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India is drying out its terrestrial carbon: An inference by multi-model estimation of primary productivities
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  • Manoj Hari,
  • Bhishma Tyagi,
  • Michael O'Sullivan,
  • Stephen Sitch
Manoj Hari
Department of Earth and Atmospheric Sciences, National Institute of Technology Rourkela, Rourkela, India, Department of Earth and Atmospheric Sciences, Department of Earth and Atmospheric Sciences

Corresponding Author:manoj_h@nitrkl.ac.in

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Bhishma Tyagi
Department of Earth and Atmospheric Sciences, National Institute of Technology Rourkela, Rourkela, India, Department of Earth and Atmospheric Sciences, Department of Earth and Atmospheric Sciences
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Michael O'Sullivan
College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, United Kingdom, College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, United Kingdom, College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, United Kingdom
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Stephen Sitch
College of Life and Environmental Sciences, University of Exeter, Exeter, United Kingdom, College of Life and Environmental Sciences, University of Exeter, Exeter, United Kingdom, College of Life and Environmental Sciences, University of Exeter, Exeter, United Kingdom
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Abstract

Terrestrial primary productivity plays a pivotal role as a forcing factor of atmospheric CO2 and drives biospheric carbon dynamics. India is one of the largest GHGs emitters, yet less is understood in carbon cycling in terrestrial ecosystems. Here we explored the trend and magnitude of gross and net productivities of India for the last two decades (2000 – 2019) by integrating satellite observation from MODIS, remote sensing-based CASA model and twenty DGVMs from the TRENDY ensemble. Preliminary results exhibited a unimodal response across the data products with an overall positive trend and a declining decadal trend for 2010 – 2019. Alongside, the SPEI drought severity index across various ecological zones indicated India was more positively sensitive to wet span than the dry. We found that the ecosystems were drastically shifting their nature to C source with a positive trend in the productivities and were mediated by the changing climate. The analysis also revealed the increasing decadal amplitude of GPP by 0.0884 Pg C/Year, NBP by 0.0096 Pg C/Year, NEP by 0.0195 Pg C/Year, NPP by 0.0448 Pg C/Year and NEE by 0.0161 Pg C/Year. CASA underestimated the magnitudes but with the temporal synchronisation of the ensemble. Seasonal variability across the agro-ecological zones was more sensitive and was an offset for the declining productivities in the primaeval forests of India. The monsoon season contributed to the interannual variability of India. Higher uncertainty in productivities was observed in the high greening areas, whereas it contradicted NBP by reflecting a stable trend. Our results underscore the nature of C variability in the terrestrial ecosystems of India; and, they indicate that C release has reacted stronger than the C uptake, which was substantially inferred from NEE across the ecological zones.