2018
DOI: 10.5194/bg-2018-62
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A Bayesian Ensemble Data Assimilation to Constrain Model Parameters and Land Use Carbon Emissions

Abstract: Abstract.A dynamic global vegetation model (DGVM) is applied in a probabilistic framework and benchmarking system to constrain uncertain model parameters by observations and to quantify carbon emissions from land-use and land-cover change (LULCC).Processes featured in DGVMs include parameters which are prone to substantial uncertainty. To cope with these uncertainties Latin Hypercube Sampling (LHS) is used to create a 1000-member perturbed parameter ensemble, which is then evaluated with 5 a diverse set of glo… Show more

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Cited by 16 publications
(16 citation statements)
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“…The losses in carbon due to land use conversion (E 1.2 ) are largest in the eastern United States and West Coast with increases in the interior of the country driven by agricultural fertilization (Figure ). The net effect (Table ) shows larger emissions earlier in the 20th century than after 1950, consistent with results of Lienert and Joos (), but other studies (Houghton & Nassikas, ) show a sink after the 1950s from land use and land cover change. The regrowth effect, which is effect of land use and land cover change on NEP itself, is 29 TgC/year, or 1.78 PgC since 1950.…”
Section: Resultssupporting
confidence: 89%
“…The losses in carbon due to land use conversion (E 1.2 ) are largest in the eastern United States and West Coast with increases in the interior of the country driven by agricultural fertilization (Figure ). The net effect (Table ) shows larger emissions earlier in the 20th century than after 1950, consistent with results of Lienert and Joos (), but other studies (Houghton & Nassikas, ) show a sink after the 1950s from land use and land cover change. The regrowth effect, which is effect of land use and land cover change on NEP itself, is 29 TgC/year, or 1.78 PgC since 1950.…”
Section: Resultssupporting
confidence: 89%
“…Finally, 7 of the 10 participating models were selected to estimate N 2 O emissions from both cropland and natural soils and to quantify the relative contributions of each driving factor. These seven models are as follows: (1) the Dynamic Land Ecosystem Model (DLEM; Tian et al, ; Xu et al, ), (2) Lund‐Potsdam‐Jena‐General Ecosystem Simulator (LPJ‐GUESS; Olin et al, ; Xu‐Ri & Prentice, ), (3) Land Processes and eXchanges model‐Bern (LPX‐Bern v1.4; Lienert & Joos, ; Stocker et al, ; Xu‐Ri & Prentice, ), (4) O‐CN (Zaehle et al, ), (5) Organising Carbon and Hydrology In Dynamic Ecosystems (ORCHIDEE, Vuichard et al ), (6) Organising Carbon and Hydrology In Dynamic Ecosystems‐Carbon Nitrogen Phosphorus (ORCHIDEE‐CNP; Goll et al, ), and (7) Vegetation Integrated Simulator for Trace gases (VISIT, Inatomi, Ito, Ishijima, & Murayama, ; Ito & Inatomi, ; See more model information in Supporting Information Table S1). Five models (DLEM, LPJ‐GUESS, ORCHIDEE, ORCHIDEE‐CNP, and VISIT) considered the effects of manure use in cropland and ran all the seven simulation experiments (S0–S6), while the other two models (LPX‐Bern and O‐CN) did not include manure effects and ran six model experiments (all except SE1).…”
Section: Methodsmentioning
confidence: 99%
“…For all sites, we conducted simulations using 10 terrestrial biosphere models: CABLE r54482.0 (Wang et al, ), DLEM v2.0 (Tian et al, ), JULES v5.2 (Clark et al, ), JSBACH v3.2 (Kaminski et al, ; Mauritsen et al, ), LPX v1.4 (Lienert & Joos, ), ORCHIDEE rev5150 (Krinner et al, ), ORCHIDEE MICT rev5308 (Guimberteau et al, ), ORCHIDEE CNP rev4520 (Goll et al, ), T&C v1.0 (Fatichi et al, ; Paschalis, Katul, Fatichi, Palmroth, & Way, ) and TECO v2.0 (Huang et al, ). All models include a land surface scheme, a hydrological component and a dynamic vegetation module.…”
Section: Methodsmentioning
confidence: 99%