Changes in the East Asian monsoon and the related river discharge under global warming conditions are investigated using 2 time-slice simulations of the IS92a scenario with a T106 atmospheric general circulation model (ECHAM4) for 1971 to 1980 and 2041 to 2050. Daily runoff and drainage calculated by the land-surface scheme are used as input to a hydrological model to diagnose changes in the Yangtze River and Zhujiang River discharges. In the future climate, the simulated annual cycle of precipitation over the southeastern coastal area of China is systematically shifted about 1 mo ahead compared with the present-day climate, and the rainy season starts 1 mo earlier for the Yangtze River Valley and North China. In line with the surface-warming distribution change, the East Asian summer monsoon (EAM) flow strengthens. This causes increased precipitation in North China. In winter, the subtropical part of the EAM flow strengthens and leads to a large increase in rainfall over the EAM region. The discharges of the Zhujiang and Yangtze rivers in the future climate decrease in the late summer and autumn, to which both increased evaporation and an early retreat of the monsoon rainfall contribute. In the early and mid-summer, the Yangtze River discharge increases, mainly due to the large increase in precipitation in the preceding months, which has been stored in the catchment.
KEY WORDS: Global warning · East Asian monsoon · Time-slice experiment · River discharge
Resale or republication not permitted without written consent of the publisherClim Res 24: [47][48][49][50][51][52][53][54][55][56][57] 2003 rently, 3 techniques are available to compensate for this problem:• dynamical downscaling via time-slice simulations with global high-resolution models; • dynamical downscaling using high-resolution regional models; • statistical downscaling. The advantages and limitations of these methods have been discussed in Cubasch et al. (1995), Lal et al. (1997), Rummukainen (1997) and IPCC (2001). In this study, we employ the time-slice simulation method (Bengtsson et al. 1995, Cubasch et al. 1996, Wilby & Wigley 1997, Déqué et al. 1998, Jones et al. 1998, May & Roeckner 2001, which uses a global atmosphere model with a horizontal resolution of 1.1°× 1.1°. Details of the model and the design of the time-slice experiments can be found in Section 2.The present-day interannual and interdecadal variability of the EAM have been extensively studied by many investigators (Ding 1991, Yasunari 1991, Lau 1992, Nitta & Hu 1996, Ji et al. 1997, Chen & Graf 1998, Bueh & Ji 1999a, Lu & Chan 1999, Samel et al. 1999, Kripalani & Kulkarni 2001. However, the EAM change under global warming conditions has hardly been investigated. Wang & Ye (1993) and Nitta & Hu (1996) found from observational data a pronounced warming trend in North China.Using observational data, Hulme et al. (1994) concluded that coinciding with warming in the last century, East Asian precipitation increased with a trend of 0.54% decade -1 , which is larger than...