Yuan‐Ming Cheng

ORCID: 0000-0002-6522-4297
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About
Contact & Profiles
Research Areas
  • Tropical and Extratropical Cyclones Research
  • Climate variability and models
  • Ocean Waves and Remote Sensing
  • Meteorological Phenomena and Simulations
  • Solar and Space Plasma Dynamics
  • Speech and Audio Processing
  • Atmospheric Ozone and Climate
  • Underwater Acoustics Research
  • Oceanographic and Atmospheric Processes
  • Nonlinear Waves and Solitons
  • Earthquake and Tsunami Effects
  • Acoustic Wave Phenomena Research

NOAA Physical Sciences Laboratory
2022-2023

Physical Sciences (United States)
2019-2020

NOAA Earth System Research Laboratory
2019-2020

Albany State University
2019

University at Albany, State University of New York
2019

National Taiwan University
2014

Abstract We analyze the stratospheric waves in models participating phase 1 of Stratosphere–troposphere Processes And their Role Climate (SPARC) Quasi‐Biennial Oscillation initiative (QBOi). All have robust Kelvin and mixed Rossby‐gravity wave modes winds temperatures at 50 hPa represent them better than most Coupled Model Intercomparison Project Phase 5 (CMIP5) models. There is still some spread among models, especially concerning waves. attribute variability equatorial QBOi part to varying...

10.1002/qj.3827 article EN Quarterly Journal of the Royal Meteorological Society 2020-05-19

Abstract Mesoscale convective systems (MCSs) produce over 50% of tropical precipitation and account for the majority extreme rainfall flooding events. MCSs are considered building blocks larger‐scale convectively coupled equatorial waves (CCEWs). While CCEWs can provide favorable environments convection, how systematically impact organized convection thereby MCS characteristics is less clear. We examine this question by analyzing a global tracking data set. During active phase CCEWs,...

10.1029/2023gl103335 article EN cc-by-nc-nd Geophysical Research Letters 2023-05-18

Abstract The dominant structural variability of African easterly waves (AEWs) is explored using an empirical orthogonal function (EOF) approach. structure AEWs obtained by projecting the wind fields from reanalysis data and satellite-derived brightness temperature T b onto principal components associated with EOF patterns filtered ( EOF) 700-hPa meridional (v700 EOF). wave depicted has confined convection circulation mostly south jet. It shares many characteristics analyzed discussed in...

10.1175/jas-d-18-0300.1 article EN Journal of the Atmospheric Sciences 2019-04-10

Abstract Observational evidence of two extratropical pathways to forcing tropical convective disturbances is documented through a statistical analysis satellite-derived OLR and ERA5 reanalysis. The mechanism the resulting are found strongly depend on structure background zonal wind. Although Rossby wave propagation prohibited in easterlies, modeling studies have shown that can still excite equatorial waves resonance between tropics extratropics. Here this “remote” pathway investigated for...

10.1175/jcli-d-22-0171.1 article EN Journal of Climate 2022-07-07

Mesoscale convective systems (MCSs) produce over 50% of tropical precipitation and account for the majority extreme rainfall flooding events. MCSs are considered building blocks larger-scale convectively coupled equatorial waves (CCEWs). While CCEWs can provide favorable environments convection, how systematically impact organized convection thereby MCS characteristics is less clear. We examine this question by analyzing a global tracking dataset. During active phase CCEWs, frequency...

10.22541/essoar.167810388.81352642/v1 preprint EN Authorea (Authorea) 2023-03-06
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