TY - JOUR
T1 - Soil organic carbon stock changes in Swedish forest soils—A comparison of uncertainties and their sources through a national inventory and two simulation models
AU - Ortiz, Carina
AU - Liski, Jari
AU - Gärdenäs, Annemieke
AU - Lehtonen, Aleksi
AU - Lundblad, Mattias
AU - Stendahl, Johan
AU - Ågren, Göran
AU - Karltun, Erik
PY - 2013
Y1 - 2013
N2 - Swedish Forest Soil Inventory (SFSI) estimates of SOC stocks and SOC changes for forest on mineral soils under Scots pine (Pinus sylvestris)/lodgepole pine (Pinus contorta) or Norway spruce (Picea abies) were compared with estimates, including uncertainties due to parameter, input and climate variability, from two process-based models (Yasso07 and Q) for the period 1994-2000. We found that the stocks, changes, inter-annual variations and uncertainties were of the same magnitude among the different methods. The mean Swedish national stocks in 2000 were estimated to be 73 (+/- 10) (95% CL) ton ha(-1) C (SFSI); 69 (+/- 9) (95% CL) ton ha(-1) C (Yasso07); and, 67 (+10; -9) (5th and 95th percentiles) ton ha(-1) C (Q). Between 1994 and 2000, the mean estimated SOC change were 6.6 (+/- 7)Tg Cyr(-1) (SFSI), 1.7 (+/- 8.8)Tg Cyr(-1) (Yasso07), and -3.2 (+10.5; -16.9)Tg Cyr(-1) (Q). Spatial variability was the main source of uncertainty for the SOC stocks and changes estimated with the SFSI. The uncertainties in the stock estimates originated from litter input for Yasso07 and from the model parameters for the Q model. In both models, litter input uncertainty was the major source of uncertainty for the estimated SOC changes, followed by climate variability and parameters. We concluded that the level of uncertainty for both methods was similar but the sources of uncertainties varied between models and measurements. Thus, comparing uncertainty between methods is difficult and further studies on SOC change estimates with related uncertainties are warranted. (C) 2013 Elsevier B.V. All rights reserved.
AB - Swedish Forest Soil Inventory (SFSI) estimates of SOC stocks and SOC changes for forest on mineral soils under Scots pine (Pinus sylvestris)/lodgepole pine (Pinus contorta) or Norway spruce (Picea abies) were compared with estimates, including uncertainties due to parameter, input and climate variability, from two process-based models (Yasso07 and Q) for the period 1994-2000. We found that the stocks, changes, inter-annual variations and uncertainties were of the same magnitude among the different methods. The mean Swedish national stocks in 2000 were estimated to be 73 (+/- 10) (95% CL) ton ha(-1) C (SFSI); 69 (+/- 9) (95% CL) ton ha(-1) C (Yasso07); and, 67 (+10; -9) (5th and 95th percentiles) ton ha(-1) C (Q). Between 1994 and 2000, the mean estimated SOC change were 6.6 (+/- 7)Tg Cyr(-1) (SFSI), 1.7 (+/- 8.8)Tg Cyr(-1) (Yasso07), and -3.2 (+10.5; -16.9)Tg Cyr(-1) (Q). Spatial variability was the main source of uncertainty for the SOC stocks and changes estimated with the SFSI. The uncertainties in the stock estimates originated from litter input for Yasso07 and from the model parameters for the Q model. In both models, litter input uncertainty was the major source of uncertainty for the estimated SOC changes, followed by climate variability and parameters. We concluded that the level of uncertainty for both methods was similar but the sources of uncertainties varied between models and measurements. Thus, comparing uncertainty between methods is difficult and further studies on SOC change estimates with related uncertainties are warranted. (C) 2013 Elsevier B.V. All rights reserved.
KW - SOC
KW - Coniferous forest soils
KW - National soil inventory
KW - Model uncertainty
KW - Climate change
KW - Reporting
KW - SOC
KW - Coniferous forest soils
KW - National soil inventory
KW - Model uncertainty
KW - Climate change
KW - Reporting
UR - https://res.slu.se/id/publ/50347
U2 - 10.1016/j.ecolmodel.2012.12.017
DO - 10.1016/j.ecolmodel.2012.12.017
M3 - Journal article
SN - 0304-3800
VL - 251
SP - 221
EP - 231
JO - Ecological Modelling
JF - Ecological Modelling
ER -