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The El Niño-Southern oscillation phenomenon /
Many climatic extremes around the globe, such as severe droughts and floods, can be attributed to the periodic warming of the equatorial Pacific sea surface, termed the El Niño or Southern Oscillation (ENSO). Advances in our understanding of ENSO, in which Edward Sarachik and Mark Cane have been ke...
| Clasificación: | Libro Electrónico |
|---|---|
| Autor principal: | |
| Otros Autores: | |
| Formato: | Electrónico eBook |
| Idioma: | Inglés |
| Publicado: |
Cambridge ; New York :
Cambridge University Press,
2010.
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| Temas: | |
| Acceso en línea: | Texto completo |
MARC
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| 100 | 1 | |a Sarachik, Edward S. | |
| 245 | 1 | 4 | |a The El Niño-Southern oscillation phenomenon / |c Edward S. Sarachik, Mark A. Cane. |
| 260 | |a Cambridge ; |a New York : |b Cambridge University Press, |c 2010. | ||
| 300 | |a 1 online resource (xiii, 369 pages) : |b illustrations, maps | ||
| 336 | |a text |b txt |2 rdacontent | ||
| 337 | |a computer |b c |2 rdamedia | ||
| 338 | |a online resource |b cr |2 rdacarrier | ||
| 504 | |a Includes bibliographical references (pages 351-363) and index. | ||
| 588 | 0 | |a Print version record. | |
| 505 | 0 | 0 | |g G1. |t Preview -- |g 2. |t observational basis -- |g 3. |t equations of motion and some simplifications -- |g 4. |t Boundary layers on both sides of the tropical ocean surface -- |g 5. |t Atmospheric processes -- |g 6. |t Ocean processes -- |g 7. |t ENSO mechanisms -- |g 8. |t ENSO prediction and short-term climate prediction -- |g 9. |t ENSO, past and future: ENSO by proxy and ENSO in the tea leaves -- |g 10. |t Using ENSO information -- |g 11. |t Postview -- |g Appendix 1. |t Some useful numbers -- |g Appendix 2. |t parabolic-cylinder functions -- |g Appendix 3. |t Modal and non-modal growth. |
| 520 | |a Many climatic extremes around the globe, such as severe droughts and floods, can be attributed to the periodic warming of the equatorial Pacific sea surface, termed the El Niño or Southern Oscillation (ENSO). Advances in our understanding of ENSO, in which Edward Sarachik and Mark Cane have been key participants, have led to marked improvements in our ability to predict its development months or seasons, allowing adaptation to global impacts. The book introduces basic concepts and builds to more detailed theoretical treatments. Chapters on the structure and dynamics of the tropical ocean and atmosphere place ENSO in a broader observational and theoretical context. Chapters on ENSO prediction, past and future, and impacts introduce broader implications of the phenomenon. This book provides an introduction to all aspects of this most important mode of global climate variability, for research workers and students of all levels in climate science, oceanography and related fields. | ||
| 546 | |a English. | ||
| 590 | |a eBooks on EBSCOhost |b EBSCO eBook Subscription Academic Collection - Worldwide | ||
| 650 | 0 | |a Southern oscillation. | |
| 651 | 0 | |a El Niño Current. | |
| 650 | 6 | |a Oscillation australe. | |
| 651 | 6 | |a El Niño, Courant. | |
| 650 | 7 | |a SCIENCE |x Earth Sciences |x Oceanography. |2 bisacsh | |
| 650 | 7 | |a NATURE |x Ecosystems & Habitats |x Oceans & Seas. |2 bisacsh | |
| 650 | 7 | |a Southern oscillation |2 fast | |
| 651 | 7 | |a Pacific Ocean |z El Niño Current |2 fast | |
| 650 | 7 | |a Allgemeine atmosphärische Zirkulation |2 gnd | |
| 650 | 7 | |a El-Niño-Phänomen |2 gnd | |
| 700 | 1 | |a Cane, Mark A. | |
| 776 | 0 | 8 | |i Print version: |a Sarachik, Edward S. |t Niño-Southern oscillation phenomenon. |d Cambridge ; New York : Cambridge University Press, 2010 |z 9780521847865 |w (DLC) 2010293528 |w (OCoLC)428024450 |
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