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利用 MODIS 和地球系统模型估算的全球陆地碳通量的比较。

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

机构信息

School of Atmospheric Sciences, Sun Yat-sen University, Key Laboratory of Tropical Atmosphere-Ocean System, Ministry of Education, Zhuhai 519000, China.

LAPC, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519000, China.

出版信息

Sci Total Environ. 2022 Mar 1;810:152231. doi: 10.1016/j.scitotenv.2021.152231. Epub 2021 Dec 8.

DOI:10.1016/j.scitotenv.2021.152231
PMID:34896141
Abstract

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.

摘要

地球系统模型(ESMs)已被广泛用于模拟全球陆地碳通量,包括总初级生产力(GPP)和净初级生产力(NPP)。评估这些 GPP 和 NPP 产品对于理解某些 ESM 在模拟全球碳循环和未来气候影响方面的有效性非常有价值。在这项工作中,我们通过将 22 个参与耦合模型比较计划(CMIP5 和 CMIP6)第五和第六阶段的 ESM 模拟的历史 GPP 和 NPP 与 MODIS 卫星数据进行比较,研究了这些模型的性能,并进一步评估了从 CMIP5 到 CMIP6 的潜在模型改进。在 CMIP6 中,22 个 ESM 估计的全球总 GPP 和 NPP 分别比 MODIS 数据高 16%和 13%。22 个 ESM 的多模型集合(MME)可以相当好地再现 MODIS 的 GPP 和 NPP 的空间分布、纬向分布和季节变化。它们在模拟草原、湿地、农田和其他生物群落的 GPP 和 NPP 方面表现优于森林。然而,在整体通量、时间和空间通量分布以及生物群落和区域通量方面,各个 ESM 模拟之间存在明显差异。MME 在几乎所有方面都优于所有单个模型。尽管与 CMIP5 相比,几个 ESM 在 CMIP6 中得到了改进,但仍有许多工作要做,以提高单个 ESM 和整体 CMIP 的性能。未来的工作需要侧重于更全面的模型机制和参数化、更高的分辨率和更合理的陆地表面方案和大气/海洋方案的耦合。

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