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![]() Exercise 4: La Niña ![]() ![]()
Atmospheric convection is confined to the Western end of the basin. Rain is abundant over Indonesia.
We can also observe the effect of La Niña on sea level and surface temperatures. They are the opposite of the El Niño year. Usually SST anomalies show a more visible pattern than altimetry anomalies. LEOWorks exercise It is possible to make some animations with the series of data we have. Open the data files from 2007-2008. Compose animations with the altimetry and SST data for this period and study them.
In the LEOWorks image processing programme open Tools/Image Animation, which brings up the Select Files for Animation window. Choose the proper animation speed. You can see the number of the slide by activating the Active Slider.
1. Can you explain what effect La Niña has over the mean sea level and SST? 2. What are the differences with respect to El Niño? Last update: 17 April 2013 ![]()
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