{"title":"基于TROPOMI太阳诱导叶绿素荧光的冠层电导全球制图在区分光照和遮荫叶片的贡献后","authors":"Xiaoping Wang , Wei He","doi":"10.1016/j.gloplacha.2025.105089","DOIUrl":null,"url":null,"abstract":"<div><div>Global mapping of terrestrial vegetation canopy conductance (G<sub>c</sub>) is of great importance for understanding the behavior of terrestrial carbon and water cycles and their interaction mechanisms. Solar-induced chlorophyll fluorescence (SIF) shows great promise in deriving global G<sub>c</sub>, yet is hindered by limited capacities in characterizing the SIF-G<sub>c</sub> relationship, particularly in high-density vegetation areas, where differentiating the contribution of sunlit and shaded leaf SIF and G<sub>c</sub> to canopy matters. Here, we developed a new SIF-G<sub>c</sub> model by differentiating the contribution of sunlit and shaded leaves using a coupled “Two-leaf” biosphere model (BEPS-LRC) and the Ball-Berry model, and derived global G<sub>c</sub> distribution from 2018 through 2020 with TROPOMI satellite SIF data and eddy covariance flux data from 40 stations. We found that sunlit leaves and shaded leaves have a similar seasonal variation in G<sub>c</sub>, but the variation is greater in the former than in the latter, and the differentiation of sunlit and shaded leaves makes SIF better track the seasonal variation of G<sub>c</sub>. Moreover, the new model reduces the dependence of canopy SIF-G<sub>c</sub> relationship on atmospheric vapor pressure deficit, with the R<sup>2</sup> of eight biomes greater than 0.5 and 0.4 in sunlit leaves and shaded leaves respectively. In addition, the model improves the accuracy of G<sub>c</sub> estimation, with the minimum R<sup>2</sup> of 0.52 (SAV), the maximum R<sup>2</sup> of 0.79 (MF and OH), and the slope ranged from 1.04 (CRO) to 1.21 (OH) with the RMSE from 1.05 (CRO) to 1.33 (OH). The global G<sub>c</sub> exhibits substantial spatial and seasonal variations, ranging from 0.05 to 1.48, with high values mainly distributed in the African plateau and Australia. This study provides a novel method for mapping global vegetation G<sub>c</sub>, which is crucial for understanding the eco-hydrological processes and predicting the fate of terrestrial carbon and water cycles in a changing climate.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"255 ","pages":"Article 105089"},"PeriodicalIF":4.0000,"publicationDate":"2025-09-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Global mapping of canopy conductance from TROPOMI solar-induced chlorophyll fluorescence after differentiating contributions of sunlit and shaded leaves\",\"authors\":\"Xiaoping Wang , Wei He\",\"doi\":\"10.1016/j.gloplacha.2025.105089\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Global mapping of terrestrial vegetation canopy conductance (G<sub>c</sub>) is of great importance for understanding the behavior of terrestrial carbon and water cycles and their interaction mechanisms. Solar-induced chlorophyll fluorescence (SIF) shows great promise in deriving global G<sub>c</sub>, yet is hindered by limited capacities in characterizing the SIF-G<sub>c</sub> relationship, particularly in high-density vegetation areas, where differentiating the contribution of sunlit and shaded leaf SIF and G<sub>c</sub> to canopy matters. Here, we developed a new SIF-G<sub>c</sub> model by differentiating the contribution of sunlit and shaded leaves using a coupled “Two-leaf” biosphere model (BEPS-LRC) and the Ball-Berry model, and derived global G<sub>c</sub> distribution from 2018 through 2020 with TROPOMI satellite SIF data and eddy covariance flux data from 40 stations. We found that sunlit leaves and shaded leaves have a similar seasonal variation in G<sub>c</sub>, but the variation is greater in the former than in the latter, and the differentiation of sunlit and shaded leaves makes SIF better track the seasonal variation of G<sub>c</sub>. Moreover, the new model reduces the dependence of canopy SIF-G<sub>c</sub> relationship on atmospheric vapor pressure deficit, with the R<sup>2</sup> of eight biomes greater than 0.5 and 0.4 in sunlit leaves and shaded leaves respectively. In addition, the model improves the accuracy of G<sub>c</sub> estimation, with the minimum R<sup>2</sup> of 0.52 (SAV), the maximum R<sup>2</sup> of 0.79 (MF and OH), and the slope ranged from 1.04 (CRO) to 1.21 (OH) with the RMSE from 1.05 (CRO) to 1.33 (OH). The global G<sub>c</sub> exhibits substantial spatial and seasonal variations, ranging from 0.05 to 1.48, with high values mainly distributed in the African plateau and Australia. This study provides a novel method for mapping global vegetation G<sub>c</sub>, which is crucial for understanding the eco-hydrological processes and predicting the fate of terrestrial carbon and water cycles in a changing climate.</div></div>\",\"PeriodicalId\":55089,\"journal\":{\"name\":\"Global and Planetary Change\",\"volume\":\"255 \",\"pages\":\"Article 105089\"},\"PeriodicalIF\":4.0000,\"publicationDate\":\"2025-09-16\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Global and Planetary Change\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0921818125003984\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOGRAPHY, PHYSICAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Global and Planetary Change","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0921818125003984","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
Global mapping of canopy conductance from TROPOMI solar-induced chlorophyll fluorescence after differentiating contributions of sunlit and shaded leaves
Global mapping of terrestrial vegetation canopy conductance (Gc) is of great importance for understanding the behavior of terrestrial carbon and water cycles and their interaction mechanisms. Solar-induced chlorophyll fluorescence (SIF) shows great promise in deriving global Gc, yet is hindered by limited capacities in characterizing the SIF-Gc relationship, particularly in high-density vegetation areas, where differentiating the contribution of sunlit and shaded leaf SIF and Gc to canopy matters. Here, we developed a new SIF-Gc model by differentiating the contribution of sunlit and shaded leaves using a coupled “Two-leaf” biosphere model (BEPS-LRC) and the Ball-Berry model, and derived global Gc distribution from 2018 through 2020 with TROPOMI satellite SIF data and eddy covariance flux data from 40 stations. We found that sunlit leaves and shaded leaves have a similar seasonal variation in Gc, but the variation is greater in the former than in the latter, and the differentiation of sunlit and shaded leaves makes SIF better track the seasonal variation of Gc. Moreover, the new model reduces the dependence of canopy SIF-Gc relationship on atmospheric vapor pressure deficit, with the R2 of eight biomes greater than 0.5 and 0.4 in sunlit leaves and shaded leaves respectively. In addition, the model improves the accuracy of Gc estimation, with the minimum R2 of 0.52 (SAV), the maximum R2 of 0.79 (MF and OH), and the slope ranged from 1.04 (CRO) to 1.21 (OH) with the RMSE from 1.05 (CRO) to 1.33 (OH). The global Gc exhibits substantial spatial and seasonal variations, ranging from 0.05 to 1.48, with high values mainly distributed in the African plateau and Australia. This study provides a novel method for mapping global vegetation Gc, which is crucial for understanding the eco-hydrological processes and predicting the fate of terrestrial carbon and water cycles in a changing climate.
期刊介绍:
The objective of the journal Global and Planetary Change is to provide a multi-disciplinary overview of the processes taking place in the Earth System and involved in planetary change over time. The journal focuses on records of the past and current state of the earth system, and future scenarios , and their link to global environmental change. Regional or process-oriented studies are welcome if they discuss global implications. Topics include, but are not limited to, changes in the dynamics and composition of the atmosphere, oceans and cryosphere, as well as climate change, sea level variation, observations/modelling of Earth processes from deep to (near-)surface and their coupling, global ecology, biogeography and the resilience/thresholds in ecosystems.
Key criteria for the consideration of manuscripts are (a) the relevance for the global scientific community and/or (b) the wider implications for global scale problems, preferably combined with (c) having a significance beyond a single discipline. A clear focus on key processes associated with planetary scale change is strongly encouraged.
Manuscripts can be submitted as either research contributions or as a review article. Every effort should be made towards the presentation of research outcomes in an understandable way for a broad readership.