Climate effects of the Globe Land30 land cover dataset on the Beijing Climate Center climate model simulations

被引:0
作者
SHI XueLi [1 ]
NIE SuPing [1 ]
JU WeiMin [2 ]
YU Le [3 ,4 ]
机构
[1] National Climate Center
[2] International Institute for Earth System Science (ESSI), Nanjing University
[3] Ministry of Education Key Laboratory for Earth System Modeling, Center for Earth System Science, Tsinghua University
[4] Joint Center for Global Change Studies
基金
中国国家自然科学基金; 国家高技术研究发展计划(863计划);
关键词
Land cover; Climate model; Application strategy; Numerical simulation; Air temperature; Precipitation;
D O I
暂无
中图分类号
P461 [气候的形成和影响气候的因素]; P435 [数值试验];
学科分类号
0706 ; 070601 ;
摘要
Land cover is one of the most basic input elements of land surface and climate models. Currently, the direct and indirect effects of land cover data on climate and climate change are receiving increasing attentions. In this study, a high resolution(30 m) global land cover dataset(Globe Land30) produced by Chinese scientists was, for the first time, used in the Beijing Climate Center Climate System Model(BCCCSM) to assess the influences of land cover dataset on land surface and climate simulations. A two-step strategy was designed to use the Globe Land30 data in the model. First, the Globe Land30 data were merged with other satellite remote sensing and climate datasets to regenerate plant functional type(PFT) data fitted for the BCCCSM. Second, the up-scaling based on an area-weighted approach was used to aggregate the fine-resolution Globe Land30 land cover type and area percentage with the coarser model grid resolutions globally. The Globe Land30-based and the BCCCSM-based land cover data had generally consistent spatial distribution features, but there were some differences between them. The simulation results of the different land cover type dataset change experiments showed that effects of the new PFT data were larger than those of the new glaciers and water bodies(lakes and wetlands). The maximum value was attained when dataset of all land cover types were changed. The positive bias of precipitation in the mid-high latitude of the northern hemisphere and the negative bias in the Amazon, as well as the negative bias of air temperature in part of the southern hemisphere, were reduced when the Globe Land30-based data were used in the BCCCSM atmosphere model. The results suggest that the Globe Land30 data are suitable for use in the BCCCSM component models and can improve the performance of the land and atmosphere simulations.
引用
收藏
页码:1754 / 1764
页数:11
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