By Allan J. Clarke

ISBN-10: 0120885484

ISBN-13: 9780120885480

Many scientists both engaged on the El Niño/Southern Oscillation (ENSO) challenge or its many purposes haven't been proficient in either the equatorial ocean and atmospheric dynamics essential to know it. This ebook seeks to beat this hassle by way of offering a step-by-step creation to ENSO, assisting the higher point graduate scholar or study scientist to benefit quick the ENSO fundamentals and be modern with the most recent ENSO learn. The textual content assumes that the reader has a data of the equations of fluid mechanics on a rotating earth and emphasizes the observations and easy actual factors of them.

Following a heritage of ENSO and a dialogue of ENSO observations in Chapters 1 and a couple of, Chapters 3-5 ponder correct equatorial ocean dynamics, Chapters 6 and nine suitable atmospheric dynamics, and Chapters 7 and eight the most paradigms for a way the Pacific Ocean and surroundings couple jointly to supply ENSO. bankruptcy eight additionally discusses the previous secret of why ENSO has a tendency to be locked in part with the seasonal cycle. winning dynamical and statistical ways to ENSO prediction are mentioned in Chapters 10 and eleven whereas bankruptcy 12 concludes the ebook with examples of ways ENSO impacts marine and chicken life.

  • Quick reference advisor and step-by-step advent to El Niño/Southern Oscillation dynamics
  • Keep knowledgeable and recent on El Niño/Southern Oscillation study and the way El Niño and the Southern Oscillation could be predicted
  • Understand how El Niño can have an effect on marine and fowl life

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Additional info for An introduction to the dynamics of El Niño and the southern oscillation

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Meteorol. , 118, 877–926. Wright, P. , 1977: The Southern Oscillation – Patterns and mechanisms of the teleconnections and the persistence. Hawaii Institute of Geophysics Report, HIG-77–13. , 1975: El Niño – The dynamic response of the equatorial Pacific Ocean to atmospheric forcing. J. Phys. , 5, 572–584. , and J. M. Wallace, 1994: The signature of ENSO in global temperature and precipitation fields derived from the microwave sounding unit. J. Climate, 7, 1719–1736. , 1993: Large-scale variability of atmospheric deep convection in relation to sea surface temperature in the tropics.

Chapter 5 shows how the wind-forced equatorial ocean low-frequency variability can be interpreted as a sum of wind-forced equatorial waves. The last part of Chapter 5 uses the concepts developed in Chapters 3–5 to explain how El Niño is generated remotely at the South American coast by equatorial winds about 10 000 km away. 2. The Linear Stratified Ocean Model Consider an ocean model with a right-handed system of axes with the x-axis eastward, the y-axis northward and the z-axis vertically upward.

H. Carpenter, 1982: Variations in sea surface temperature and surface wind fields associated with the Southern Oscillation/El Niño. Mon. , 110, 354–384. Slutz, R. , S. D. Woodruff, R. L. Jenne, and P. M. Steurer, 1985: A comprehensive ocean-atmosphere data set. Bull. Am. , 68, 1239–1250. Troup, A. , 1965: The Southern Oscillation. Q. J. R. Meteorol. , 91, 490–506. Walker, G. , 1924: Correlation in seasonal variations in weather, IX. A further study of world-weather. Mem. Indian Meteorol. Dep. 24, 275–332.

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An introduction to the dynamics of El Niño and the southern oscillation by Allan J. Clarke


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