However, there are significant differences. Ignoring for a moment the sea-level effects of currents, winds, and other forces, recall the previous discussion that much of the early El Niño signal occurs below the ocean surface. It takes some time for heating at 100 m to reach the surface. However, the changes will be seen by sea-level measured by altimetry or the moored buoys which monitor temperature to a deep level as they are happening. This means that altimetry can see El Niño signals slightly before the SST measurements can. The difference in time is only slight, about two weeks to a month. However by combining the two measurements one can get a more complete picture of how El Niño evolves.
The next four slides will demonstrate this by showing complementary sea-level and SST anomalies for each month during 1997. The fifth slide following will summarize important events during the evolution of the 1997 El Niño.
Slide 17 of 27
Last Modified: Fri, Jul 2, 1998
CSR/TSGC Team Web