3,212 research outputs found

    Regolith-atmosphere exchange of water in Mars' recent past

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    We investigate the exchange of water vapour between the regolith and atmosphere of Mars, and how it varies with different orbital parameters, atmospheric dust contents and surface water ice reservoirs. This is achieved through the coupling of a global circulation model (GCM) and a regolith diffusion model. GCM simulations are performed for hundreds of Mars years, with additional one-dimensional simulations performed for 50 kyr. At obliquities ε = 15° and 30°, the thermal inertia and albedo of the regolith have more control on the subsurface water distribution than changes to the eccentricity or solar longitude of perihelion. At ε = 45°, atmospheric water vapour abundances become much larger, allowing stable subsurface ice to form in the tropics and mid-latitudes. The circulation of the atmosphere is important in producing the subsurface water distribution, with increased water content in various locations due to vapour transport by topographically-steered flows and stationary waves. As these circulation patterns are due to topographic features, it is likely the same regions will also experience locally large amounts of subsurface water at different epochs. The dustiness of the atmosphere plays an important role in the distribution of subsurface water, with a dusty atmosphere resulting in a wetter water cycle and increased stability of subsurface ice deposits

    Casually Evolving Creative Technology Systems

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    Smoothed particle magnetohydrodynamic simulations of protostellar outflows with misaligned magnetic field and rotation axes

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    We have developed a modified form of the equations of smoothed particle magnetohydrodynamics which are stable in the presence of very steep density gradients. Using this formalism, we have performed simulations of the collapse of magnetised molecular cloud cores to form protostars and drive outflows. Our stable formalism allows for smaller sink particles (< 5 AU) than used previously and the investigation of the effect of varying the angle, {\theta}, between the initial field axis and the rotation axis. The nature of the outflows depends strongly on this angle: jet-like outflows are not produced at all when {\theta} > 30{\deg}, and a collimated outflow is not sustained when {\theta} > 10{\deg}. No substantial outflows of any kind are produced when {\theta} > 60{\deg}. This may place constraints on the geometry of the magnetic field in molecular clouds where bipolar outflows are seen.Comment: Accepted for publication in MNRAS, 13 pages, 14 figures. Animations can be found at http://www.astro.ex.ac.uk/people/blewis/research/outflows_misaligned_fields.htm

    Legislatively Directed Judicial Activism: Some Reflections on the Meaning of the Civil Justice Reform Act

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    With the Civil Justice Reform Act (CJRA), Congress attempted to further a trend that the federal judiciary had undertaken largely on its own initiative. Sensing a critical need to address the mounting expense and delay of federal civil litigation, Congress, like the judiciary, sought to increase the degree of early and active involvement of judges in the adjudicatory process. The result of this mandate has been a further emphasis on the role of the judge as a case manager. As a necessary corollary, the liberty and self-determination of individual litigants-ideals that have historically been seen as philosophical cornerstones of the Anglo-American adjudicative process-have been correspondingly diminished. In this Article, the authors examine the departure from the philosophical moorings of the Anglo-American system of justice that implementation of the CJRA represents and consider whether the gains to be achieved by the Act, if successful, offset the potential costs to the litigants that the Act imposes

    Legislatively Directed Judicial Activism: Some Reflections on the Meaning of the Civil Justice Reform Act, 28 U. Mich. J.L. Reform 305 (1995)

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    With the Civil Justice Reform Act (CJRA), Congress attempted to further a trend that the federal judiciary had undertaken largely on its own initiative. Sensing a critical need to address the mounting expense and delay of federal civil litigation, Congress, like the judiciary, sought to increase the degree of early and active involvement of judges in the adjudicatory process. The result of this mandate has been a further emphasis on the role of the judge as a case manager. As a necessary corollary, the liberty and self-determination of individual litigants-ideals that have historically been seen as philosophical cornerstones of the Anglo-American adjudicative process-have been correspondingly diminished. In this Article, the authors examine the departure from the philosophical moorings of the Anglo-American system of justice that implementation of the CJRA represents and consider whether the gains to be achieved by the Act, if successful, offset the potential costs to the litigants that the Act imposes

    Future Type Ia Supernova Data as Tests of Dark Energy from Modified Friedmann Equations

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    In the Cardassian model, dark energy density arises from modifications to the Friedmann equation, which becomes H^2 = g(\rhom), where g(\rhom) is a new function of the energy density. The universe is flat, matter dominated, and accelerating. The distance redshift relation predictions of generalized Cardassian models can be very different from generic quintessence models, and can be differentiated with data from upcoming pencil beam surveys of Type Ia Supernovae such as SNAP. We have found the interesting result that, once Ωm\Omega_m is known to 10% accuracy, SNAP will be able to determine the sign of the time dependence of the dark energy density. Knowledge of this sign (which is related to the weak energy condition) will provide a first discrimination between various cosmological models that fit the current observational data (cosmological constant, quintessence, Cardassian expansion). Further, we have performed Monte Carlo simulations to illustrate how well one can reproduce the form of the dark energy density with SNAP. To be concrete we study a class of two parameter (nn,qq) generalized Cardassian models that includes the original Cardassian model (parametrized by nn only) as a special case. Examples are given of MP Cardassian models that fit current supernovae and CMB data, and prospects for differentiating between MP Cardassian and other models in future data are discussed. We also note that some Cardassian models can satisfy the weak energy condition w>−1w>-1 even with a dark energy component that has an effective equation of state wX<−1w_X < -1.Comment: revised version accepted by Ap

    Evaluation of vector sensors for adaptive equalization in underwater acoustic communication

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    Submitted in partial fulfillment of the requirements for the degree of Master of Science at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution September 2014Underwater acoustic communication is an extremely complex field that faces many challenges due to the time-varying nature of the ocean environment. Vector sensors are a proven technology that when utilizing their directional sensing capabilities allows us to minimize the effect of interfering noise sources. A traditional pressure sensor array has been the standard for years but suffers at degraded signal to noise ratios (SNR) and requires maneuvers or a lengthly array aperture to direction find. This thesis explores the effect of utilizing a vector sensor array to steer to the direction of signal arrival and the effect it has on equalization of the signal at degraded SNRs. It was demonstrated that utilizing a single vector sensor we were able steer to the direction of arrival and improve the ability of an equalizer to determine the transmitted signal. This improvement was most prominent when the SNR was degraded to levels of 0 and 10 dB where the performance of the vector sensor outperformed that of the pressure sensor in nearly 100% of cases. Finally, this performance improvement occured with a savings in computational expense.ONR Grants #N00014-11-10426 and #N00014-07-1073
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