Dw. Zheng et G. Chen, RELATION BETWEEN EQUATORIAL OCEANIC ACTIVITIES AND LOD CHANGES, Science in China. Series A, Mathematics, Physics, Astronomy & Technological Sciences, 37(3), 1994, pp. 341-347
The time series of the length of day (LOD) and the observational Pacif
ic sea level during 1962.0 - 1990.0 are used to study the relation bet
ween Earth rotation and equatorial oceanic activities. The results sho
w that (i) the sea level is apparently rising at an average rate of ab
out 1.75 +/- .01 mm/a during the past 30 years; (ii) there are large-s
cale eastward and westward water motions in the upper equatorial Pacif
ic zone, which, according to the dynamical analysis of the angular mom
entum of the large-scale sea water motion in Pacific Ocean related to
the Earth rotation axis accounts for about 30% of the change in intera
nnual Earth rotation rate; (iii) the interannual changes in Earth rota
tion also cause changes in the distribution of the water mass in equat
orial Pacific, and affect the formation of ENSO events. Based on these
results, we give a new model for the interaction between equatorial o
cean and Earth rotation.