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Knox, Robert Jackson, Benjamin Poulter, Gavin McNicol, Etienne Fluet-Chouinard, Zhen Zhang, Gustaf Hugelius, Philippe Bousquet, Josep G. Richardson, Benjamin R, K. Glaser, Nyoman Suryadiputra, Reza Lubis, Truly Santika, Rory Padfield, Sofyan Kurnianto, Panut Hadisiswoyo, Teck Wyn Lim, Susan E.
Furthermore, differences in the land CO2 fluxes from SVR-NEE and GOSAT Level 4A were partially explained by accounting for the differences in the definition of land CO2 fluxes. The litter decomposition rate was 0. All rights reserved. FCH4 was positively associated with GWL or soil moisture in a quadratic form. Morin, Mats B. These data-driven estimates can provide a new opportunity to assess CO2 fluxes in Asia and evaluate and constrain terrestrial ecosystem models. The differences in the relationship between PD and GWL indicate that separate estimations are required for each type of land. It is essential to quantify the CO2 balance of the ecosystem and understand how the CO2 balance responds to environmental changes to predict the role of PSF in global carbon cycles. Monthly mean FCH4 was always positive during the 18 months, even in the driest month with mean GWL of —30 cm. Mean annual gap-filled CO2 emissions were 1. da Rocha, Scott R. Krauss, Lars Kutzbach, Annalea Lohila, Bhaskar Mitra, Timothy H. Hollinger, Hiroki Iwata, Minseok Kang, Janina Klatt, Ken W. Through the land conversion, peat carbon has become vulnerable and potentially changes to a great carbon dioxide CO2 source to the atmosphere. The negative annual NEE was equivalent to those of some tropical rain forests on mineral soil, but was more negative than g C m -2 yr -1 for an almost undrained PSF in Central Kalimantan, Indonesia Hirano et al. Canadell, Marielle Saunois, Dario Papale, Housen Chu, Trevor F. The aim of this study was to investigate temperature sensitivities of these processes and the effect of climate warming on the annual terrestrial net ecosystem CO2 exchange globally in the boreal and temperate regions. Evaluation of spatially estimated NEE with net atmosphere-land CO2 fluxes of Greenhouse Gases Observing Satellite GOSAT Level 4A product shows that monthly variations of these data were consistent in Siberia and East Asia; meanwhile, inconsistency was found in South Asia and Southeast Asia. Manzi, Antonio D. The litter bag method LB and chamber method with litter addition and removal treatments C-LART have been used to quantify the litter decomposition rate and its resultant CO2 flux. Data-driven estimation was conducted by using a machine learning algorithm: support vector regression SVR , with remote sensing data for to period. Q 10sG was negatively correlated to the mean annual temperature MAT , whereas Q 10sR was independent of MAT. Smith, Catherine M. Denial of long-term issues with agriculture on tropical peatlands will have devastating consequences Lahiru S. Desai, Eugenie Euskirchen, Thomas Friborg, Daniele Gasbarra, Ignacio Goded, Mathias Goeckede, Martin Heimann, Manuel Helbig, Takashi Hirano, David Y. Miller, Antonio O. Nobre, Plinio B. At DB, PD and GWL showed significant positive and negative relationships during the dry and wet seasons, respectively. However, filed studies based on the ecosystem-scale monitoring of CO2 flux are quite limited. In this study, we developed such a standardized database using 54 sites from various databases by applying consistent postprocessing for data-driven estimation of gross primary productivity GPP and net ecosystem CO2 exchange NEE. Saitoh, Kentaro Takagi, Andrej Varlagin, M. Daily RE was significantly greater in the dry period mainly because of lower groundwater level GWL. Owing to the huge soil carbon stock and high groundwater level GWL , tropical peatlands potentially represent a significant source of methane CH4 to the atmosphere. Lower GWL enhances peat aeration and potentially increases oxidative peat decomposition, which results in higher soil CO2 efflux. Wijedasa, Jyrki Jauhiainen, Mari Kononen, Maija Lampela, Harri Vasander, Marie-Claire Leblanc, Stephanie Evers, Thomas E. Annual soil respiration in the control plot was gC m -2 yr -1 , which was approximately twice as high as the mean of temperate evergreen forests in the world. Annual FCH4 from March through February was 7.