1,915 research outputs found

    Heat transfer in DIRSIG an infrared synthetic scene generation model

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    Improvements to the thermodynamic model in the RIT Digital Imaging and Remote Sensing Lab\u27s synthetic image generation software model, DIRSIG, were made to account for three forms of heat transfer: conduction, convection, and radiation from an internal heat source. A validation was completed that collected truth data and evaluated the performance of the modifications. The simulated contrast of the final temperature images was relatively close to truth contrast. In addition, the exposed area term from the thermodynamic model was modified with the DIRSIG shape factor calculation for four different scenarios to improve background object temperature interactions. The best scenario was a replacement of the exposed area with the shape factor in the sky/background temperature equation. Finally, interpolation on weather data to decrease discrete shadow edges was performed and evaluated. This approach significandy reduced edge effects, but due to incorrect scene geometry, previous simulated imagery and previous truth imagery did not coincide, making final conclusions difficult to predict

    Vibrato

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    Architecture & Allied Art

    Vibrato

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    Architecture & Allied Art

    Relationship of perceived ability and playing time to team climate

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    This study was initiated in an attempt to assess the team climate in various basketball environments and how an individual\u27s perceived ability and playing time may affect team climate. [This is an excerpt from the abstract. For the complete abstract, please see the document.

    Using Micro-Gravity Techniques to Map Alluvium Thickness and Pleistocene Location of the West Branch of the Susquehanna River Near Muncy, Pennsylvania

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    Laurentide glaciation during the early Pleistocene (~970 ka) dammed the southeast-flowing West Branch of the Susquehanna River (WBSR), scouring bedrock and creating 100-km-long glacial Lake Lesley near the Great Bend at Muncy, Pennsylvania (Ramage et al., 1998). Local drill logs and well data indicate that subsequent paleo-outwash floods and modern fluvial processes have deposited as much as 30 meters of alluvium in this area, but little is known about the valley fill architecture and the bedrock-alluvium interface. By gaining a greater understanding of the bedrock-alluvium interface the project will not only supplement existing depth to bedrock information, but also provide information pertinent to the evolution of the Muncy Valley landscape. This project determined if variations in the thickness of the valley fill were detectable using micro-gravity techniques to map the bedrock-alluvium interface. The gravity method was deemed appropriate due to scale of the study area (~30 km2), ease of operation by a single person, and the available geophysical equipment. A LaCoste and Romberg Gravitron unit was used to collect gravitational field readings at 49 locations over 5 transects across the Muncy Creek and Susquehanna River valleys (approximately 30 km2), with at least two gravity base stations per transect. Precise latitude, longitude and ground surface elevation at each location were measured using an OPUS corrected Trimble RTK-GPS unit. Base stations were chosen based on ease of access due to the necessity of repeat measurements. Gravity measurement locations were selected and marked to provide easy access and repeat measurements. The gravimeter was returned to a base station within every two hours and a looping procedure was used to determine drift and maximize confidence in the gravity measurements. A two-minute calibration reading at each station was used to minimize any tares in the data. The Gravitron digitally recorded finite impulse response filtered gravity measurements every 20 seconds at each station. A measurement period of 15 minutes was used for each base station occupation and a minimum of 5 minutes at all other locations. Longer or multiple measurements were utilized at some sites if drift or other externalities (i.e. train or truck traffic) were effecting readings. Average, median, standard deviation and 95% confidence interval were calculated for each station. Tidal, drift, latitude, free-air, Bouguer and terrain corrections were then applied. The results show that the gravitational field decreases as alluvium thickness increases across the axes of the Susquehanna River and Muncy Creek valleys. However, the location of the gravity low does not correspond with the present-day location of the West Branch of the Susquehanna River (WBSR), suggesting that the WBSR may have been constrained along Bald Eagle Mountain by a glacial lobe originating from the Muncy Creek Valley to the northeast. Using a 3-D inversion model, the topography of the bedrock-alluvium interface was determined over the extent of the study area using a density contrast of -0.8 g/cm3. Our results are consistent with the bedrock geometry of the area, and provide a low-cost, non-invasive and efficient method for exploring the subsurface and for supplementing existing well data

    CL2. Psi4NumPy: An Interactive Quantum Chemistry Programming Environment for Reference Implementation, Rapid Development, and Education

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    A cornerstone of the development of novel quantum chemistry methods is the translation of paper-and-pencil theory into an eļ¬ƒcient computer program. To do this, low-level programming languages are typically employed; however, such implementations tend to be convoluted, as raw speed is the focus rather than either readability or reproducibil-ity. Any attempt at re-implementation must then proceed with the originally published equations as the only reference, whereby critical programming details must be re-discovered through a similarly heroic eļ¬€ort to the original implementation. To address these issues, the Psi4NumPy project [1] leverages the Psi4 quantum chemistry package and the Nu-merical Python (NumPy)library to create an interactive quantum chemistry programming environment for reference implementations, rapid development, and education. This envi-ronment allows for quantum chemistry-speciļ¬c quantities computed with Psi4 and strided tensor manipulations performed with NumPy to be called directly from within the high-level Python programming language. Therefore, implementations of novel methods may be devel-oped quickly and programmed concisely, while maintaining a relatively low execution time. Provided as a series of short Python scripts, reference implementations for a variety of pop-ular quantum chemistry methods (including Hartreeā€“Fock, MĆøllerā€“Plesset, coupled cluster, electron propagator, and symmetry-adapted perturbation theories) address the community need for clear, readable programs which disseminate the details of such methodsā€™ implemen-tation. Additionally, interactive tutorials discussing both the theory and implementation of these methods and others oļ¬€er a unique educational framework for novice and experienced quantum chemists alike. Daniel G. A. Smith, Georgia Institute of Technology Dominic A. Sirianni, Georgia Institute of Technology Lori A. Burns, Georgia Institute of Technology Konrad Patkowski, Auburn University C. David Sherrill, Georgia Institute of Technolog
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