2018
DOI: 10.1007/s13143-017-0049-9
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Effect of Data Assimilation Parameters on The Optimized Surface CO2 Flux in Asia

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Cited by 10 publications
(14 citation statements)
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“…CT2013B, developed by the Earth System Research Laboratory (ESRL) at the National Oceanic and Atmospheric Administration (NOAA), was used for this study. CT2013B estimates the surface CO 2 flux using inverse modeling and has been widely used to calculate surface CO 2 fluxes in North America, Europe, and Asia (Peters et al, 2004(Peters et al, , 2005(Peters et al, , 2007(Peters et al, , 2010Kim et al, 2012Kim et al, , 2014aKim et al, , 2014bKim et al, , 2016Kim et al, , 2017Kim et al, , 2018aCheng et al, 2013).…”
Section: Carbontracker and Data Assimilation Methodsmentioning
confidence: 99%
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“…CT2013B, developed by the Earth System Research Laboratory (ESRL) at the National Oceanic and Atmospheric Administration (NOAA), was used for this study. CT2013B estimates the surface CO 2 flux using inverse modeling and has been widely used to calculate surface CO 2 fluxes in North America, Europe, and Asia (Peters et al, 2004(Peters et al, , 2005(Peters et al, , 2007(Peters et al, , 2010Kim et al, 2012Kim et al, , 2014aKim et al, , 2014bKim et al, , 2016Kim et al, , 2017Kim et al, , 2018aCheng et al, 2013).…”
Section: Carbontracker and Data Assimilation Methodsmentioning
confidence: 99%
“…28 The experiment that adds 10 observation sites to the existing 18 NOAA observation network sites with the normalized self-sensitivity and ecoregion information (1-2 stations for each ecoregion). By calculating the ensemble mean and perturbation independently, the underestimation of the analysis error covariance could be prevented (Whitaker and Hamill, 2002;Kim et al, 2012). P b H T and HP b H T can be calculated as follows:…”
Section: Necoss1_18mentioning
confidence: 99%
“…CT2013B, developed by the Earth System Research Laboratory (ESRL) at the National Oceanic and Atmospheric Administration (NOAA), was used for this study. CT2013B estimates the surface carbon flux using inverse modeling and has been widely used to calculate surface carbon fluxes in North America, 5 Europe, and Asia (Peters et al, 2004(Peters et al, , 2005(Peters et al, , 2007(Peters et al, , 2010Kim et al, 2012Kim et al, , 2014aKim et al, , 2014bKim et al, , 2017Cheng et al, 2013;Kim et al, 2016Kim et al, , 2018aKim et al, , 2018b.…”
Section: Carbontracker and Data Assimilation Methodsmentioning
confidence: 99%
“…To investigate the reduction of uncertainties for each experiment after data assimilation, uncertainty reduction (UR; Peters et al, 2005;Meirink et al, 2008;Chevallier et al, 2009b, Feng et al, 2009Kim et al, 2014a, Kim et al, 2018b was calculated as:…”
Section: Simulated Hypothetical Observation and Experimental Setupmentioning
confidence: 99%
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