Skip to main content
Log in

Adventures in Data Analysis: The TAO Array and the 1997–1998 El Niño

  • Published:
Mathematical Geology Aims and scope Submit manuscript

Abstract

Traditional undergraduate education in earth sciences does not emphasize data acquisition, analysis, or assessment. However, arrival of the information age dictates that earth sciences graduates be imbued with fundamental skills to organize, evaluate and process large data sets. Fortunately, the proliferation of remotely sensed data and its availability via the Internet provides many opportunities for earth science educators to meet these needs. Exercises to introduce students to data analysis have been designed utilizing data from the Tropical Atmosphere–Ocean (TAO) Array and the 1997–1998 El Niño episode in the tropical Pacific Ocean. The TAO Array is a grid of 69 buoys moored across the equatorial Pacific Ocean (8°N to 8°S and 95°W to 143°E) recording environmental data relevant to El Niño—Southern Oscillation (ENSO) processes. Data from the TAO Array is available in near-real-time (http://www.pmel.noaa.gov/toga-tao/realtime.html) or as archived ASCII files (http://www.pmel.noaa.gov/toga-tao/data-delivery.html) providing daily (sometimes hourly) records of environmental parameters for each buoy in the grid. Student exercises in data analysis begin with downloading data from buoy locations, parsing the data into spreadsheets, and organizing data by environmental parameter into yearly and monthly data sets. Analyses of reconstructed data include calculations of long-term averages of environmental parameters, seasonal climatologies, monthly climatologies and calculation of long-term, seasonal, and monthly anomalies. Finally, monthly anomaly maps produced by students are loaded sequentially into GIF-animation software to create time-series images illustrating the progress and development of the 1997–1998 El Niño event.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

REFERENCES

  • Anderson, R. Y., 1992, Long-term changes in the frequency of occurrence of El Niño events, in Diaz, H. F., and Markgraf, V., eds., El Niño: Historical paleoclimatic aspects of the Southern Oscillation: Cambridge University Press, Cambridge, UK, p. 193–200.

    Google Scholar 

  • Anonymous, 1995, El Niño watching on World Wide Web: Sea Frontiers, Fall 1995, p. 26–29.

  • Allan, R., Lindesay, J., and Parker, D., 1996, El Niño Southern Oscillation and climatic variability: CSIRO Publishing, Collingwood, Victoria, Australia, 405 p.

    Google Scholar 

  • Atlas, R., Bloom, S. C., Hoffman, R. N., Ardizzone, J. V., and Brin, G., 1991, Space-based surface wind vectors to aid understanding of air-sea interactions: EOS, Trans. Am. Geophys. Union, v. 72, p. 201–208.

    Google Scholar 

  • Bjerknes, J., 1966, A possible response of the atmospheric Hadley circulation to equatorial anomalies of ocean temperature: Tellus, v. 18, p. 820–829.

    Google Scholar 

  • Bjerknes, J., 1969, Atmospheric teleconnections from the equatioral Pacific: Mon. Whether Rev., v. 97 p. 163–172.

    Google Scholar 

  • Bjerknes, J., 1972, Large-scale amospheric response to the 1964–65 Pacific equatorial warming: Jour. Phys. Oceanography, v. 2, p. 212–217.

    Google Scholar 

  • Boutin, J., and Etcheto, J., 1996, Consistency of GEOSAT, SSM/I and ERS1 global surface wind speeds; comparison with in-situ data: Jour. Atmos. Ocean. Tech., v. 13, p. 183–187.

    Google Scholar 

  • Busalacchi, A. J., McPhaden, M. J., and Picaut, J., 1994,Variability in the equational Pacific sea surface topography during the verification phase of the TOPEX/POSEIDON mission: Jour. Geophys Res., v. 99, p. 24,725-24,738.

    Google Scholar 

  • Cane, M., 1986, El Niño: Ann. Rev. of Earth and Planetary Sci., v. 14, p. 43–70.

    Google Scholar 

  • Cheney, R. E., Douglas, B. C., and Miller, L., 1989, Evaluation of GEOSAT altimeter data with application to tropical Pacific sea-level variability: Jour. Geophys. Res., v. 94, p. 4737–4747.

    Google Scholar 

  • Diaz, H. F., and Markgraf, V., eds., 1992, El Nino: Historical paleoclimatic aspects of the Southern Oscillation: Cambridge University Press, Cambridge, UK, 476 p.

  • Freitag, H. P., Mangum, L. J., and McPhaden, M. J., 1995, Tropical Atmosphere Ocean Array—Update: Sea Tech., v. 36, No. 10, p. 47–50.

    Google Scholar 

  • Giese, B. S., Carton, J. A., and Holl, L. J., 1994, Sea level variability in the eastern tropical Pacific as observed by TOPEX and Tropical Ocean-Global Atmosphere Tropical Atmosphere-Ocean Experiment: Jour. Geophys. Res., v. 99, p. 24,739-24,748.

    Google Scholar 

  • Goddard, L., and Graham, N. E., 1997, El Niño in the 1990's: Jour. Geophys. Res., v. 102, p. 10,423–10,436.

    Google Scholar 

  • Halpern, D., 1993, Validation of special sensor microwave imager monthly-mean wind speed from July 1987 to December 1989: IEEE Transactions on Geoscience and Remote Sensing, v. 31, p. 692–699.

    Google Scholar 

  • Halpern, D., and Ji, M., 1993, An evaluation of the National Meterological Center weekly hindcast of upper-ocean temperature along the eastern Pacific equator in January 1992: Jour. Climate, v. 6, p. 1221–1226.

    Google Scholar 

  • Halpern, D., Chao, Y., Ma, C.-C., and Mechoso, C. R., 1995, Comparison of tropical Pacific temperature and current simulations with two vertical mixing schemes embedded in an ocean general circulation model and reference to observations: Jour. Geophys. Res., v. 100, p. 2515–2522.

    Google Scholar 

  • Hayes, S. P., 1989, The Tropical Atmosphere Ocean (TOGA-TAO) mooring array: Proc. of the Int. Symp. on Japanese Pacific Climate Study (JAPACS), Tsukuba, Japan, October 1989.

  • Hayes, S. P., 1990, The TOGA Tropical Atmosphere-Ocean (TAO) Array: Proc. of the U.S.-JAPAN Bilateral Meeting on Tropical Air-Sea Interaction, Seattle, Washington, September 10–14, 1990.

  • Hayes, S. P., Mangum, L. J., Picaut, J., Sumi, A., and Takeuchi, K., 1991, TOGA-TAO: A moored array for real-time measurements in the tropical Pacific Ocean: Bull. Am. Met. Soc., v. 72, 339–347.

    Google Scholar 

  • Hayes, S. P., McPhaden, M. J., Leetmaa, A., and Reynolds, R., 1989, Real-time monitoring of the tropical Pacific Ocean: EOS, Trans. Am. Geophys. Union, v. 70, p. 1149.

    Google Scholar 

  • Hilton, A., 1997, Special Section—Climate data from the TOGA-TAO Buoy Array: Pacific ENSO Update, v. 3, No. 1, p. 9.

    Google Scholar 

  • Ji, M., and Smith, T. M., 1995, Ocean model response to temperature data assimilation and varying surface wind stress: Intercomparisons and implications for climate forecast: Mon. Weather Rev., v. 123, p. 1811–1821.

    Google Scholar 

  • Katz, E. J., Busalacchi, A., Bushnell, M., Gonzalez, F. I., Gourdeau, L., McPhaden, M. J., and Picaut, J., 1995, A comparison of coincidental time series of the ocean surface height by satellite altimeter, mooring, and inverted echo sounder: Jour. Geophys. Res., v. 100, p. 25,101–25,108.

    Google Scholar 

  • Kleeman, R., Coleman, R. A., Smith, N. R., and Power, S. B., 1996, A recent change in the mean state of the Pacific basin climate: Observational evidence and atmospheric and oceanic responses: Jour. Geophys. Res., v. 101, p. 20,483–20,500.

    Google Scholar 

  • Kleeman, R., Moore, A. M., and Smith, N. R., 1995, Assimilation of subsurface thermal data into a simple ocean model for the initialization of an intermediate tropical coupled ocean-atmosphere forecast model: Mon. Weather Rev., v. 123, p. 3103–3113.

    Google Scholar 

  • Latif, M., Biercamp, J., von Storch, H., McPhaden, M. J., and Kirk, E., 1990, Analyses of tropical anomalies simulated by an AGCM: Jour. Climate, v. 3, p. 509–521.

    Google Scholar 

  • Liu, W. T., Tang, W., and Atlas, R., 1996, Responses of the tropical Pacific to wind forcing as observed by spaceborne sensors and simulated by an ocean general circulation model: Jour. Geophys. Res., v. 101, p. 16,345–16,360.

    Google Scholar 

  • McPhaden, M. J., 1995a, Moored buoys used for El Niño prediction: Fisheries Newsletter, v. 74, p. 38–40.

    Google Scholar 

  • McPhaden, M. J., 1995b, The Tropical Atmosphere-Ocean Array is completed. Bull. Am. Met. Soc., v. 76, p. 739–741.

    Google Scholar 

  • McPhaden, M. J., 1993, TOGA-TAO and the 1991–93 El Niño-Southern Oscillation Event: Oceanography, v. 6, p. 36–44.

    Google Scholar 

  • McPhaden, M. J., and Hayes, S. P., 1991,On the variability of winds, sea surface temperature and surface layer heat content in the western equatorial Pacific: Jour. of Geophys. Res., v. 96, p. 3331–3342.

    Google Scholar 

  • Menkes, C., Boulanger, J.-P., and Busalacchi, A. J., 1995, Evaluation of TOPEX and basin-wide Tropical Ocean and Global Atmosphere-Tropical Atmosphere Ocean sea surface topographies and derived geostrophic currents: Jour. Geophys. Res., v. 100, p. 25,087–25,100.

    Google Scholar 

  • Miller, R. N., 1990, Tropical data assimilation experiments with simulated data: The impact of the TOGA-TAO array: Jour. Geophys. Res., v. 95, p. 11,461–11,482.

    Google Scholar 

  • Nowlin, W. D., Smith, N., Needler, G., Taylor, P. K., Weller, R., Schmitt, R., Merlivat, L., Vézina, A., Alexiou, A., McPhaden, M. J., and Wakatsuchi, M., 1996, An Ocean Observing System for climate: Bull. Am. Met. Soc., v. 77, p. 2243–2273.

    Google Scholar 

  • Philander, G. S., 1998, Who is El Niño?: EOS Trans. Am. Geophys. Union, v. 79, p. 239.

    Google Scholar 

  • Philander, G. S., 1990, El Niño, La Niña, and the Southern Oscillation: Academic Press, San Diego, CA, 293 p.

    Google Scholar 

  • Picaut, J., Busalacchi, A. J., McPhaden, M. J., and Camusat, B., 1990, Validation of the geostrophic method for estimating zonal currents at the equator from GEOSAT altimeter data: Jour. Geophys. Res., v. 95, p. 3015–3024.

    Google Scholar 

  • Picaut, J., Busalacchi, A. J., McPhaden, M. J., Gourdeau, L., Gonzalez, F. I., and Hackert, E. C., 1995, Open-ocean validation of TOPEX/POSEIDON sea level in the western equatorial Pacific Jour. Geophys. Res., v. 100, p. 25,109–25,127.

    Google Scholar 

  • Pond, S., and Pickard, G. L., 1986, Introductory dynamical oceanography: Pergamon Press, Oxford, UK, 329 p.

    Google Scholar 

  • Ramage, C. S., 1986, El Niño: Sci. Am., v. 254, p. 76–83.

    Google Scholar 

  • Rasmusson, E. M., 1985, El Niño and variations in climate: Am. Scientist, v. 73, p. 168–177.

    Google Scholar 

  • Reynolds, R. W., Arpe, K., Gordon, C., Hayes, S. P., Leetmaa, A., and McPhaden, M. J., 1989, A comparison of tropical Pacific surface wind analyses: Jour. Climate, v. 2, p. 105–111.

    Google Scholar 

  • Reynolds, R.W., and Smith, T. M., 1995, A high-resolution global sea surface temperature climatology: Jour. Climate, v. 8, p. 1571–1583.

    Google Scholar 

  • Rothstein, L. M., and Chen, D., 1996, The El Niño/Southern Oscillation Phenomenon: Oceanus, v. 39, p. 39–41.

    Google Scholar 

  • Rufenach, C., 1995, A new relationship between radar cross-section and ocean surface wind speed using ERS-1 scatterometer and buoy measurements: Int. Jour. Rem. Sensing, v. 16, p. 3629–3647.

    Google Scholar 

  • Sagalyn, R., 1996, The great American Web book: A citizen's guide to the treasures of the U.S. government on the World Wide Web: Random House, New York, 257 p.

    Google Scholar 

  • Steffin, O., and McPhaden, M. J., 1992, The TOGA-TAO Array. Argos Newsletter, Special Issue on Operational Program, p. 8–11.

  • Walker, G. T., 1924, Correlation in seasonal variations of weather, IX:A further study ofworld weather: Mem India Met. Dept., v. 24, p. 275–332.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Boss, S.K. Adventures in Data Analysis: The TAO Array and the 1997–1998 El Niño. Mathematical Geology 32, 159–185 (2000). https://doi.org/10.1023/A:1007523322222

Download citation

  • Issue Date:

  • DOI: https://doi.org/10.1023/A:1007523322222

Navigation