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Climate dynamics: why does climate vary?

1, 2010

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Why do we have El Niño: quantifying a diabatic and nonlinear perspective using observations

Climate dynamics, 2019-06, Vol.52 (11), p.6705-6717

2019

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A Further Study on the Simulation of Cloud-Radiative Feedbacks in the ENSO Cycle in the Tropical Pacific with a Focus on the Asymmetry

한국기상학회지, 2019, 55(3), , pp.303-316

2019

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Precipitation and Moisture in Four Leading CMIP5 Models: Biases across Large-Scale Circulation Regimes and Their Attribution to Dynamic and Thermodynamic Factors

Journal of climate, 2018-07, Vol.31 (13), p.5089-5106

2018

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Weak ENSO Asymmetry Due to Weak Nonlinear Air-Sea Interaction in CMIP5 Climate Models

Advances in atmospheric sciences, 2016-03, Vol.33 (3), p.352-364

2016

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A Further Study of ENSO Rectification: Results from an OGCM with a Seasonal Cycle

Journal of climate, 2015-02, Vol.28 (4), p.1362-1382

2015

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A Nonlinear Cause for the Seasonal Predictability Barrier of SST Anomaly in the Tropical Pacific

Journal of geophysical research. Oceans, 2022-10, Vol.127 (10), p.n/a

2022

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Contrasting Cloud Radiative Feedbacks during Warm Pool and Cold Tongue El Niños

SOLA, 2018, Vol.14, pp.126-131

2018

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Western Pacific Warm Pool and ENSO Asymmetry in CMIP3 Models

Advances in atmospheric sciences, 2013-05, Vol.30 (3), p.940-953

孙燕 De-Zheng SUN 吴立新王凡

2013

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A regulatory effect of ENSO on the time-mean thermal stratification of the equatorial upper ocean

Geophysical research letters, 2006-04, Vol.33 (7), p.L07710-n/a

2006

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What causes the excessive response of clear-sky greenhouse effect to El Niño warming in Community Atmosphere Models?

Journal of Geophysical Research - Atmospheres, 2008-01, Vol.113 (D2), p.D02108-n/a

2008

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Response of water vapor and clouds to El Niño warming in three National Center for Atmospheric Research atmospheric models

Journal of Geophysical Research - Atmospheres, 2006-09, Vol.111 (D17), p.D17103-n/a

2006

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An Evaluation Analysis for Computed Tomography Image Quality of Primary Liver Cancer Lesions Based on Deep Learning Image Reconstruction

Current medical imaging reviews, 2024, Vol.20, p.1

2024

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The role of the Indian Ocean in determining the tropical pacific SST response to radiative forcing in an idealized model

Dynamics of atmospheres and oceans, 2019-06, Vol.86, p.1-9

2019

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Water vapor and cloud radiative forcings over the Pacific Ocean simulated by the LASG/IAP AGCM: Sensitivity to convection schemes

Advances in atmospheric sciences, 2011-01, Vol.28 (1), p.80-98

2011

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The Diabatic and Nonlinear Aspects of the El Niño–Southern Oscillation: Implications for Its Past and Future Behavior

Climate Dynamics, 2010, Vol.189, p.79-103

2010

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A Brief Introduction to El Niño and La Niña

Climate Dynamics, 2010, Vol.189, p.53-64

2010

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Regime Behavior in the Sea Surface Temperature-Cloud Radiative Forcing Relationships over the Pacific Cold Tongue Region

Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao, 2010, Vol.3 (5), p.271-276

2010

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ENSO Asymmetry in CMIP6 Models

Journal of climate, 2022-09, Vol.35 (17), p.5555-5572

2022

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Arctic Sea Ice and the Potential for Abrupt Loss

Climate Dynamics: Why Does Climate Vary?, 2010, p.181-191

2010

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Factors Determining the Asymmetry of ENSO

Journal of climate, 2017-08, Vol.30 (16), p.6097

2017

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The Control of Meridional Differential Surface Heating Over the Level of Enso Activity: A Heat‐Pump Hypothesis

Earth's Climate, 2004, p.71-83

2004

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Design and Implementation of MP3 Player Based on FPGA

Applied Mechanics and Materials, 2013-10, Vol.443 (Computer-Aided Design, Manufacturing, Modeling and Simulation III), p.746-749

Sun, De Zheng

2013

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Preface

Atmospheric research, 2009-09, Vol.94 (1), p.1-2

2009

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Response of water vapor and clouds to el Nino warming in three National Center for Atmospheric Research atmospheric models

Journal of Geophysical Research. D. Atmospheres, 2006-09, Vol.111 (D17)

2006

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Climate dynamics: why does climate vary?

Why do we have El Niño: quantifying a diabatic and nonlinear perspective using observations

A Further Study on the Simulation of Cloud-Radiative Feedbacks in the ENSO Cycle in the Tropical Pacific with a Focus on the Asymmetry

Precipitation and Moisture in Four Leading CMIP5 Models: Biases across Large-Scale Circulation Regimes and Their Attribution to Dynamic and Thermodynamic Factors

Weak ENSO Asymmetry Due to Weak Nonlinear Air-Sea Interaction in CMIP5 Climate Models

A Further Study of ENSO Rectification: Results from an OGCM with a Seasonal Cycle

A Nonlinear Cause for the Seasonal Predictability Barrier of SST Anomaly in the Tropical Pacific

Contrasting Cloud Radiative Feedbacks during Warm Pool and Cold Tongue El Niños

Western Pacific Warm Pool and ENSO Asymmetry in CMIP3 Models

A regulatory effect of ENSO on the time-mean thermal stratification of the equatorial upper ocean

What causes the excessive response of clear-sky greenhouse effect to El Niño warming in Community Atmosphere Models?

Response of water vapor and clouds to El Niño warming in three National Center for Atmospheric Research atmospheric models

An Evaluation Analysis for Computed Tomography Image Quality of Primary Liver Cancer Lesions Based on Deep Learning Image Reconstruction

The role of the Indian Ocean in determining the tropical pacific SST response to radiative forcing in an idealized model

Water vapor and cloud radiative forcings over the Pacific Ocean simulated by the LASG/IAP AGCM: Sensitivity to convection schemes

The Diabatic and Nonlinear Aspects of the El Niño–Southern Oscillation: Implications for Its Past and Future Behavior

A Brief Introduction to El Niño and La Niña

Regime Behavior in the Sea Surface Temperature-Cloud Radiative Forcing Relationships over the Pacific Cold Tongue Region

ENSO Asymmetry in CMIP6 Models

Arctic Sea Ice and the Potential for Abrupt Loss

Factors Determining the Asymmetry of ENSO

The Control of Meridional Differential Surface Heating Over the Level of Enso Activity: A Heat‐Pump Hypothesis

Design and Implementation of MP3 Player Based on FPGA

Preface

Response of water vapor and clouds to el Nino warming in three National Center for Atmospheric Research atmospheric models

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