A Two Level Model of the Steady State Response of the Atmosphere to Midlatitude Heating with Various Zonal Structures
Author:
Affiliation:
1. Departments of Mathematics and Oceanography, University of British Columbia Vancouver
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/65/4/65_4_537/_pdf
Reference23 articles.
1. Barnett, T.P., "On the nature and causes of large-scale thermal variability in the central North Pacific," Journal of Physical Oceanography 11, 887-904(1981).
2. Chervin, R.M., Kutzbach, J.E., Houghton, D.D., and Gallimore, R.G., "Response of the NCAR general circulation model to prescribed changes in ocean surface temperature, II, Midlatitude and subtropical changes," Journal of the Atmospheric Sciences 37, 308-322 (1980).
3. Davis, R.E., "Predictability of sea surface temperature and sea level pressure anomalies over the North Pacific Ocean," Journal of Physical Oceanography 6, 249-266 (1976).
4. Davis, R.E., "Predictability of sea level pressure anomalies over the North Pacific Ocean," Journal of Physical Oceanography 8, 233-246 (1978).
5. Egger, J., "On the linear theory of the atmospheric response to sea surface temperature anomalies," Journal of the Atmospheric Sciences 34, 603-614(1977).
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1. A Time Dependent Model of the Atmospheric Response to Midlatitude Heating with Various Zonal Structures;Journal of the Meteorological Society of Japan. Ser. II;1988
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