Mesoscale

In this study, the fifth-generation Pennsylvania State University–National Center for Atmospheric Research Mesoscale Model (MM5) with three-dimensional variational data assimilation (3DVAR) is utilized to investigate influences of GPS occultation refractivity on simulations of typhoons past Taiwan. Two recent cases were simulated, including Typhoon Nari in September 2001 and Typhoon Nakri in July 2002. The GPS observation data are taken from the Challenging Minisatellite Payload for Geophysical Research and Application (CHAMP) and Satélite de Aplicaciones Científicas-C (SAC-C) satellites that provide several retrieved refractivity profiles in the simulated domain near the initialization time. Through 3DVAR, the observed refractivity can be quickly ingested into the model initial conditions to recover the information over the ocean. The initial moisture increments from ingested GPS refractivity soundings exhibit a maximum magnitude of about 1.5 g kg−1 associated with temperature incr...

Concrete is considered as a 3-phase composite material; mortar matrix, aggregates, and interfacial transmission zone (ITZ). In order to investigate the contribution of each phase to the strength and damage response of concrete, 2-D and 3-D meso-scale simulations based on a coupled plasticity-damage model are carried out. The aggregates are modeled as a linear-elastic material, whereas the mortar matrix and ITZ are modeled using a coupled plasticity-damage model with different tensile and compressive mechanical behavior. Aggregate shape, distribution, and volume fraction are considered as simulated variables. The effect of the ITZ thickness and the strength of the ITZ and mortar matrix are also evaluated. It is shown that the behavior of concrete is merely dependent on the aggregate distribution and the strength of the mortar matrix, but dependent on aggregate shape, size, and volume fraction, and the thickness and strength of the ITZ.

The field of interactive music systems (IMSs), beginning in the 1980s, is still relatively young and fast moving. The field of music theory-analysis, during the same period (since 1980), has undergone a major transformation in terms of technological innovations, flexibility, and breadth. The two fields have not really caught up with each other. It will be interesting to see what arises as they do — especially as both fields have become more concerned with the role of the body and embodied cognition. Framed in terms of contrasting epistemological orientations, this essay considers some relevant developments in IMSs, music cognition, and music theory and analysis, leading up to the present.  The most popular approaches to music cognition and to IMS design are rationalist (Ashby 2010), exploiting the ‘correct’ embodiments of music (Godøy 2004, Leman 2007, Paine 2009) based on affordances (Gibson 1977, Kelso 1998). This essay, however, advocates a pragmatist (Ashby 2010) approach inspired by music analysis and exploiting the potential of kinesthetic learning (associative learning). Prompted by a progressive approach to music analysis, theory, perception, and cognition (Dubiel 1999, Mailman 2007), interactive music technology can also be constructive, flexible, and progressive, by exploiting kinesthetic learning from immersion in new and unusual motion-to-sound mappings derived from dynamic formal processes in analysed music. In this way, immersive interactive systems offer an opportunity systematically to learn new associations based on principles theorised in response to analysis. Experience of these systems essentially ‘rewires the brain’, thereby exemplifying what Korsyn (2004) has attributed to Lewin’s (1986, 1987) approach to music perception: the ironist approach, as formulated by Rorty (1989). Thus a pragmatist ironist experimental (PIE) approach is articulated. Rather than committing to any particular ways music is already embodied, this approach acknowledges the flexible nature of embodied musical experience. It forges and uses interactive music technologies continually to redescribe and therefore reform how music is embodied, thereby disembodying to re-embody music, expanding how music is heard, contemplated and experienced.

Twenty-eight predecessor rain events (PREs) that occurred over the United States east of the Rockies during 1995–2008 are examined from a synoptic climatology and case study perspective. PREs are coherent mesoscale regions of heavy rainfall, with rainfall rates ≥100 mm (24 h)−1, that can occur approximately 1000 km poleward of recurving tropical cyclones (TCs). PREs occur most commonly in August and September, and approximately 36 h prior to the arrival of the main rain shield associated with the TC. A distinguishing feature of PREs is that they are sustained by deep tropical moisture that is transported poleward directly from the TC. PREs are high-impact weather events that can often result in significant inland flooding, either from the PRE itself or from the subsequent arrival of the main rain shield associated with the TC that falls onto soils already saturated by the PRE. The composite analysis shows that on the synoptic-scale, PREs form in the equatorward jet-entrance region o...

This study provides a contribution to the research field of 3D-printed earthen buildings, focusing, for the first time, on the load-bearing capacity of these structures. The study involves the entire production and testing process of the earthen elements, from the design, to the preparation of the mixture and the 3D printing, up to the uniaxial compression test on a wall segment. The results indicate that 3D-printed earthen elements have a compressive strength of 2.32 MPa, comparable to that of rammed earth structures. The experimental data also made it possible to draw conclusions on the action of the infill, which seems to have the function of stopping the propagation of cracks. This has a positive effect on the overall behavior of 3D-printed earthen elements, since it avoids the onset of dilative behavior in the final stages of the load test and maintains ultimate load values higher than 50% of the maximum load.

The Madden–Julian oscillation (MJO) produced by a mesoscale model is investigated using standardized statistical diagnostics. Results show that upper- and lower-level zonal winds display the correct MJO structure, phase speed (8 m s−1) and space–time power spectrum. However, the simulated free atmosphere moisture, outgoing longwave radiation and precipitation do not exhibit any clear MJO signal. Yet, the boundary layer moisture, moist static energy and atmospheric instability, measured using a moist static energy instability index, have clear MJO signals. A significant finding is the ability of the model to simulate a realistic MJO phase speed in the winds without reproducing the MJO wind-convection coupling or a realistic propagation in the free atmosphere water vapor. This study suggests that the convergence of boundary layer moisture and the discharge and recharge of the moist static energy and atmospheric instability may be responsible for controlling the speed of propagation of the MJO circulation.

The current study describes a technique for downscaling climatological data in areas with limited or no grid data. In cases where grid data are unavailable and the researcher is called to operate on a regional or in the mesoscale and produce detailed and not coarse results, this technique can be a helping hand. It constitutes a combination of statistical downscaling through multi-linear regression techniques and dynamical downscaling by employing Geographical Information Systems, and it can be used in order to spatially interpolate with high resolution various climatological variables. The application of the described technique was applied on 3 agricultural areas that present different climate conditions and are characterised by complex topography. The results indicated that the current technique delivered very sufficient results as the adjusted coefficient (R 2) appears with high values in almost every case. Areas characterized by Mediterranean type of climate with hot summers (Csa) showed the strongest presumption against null hypothesis; while areas characterized by a combination of different Mediterranean climate types (Csa and Csb) used the most coefficients in the multi-linear procedure and produced relatively good results. Areas facing continental climate conditions delivered satisfactorily results, although most of the examined coefficients are presented with medium presumption against null hypothesis. Concluding, the described technique can be used for every type of climate in almost every terrain for the accurate representation of various climatological variables in the mesoscale.

During the Eddy Experiment, two synchronous GPS receivers were flown at 1 km altitude to collect L1 signals and their reflections from the sea surface for assessment of altimetric precision and accuracy. Wind speed (U10) was around 10 m/s, and SWH up to 2 m. A geophysical parametric waveform model was used for retracking and estimation of the lapse between

A theoretical formalism for nongeostrophic eddy transport in zonal-mean flows, using a transformed Eulerian-mean (TEM) approach in z coordinates, is discussed. By using Andrews and McIntyre's coordinate-independent definition of the “quasi-Stokes ...