Abstract
The principal variability patterns (EOF) of the anomalies of total heat transfer from ocean to atmosphere computed from 30 years' monthly averaged data over the North Pacific Ocean (20°–60°N) showed variability was dominated by two patterns: a bipolar pattern and a dominantly positive or negative pattern depending on the sign of the time series coefficients. The atmosphere contributes greatly to the marine heating anomalies in most of the North Pacific in all seasons. In winter, a positive feedback is formed between the Aleutian Low and the marine heating anomalies; in summer, the marine heating anomalies are controlled by the heating on the Qinghai-Tibetan Plateau. Both patterns have a winter correlation with the Southern Oscillation Index.
Similar content being viewed by others
References
Bjerknes, J., 1969. Atmospheric teleconnections from the equatorial Pacific.Mon. Wea. Rev. 97:163–172.
Convey, D.L. and S. Hastenrath, 1978. The Pacific E1 Niño phenomenon and the Atlantic circulation.Mon. Wea. Rev. 106:1280–1291.
Davis, R. E., 1976. Predictability of the sea surface temperature and sea level pressure anomalies over the North Pacific Ocean.J. Phys. Oceanogr. 6:249–266.
Frankignoul, C., 1985. Sea surface temperature anomalies, planetary waves, and air-sea feedback in the middle latitudes.Rev. Geophys. 23:357–390.
Kawamura, R., 1984. Relation between atmospheric circulation and dominant sea surface temperature anomaly patterns in the North Pacific during the northern winter.J. Metero. Soc. Japan 62:910–916.
Kraus, E.B., 1972. Atmosphere Ocean Interaction. Clarendon press. Oxford, pp. 200–254.
Love, G., 1985. A study of the linear relationships between the monthly mean fields of sea surface temperature, mean sea level pressure and cloudiness over the northwest Pacific.J. Meteoro. Soc. Japan 63:201–209.
Namias, J., 1973. Thermal communication between the sea surface and the lower troposphere.J. Phys. Oceanogr. 3:373–378.
Namias J., 1976. Negative ocean-air feedback system over the North Pacific in the transition from warm to cold seasons.Mon. Wea. Rev. 104:1107–1121.
Namias, J. and D. R. Cayan, 1981. Large scale air-sea interactions and short period climatic fluctuations.Science 214:869–876.
Pan, Y. H. and Oort, D. R., 1983. Global temperature anomalies in the Eastern Pacific Ocean for the 1958–1973 period.Mon. Wea. Rev. 111:1244–1259.
Storch, E. R. and G. Hannoschock, 1985. Statistical aspects of estimated principal vectors (EOFs) based on small sample sizes.J. Climate Appl. Meteorol. 24:231–240.
Wallace, J. M. and Gutzler, D. S., 1981. Teleconnections in the geopotential height during the Northerr. Hemisphere winter.Mon. Wea. Rev. 109:784–812.
Wang S. W., Zhao Z. C. and Chen Z. L., 1983. The persistence and the rhythm of anomalies of monthly mean atmospheric circulation in relation to ocean atmosphere interaction.Acta. Meteor. Sinica 41:33–42.
Yen, D. C., 1981. Some characteristics of the summer circulation over the Qinghai Tibet Plateau and its neighborhood.Bull. Amer. Meteorl. Soc. 62:14–19.
Author information
Authors and Affiliations
Additional information
Contribution No. 1534 from the Institute of Oceanology, Academia Sinica
Rights and permissions
About this article
Cite this article
Yongping, Z., McBean, G.A. Principal North Pacific heating anomaly patterns and their relations to the atmospheric circulation. Chin. J. Ocean. Limnol. 7, 123–134 (1989). https://doi.org/10.1007/BF02842748
Received:
Issue Date:
DOI: https://doi.org/10.1007/BF02842748