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2022 ◽  
Author(s):  
Atiqah Azhari ◽  
Andrea Bizzego ◽  
Gianluca Esposito

Abstract Parent-child dyads who are mutually attuned to each other during social interactions display interpersonal synchrony that can be observed overtly, in the form of joint behaviours, and biologically, such as through the temporal coordination of brain signals called inter-brain synchrony. Joint play provides ample opportunities for parent-child dyads to engage in matching interactions which not just facilitate the formation of bonds but also alleviate parenting stress in caregivers. Despite the beneficial effects of play on parents and the parent-child relationship, no study has investigated the dyadic neural mechanism by which this occurs. The present functional Near-infrared Spectroscopy (fNIRS) study aimed to examine the association between parenting stress and inter-brain synchrony in the prefrontal cortex of 31 mother-child and 29 father-child dyads while they engaged in shared play for 10 minutes. Shared play was miro-analytically coded into joint (i.e., in-phase matching of dyadic behaviours) and non-joint (i.e., no matching of dyadic behaviours) segments. Inter-brain synchrony was computed using cross-correlations over 15 s, 20 s, 25 s, 30 s and 35 s fixed-length windows of joint and non-joint play segments. Analyses of Covariance revealed that dyads with more parenting stress exhibited greater inter-brain synchrony in the frontal left cluster of the prefrontal cortex, but only for the 35 s fixed-length window. This finding suggests that continuous and positive instances of joint play may disproportionately benefit dyads who reported greater parenting stress, entraining underlying brain activation patterns involved in social cognition. Mother-child dyads also showed greater inter-brain synchrony than father-child dyads, alluding to possible gender differences in the effect of play on dyads. Findings present evidence of a potential dyadic neural pathway by which play benefits the parent-child relationship.


Algorithms ◽  
2021 ◽  
Vol 14 (12) ◽  
pp. 359
Author(s):  
Dmitry Kosolobov ◽  
Daniel Valenzuela

The Lempel-Ziv parsing (LZ77) is a widely popular construction lying at the heart of many compression algorithms. These algorithms usually treat the data as a sequence of bytes, i.e., blocks of fixed length 8. Another common option is to view the data as a sequence of bits. We investigate the following natural question: what is the relationship between the LZ77 parsings of the same data interpreted as a sequence of fixed-length blocks and as a sequence of bits (or other “elementary” letters)? In this paper, we prove that, for any integer b>1, the number z of phrases in the LZ77 parsing of a string of length n and the number zb of phrases in the LZ77 parsing of the same string in which blocks of length b are interpreted as separate letters (e.g., b=8 in case of bytes) are related as zb=O(bzlognz). The bound holds for both “overlapping” and “non-overlapping” versions of LZ77. Further, we establish a tight bound zb=O(bz) for the special case when each phrase in the LZ77 parsing of the string has a “phrase-aligned” earlier occurrence (an occurrence equal to the concatenation of consecutive phrases). The latter is an important particular case of parsing produced, for instance, by grammar-based compression methods.


2021 ◽  
Vol 18 ◽  
pp. 100286
Author(s):  
Jacob Ricker ◽  
Kevin O. Douglass ◽  
Jay Hendricks ◽  
Sarah White ◽  
Sergei Syssoev

2021 ◽  
Author(s):  
Xiaoxu Shi ◽  
Martin Werner ◽  
Carolin Krug ◽  
Chris M. Brierley ◽  
Anni Zhao ◽  
...  

Abstract. Numerical modelling enables a comprehensive understanding not only of the Earth's system today, but also of the past. To date, a significant amount of time and effort has been devoted to paleoclimate modeling and analysis, which involves the latest and most advanced Paleoclimate Modelling Intercomparison Project phase 4 (PMIP4). The definition of seasonality, which is influenced by slow variations in the Earth's orbital parameters, plays a key role in determining the calculated seasonal cycle of the climate. In contrast to the classical calendar used today, where the lengths of the months and seasons are fixed, the angular calendar calculates the lengths of the months and seasons according to a fixed number of degrees along the Earth's orbit. When comparing simulation results for different time intervals, it is essential to account for the angular calendar to ensure that the data for comparison is from the same position along the Earth's orbit. Most models use the classical "fixed-length" calendar, which can lead to strong distortions of the monthly and seasonal values, especially for the climate of the past. Here, by analyzing daily outputs from multiple PMIP4 model simulations, we examine calendar effects on surface air temperature and precipitation under mid-Holocene, last interglacial, and pre-industrial climate conditions. We conclude that: (a) The largest cooling bias occurs in autumn when the classical calendar is applied for the mid-Holocene and last interglacial. (b) The sign of the temperature anomalies between the Last Interglacial and pre-industrial in boreal autumn can be reversed after the switch from classical to angular calendar, particularly over the Northern Hemisphere continents. (c) Precipitation over West Africa is overestimated in boreal summer and underestimated in boreal autumn when the "fixed-length" seasonal cycle is applied. (d) Finally, correcting the calendar based on the monthly model results can reduce the biases to a large extent, but not completely eliminate them. In addition, we examine the calendar effects in 3 transient simulations for 6–0 ka by AWI-ESM, MPI-ESM, and IPSL. We find significant discrepancies between adjusted and unadjusted temperature values over ice-free continents for both hemispheres in boreal autumn. While for other seasons the deviations are relatively small. A drying bias can be found in the summer monsoon precipitation in Africa (in the "fixed-length" calendar), whereby the magnitude of bias becomes smaller over time. Overall, our study underlines the importance of the application of calendar transformation in the analysis of climate simulations. Neglecting the calendar effects could lead to a profound artificial distortion of the calculated seasonal cycle of surface air temperature and precipitation. One important fact to be noted here is that the discrepancy in seasonality under different calendars is an analysis bias and is highly depends on the choice of the reference position/date (usually the vernal equinox, which is set to 31th March) on the Earth's ellipse around the sun. Different model groups may apply different reference dates, so ensuring a consistent reference date and seasonal definition is key when we compare results across multiple models.


2021 ◽  
Author(s):  
Giulia Cervia ◽  
Tobias J. Oechtering ◽  
Mikael Skoglund
Keyword(s):  

2021 ◽  
Author(s):  
Xin Song ◽  
Yurong Liao ◽  
Zhe Zhang ◽  
Shuyan Ni ◽  
Tuofeng Lei
Keyword(s):  

2021 ◽  
Vol 27 (10) ◽  
pp. 531-541
Author(s):  
G. N. Zhukova ◽  
◽  
M. V. Ulyanov ◽  
◽  

The problem of constructing a periodic sequence consisting of at least eight periods is considered, based on a given sequence obtained from an unknown periodic sequence, also containing at least eight periods, by introducing noise of deletion, replacement, and insertion of symbols. To construct a periodic sequence that approximates a given one, distorted by noise, it is first required to estimate the length of the repeating fragment (period). Further, the distorted original sequence is divided into successive sections of equal length; the length takes on integer values from 80 to 120 % of the period estimate. Each obtained section is compared with each of the remaining sections, a section is selected to build a periodic sequence that has the minimum edit distance (Levenshtein distance) to any of the remaining sections, minimization is carried out over all sections of a fixed length, and then along all lengths from 80 to 120 % of period estimates. For correct comparison of fragments of different lengths, we consider the ration between the edit distance and the length of the fragment. The length of a fragment that minimizes the ratio of the edit distance to another fragment of the same length to the fragment length is considered the period of the approximating periodic sequence, and the fragment itself, repeating the required number of times, forms an approximating sequence. The constructed sequence may contain an incomplete repeating fragment at the end. The quality of the approximation is estimated by the ratio of the edit distance from the original distorted sequence to the constructed periodic sequence of the same length and this length.


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