Y. Wang

ORCID: 0009-0004-2217-4439
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About
Contact & Profiles
Research Areas
  • Atmospheric Ozone and Climate
  • Quantum Chromodynamics and Particle Interactions
  • Atmospheric chemistry and aerosols
  • Particle physics theoretical and experimental studies
  • Astrophysics and Star Formation Studies
  • Astro and Planetary Science
  • Atmospheric and Environmental Gas Dynamics
  • Nuclear physics research studies
  • Atomic and Molecular Physics
  • Advanced NMR Techniques and Applications
  • Stellar, planetary, and galactic studies
  • High-Energy Particle Collisions Research
  • Solar and Space Plasma Dynamics
  • Air Quality and Health Impacts
  • Climate variability and models
  • Mass Spectrometry Techniques and Applications

Tsinghua University
2014-2023

Jilin University
2023

Rutgers, The State University of New Jersey
2002-2015

Georgia Institute of Technology
2007

Abstract Tropospheric ozone plays a major role in Earth’s atmospheric chemistry processes and also acts as an air pollutant greenhouse gas. Due to its short lifetime, dependence on sunlight precursor emissions from natural anthropogenic sources, tropospheric ozone’s abundance is highly variable space time seasonal, interannual decadal time-scales. Recent, sometimes rapid, changes observed mixing ratios inspired us produce this up-to-date overview of global distribution trends. Much the text...

10.12952/journal.elementa.000029 article EN cc-by Elementa Science of the Anthropocene 2014-01-01

We define the radiative forcings used in climate simulations with SI2000 version of Goddard Institute for Space Studies (GISS) global model. These include temporal variations well‐mixed greenhouse gases, stratospheric aerosols, solar irradiance, ozone, water vapor, and tropospheric aerosols. Our illustrations focus on period 1951–2050, but we make full data sets available those which have earlier data. illustrate response to these model specified sea surface temperature a simple Q ‐flux...

10.1029/2001jd001143 article EN Journal of Geophysical Research Atmospheres 2002-09-20

Planets, embedded in their natal discs, harbour hot envelopes. When pebbles are accreted by these planets, the contained volatile components may sublimate, enriching envelope and potentially changing its thermodynamical properties. However, envelopes of planets actively exchange material with disc, which would limit buildup a vapour-rich atmosphere. To properly investigate processes, we have developed new phase change module to treat sublimation process hydrodynamical simultions. Combined...

10.1093/mnras/stad1753 article EN Monthly Notices of the Royal Astronomical Society 2023-06-16

Context. Protoplanetary disks, the birthplaces of planets, commonly feature bright rings and dark gaps in both continuum line emission maps. Accreting planets interact with disk, not only through gravity, but also by changing local irradiation elemental abundances, which are essential ingredients for disk chemistry. Aims. We propose that giant planet accretion can leave chemical footprints gas to planet, potentially leads spatial coincidence molecular emissions ALMA observations. Methods....

10.1051/0004-6361/202346637 article EN cc-by Astronomy and Astrophysics 2023-08-04

Fourier transform spectrum and its fit with the colored arrows indicating individual hyperfine structure components distinguished by transition rules.

10.1039/d3ja00160a article EN Journal of Analytical Atomic Spectrometry 2023-11-21

New results are reported from a measurement of $\pi^0$ electroproduction near threshold using the $p(e,e^{\prime} p)\pi^0$ reaction. The experiment was designed to determine precisely energy dependence $s-$ and $p-$wave electromagnetic multipoles as stringent test predictions Chiral Perturbation Theory (ChPT). data were taken with an electron beam 1192 MeV two-spectrometer setup in Hall A at Jefferson Lab. For first time, complete coverage $\phi^*_{\pi}$ $\theta^*_{\pi}$ angles $p \pi^0$...

10.1103/physrevlett.114.192503 article EN publisher-specific-oa Physical Review Letters 2015-05-13

Abstract. Trace gas measurements of TOPSE and TRACE-P experiments corresponding global GEOS-CHEM model simulations are analyzed with the Positive Matrix Factorization (PMF) method for evaluation purposes. Specially, we evaluate simulated contributions to O3 variability from stratospheric transport, intercontinental production urban/industry biomass burning/biogenic sources. We select a suite relatively long-lived tracers, including 7 chemicals (O3, NOy, PAN, CO, C3H8, CH3Cl, 7Be) 1 dynamic...

10.5194/acpd-7-15495-2007 preprint EN cc-by 2007-11-02
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