Journal
GLOBAL BIOGEOCHEMICAL CYCLES
Volume 37, Issue 3, Pages -Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2022GB007462
Keywords
remote sensing; land surface phenology; vegetation productivity; carbon cycle; climate change; GPP
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Vegetation green leaf phenology has a direct impact on the gross primary productivity (GPP) of terrestrial ecosystems. Satellite observations of land surface phenology (LSP) provide a valuable tool for monitoring the timing of vegetation green leaf development. However, discrepancies between satellite-derived LSP proxies and in situ measurements of GPP make it challenging to quantify the effects of climate-induced changes in green leaf phenology on annual GPP.
Vegetation green leaf phenology directly impacts gross primary productivity (GPP) of terrestrial ecosystems. Satellite observations of land surface phenology (LSP) provide an important means to monitor the key timing of vegetation green leaf development. However, differences between satellite-derived LSP proxies and in situ measurements of GPP make it difficult to quantify the impact of climate-induced changes in green leaf phenology on annual GPP. Here, we used 1,110 site-years of GPP measurements from eddy-covariance towers in association with time series of satellite LSP observations from 2000 to 2014 to show that while satellite LSP explains a large proportion of variation in annual GPP, changes in green-leaf-based growing season length (GSL, leaf development period from spring to autumn) had less impact on annual GPP by similar to 30% than GSL changes in GPP-based photosynthetic duration. Further, maximum leaf greenness explained substantially more variance in annual GPP than green leaf GSL, highlighting the role of future vegetation greening trends on large-scale carbon budgets. Site-level variability contributes a substantial proportion of annual GPP variance in the model based on LSP metrics, suggesting the importance of local environmental factors altering regional GPP. We conclude that satellite LSP-based inferences regarding large-scale dynamics in GPP need to consider changes in both green leaf GSL and maximum greenness.
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