Shu Wang

ORCID: 0000-0001-9239-9933
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About
Contact & Profiles
Research Areas
  • Climate variability and models
  • Meteorological Phenomena and Simulations
  • Advanced oxidation water treatment
  • Membrane Separation Technologies
  • Environmental and Agricultural Sciences
  • Membrane-based Ion Separation Techniques
  • Water Quality Monitoring Technologies
  • Environmental remediation with nanomaterials
  • Soil Moisture and Remote Sensing
  • Hydrology and Watershed Management Studies
  • Water Quality Monitoring and Analysis
  • Groundwater and Isotope Geochemistry
  • Advanced Photocatalysis Techniques
  • Cryospheric studies and observations
  • Atmospheric aerosols and clouds
  • Precipitation Measurement and Analysis
  • Remote Sensing and Land Use
  • Water Quality and Pollution Assessment
  • Adsorption and biosorption for pollutant removal
  • Microgrid Control and Optimization
  • Water Resources and Sustainability
  • Aquatic Ecosystems and Phytoplankton Dynamics
  • Smart Grid Energy Management
  • Geochemistry and Geologic Mapping
  • Plant Water Relations and Carbon Dynamics

China Electric Power Research Institute
2017-2024

North China Electric Power University
2016-2024

State Key Joint Laboratory of Environment Simulation and Pollution Control
2015-2023

Tsinghua University
2015-2023

China Academy of Urban Planning and Design
2023

Huangshan University
2023

State Key Laboratory of Pollution Control and Resource Reuse
2018-2022

Nanjing University
2007-2022

China Meteorological Administration
2017-2022

Northeastern University
2022

Abstract The precipitation partitioning between evapotranspiration (ET) and runoff (R) at the land surface is controlled by atmospheric boundary layer terrestrial hydrological processes. These processes in models are manifested primarily as stomatal conductance, soil moisture limitation factor to transpiration (β‐factor), turbulence, generation. What sensitivities of parameterizations these processes? To address this overarching question, annual seasonal means ET R over conterminous United...

10.1029/2017wr022236 article EN cc-by-nc-nd Water Resources Research 2018-12-15

Phosphonate is an important category of highly soluble organophosphorus in contaminated waters, and its oxidative transformation into phosphate usually a prerequisite step to achieve the in-depth removal total phosphorus. Currently, selective oxidation phosphonate urgently desired as conventional advanced processes suffer from severe matrix interferences. Herein, we employed 1-hydroxyethylidene-1,1-diphosphonic acid (HEDP) model demonstrated efficient by Cu(II)/H2O2 process at alkaline pH....

10.1021/acs.est.1c06471 article EN Environmental Science & Technology 2021-12-14

Based on a new multi-source dataset (GLDP-V1.0) recently developed in China Meteorological Administration, we employed precipitation indices including percentile-based of light (below the 50th percentile), moderate (between and 90th intense (above percentile) precipitation, maximum 1-day, 3-day, 5-day amounts (RX1DAY, RX3DAY, RX5DAY, respectively), consecutive wet dry days (CWDs CDDs) to analyze variations extreme events Hindu Kush Himalayan (HKH) during 1961–2012. The main results are...

10.1016/j.accre.2017.08.002 article EN cc-by-nc-nd Advances in Climate Change Research 2017-08-12

Traditional harsh chemical cleaning-in-place (CIP) is corrosive to membranes but has limited inhibition on refouling, a tough problem for long-term operation of reverse osmosis (RO). Mild enzymatic cleaning (at pH 9) promising alternative lacks verification and insightful elucidation. In this study, we investigated the instantaneous efficiency, postcleaning biological effect CIP (compounded with lipase, protease, sodium dodecyl sulfate) practical RO during 500 h multicycle operation. The had...

10.1021/acs.est.0c04735 article EN Environmental Science & Technology 2021-01-25

Abstract Ongoing global warming has a strong influence on regional hydrological cycles. The upper reaches of the Yangtze River (UYR) are highly vulnerable to extreme droughts and floods, but lack long‐term streamflow observations limited our understanding influences. Here, we establish an annually resolved absolutely dated tree‐ring oxygen ( δ 18 O) isotope chronology use it reconstruct summer history UYR between 1260 2017. experienced 79 floods 107 over this period. We found trend toward...

10.1029/2021jd036109 article EN Journal of Geophysical Research Atmospheres 2022-05-11

The IMERG V06 hourly rainfall product at daily and scales was evaluated during the warm season (May to September) from 2015 2020 using 651 high-quality rain-gauge stations over Tibetan Plateau (TP). Based on observed precipitation, four categories were classified: light (0–12 mm·d−1), moderate (12–20.1 torrential (20.1–32.2 extreme (>32.2 mm·d−1). Precipitation frequency intensity calculated further validate accuracy suitability of estimated-precipitation product. At scale, underestimated...

10.3390/atmos14111653 article EN cc-by Atmosphere 2023-11-03

Quantifying roughness effects on ground surface emissivity is an important step in obtaining high-quality soil moisture products from large-scale passive microwave sensors. In this study, we used a semi-empirical method to evaluate (parameterized here by the parameter) global scale AMSR-E (Advanced Microwave Scanning Radiometer for EOS) observations. brightness temperatures at 6.9 GHz obtained January 2009 September 2011, together with estimations of SMOS (Soil Moisture and Ocean Salinity)...

10.3390/rs70505734 article EN cc-by Remote Sensing 2015-05-05

Groundwater in coastal aquifers is often affected by seawater intrusion, resulting water quality deterioration. Using groundwater influenced intrusion for irrigation can lead to crop failure, erosion of machinery and pipes, adverse effects on farming. In this study, the results testing, methods statistical analysis, ion ratios, a Piper diagram, variety suitability models were used analyze chemical composition influence intrusion. The result shows that content Na+, K+, Ca2+, Mg2+, Cl−, SO42−...

10.3390/w12123460 article EN Water 2020-12-09
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