Blue Streak

The Blue Streak, named for the Sandusky, Ohio athletic teams, opened in 1964. It was the first new wooden roller coaster at the park since the Cyclone in 1929. A classic out-and-back coaster with a fast and hilly ride, the 78-foot-high Blue Streak is a long time guest favorite. It celebrated its 50th anniversary in 2014.

THE IMPACT OF UPPER-LEVEL PROCESSES ON THE INTENSITY AND STRUCTURAL CHANGES OF HURRICANE SANDY (2012)

The first part of this study examines the relative roles of frontogenesis and tropopause undulation in determining the intensity and structural changes of Hurricane Sandy (2012) using a high-resolution cloud-resolving model. A 138-h simulation reproduces Sandy’s four distinct development stages: (i) rapid intensification, (ii) weakening, (iii) steady maximum surface wind but with large continued sea-level pressure (SLP) falls, and (iv) re-intensification. Results show typical correlations between intensity changes, sea-surface temperature and vertical wind shear during the first two stages. The large SLP falls during the last two stages are mostly caused by Sandy’s moving northward into lower-tropopause regions associated with an eastward-propagating midlatitude trough, where the associated lower-stratospheric warm air wraps into the storm and its surrounding areas. The steady maximum surface wind occurs because of the widespread SLP falls with weak pressure gradients lacking significant inward advection of absolute angular momentum (AAM). Meanwhile, there is a continuous frontogenesis in the outer region during the last three stages. Cyclonic inward advection of AAM along each frontal rainband accounts for the continued expansion of the tropical-storm-force wind and structural changes, while deep convection in the eyewall and merging of the final two survived frontal rainbands generate a spiraling jet in Sandy’s northwestern quadrant, leading to its re-intensification prior to landfall. The physical, kinematic and dynamic aspects of an upper-level outflow layer and its possible impact on the re-intensification of Sandy are examined in the second part of this study. Above the outflow layer isentropes are tilted downward with radius as a result of the development of deep convection and an approaching upper-level trough, causing weak subsidence. Its maximum outward radial velocity is located above the cloud top, so the outflow channel experiences cloud-induced long-wave cooling. Because Sandy has two distinct convective regions (an eyewall and a frontal rainband), it has multiple outflow layers, with the eyewall’s outflow layer located above that of the frontal rainband. During the re-intensification stage, the eyewall’s outflow layer interacts with a jet stream ahead of the upper-level trough axis. Because of the presence of inertial instability on the anticyclonic side of the jet stream and symmetric instability in the inner region of the outflow layer, Sandy’s secondary circulation intensifies. Its re-intensification ceases when these instabilities disappear. The relationship between the intensity of the secondary circulation and dynamic instabilities of the outflow layer suggests that the re-intensification occurs in response to these instabilities. Additionally, it is verified that the long-wave cooling in the outflow layer helps induce symmetric instability by reducing static stability.

A coupled ocean-atmosphere system for short term forecasting in the southern european seas

This coupled model combines two state-of-the-art numerical models, NEMO for the oceanic component and WRF for the atmospheric component and implements them at an appropriate resolution. The oceanic model has been implemented starting from the Mediterranean Forecasting System with a resolution of 1/24° and the domain was extended to exactly match the grid of a newly implemented atmospheric model for the same area. The uncoupled ocean model has been validated against SST observed data, both in the simulation of an extreme event and in the short-term forecast of two seasonal periods. A new setup of the model was successfully tested in which the downward radiative fluxes were prescribed from atmospheric forecasts. Various physical schemes, domain, boundary, and initial conditions were tested with the atmospheric model to obtain the best representation of medicane Ianos. The heat fluxes calculated by the uncoupled models were compared to determine which setup gave the best energy balance between the components of the coupled model. The coupling strategy used is the traditional one, where the ocean is driven by the surface stress, heat fluxes, and radiative fluxes computed in the atmospheric component, which in turn receives the SST and surface currents. As expected, the overall skills of the coupled model are slightly degraded compared to the uncoupled models, even though the positioning and timing of the cyclone at the time of the landfall is enhanced. The mean heat fluxes do not change compared to the uncoupled model, whereas the pattern of the shortwave radiation and latent heat is changed. Moreover, the two energy fluxes are larger in absolute values than those calculated with the MFS formulas. The fact that they have opposite signs give raise to a compensation error that limits the overall degradation of the coupled simulation.

Benchmarking di sistemi di additive manufacturing in termini di precisione di forma con ispirazione al sistema GD&T

Questo studio si pone come obiettivo lo sviluppo e la sperimentazione di un metodo per eseguire un benchmarking di due diversi sistemi di Additive Manufacturing mediante macchina di misura a coordinate Renishaw Cyclone. In particolare sono valutate le prestazioni in termini di precisione di forma di un sistema di tipo FDM e di uno di tipo PolyJet al fine di ottenere dati indicanti le potenzialità di queste due tecnologie per parti di piccole dimensioni. Dopo un’introduzione generale sull’Additive Manufacturing, si scende nei dettagli delle due tecniche oggetto dello studio e si discute di come strutturare il piano sperimentale in funzione degli obiettivi dell’attività e dei metodi scelti per l’acquisizione e la valutazione dei dati. Si parte, infatti, con la fabbricazione di un modello di benchmark, le cui geometrie vengono poi rilevate tramite una macchina di misura a coordinate per ottenere i valori di precisione di forma, che sono presentati come tolleranze geometriche del sistema GD&T. Successivamente, si descrivono tutte le fasi dell’attività sperimentale, iniziando con l’ideazione del modello di benchmark e proseguendo con i processi di fabbricazione e misurazione, per poi arrivare alla deduzione dei valori di precisione di forma tramite un post-processing dei dati. Infine, si presentano i valori di tolleranza ottenuti e si traggono le conclusioni riguardo la riuscita dell’attività sperimentale e il confronto tra le due tecnologie di Additive Manufacturing.