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East Asian monsoon /
The East Asian summer monsoon has complex space and time structures that are distinct from the South Asian summer monsoon. It covers both subtropics and midlatitudes and its rainfall tends to be concentrated in rain belts that stretch for many thousands of kilometers and affect China, Japan, Korea,...
| Clasificación: | Libro Electrónico |
|---|---|
| Otros Autores: | |
| Formato: | Electrónico eBook |
| Idioma: | Inglés |
| Publicado: |
Singapore :
World Scientific,
Ã2004.
|
| Colección: | World Scientific series on meteorology of East Asia ;
v. 2. |
| Temas: | |
| Acceso en línea: | Texto completo |
MARC
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| 245 | 0 | 0 | |a East Asian monsoon / |c edited by C.-P. Chang. |
| 260 | |a Singapore : |b World Scientific, |c Ã2004. | ||
| 300 | |a 1 online resource (viii, 564 pages) : |b illustrations (some color), maps (some color) | ||
| 336 | |a text |b txt |2 rdacontent | ||
| 337 | |a computer |b c |2 rdamedia | ||
| 338 | |a online resource |b cr |2 rdacarrier | ||
| 347 | |a data file |2 rda | ||
| 490 | 1 | |a World Scientific series on meteorology of East Asia ; |v . 2 | |
| 504 | |a Includes bibliographical references. | ||
| 588 | 0 | |a Print version record. | |
| 505 | 0 | |a PREFACE; CONTENTS; Part I East Asian Summer and Winter Monsoon; 1. SEASONAL MARCH OF THE EAST-ASIAN SUMMER MONSOON; 2. THE EAST ASIA WINTER MONSOON; 3. MARITIME CONTINENT MONSOON: ANNUAL CYCLE AND BOREAL WINTER VARIABILITY; Part II Interannual Variations; 4. INTERANNUAL VARIABILITY, GLOBAL TELECONNECTION, AND POTENTIAL PREDICTABILITY ASSOCIATED WITH THE ASIAN SUMMER MONSOON; 5. EAST ASIAN MONSOON-ENSO INTERACTIONS; 6. CLIMATE VARIATIONS OF THE SUMMER MONSOON OVER CHINA; Part III General Circulation Modeling. | |
| 520 | |a The East Asian summer monsoon has complex space and time structures that are distinct from the South Asian summer monsoon. It covers both subtropics and midlatitudes and its rainfall tends to be concentrated in rain belts that stretch for many thousands of kilometers and affect China, Japan, Korea, and the surrounding areas. The circulation of the East Asian winter monsoon encompasses a large meridional domain with cold air outbreaks emanating from the Siberian high and penetrates deeply into the equatorial Maritime Continent region, where the center of maximum rainfall has long been recognize. | ||
| 590 | |a ProQuest Ebook Central |b Ebook Central Academic Complete | ||
| 650 | 0 | |a Monsoons |z East Asia. | |
| 650 | 0 | |a Winds |z East Asia. | |
| 650 | 7 | |a Monsoons |2 fast | |
| 650 | 7 | |a Winds |2 fast | |
| 651 | 7 | |a East Asia |2 fast | |
| 655 | 4 | |a Computer network resources. | |
| 700 | 1 | |a Chang, C.-P. |q (Chih-Pei) |1 https://id.oclc.org/worldcat/entity/E39PCjGjbCfthfyBVvj3X6TgVd | |
| 776 | 1 | |z 9789812387691 | |
| 830 | 0 | |a World Scientific series on meteorology of East Asia ; |v v. 2. | |
| 856 | 4 | 0 | |u https://ebookcentral.uam.elogim.com/lib/uam-ebooks/detail.action?docID=296111 |z Texto completo |
| 938 | |a EBL - Ebook Library |b EBLB |n EBL296111 | ||
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