-
Abstract:
The EOF thechnique is employed to investigate the characteristic modes of spatial distribution and features of temporal variation in the context of 1970-1989 wind stress and SSTA datasets over the tropical Pacific. Results show similar variation in the time coefficients of the first eigenvectors for the wind stress and SSTA fields, revealing air-sea interaction and coupling at the multiple space/time scales,which are in fairly good correspondence to the E1 Nino cycle.
-
References
|
[1]
|
Barnett T T,1991. The interaction of multiple time scales in the tropical climate system. J. Climate 4:209-285. |
|
[2]
|
Bierknes J,1969. Atmospheric teleconnections from the equatorial Pacific. Mon. Wea. Rev., 97:163-172. |
|
[3]
|
Gi11AE,1985. Elements of coupled ocean-atmosphere models,in J. C. J. Nohoul (ed.)Coupled Ocean-Atmosphere Models of Elsovier Oceanog-aphy Series,40:303-327. |
|
[4]
|
Li Chongyin,1988. Frequent activities of highly vigorous East-China deep troughs in relation to El Nino genesis. Actor Scientia Sinica (Ser. B),667-674. |
|
[5]
|
Li Jun,Wang Panxing,He Jinhai,1989. Analysis of January SST correlation structures on a global basis. J. Nanjing Inst. Meteor.,12:34-43 (in Chinese with English abstract). |
|
[6]
|
Philander S G. Yamagata T,Pecaunawsri R C,1984. Unstable air-sea interaction in the tropics.J. Atmos. Sci.,41:604-613. |
|
[7]
|
Weare B C,1977. Empirical orthogonal analysis of Atlantic ocean surface temperature. Quart. J. R.Met. Soc.,103:467-476. |
|
[8]
|
Weare B C. Nasstrom J S. 1982. Examples of extended empirical orthogonal function analysis. Mon. Wea. Rev.,110:481-485. |
-
-
-
粤公网安备 4401069904700002号
DownLoad: