Paul H. Chan scite author profile

The tropical ocean-atmosphere exhibits two prominent modes of low-frequency oscillations, i.e., the "40-50" day oscillation and the El Nino/Southern Oscillation (ENSO). The two phenomena are viewed in the same perspective from 10 years of satellite-derived outgoing-longwave-radiation data. Results reveal some interesting features that may lead to new insights into the understanding of the two phenomena.

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Paul H. Chan

Aspects of the 40–50 Day Oscillation during the Northern Summer as Inferred from Outgoing Longwave Radiation

Aspects of the 40–50 Day Oscillation during the Northern Winter as Inferred from Outgoing Longwave Radiation

Intraseasonal and Interannual Variations of Tropical Convection: A Possible Link between the 40–50 Day Oscillation and ENSO?

Short-Term Climate Variability and Atmospheric Teleconnections from Satellite-Observed Outgoing Longwave Radiation. Part I: Simultaneous Relationships

The 40–50 Day Oscillation and the El Niño/Southern Oscillation: A New Perspective

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