TROPOMI observations allow for robust exploration of the relationship between solar-induced chlorophyll fluorescence and terrestrial gross primary production

被引:69
作者
Li, Xing [1 ,2 ]
Xiao, Jingfeng [1 ]
机构
[1] Univ New Hampshire, Inst Study Earth Oceans & Space, Earth Syst Res Ctr, Durham, NH 03824 USA
[2] Seoul Natl Univ, Res Inst Agr & Life Sci, Seoul, South Korea
基金
美国国家科学基金会; 美国国家航空航天局;
关键词
Carbon cycle; Sun-induced fluorescence; Gross primary productivity; Eddy covariance; Photosynthesis; Photosynthetic pathway; Water stress; Spatial and temporal integration; Climate change; AmeriFlux; PHOTOSYNTHESIS; ASSIMILATION; RETRIEVAL; SPACE;
D O I
10.1016/j.rse.2021.112748
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Solar-induced chlorophyll fluorescence (SIF) observed by satellites has advanced the monitoring of terrestrial photosynthesis regionally and globally. The relationship between SIF and gross primary production (GPP) at leaf, canopy, and ecosystem scales has received tremendous attention in recent years. It remains controversial whether the SIF-GPP relationship at the ecosystem scale is universal or dependent upon vegetation type. New SIF observations from the TROPOspheric Monitoring Instrument (TROPOMI) with unprecedented high spatial and temporal resolution provide a new opportunity to elucidate the SIF-GPP relationship. Here, we examine the SIF-GPP relationship for seven major vegetation types across the U.S. with TROPOMI SIF and in-situ GPP data for 83 eddy covariance flux sites. We find that TROPOMI SIF shows a strong and consistent relationship with tower based GPP at both satellite footprint and grid-cell levels. The slope of the SIF-GPP relationship is similar among all the vegetation types except croplands, demonstrating a nearly universal (converging to similar to 13.5 g C m(-2) d(-1)/W m(-2) mu m(-1) sr(-1)) rather than vegetation type-specific SIF-GPP relationship. This confirms that TROPOMI SIF can be used as a proxy for GPP across a wide variety of vegetation types, and can also be used to quantify GPP by avoiding uncertainty associated with land cover maps. The C-4 crops have a much higher slope than the C-3 crops, and therefore croplands tend to have a higher slope than C-3-dominated vegetation types (e.g., forests, shrublands, savannas). We also find that the TROPOMI SIF is well correlated with GPP under normal or wetter conditions, while their relationship becomes weaker under water stress. Our TROPOMI-based study could improve our understanding of the SIF-GPP relationship at the ecosystem scale and advance the mapping of GPP globally with SIF observations from space.
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页数:13
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