Intercomparison of global terrestrial carbon fluxes estimated by MODIS and Earth system models

初级生产 生物群落 耦合模型比对项目 环境科学 地球系统科学 卫星 碳循环 气候学 大气科学 碳通量 气候模式 气候变化 生态系统 地质学 生态学 海洋学 航空航天工程 工程类 生物
作者
Qiwen Hu,Tingting Li,Xi Deng,Tongwen Wu,Panmao Zhai,Danqing Huang,Xingwang Fan,Yakun Zhu,Yongcheng Lin,Xiucheng Xiao,Xianyan Chen,Xiaosong Zhao,Lili Wang,Zhangcai Qin
出处
期刊:Science of The Total Environment [Elsevier BV]
卷期号:810: 152231-152231 被引量:48
标识
DOI:10.1016/j.scitotenv.2021.152231
摘要

Earth system models (ESMs) have been widely used to simulate global terrestrial carbon fluxes, including gross primary production (GPP) and net primary production (NPP). Assessment of such GPP and NPP products can be valuable for understanding the efficacy of certain ESMs in simulating the global carbon cycle and future climate impacts. In this work, we studied the model performance of 22 ESMs participating in the fifth and sixth phases of the Coupled Model Intercomparison Project (CMIP5 and CMIP6) by comparing historical GPP and NPP simulations with satellite data from MODIS and further evaluating potential model improvement from CMIP5 to CMIP6. In CMIP6, the average global total GPP and NPP estimated by the 22 ESMs are 16% and 13% higher than MODIS data, respectively. The multi-model ensembles (MME) of the 22 ESMs can fairly reproduce the spatial distribution, zonal distribution and seasonal variations of both GPP and NPP from MODIS. They perform much better in simulating GPP and NPP for grasslands, wetlands, croplands and other biomes than forests. However, there are noticeable differences among individual ESM simulations in terms of overall fluxes, temporal and spatial flux distributions, and fluxes by biome and region. The MME consistently outperforms all individual models in nearly every respect. Even though several ESMs have been improved in CMIP6 relative to CMIP5, there is still much work to be done to improve individual ESM and overall CMIP performance. Future work needs to focus on more comprehensive model mechanisms and parametrizations, higher resolution and more reasonable coupling of land surface schemes and atmospheric/oceanic schemes.

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