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An inspection of the PMEL analysis of the Pacific water volume anomalies (a measure of ocean heat content) indicates a most curious behavior of the Pacific Ocean temperatures during this La Nina.
The figure I'm looking at is our attribution toolbox:
http://www.cdc.noaa.gov/CSI/tools.html
Go to Current Conditions item 6, and select the Warm Water
Volume: East vs West
In the PMEL analysis of the 25-yr history of water water volume
anomaly, there have occurred 3 prior La Nina periods - roughly around 1984,
1988, 1999. In all those, a (low)
cold water volume anomaly in the west Pacific preceeds the low (cold) water
volume anomaly in the east Pacific (and also the SST cooling of the eastern
Pacific) by about 6 months or so from my read of the graph.
The current La Nina has seen no low (cold) water volume
anomaly in the west Pacific, either as a precursor for this event in spring
2007, or as a current condition this Fall 2007.
The questions I'd like to toss out to CSI team for discussion
are:
Q1: Is there
something unique about the physical processes responsible for this La Nina
relative to its prior 3 ancestors?
Q2: Has this
differnence in antecdent Pacific basin conditions affected the predictability
of this La Nina relative to its prior 3 ancestors?
Q3: What is the physical role of the antecedent water volume
anomalies in the western Pacific for subsequent ENSO development (it seems to
be neither a necessary nor a sufficient factor for ENSO development)
Q4: To my eye, there is a hint in the PMEL historical
analysis that conditions of low water volume anomalies in the easterm Pacific have a longer time scale than
the opposite phased anomalies. Is
there reason, based upon current water volume condition, and historical events,
to suspect that 2008 will be more likely La Nina rather than El Nina? (I note
that many prediction models show this La Nina terminating in spring 2008)