Y. Wang

ORCID: 0000-0002-4737-8305
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About
Contact & Profiles
Research Areas
  • Climate variability and models
  • Oceanographic and Atmospheric Processes
  • Hydrology and Watershed Management Studies
  • Climate change and permafrost
  • Precipitation Measurement and Analysis
  • Ocean Waves and Remote Sensing
  • Flood Risk Assessment and Management
  • Marine and fisheries research
  • Arctic and Antarctic ice dynamics

Gansu Meteorological Bureau
2017-2024

Lanzhou University
2024

First Institute of Oceanography
2021

Ministry of Natural Resources
2021

South China Sea Institute Of Oceanology
2021

Abstract Volume, heat and freshwater transports from the South China Sea (SCS) to Java through Karimata Strait are estimated based on direct measurements of current, temperature, salinity, satellite observations. Subject strong seasonal variability, volume, heat, −1.98 ± 0.23 Sv (1 = 10 6 m 3 /s), −209.68 15.19 TW 12 W), −99.87 15.11 mSv ‐3 Sv) in boreal winter, 0.47 0.20 Sv, 61.06 15.46 TW, 31.67 8.76 summer, respectively (negative transport defined SCS Sea). The annual mean −0.78 0.12...

10.1029/2020jc016608 article EN Journal of Geophysical Research Oceans 2021-01-21

Abstract Topography and spatial patterns of landscape significantly affect distribution precipitation and, in turn, hydrological modelling, especially high elevation, mountainous watersheds arid regions. This study incorporates a physically based inverse distance elevation weighted (PBIDEW) method into distributed conceptual model, large basin runoff compared with an (IDW) to assess the performances both methods estimation for modelling at watershed scale. The PBIDEW considers impacts...

10.1002/rra.3147 article EN River Research and Applications 2017-04-10

Abstract Using the ERA‐5 reanalysis datasets, NCEP/NCAR sea ice concentration (SIC) and observed winter surface wind speed (WSWS) in northwest China during 1979–2020, this study examined regime shift of leading mode WSWS investigated its possible link with Barents–Kara Sea (BKS) SIC. The showed negative anomalies southern northeastern Xinjiang, Gansu, western northern Shaanxi Provinces, positive northwestern middle Qinghai Ningxia Provinces. signs is generally opposite to their trends...

10.1002/joc.8399 article EN International Journal of Climatology 2024-02-26
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