Tham khảo tài liệu 'global warming part 14', kỹ thuật - công nghệ, cơ khí - chế tạo máy phục vụ nhu cầu học tập, nghiên cứu và làm việc hiệu quả | Simulating Alpine Tundra Vegetation Dynamics in Response to Global Warming in China 239 values for monthly temperature monthly percentage of potential sunshine hours and monthly total precipitation throughout China and its adjacent regions. An atmospheric CO2 concentration of 340 ppmv was used to link BIOME4 to the present-day baseline simulation. Biomes Plant functional types Tropical broad-leaved evergreen Tropical Sub-tropical broad-leaved forest broad-leaved raingreen Temperate broadleaved evergreen Mantane broad-leaved forest Temperate broad-leaved evergreen Temperate broad-leaved summergreen Temperate coniferous-leaf evergreen Sub-alpine coniferous-leaf forest Temperate summergreen conifer Boreal coniferous-leaf evergreen Montane shrub steppe Temperate xerophytic shrub Temperate grass Montane steppe Temperate grass Temperate xerophytic shrub Alpine meadow Cold graminoid or forb Cushion forb Alpine steppe Cold graminoid or forb Cold shrub Montane desert Cold shrub Cold graminoid or forb Alpine desert Cold shrub Cold graminoid or forb Temperate broad-leaved summergreen Deciduous coniferous broad-leaf forest Temperate coniferous-leaf evergreen Temperate summergreen conifer Table 7. Biomes and plant functional types on the Tibetan Plateau at present Future climate projection The climatic conditions under increasing greenhousegas concentrations and sulfate aerosols have been simulated by atmospheric general circulation models AGCMs . These models were commonly used in the construction and application of climate change scenarios for climate change impacts assessments Neilson et al. 1998 Cramer et al. 2001 . HadCM3 is a coupled atmosphere-ocean GCM developed at the Hadley Centre Cox et al. 1999 . The model was driven by computing the averages for 1931-1960 and for 2070-2099. We used the mean climate anomalies and then interpolated the anomalies to the grid in high resolution Fig. 9 . The anomalies were added to the baseline climatology to produce the climate .
