Autor: Liu, YunyunLiang, PingSun, Ying
Wydawca: Elsevier
Dostępność: 3-6 tygodni
Cena: 668,85 zł
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ISBN13: |
9780128158814 |
Autor: |
Liu, YunyunLiang, PingSun, Ying |
Oprawa: |
Paperback |
Rok Wydania: |
2019-07-16 |
Tematy: |
PHVJ |
The Asian Summer Monsoon: Characteristics, Variability, Teleconnections and Projection focuses on the connections between the Indian Summer and East Asian Summer Monsoons, also including the South China Sea Summer Monsoon. While these systems have profound differences, their interactions have significant impacts on the climatic regimes in the region and throughout the world. In summer, the ASM engine pumps moisture transported across thousands of miles from the Indian and Pacific Oceans to the monsoon regions, producing heavy rains over south and east Asia and its adjacent marginal seas. This book reviews the different subsystems and their impact, providing guidance to enhance prediction models.
Part I: Holistic characteristics of the Asian summer monsoon (ASM) system 1. Basic features of the ASM system
2. Seasonal transition of the moisture transport in the Asian monsoon region
Part II: Variability and predictability of the EASM at subseasonal timescale 3. Characteristics of the intraseasonal oscillation of East Asian Meiyu
4. Subseasonal prediction of the EASM
Part III: Interannual variability of the EASM system and its possible mechanism 5. Characteristics of the western Pacific subtropical high (WPSH) and summer rainfall anomalies
6. Tropospheric biennial oscillation (TBO) of the WPSH and its relationships with the tropical sea surface temperature and atmospheric circulation anomalies
7. TBO of monsoon rainfall and its association with El Niño - southern oscillation
Part IV: Teleconnections in the Asian monsoon region in the onset and culmination phases 8. Northern teleconnection between the Indian summer monsoon (ISM) and rainfall anomalies in northern China
9. Southern teleconnection between the ISM onset and Meiyu in China
10. Simulations and projections of the WPSH
11. Projection of future changes in the ASM under global warming conditions
12. Responses of the ISM and the EASM to different land-sea temperature increases under a warming scenario
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