The Role of Acoustic Signal Partitions in Listener Categorization of Musical Phrases

1986 ◽  
Vol 4 (2) ◽  
pp. 185-213 ◽  
Author(s):  
Roger A. Kendall

An experiment was designed to assess the relative contribution to listener categorization strategies of various temporal partitions of the acoustic signal for trumpet, clarinet, and violin. The role of context, whole phrase versus single note, was also evaluated. Analog recordings of three folk-song phrases performed on two clarinets, violins, and trumpets were digitized. A computer program was developed for digital signal editing. Signal edit conditions included normal, time-variant steady-state alone, transients alone, and static steady state with and without transients. Musicians and nonmusicians responded to a matching procedure in which unedited signals of one phrase were choice stimuli and edited signals for two different phrases served as models. Two replications of all possible combinations of instrument, phrase, and edit conditions were presented for a total of 72 items. Two additional groups of musicians and nonmusicians participated in an identical procedure in which the stimuli were single notes extracted from two phrases. Analyses revealed that, for the whole-phrase signals, there was no case in which the means obtained with the "normal" signal and the "time variant steady state alone" signal were statistically different; these means were always statistically higher than the "transients alone" mean. It was concluded that transients were neither sufficient nor necessary for the categorization of trumpet, clarinet, and violin in whole-phrase contexts. The time- variant quasi-steady state was sufficient and necessary for the categorization of trumpet and violin phrases, and it was sufficient but not necessary for the categorization of clarinet phrases. For the single- note stimuli, "transients alone" yielded means statistically equivalent to the "normal" and "time variant steady state alone" means. It was concluded that transients were sufficient, but not necessary, for instrument categorization in single-note contexts. The whole-phrase context yielded significantly higher means than the single-note context; music majors performed the task with greater accuracy than nonmusic majors.

1984 ◽  
Vol 64 (5) ◽  
pp. 47-48 ◽  
Author(s):  
M. K. THEODOROU ◽  
D. J. GASCOYNE ◽  
D. E. BEEVER

Anaerobic, forage-containing medium was inoculated with rumen fluid and consecutive batch cultures were established. Microbial communities were maintained and cultures demonstrated quasi-steady-state. The VFA proportions from consecutive batch cultures which were transferred at 3-day intervals were similar to those obtained in vivo. Key words: Microbial ecology, rumen, batch culture


2005 ◽  
Vol 62 (2) ◽  
pp. 542-550 ◽  
Author(s):  
John Persing ◽  
Michael T. Montgomery

Abstract In numerical simulations using an axisymmetric, cloud-resolving hurricane model, hurricane intensity shows quasi-steady-state behavior. This quasi-steady intensity is interpreted as the maximum possible intensity (MPI) of the model. Within the literature, numerical demonstrations have confirmed theoretically anticipated influences on hurricane intensity such as sea surface temperature, outflow temperature, and surface exchange coefficients of momentum and enthalpy. Here these investigations are extended by considering the role of environmental convective available potential energy (CAPE) on hurricane intensity. It is found that environmental CAPE (independent of changes to the outflow level) has no significant influence on numerically simulated maximum hurricane intensity. Within this framework, MPI theories that are sensitive to environmental CAPE should be discarded.


2021 ◽  
Author(s):  
Joel Leonard ◽  
Kelin Whipple

<p>Dynamic climates featuring spatially and temporally variable precipitation patterns are ubiquitous in mountain settings. To understand the role of climate on landscape evolution in such settings, and how climate change-related signals might be translated into the sedimentary realm, this variability must be addressed. Here, we present an analysis of how spatial gradients and temporal changes in rainfall combine to affect both the steady state form and transient evolution of river profiles of large transverse river basins as predicted by the stream power model. Where rainfall is uniform, the stream power model predicts that topographic metrics, like fluvial relief and normalized channel steepness index (k<sub>sn</sub>), vary inversely and monotonically with rainfall at steady state. In contrast, we find that these relationships are more complex and can be inverted in many circumstances, even at steady state, in the presence of orographic rainfall gradients. An important consequence of this is that correlations between average rainfall (climate) and topography are always weaker in catchments that experience rainfall gradients relative to expectations based on uniformly distributed rainfall. Moreover, dispersion caused by rainfall gradients is systematic, varying both with the polarity (i.e., generally increasing vs. decreasing downstream) and intensity of the gradient. Therefore, even in quasi-steady-state, rainfall gradients have the potential to obscure or distort the influence of climate on landscapes if they are not accounted for. In addition, we find that temporal changes in spatially variable rainfall patterns can produce complex erosional and morphological responses that can be contrary to expectations based on the change in mean rainfall. Specifically, enhanced incision and surface uplift may occur simultaneously in different parts of a landscape in a pattern that evolves during the transient response to climate change, complicating prediction of the net erosional and topographic response to climate change. Thus, transient responses to the orographic distribution of rainfall may misleadingly appear inconsistent with erosional or morphological responses expected for a relative change in average climate. Additionally, topographic indications of transient adjustment, even to a dramatic change in orographic precipitation, can be subtle enough that a landscape can appear to be in quasi-steady-state. In such cases, spatial gradients in erosion rate driven by a change in orographic precipitation pattern may be mistakenly interpreted as recording spatial gradients in rock uplift rate, potentially at once obscuring an important influence of climate and misinterpreting tectonic drivers of landscape evolution. Finally, we explore the use of a variant of normalized channel steepness index (k<sub>sn-q</sub>) that is able to incorporate the influence of spatially variable in rainfall based on the stream power model. Importantly, we find that k<sub>sn-q</sub> preforms well to help diagnose and quantify the role of climate acting in a landscape, in particular during transient adjustment to changes in rainfall patterns where the standard channel steepness metric (k<sub>sn</sub>) may be misleading.</p>


2008 ◽  
Vol 45 ◽  
pp. 161-176 ◽  
Author(s):  
Eduardo D. Sontag

This paper discusses a theoretical method for the “reverse engineering” of networks based solely on steady-state (and quasi-steady-state) data.


10.2514/3.895 ◽  
1997 ◽  
Vol 11 ◽  
pp. 306-309 ◽  
Author(s):  
Edwin H. Olmstead ◽  
Edward S. Taylor ◽  
Meng Wang ◽  
Parviz Moin ◽  
Scott K. Thomas ◽  
...  

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