数据简介: | 数值模式:最新通用地球系统模式CESM1;试验设计:将青藏高原地形(60-110E,20-40N)降低为当前的20%,30%,…,95%,100%,对应试验名称0.2TP,0.3TP,…,0.95TP,TP;边界条件:1870年,CO2浓度280ppm。积分时间:12年,试验结果对外共享第10-12年的平均场 T: Temperature; U: Zonal wind; V: Meridional wind; Z3: Geopotential Height (above sea level); OMEGA: Vertical velocity (pressure); PSL: Sea level pressure; PS: Surface pressure; TS: Surface temperature (radiative); PRECT:(PRECC: Convective precipitation rate (liq + ice) + PRECL: Convective precipitation rate (liq + ice)); Q: Specific humidity。参考文献:1)Li Xinzhou, Pan Zaitao and Liu Xiaodong, 2016: Numerical simulation of influence of Tibetan Plateau uplift on winter dust cycle in Asian arid regions, Environmental Earth Sciences,75(7), 1-12, doi: 10.1007/s12665-016-5403-1。2)李新周,2016:青藏高原阶段性隆升对亚洲干旱半干旱区冬季粉尘循环的影响. 地球环境学报,7(1):1-12. |