A5008387698- Hydrology and Watershed Management Studies
- Groundwater and Isotope Geochemistry
- Arctic and Antarctic ice dynamics
- Cryospheric studies and observations
- Geology and Paleoclimatology Research
- Climate change and permafrost
- Groundwater flow and contamination studies
- Flood Risk Assessment and Management
- Groundwater and Watershed Analysis
- Radioactive contamination and transfer
- Radioactivity and Radon Measurements
- Meteorological Phenomena and Simulations
- Soil erosion and sediment transport
- Methane Hydrates and Related Phenomena
- Soil Moisture and Remote Sensing
- Climate variability and models
- Atmospheric and Environmental Gas Dynamics
- Isotope Analysis in Ecology
- Environmental and Agricultural Sciences
- Nuclear and radioactivity studies
- Hydrocarbon exploration and reservoir analysis
- Geological and Geochemical Analysis
- Soil and Unsaturated Flow
- Precipitation Measurement and Analysis
- Geophysics and Gravity Measurements
Hohai University
2013-2025
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering
2010-2023
Abstract The exchange rate is often characterized by spatio‐temporal heterogeneity, but the patterns of have rarely been quantified, especially in water transfer lakes. This study was conducted from March to July 2021. tracer data δ 2 H, 18 O ( n = 121), 222 Rn 522), Cl 151), TDS 155) lake water, shallow groundwater (7–10 m), deep (25–40 and an improved single‐well radon model were applied 3 (A, B C) typical areas (~1 km ) Hongze lake. results show that during period (March May) rising level...
Permafrost degradation on the Tibetan Plateau (TP) is anticipated to result in thaw of permafrost carbon. Existing studies have been conducted assess future frozen carbon TP, primarily focusing deepening active layer while neglecting impact area shrinkage. This oversight may lead a significant underestimation potential Our research underscores pivotal role shrinkage estimating findings reveal that when combined effects and are considered, rates various radiative forcing scenarios nearly four...
ABSTRACT The complex orography of the Tibetan plateau (TP) and scarcity uneven spatial distribution meteorological stations present significant challenges in accurately estimating variables for hydrological simulations. This study aims to enhance accuracy daily precipitation temperature interpolation simulations Lhasa River Basin (LRB), particularly during flood events. We evaluate compare performance deterministic Inverse Distance Weighting—IDW geostatistical (Ordinary Kriging—OK Kriging...
Lakes are sensitive to environmental changes, and an example of this change is the decreased water level in Yamzho Yumco Lake (YYL, southern Tibetan Plateau), which opposite reported expansion most other lakes Plateau. In study, we report a high-resolution dataset daily monitored levels from 1974 2010 YYL, was used elucidate annual seasonal variations lake level. These data coupled stable isotope signals balance model provide overall picture factors processes affecting lake. The revealed...
Abstract. Hydrological processes in the karst basin are controlled by permeable multi-media consisting of soil pores, epikarst fractures and underground conduits. Distributed modeling hydrological dynamics such heterogeneously hydrogeological conditions is a challenging task. Based on multi-layer structure distributed hydrology-soil-vegetation model (DHSVM), for was developed integrating mathematical routings porous Darcy flow, fissure flow channel flow. Specifically, infiltration saturated...
The Tibetan Plateau (TP) has undergone significant warming and humidification in recent years, resulting rapid permafrost degradation spatiotemporal variations hydrological processes, such as subsurface water transport, hydrothermal conversion, runoff generation. Understanding the mechanisms of processes areas under changing climate is crucial for accurately evaluating responses on TP. This communication comprehensively discusses TP climate. Topics include conditions states, transport...