Wenshi Lin

ORCID: 0000-0002-5767-0051
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About
Contact & Profiles
Research Areas
  • Meteorological Phenomena and Simulations
  • Tropical and Extratropical Cyclones Research
  • Climate variability and models
  • Atmospheric aerosols and clouds
  • Atmospheric chemistry and aerosols
  • Urban Heat Island Mitigation
  • Remote Sensing and Land Use
  • Atmospheric Ozone and Climate
  • Environmental Changes in China
  • Ocean Waves and Remote Sensing
  • Oceanographic and Atmospheric Processes
  • Fire effects on ecosystems
  • Land Use and Ecosystem Services
  • Cryospheric studies and observations
  • Air Quality and Health Impacts
  • Solar Radiation and Photovoltaics
  • Solar and Space Plasma Dynamics
  • 3D Modeling in Geospatial Applications
  • Geophysics and Gravity Measurements
  • Atmospheric and Environmental Gas Dynamics
  • Plant Water Relations and Carbon Dynamics
  • Geographic Information Systems Studies
  • Precipitation Measurement and Analysis
  • Coastal and Marine Management
  • Ionosphere and magnetosphere dynamics

Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)
2019-2025

Sun Yat-sen University
2012-2025

Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai)
2019-2025

Zhejiang Environmental Monitoring Center
2009

Nanjing University
2009

Abstract The western North Pacific anticyclone (WNPAC) significantly influences the East Asian climate and is modulated by tropical sea surface temperature (SST). This study uses 142 AMIP simulations from 33 Coupled Model Intercomparison Project (CMIP6) models to quantify contributions of SST interannual variability WNPAC. forcing accounts for 66%, 77%, 49% WNPAC variance in winter, spring, summer, respectively. persistence depends on relaying effects three oceans. CMIP6 exhibit excessive...

10.1029/2023gl107080 article EN cc-by-nc-nd Geophysical Research Letters 2024-02-03

Atmospheric dynamical and chemical models are conducted to explore impacts of urban land-use change on ozone concentrations over the Pearl River Delta (PRD) region, China. Two scenarios distributions used represent early 1990s current distributions. Urbanization increases 2-d averaged daytime (nighttime) temperature by 0.8°C (1.5 °C) reduces wind speed about 20% PRD areas. The boundary layer depth is up 400 m deeper, while there a 50-m increase during nighttime. combination these seemly...

10.1111/j.1600-0889.2007.00271.x article EN cc-by Tellus B 2007-01-01

Abstract A significant relationship exists between the Indian Ocean Dipole (IOD) and following year’s El Niño-Southern Oscillation (ENSO), in spite of uncertainty associated mechanisms. Here we show that spring sea surface temperature (SST) anomalies over southeastern (SEIO) play a bridging role teleconnection IOD subsequent ENSO. positive could induce tendency SST SEIO region from autumn to winter, primarily through cloud-radiation-SST feedback, forming an anomalous warming which persists...

10.1175/jcli-d-24-0263.1 article EN Journal of Climate 2025-01-28

Abstract Taking Typhoon Usagi (2013) as an example, this study used the Weather Research and Forecasting Model with Chemistry to investigate influence of anthropogenic aerosols on typhoons. Three simulations (CTL, CLEAN, EXTREME) were designed according emission intensity pollution. The results showed that although pollution did not demonstrate clear track strength typhoon, it clearly changed precipitation, distribution water hydrometeors, microphysical processes. In CLEAN experiment,...

10.1175/jas-d-15-0202.1 article EN other-oa Journal of the Atmospheric Sciences 2016-01-15

Abstract This study investigated heavy frontal rainfall that occurred on 13–14 October 2011 over the Pearl River Delta (PRD) in China. The rainstorm was simulated using WRF-ARW Model (version 3.3), which included its urban canopy model. Although model-simulated convection 2 h early and second precipitation peak underestimated, model represented formation, development, extinction of captured distribution value. In addition, averaged value 49.7 W m −2 taken as anthropogenic heat flux (AHF)...

10.1175/jamc-d-18-0296.1 article EN Journal of Applied Meteorology and Climatology 2020-01-15

Substantial biomass burning (BB) activities in Indochina during March and April of each year generate aerosols that are transported via westerly winds to southern China. These BB have both radiative (direct semi-direct) indirect effects on the climate. This study evaluates impacts 2013 atmospheric conditions China using WRF-Chem sensitivity simulations. We show atmosphere becomes drier hotter under aerosol effect China, while changes linked opposite. The former (the latter) rises (reduces)...

10.4209/aaqr.2019.01.0028 article EN cc-by Aerosol and Air Quality Research 2019-01-01

Abstract This study used the Weather Research and Forecasting model with chemistry (WRF‐Chem) a parameterization for emissions of sea‐salt aerosols to assess effects on tropical cyclone. A control simulation (Ctl) emission flux that is one‐tenth in Ctl (Low) were conducted. Results show enhance condensation process, promoting vertical motion precipitation Peak value 120% Low. Enhanced results increase water vapor transport upper atmosphere, which promotes deposition growth cloud ice...

10.1002/asl.936 article EN cc-by Atmospheric Science Letters 2019-07-31

Abstract A record‐breaking rainfall event was initiated between the urban heat island (UHI) and a small trumpet‐shaped mountain (Huadu Mountain) to its north in Guangzhou City at midnight of May 6, 2017. Numerically simulating convection initiation (CI) challenging due insufficient model resolution inaccurate boundary layer parameterization, this study therefore examined pre‐convective mesoscale processes based on their four‐dimensional analyses obtained through data assimilation radar...

10.1029/2021jd034839 article EN Journal of Geophysical Research Atmospheres 2021-08-03

Abstract As one of the deep convection systems, tropical cyclones (TCs) could significantly affect thermodynamic structure and cloud microphysical processes near tropopause, which may cause changes in troposphere stratosphere water vapour activity, with important influences on global climate change. However, effects TCs tropopause lower remain unclear. Here, we use satellite data from year 2012 to 2016 assess effect at over Northwest Pacific Ocean. It is found that decrease temperature...

10.1002/asl.1006 article EN Atmospheric Science Letters 2020-08-22

Abstract The recently developed maximum entropy production (MEP) model, an alternative parameterization of surface heat fluxes, is incorporated into the Weather Research and Forecasting (WRF) model. A pair WRF cloud‐resolving experiments (5 km grids) using bulk transfer model (WRF default) MEP fluxes are performed to hindcast October Madden‐Julian oscillation (MJO) event observed during 2011 Dynamics MJO (DYNAMO) field campaign. simulated latent sensible in runs general consistent with situ...

10.1002/2017ms001175 article EN cc-by-nc-nd Journal of Advances in Modeling Earth Systems 2017-10-27

We investigate the effects of sea-salt aerosol (SSA) activated as cloud condensation nuclei on microphysical processes, precipitation, and thermodynamics a tropical cyclone (TC). The Weather Research Forecasting model coupled with Chemistry (WRF-Chem) was used together parameterization SSA production. Three simulations, different levels emission (CTL, LOW, HIGH), were conducted. simulation results show that contributes to processes autoconversion water accretion by rain, thereby promoting...

10.1007/s13351-019-8108-z article EN Journal of Meteorological Research 2019-02-01

Abstract The effects of sea salt aerosols (SSA) on cloud microphysical processes, precipitation, and upper troposphere/lower stratosphere water vapour in tropical cyclones were studied with the Weather Research Forecasting Chemistry model. Two numerical experiments conducted: a control experiment (CTL) an emission intensity one-tenth that CTL (CLEAN). Results show increased SSA concentrations, production rates auto-conversion to form rain, accretion by rain experiment, leading increase...

10.1038/s41598-019-51757-x article EN cc-by Scientific Reports 2019-10-22
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