Abstract:In this study, we propose a direction-controlled nonlinear least squares estimation model that combines the penalty function and sequential quadratic programming. The least squares model is transformed into a sequential quadratic programming model, allowing for the iteration direction to be controlled. An ill-conditioned matrix is processed by our model; the least squares estimate, the ridge estimate, and the results are compared based on a combination of qualitative and quantitative analyses. For comparison, … Show more
“…Zhang et al (2017) estimated that the amount of N inputs from livestock manure applied to European croplands was 3.9 Tg N in 2014, for a cropland area of 127 Mha in 2015 (Goldewijk et al, 2017). Cattle manure, which represents the highest proportion of manure produced and applied to croplands, has an average C : N ratio ranging between 10 and 30 (multiple sources from Fuchs et al, 2014, andPellerin et al, 2019). With these data, we can roughly estimate the application of C manure from livestock in European agricultural soils as ranging between 0.30 and 0.92 MgC ha −1 each year.…”
Section: Simulated Carbon Inputs and Experimental Carbon Addition Treatmentsmentioning
Abstract. The 4 per 1000 initiative aims to maintain and increase soil organic carbon (SOC) stocks for soil fertility, food security, and climate change
adaptation and mitigation. One way to enhance SOC stocks is to increase carbon (C) inputs to the soil. In this study, we assessed the amount of organic C inputs that are necessary to reach a target of SOC stocks increase by
4 ‰ yr−1 on average, for 30 years, at 14 long-term agricultural sites in Europe. We used the Century model to simulate SOC
stocks and assessed the required level of additional C inputs to reach the 4 per 1000 target at these sites. Then, we analyzed how this would change
under future scenarios of temperature increase. Initial stocks were simulated assuming steady state. We compared modeled C inputs to different
treatments of additional C used on the experimental sites (exogenous organic matter addition and one treatment with different crop rotations). The
model was calibrated to fit the control plots, i.e. conventional management without additional C inputs from exogenous organic matter or changes in
crop rotations, and was able to reproduce the SOC stock dynamics. We found that, on average among the selected experimental sites, annual C inputs will have to increase by 43.15 ± 5.05 %, which is
0.66 ± 0.23 MgCha-1yr-1 (mean ± standard error), with respect to the initial C inputs in the control treatment. The
simulated amount of C input required to reach the 4 ‰ SOC increase was lower than or similar to the amount of C input actually used in the
majority of the additional C input treatments of the long-term experiments. However, Century might be overestimating the effect of additional
C inputs on SOC stocks. At the experimental sites, we found that treatments with additional C inputs were increasing by 0.25 % on average. This
means that the C inputs required to reach the 4 per 1000 target might actually be much higher. Furthermore, we estimated that annual C inputs will
have to increase even more due to climate warming, that is 54 % more and 120 % more for a 1 and 5 ∘C warming,
respectively. We showed that modeled C inputs required to reach the target depended linearly on the initial SOC stocks, raising concern on the
feasibility of the 4 per 1000 objective in soils with a higher potential contribution to C sequestration, that is soils with high SOC stocks. Our
work highlights the challenge of increasing SOC stocks at a large scale and in a future with a warmer climate.
“…Zhang et al (2017) estimated that the amount of N inputs from livestock manure applied to European croplands was 3.9 Tg N in 2014, for a cropland area of 127 Mha in 2015 (Goldewijk et al, 2017). Cattle manure, which represents the highest proportion of manure produced and applied to croplands, has an average C : N ratio ranging between 10 and 30 (multiple sources from Fuchs et al, 2014, andPellerin et al, 2019). With these data, we can roughly estimate the application of C manure from livestock in European agricultural soils as ranging between 0.30 and 0.92 MgC ha −1 each year.…”
Section: Simulated Carbon Inputs and Experimental Carbon Addition Treatmentsmentioning
Abstract. The 4 per 1000 initiative aims to maintain and increase soil organic carbon (SOC) stocks for soil fertility, food security, and climate change
adaptation and mitigation. One way to enhance SOC stocks is to increase carbon (C) inputs to the soil. In this study, we assessed the amount of organic C inputs that are necessary to reach a target of SOC stocks increase by
4 ‰ yr−1 on average, for 30 years, at 14 long-term agricultural sites in Europe. We used the Century model to simulate SOC
stocks and assessed the required level of additional C inputs to reach the 4 per 1000 target at these sites. Then, we analyzed how this would change
under future scenarios of temperature increase. Initial stocks were simulated assuming steady state. We compared modeled C inputs to different
treatments of additional C used on the experimental sites (exogenous organic matter addition and one treatment with different crop rotations). The
model was calibrated to fit the control plots, i.e. conventional management without additional C inputs from exogenous organic matter or changes in
crop rotations, and was able to reproduce the SOC stock dynamics. We found that, on average among the selected experimental sites, annual C inputs will have to increase by 43.15 ± 5.05 %, which is
0.66 ± 0.23 MgCha-1yr-1 (mean ± standard error), with respect to the initial C inputs in the control treatment. The
simulated amount of C input required to reach the 4 ‰ SOC increase was lower than or similar to the amount of C input actually used in the
majority of the additional C input treatments of the long-term experiments. However, Century might be overestimating the effect of additional
C inputs on SOC stocks. At the experimental sites, we found that treatments with additional C inputs were increasing by 0.25 % on average. This
means that the C inputs required to reach the 4 per 1000 target might actually be much higher. Furthermore, we estimated that annual C inputs will
have to increase even more due to climate warming, that is 54 % more and 120 % more for a 1 and 5 ∘C warming,
respectively. We showed that modeled C inputs required to reach the target depended linearly on the initial SOC stocks, raising concern on the
feasibility of the 4 per 1000 objective in soils with a higher potential contribution to C sequestration, that is soils with high SOC stocks. Our
work highlights the challenge of increasing SOC stocks at a large scale and in a future with a warmer climate.
“…e objective function only containing nonlinear parameters is optimized using the LM algorithm. To ensure global optimization, once the nonlinear parameters are calculated for a given iteration, the linear parameters are calculated using equation (15) until the overall gradient is less than a threshold value. For the convenience of expression, in the following text, the traditional LM method without the separation of parameters is referred to as LM unSep .…”
Section: Optimal Estimation Methods For Waveform Gaussianmentioning
confidence: 99%
“…In general, the Gaussian decomposition of waveforms consists of two steps: (1) determining the number of Gaussian components and their initial parameters and (2) optimizing and postprocessing the characteristic parameters. A majority of parameter estimation methods regard all Gaussian parameters as nonlinear variables [15] and then employ the nonlinear optimization method to solve the parameters. Liu et al [16] combined this method with sequential quadratic programming (SQP), developing a gradient-based optimization algorithm; it determined the optimal time delays and system parameters in a novel dynamic optimization problem for nonlinear multistage systems.…”
Light detection and ranging (LiDAR) is commonly used to create high-resolution maps; however, the efficiency and convergence of parameter estimation are difficult. To address this issue, we evaluated the structural characteristics of received LiDAR signals by decomposing them into Gaussian functions and applied the variable projection algorithm of the separable nonlinear least-squares problem to the process of waveform fitting. First, using a variable projection algorithm, we separated the linear (amplitude) and nonlinear (center position and width) parameters in the Gaussian function model; the linear parameters are expressed with nonlinear parameters by the function. Thereafter, the optimal estimation of the characteristic parameters of the Gaussian function components was transformed into a least-squares problem only comprising nonlinear parameters. Finally, the Levenberg–Marquardt algorithm was used to solve these nonlinear parameters, whereas the linear parameters were calculated simultaneously in each iteration, and the estimation results satisfying the nonlinear least-square criterion were obtained. Five groups of waveform decomposition simulation data and ICESat/GLAS satellite LiDAR waveform data were used for the parameter estimation experiments. During the experiments, for the same accuracy, the separable nonlinear least-squares optimization method required fewer iterations and lesser calculation time than the traditional method of not separating parameters; the maximum number of iterations was reached before the traditional method converged to the optimal estimate. The method of separating variables only required 14 iterations to obtain the optimal estimate, reducing the computational time from 1128 s to 130 s. Therefore, the application of the separable nonlinear least-squares problem can improve the calculation efficiency and convergence speed of the parameter solution process. It can also provide a new method for parameter estimation in the Gaussian model for LiDAR waveform decomposition.
“…Its basic principle is to generate an interferogram by conjugate multiplication of two radar complex images before and after deformation, remove topographical factors using the difference from the external DEM to generate a differential interferogram, and then extract the deformation information of the ground targets from the differential interferogram. [16][17][18][19] Phase φ of the interferogram is closely related to the radar imaging parameters, antenna position, incident angle, and the elevation of the ground targets, which can be expressed as E Q -T A R G E T ; t e m p : i n t r a l i n k -; e 0 0 1 ; 1 1 6 ; 9 7 φ ¼ φ flat þ φ topo þ φ def þ φ atm þ φ noise ;…”
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