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Ping Chang

Researcher at Texas A&M University

Publications -  205
Citations -  15655

Ping Chang is an academic researcher from Texas A&M University. The author has contributed to research in topics: Sea surface temperature & Tropical Atlantic. The author has an hindex of 53, co-authored 184 publications receiving 13591 citations. Previous affiliations of Ping Chang include Ocean University of China & University of Washington.

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Weakening Atlantic Niño-Pacific connection under greenhouse warming.

TL;DR: It is shown that greenhouse warming leads to a weakened influence from the Atlantic Niño/Niña on the Pacific ENSO, which is projected to be less affected by theAtlantic Niño/ Niña and more challenging to predict as an Atlantic precursor weakens.
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The Barrier Layer of the Atlantic Warmpool: Formation Mechanism and Influence on the Mean Climate

TL;DR: In this article, the authors used a coupled general circulation model (CGCM) to perform a set of idealised numerical experiments to test and understand the sensitivity of the barrier layer (BL) and consequently sea surface temperature (SST) bias in the NWTA region to freshwater flux and hence the upper ocean salinity stratification.
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Rossby wave packets in baroclinic mean currents

TL;DR: In this paper, a WKB description of the propagation of Rossby wave packets in a shallow water model of the tropical oceans indicates that the presence of the baroclinic mean currents can modify the characteristics of wave propagation significantly.
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Prediction of tropical Atlantic sea surface temperature

TL;DR: In this paper, the authors show that the variability of sea surface temperature (SST) in the tropical Atlantic Ocean has a significant influence on the rainfall over Northeast Brazil and the Sahel, and the predictability of the SST fluctuations in this region has been a central concern for Atlantic climate studies.
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Maintenance of mid-latitude oceanic fronts by mesoscale eddies.

TL;DR: Using high-resolution climate simulations, it is found that the vertical heat transport by ocean mesoscale eddies acts as an important heat supplier to the surface ocean in frontal regions, tightly related to the atmospheric forcing.