2.4 mm yr −1 in...

10.1175/jcli-d-17-0236.1 article EN other-oa Journal of Climate 2018-01-11

Abstract Accurate quantification of terrestrial evapotranspiration and ecosystem productivity is significant merit to better understand predict the response energy, water, carbon budgets under climate change. Existing diagnostic models have different focus on either water or flux estimates with various model complexity uncertainties induced by distinct representation coupling between processes. Here, we propose a estimate gross primary production that based biophysical mechanism yet simple...

10.1002/eco.1974 article EN Ecohydrology 2018-03-10

Abstract Vegetation restoration over degraded drylands has considerable climate, carbon and ecosystem benefits, yet its water impacts remain contentious. Previous studies suggest that extra vegetation in could lead to decreased soil moisture runoff caused by enhanced evapotranspiration. However, these ignore important vegetation‐climate feedbacks can partially offset such negative consequences. Here, we examine how revegetation affects budgets China's Loess Plateau, where the world's largest...

10.1029/2022gl098025 article EN cc-by-nc Geophysical Research Letters 2022-04-22

10.1007/s40641-024-00198-4 article EN Current Climate Change Reports 2024-10-02
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