The Asian summer monsoon : characteristics, variability, teleconnections and projection /

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 signif...

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Detalles Bibliográficos
Clasificación:Libro Electrónico
Autores principales: Liu, Yunyun (Autor), Liang, Ping (Autor), Sun, Ying (Autor)
Formato: Electrónico eBook
Idioma:Inglés
Publicado: Amsterdam, Netherlands : Elsevier, [2019]
Temas:
Monsoons > Asia.
Moussons > Asie.
Monsoons
Asia
Acceso en línea:Texto completo
Tabla de Contenidos:
  • <P><b>Part I: Holistic characteristics of the Asian summer monsoon (ASM) system</b> 1. Basic features of the ASM system</p> <p>2. Seasonal transition of the moisture transport in the Asian monsoon region</p> <b> <p>Part II: Variability and predictability of the EASM at subseasonal timescale </b>3. Characteristics of the intraseasonal oscillation of East Asian Meiyu</p> <p>4. Subseasonal prediction of the EASM </p> <b> <p>Part III: Interannual variability of the EASM system and its possible mechanism </b>5. Characteristics of the western Pacific subtropical high (WPSH) and summer rainfall anomalies</p> <p>6. Tropospheric biennial oscillation (TBO) of the WPSH and its relationships with the tropical sea surface temperature and atmospheric circulation anomalies</p> <p>7. TBO of monsoon rainfall and its association with El Ni&#xFFFD;no
  • southern oscillation</p> <p><b>Part IV: Teleconnections in the Asian monsoon region in the onset and culmination phases</b> 8. Northern teleconnection between the Indian summer monsoon (ISM) and rainfall anomalies in northern China</p> <p>9. Southern teleconnection between the ISM onset and Meiyu in China</p> <p>10. Simulations and projections of the WPSH</p> <p>11. Projection of future changes in the ASM under global warming conditions</p> <p>12. Responses of the ISM and the EASM to different land-sea temperature increases under a warming scenario</p>

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