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dc.contributorGiese, Benjamin
dc.creatorPerugachi Salamea, Carlos
dc.date.accessioned2012-02-14T22:19:43Z
dc.date.accessioned2012-02-16T16:19:15Z
dc.date.accessioned2017-04-07T19:59:32Z
dc.date.available2012-02-14T22:19:43Z
dc.date.available2012-02-16T16:19:15Z
dc.date.available2017-04-07T19:59:32Z
dc.date.created2011-12
dc.date.issued2012-02-14
dc.identifier.urihttp://hdl.handle.net/1969.1/ETD-TAMU-2011-12-10374
dc.description.abstractThe ocean reanalysis Simple Ocean Data Assimilation (SODA) 2.2.4 is used to explore the changes in upwelling from normal conditions to either El Nino or La Nina conditions. Physical and thermodynamic variables from the reanalysis are used to explore the structure and behavior of El Nino Southern Oscillation (ENSO) events. The results of this analysis show that sea surface temperature (SST), entrainment velocity, wind stress, mixed layer depth, wind curl, and heat content anomalies are in general agreement with ENSO theory. Interestingly, the distribution of upwelling based on the entrainment velocity is very patchy, which led us to explore zonal and meridional sections of vertical velocity. We used three methods to compute changes in upwelling during ENSO events. The first method computes upwelling within the areas of SST anomalies during ENSO events. During El Nino events upwelling shows prominent decadal variability, while during La Nina the decadal variability is weaker. A new upwelling index is used for the second method, and upwelling is computed in the areas of strong upwelling anomalies. The variability of upwelling is higher in periods of reduced upwelling than in periods of strong upwelling. Despite the fact that the new index is computed independently, it agrees in the timing of the index used to define ENSO events for this research. The first and second methods show that the amplitude of SST anomalies and upwelling anomalies do not have a direct relationship, suggesting that upwelling does not explain all of the variance in SST. The last method used is to compute changes in upwelling in the Nino 1+2 region during ENSO events. In the east Pacific there is almost no correlation between upwelling and SST anomalies during ENSO, but this might be attributed to the fact that the Nino 1+2 region is a relatively small region compared to the Nino 3.4 region that is used to define ENSO events. In general, the time series of SST and upwelling anomalies agree well just in the cases when ENSO events are prominently in the eastern Pacific. A comparison between yearly fisheries data from Ecuador and Peru and monthly data of SST anomalies during ENSO years is presented showing that during El Nino events the fish catch decreases and during La Nina events the fish catch increases. We infer that the increase or decrease in fish catch is associated to changes in fish populations, and that these changes are mainly due to availability of nutrients and changes in temperature during ENSO events.
dc.language.isoen_US
dc.subjectEl Ni?o Southern Oscillation
dc.subjectENSO
dc.subjectSODA
dc.subjectupwelling
dc.subjectEastern Equatorial Pacific
dc.titleAnalysis of Upwelling Changes in the Eastern Equatorial Pacific during El Ni?o Southern Oscillation
dc.typeThesis


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