Interannual variation of global atmospheric angular momentum

• Published in: Journal of the atmospheric sciences Vol. 53; no. 19; pp. 2852 - 2857
• Main Authors: CHEN, T.-C, TRIBBIA, J. J, YEN, M.-C
• Format: Journal Article
• Language: English
• Published: Boston, MA American Meteorological Society 01.10.1996
• Subjects: Earth, ocean, space; Exact sciences and technology; External geophysics; Meteorology; Other topics in atmospheric geophysics; Atmospheric circulation; Anomaly; El Nino; Southern oscillation; Angular momentum; Interannual variation
• ISSN: 0022-4928; 1520-0469
• DOI: 10.1175/1520-0469(1996)053<2852:ivogaa>2.0.co;2

The relative atmospheric angular momentum (RAM) integrated over the globe is an explicit variable representing the state of the atmospheric general circulation. After removing the annual, semiannual, and higher-frequency components, the filtered global RAM time series for the past 14 years (1979-92) is highly correlated with both the Southern Oscillation index and the tropical Pacific sea surface temperature averaged over Area NINO-3 (5 degrees S-5 degrees N, 150 degrees W-90 degrees W). The interannual variation of global RAM is coherent with the poleward propagation of RAM anomalies. The global RAM anomalies reach their minimum values when westerly anomalies emerge in the Tropics and higher latitudes during a cold El Nino-Southern Oscillation (ENSO) event. On the other hand, global RAM anomalies attain their maximum values when westerly anomalies arrive at the subtropics of both hemispheres during a warm ENSO event. It is demonstrated that the poleward propagation of RAM anomalies results from the flip-flop oscillation of the anomalous circulation between cold and warm ENSO events.