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Fujun Niu

Dados Biográficos

ID7892307
NOMEFujun Niu
PRENOMESFujun
SOBRENOMENiu
ASSINATURANIU F
AFILIAÇÕESSouth China University of Technology
ORCID0000-0003-0524-2618
VERIFICADOSim
TOTAL DE OBRAS4
TOTAL DE CITAÇÕES0
TOTAL COMO AUTOR4
TOTAL COMO EDITOR0
PRIMEIRO ANO DE PUBLICAÇÃO2014
ANO MAIS RECENTE DE PUBLICAÇÃO2026
ÍNDICE H0
  • Deformation Characteristics of a Thermokarst Lake by Integrated Methodology in Permafrost Regions of the Qinghai–Tibetan Plateau

    Open Access•Peifeng He, Fujun Niu et al.•ARTICLE•Land Degradation and Development•2026

    The development of thermokarst lakes on the Qinghai–Tibetan Plateau (QTP) serves as a prominent indicator of permafrost degradation driven by climate warming and increased humidity. However, quantitative observations of surface change and relationships between lakes and permafrost during thermokarst development remain inadequate. This study utilized long‐term terrestrial laser scanning (TLS) to capture high‐resolution data on the surface contour …

  • Primarily investigation with multiple methods on permafrost state around a rapid change lake in the interior of the Tibet Plateau

    Open Access•Zekun Ding, Fujun Niu et al.•ARTICLE•Environmental Research Letters•2023

    Changes of the lakes on high-altitude regions of the Tibet Plateau influence the state of the surrounding permafrost. Due to the climate warming and wetting trend, extreme events including lake outburst has occurred more frequent. In 2011, an outburst event occurred on the Zonag Lake and this event changed the water distribution in the basin, leading a rapid expansion of the Tailwater lake, named as the Salt Lake. However, the construction of the…

  • Temporal and Spatial Variation Characteristics of Water Quality in the Middle and Lower Reaches of the Lijiang River, China and Their Responses to Environmental Factors

    Open Access•Dantong Zhu, Xiangju Cheng et al.•ARTICLE•International Journal of…•2022

    As the climate and the external environment have changed, the environmental factors of the Lijiang River Basin (LRB) have changed, posing new threats to the environmental quality, ecosystem balance, and management and protection of the water environment of the Lijiang River. Water quality indicators and environmental factors vary spatially along the Lijiang River, which runs through urban areas, farmland, and karst areas. However, research on the…

  • Assessing soil erosion and control factors by radiometric technique in the source region of the Yellow River, Tibetan Plateau

    Open Access•Yibo Wang, Fujun Niu et al.•ARTICLE•Quaternary Research•2014

    Measurements of 137 Cs concentration in soils were made in a representative catchment to quantify erosion rates and identify the main factors involved in the erosion in the source region of the Yellow River in the Tibetan Plateau. In order to estimate erosion rates in terms of the main factors affecting soil loss, samples were collected taking into account the slope and vegetation cover along six selected transects within the Dari County catchmen…

Sem obras proeminentes nesta página.

  • Assessing soil erosion and control factors by radiometric technique in the source region of the Yellow River, Tibetan Plateau

    Open Access•Yibo Wang, Fujun Niu et al.•ARTICLE•Quaternary Research•2014

    Measurements of 137 Cs concentration in soils were made in a representative catchment to quantify erosion rates and identify the main factors involved in the erosion in the source region of the Yellow River in the Tibetan Plateau. In order to estimate erosion rates in terms of the main factors affecting soil loss, samples were collected taking into account the slope and vegetation cover along six selected transects within the Dari County catchmen…

  • Temporal and Spatial Variation Characteristics of Water Quality in the Middle and Lower Reaches of the Lijiang River, China and Their Responses to Environmental Factors

    Open Access•Dantong Zhu, Xiangju Cheng et al.•ARTICLE•International Journal of…•2022

    As the climate and the external environment have changed, the environmental factors of the Lijiang River Basin (LRB) have changed, posing new threats to the environmental quality, ecosystem balance, and management and protection of the water environment of the Lijiang River. Water quality indicators and environmental factors vary spatially along the Lijiang River, which runs through urban areas, farmland, and karst areas. However, research on the…

  • Primarily investigation with multiple methods on permafrost state around a rapid change lake in the interior of the Tibet Plateau

    Open Access•Zekun Ding, Fujun Niu et al.•ARTICLE•Environmental Research Letters•2023

    Changes of the lakes on high-altitude regions of the Tibet Plateau influence the state of the surrounding permafrost. Due to the climate warming and wetting trend, extreme events including lake outburst has occurred more frequent. In 2011, an outburst event occurred on the Zonag Lake and this event changed the water distribution in the basin, leading a rapid expansion of the Tailwater lake, named as the Salt Lake. However, the construction of the…

  • Deformation Characteristics of a Thermokarst Lake by Integrated Methodology in Permafrost Regions of the Qinghai–Tibetan Plateau

    Open Access•Peifeng He, Fujun Niu et al.•ARTICLE•Land Degradation and Development•2026

    The development of thermokarst lakes on the Qinghai–Tibetan Plateau (QTP) serves as a prominent indicator of permafrost degradation driven by climate warming and increased humidity. However, quantitative observations of surface change and relationships between lakes and permafrost during thermokarst development remain inadequate. This study utilized long‐term terrestrial laser scanning (TLS) to capture high‐resolution data on the surface contour …

Climate change and permafrost (3 obras) · Cryospheric studies and observations (2 obras) · Drainage basin (2 obras) · Environmental Science (2 obras) · Geography (2 obras) · Geomorphology (2 obras) · Hydrology (agriculture (2 obras) · Permafrost (2 obras) · Thermokarst (2 obras) · Active layer (1 obras)

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