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dc.contributor.authorNayagam, Lorna Raja
dc.contributor.authorMaksyutov, Shamil
dc.contributor.authorJanardanan, Rajesh
dc.contributor.authorOda, Tomohiro
dc.contributor.authorTiwari, Yogesh K.
dc.contributor.authorSreenivas, Gaddamidi
dc.contributor.authorDatye, Amey
dc.contributor.authorJain, Chaithanya D.
dc.contributor.authorRatnam, Madineni Venkat
dc.contributor.authorSinha, Vinayak
dc.contributor.authorHakkim, Haseeb
dc.contributor.authorTerao, Yukio
dc.contributor.authorNaja, Manish
dc.contributor.authorAhmed, Md. Kawser
dc.contributor.authorMukai, Hitoshi
dc.contributor.authorZeng, Jiye
dc.contributor.authorKaiser, Johannes
dc.contributor.authorSomeya, Yu
dc.contributor.authorYoshida, Yukio
dc.date.accessioned2025-01-30T13:08:41Z
dc.date.available2025-01-30T13:08:41Z
dc.date.created2025-01-29T11:06:04Z
dc.date.issued2025
dc.identifier.citationRemote Sensing. 2024, 17, 450.en_US
dc.identifier.issn2072-4292
dc.identifier.urihttps://hdl.handle.net/11250/3175419
dc.description.abstractThe carbon sink over land plays a key role in the mitigation of climate change by removing carbon dioxide (CO2) from the atmosphere. Accurately assessing the land sink capacity across regions should contribute to better future climate projections and help guide the mitigation of global emissions towards the Paris Agreement. This study estimates terrestrial CO2 fluxes over India using a high-resolution global inverse model that assimilates surface observations from the global observation network and the Indian subcontinent, airborne sampling from Brazil, and data from the Greenhouse gas Observing SATellite (GOSAT) satellite. The inverse model optimizes terrestrial biosphere fluxes and ocean-atmosphere CO2 exchanges independently, and it obtains CO2 fluxes over large land and ocean regions that are comparable to a multi-model estimate from a previous model intercomparison study. The sensitivity of optimized fluxes to the weights of the GOSAT satellite data and regional surface station data in the inverse calculations is also examined. It was found that the carbon sink over the South Asian region is reduced when the weight of the GOSAT data is reduced along with a stricter data filtering. Over India, our result shows a carbon sink of 0.040 ± 0.133 PgC yr−1 using both GOSAT and global surface data, while the sink increases to 0.147 ± 0.094 PgC yr−1 by adding data from the Indian subcontinent. This demonstrates that surface observations from the Indian subcontinent provide a significant additional constraint on the flux estimates, suggesting an increased sink over the region. Thus, this study highlights the importance of Indian sub-continental measurements in estimating the terrestrial CO2 fluxes over India. Additionally, the findings suggest that obtaining robust estimates solely using the GOSAT satellite data could be challenging since the GOSAT satellite data yield significantly varies over seasons, particularly with increased rain and cloud frequency.en_US
dc.language.isoengen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleIndian Land Carbon Sink Estimated from Surface and GOSAT Observationsen_US
dc.title.alternativeIndian Land Carbon Sink Estimated from Surface and GOSAT Observationsen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holder© 2025 by the authors. Licensee MDPI, Basel, Switzerland.en_US
dc.source.volume17en_US
dc.source.journalRemote Sensingen_US
dc.source.issue3en_US
dc.identifier.doi10.3390/rs17030450
dc.identifier.cristin2350909
dc.relation.projectNILU: 124007en_US
dc.source.articlenumber450en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal