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Probabilistic estimation of depth-resolved profiles of soil thermal diffusivity from temperature time series: Supporting Data
This dataset consists of soil temperature time series that were used to estimate soil thermal diffusivity and its uncertainty trough the probabilistic modelling approach developed and presented in the article named "Probabilistic estimation of depth-resolved profiles of soil thermal diffusivity from temperature time series" and published in Earth Surface Dynamics. There are two compressed (.zip) files that contains synthetic (Synthetic_soiltemp_Teller.zip) and field (Field_soiltemp_Teller.zip) data. There is one MATLAB file that requires MATLAB to execute but any text editor can open it. The Synthetic_soiltemp_Teller.zip file includes 5 comma-delimited data files (.csv) each of which contains soil temperature time series generated through forward modeling (i.e., heat-conduction process in a heterogeneous medium using an explicit finite difference method) to mimic various types of temperature gradients, trend and fluctuations. These synthetic soil temperatures were used to investigate the impact of different environmental conditions on the uncertainty of thermal diffusivity estimates. The Field_soiltemp_Teller.zip file contains 28 comma-delimited data files (.csv) out of which (a) 27 files includes soil temperature time series recorded from 27 temperature probes located in a site along Teller Road about 40 km northwest of Nome, Alaska (64.72°N, 165.94°W), (b) one includes the name and coordinates of the 27 probes. These field soil temperatures were used to infer soil thermal diffusivity at numerous locations and depths in a discontinuous permafrost environment, and to evaluate the links between the estimated soil thermal diffusivity values and soil physical properties. The comma-delimited data files (.csv) of the synthetic and field soil temperature time series includes date and time (UTC) in the first column and soil temperature from 5 cm below the ground surface to 1.05 m depth (with 5 or 10 cm spacing between sensors) in the other columns. The measurements were acquired every 15 minutes. The Next-Generation Ecosystem Experiments: Arctic (NGEE Arctic), was a research effort to reduce uncertainty in Earth System Models by developing a predictive understanding of carbon-rich Arctic ecosystems and feedbacks to climate. NGEE Arctic was supported by the Department of Energy's Office of Biological and Environmental Research. The NGEE Arctic project had two field research sites: 1) located within the Arctic polygonal tundra coastal region on the Barrow Environmental Observatory (BEO) and the North Slope near Utqiagvik (Barrow), Alaska and 2) multiple areas on the discontinuous permafrost region of the Seward Peninsula north of Nome, Alaska. Through observations, experiments, and synthesis with existing datasets, NGEE Arctic provided an enhanced knowledge base for multi-scale modeling and contributed to improved process representation at global pan-Arctic scales within the Department of Energy's Earth system Model (the Energy Exascale Earth System Model, or E3SM), and specifically within the E3SM Land Model component (ELM).
Scattering of radio frequency waves by randomly modulated density interfaces in the edge of fusion plasmas
In the scrape-off layer and the edge region of a tokamak, the plasma is strongly turbulent and scatters the radio frequency (RF) electromagnetic waves that propagate through this region. It is important to know, whether used for diagnostics or for heating and current drive, the spectral properties of these scattered RF waves. The spectral changes influences the interpretation of the diagnostic-data obtained and the current and heating profiles. A full-wave, 3D electromagnetic code ScaRF (see Papadopoulos et al. 2019) has been developed for studying the RF wave propagation through turbulent plasma. ScaRF is a finite-difference frequency-domain (FDFD) method for solving Maxwell's equations. The magnetized plasma is defined through the cold plasma, anisotropic permittivity tensor. As a result, ScaRF can be used to study the scattering of any cold plasma RF wave. It can be for the study of scattering of electron cyclotron waves in ITER-type and medium-sized tokamaks such as TCV, ASDEX-U, DIII-D. For the case of medium-sized tokamaks, there's experimental evidence that drift waves and rippling modes are present in the edge region (see Ritz et al. 1984). Hence, we study the scattering of RF waves by periodic density interfaces (plasma gratings) in the form of a superposition of spatial modes with varying periodicity and random amplitudes (see Papadopoulos et al. 2019). The power reflection coefficient (a random variable) is calculated for different realizations of the density interface. In this work, the uncertainty of the power reflection coefficient is rigorously quantified by use of the Polynomial Chaos Expansion (see Xiu & Karniadakis 2002) method in conjunction with the Smolyak sparse grid integration (see Papadopoulos et al. 2018) (PCE-SG). The PCE-SG method is proven accurate and much more efficient (roughly 2-orders of magnitude shorter execution time) compared to alternative methods such as the Monte Carlo (MC) approach.
Numerical Analysis of the Transient Response of Advanced Thermal Protection Systems for Atmospheric Entry
Equations for the transfer of heat through thermal protection shields are derived in finite difference form. These equations are applicable to charring ablators, impregnated ceramics, subliming ablators, heat sinks, and insulating materials and have been programed for solution on a high-speed digital computer. In the program, thermal properties can be functions of temperature. Provision is made for analysis of heat shields subjected to simultaneous convective and radiative heat inputs. Some typical results are presented. Limited comparisons with experimental results are made.
Optimal control in second-order relay-pulse systems
Automatic control of two-dimensional motion of material point described by two finite difference equations
Longitudinal shear loading of a unidirectional composite.
Fiber reinforced composite material behavior examined from shear loading tests, using finite difference analysis for representative PDEs
Base flow field investigation on the S-2 stage
Modified computer program using finite difference method for calculating base flow field and dissipation for Saturn S-2 stage
Teddy - A two-dimensional Lagrangian code for determining the wave propagation in elastic-plastic media
Finite difference methods and two dimensional Lagrangian code for determining wave propagation in elastic-plastic media - TEDDY program
An analysis of the coupled chemically reacting boundary layer and charring ablator, part 1 Summary report
Analyses and finite difference procedure for predicting transient in-depth response of charring ablation materials
A study of the transient flow field ahead of a sphere which has been struck by a normal shock wave
Finite difference method of solving normal shock wave-sphere interaction problem for ideal and real gas flow fields
One-dimensional analysis of the hypervelocity impact of a pellet onto a thin bumper
One dimensional analysis of hypervelocity impact of pellet onto thin bumper using finite difference techniques
Numerical solution for flux components in potential flow.
Numerical solution for second order finite difference differential equations, defining flux components in potential flow
Jet-shock interactions.
Finite difference scheme from method of characteristics to investigate flow field and intersecting exhaust plumes from nozzles
Numerical solutions of compressible and incompressible laminar separated flows.
Numerical techniques and solutions for compressible and incompressible laminar separated flows using time dependent finite difference equations
Problems of rocket exhaust plume interactions.
Three dimensional interaction of multirocket vehicle exhaust jet plumes calculated, using finite difference analog to inviscid flow equations
A numerical procedure for calculating stress and deformation near a slit in a three- dimensional elastic-plastic solid.
Finite difference procedure to compute stress and deformation near slit in three dimensional elastic plastic solid
Turbulent mixing of a jet in a coflowing stream.
Turbulent mixing of injected jet with coflowing outer stream, using finite difference treatment for equations of motion
MAGNTY - Program for calculating velocities in magnified region of turbomachines
Computer program, MAGNFY, calculates the velocity distribution through the passage between and over blade surfaces of blade rows for turbines and compressors. Using the input of other programs, MAGNFY obtains velocities on smaller than normal finite difference mesh in any part of the blade-to-blade passage.