15 research outputs found
Description of the idealized bed roughness effects on tracer transport in water flumes by applying the strange attractor multifractal analysis
River hydrodynamicsTurbulent open channel flow and transport phenomen
A sliding window-based algorithm for faster transformation of time series into complex networks
A new alternative method to approximate the Visibility Graph (VG) of a time
series has been introduced here. It exploits the fact that most of the nodes in
the resulting network are not connected to those that are far away from them.
This means that the adjacency matrix is almost empty, and its nonzero values
are close to the main diagonal. This new method is called Sliding Visibility
Graph (SVG). Numerical tests have been performed for several time series,
showing a time efficiency that scales linearly with the size of the series
[O(N)], in contrast to the original VG that does so quadratically [O(N2)]. This
fact is noticeably convenient when dealing with very large time series. The
results obtained from the SVG of the studied time series have been compared to
the exact values of the original VG. As expected, the SVG outcomes converge
very rapidly to the desired ones, especially for random and stochastic series.
Also, this method can be extended to the analysis of time series that evolve in
real time, since it does not require the entire dataset to perform the analysis
but a shorter segment of it. The length segment can remain constant, making
possible a simple analysis as the series evolves in time.Comment: 33 pages, 8 figure
Checking complex networks indicators in search of singular episodes of the photochemical smog
A set of indicators derived from the analysis of complex networks have been
introduced to identify singularities on a time series. To that end, the
Visibility Graphs (VG) from three different signals related to photochemical
smog (O3, NO2 concentration and temperature) have been computed. From the
resulting complex network, the centrality parameters have been obtained and
compared among them. Besides, they have been contrasted to two others that
arise from a multifractal point of view, that have been widely used for
singularity detection in many fields: the Holder and singularity exponents
(specially the first one of them). The outcomes show that the complex network
indicators give equivalent results to those already tested, even exhibiting
some advantages such as the unambiguity and the more selective results. This
suggest a favorable position as supplementary sources of information when
detecting singularities in several environmental variables, such as pollutant
concentration or temperature.Comment: 32 pages, 7 figure
Multifractal detrended fluctuation analysis of rainfall time series in the Guadeloupe archipelago
Due to the vulnerability of the Caribbean islands to the climate change
issue, it is important to investigate the behavior of rainfall. In addition,
the soil of the French West Indies Islands has been contaminated by an
insecticide (Chlordecone) whose decontamination is mainly done by drainage
water. Thus, it is crucial to investigate the fluctuations of rainfall in these
complex environments. In this study, 19 daily rainfall series recorded in
different stations of Guadeloupe archipelago from 2005 to 2014 were analyzed
with the multifractal detrended fluctuation analysis (MF-DFA) method. The aim
of this work is to characterize the long-range correlations and multifractal
properties of the time series and to find geographical patterns over the three
most important islands. This is the first study that addresses the analysis of
multifractal properties of rainfall series in the Caribbean islands. This
region is typically characterized by the almost constant influence of the trade
winds and a high exposure to changes in the general atmospheric circulation. 12
stations exhibit two different power-law scaling regions in rainfall series,
with distinct long-range correlations and multifractal properties for large and
small scales. On the contrary, the rest of stations only show a single region
of scales for relatively small scales. Hurst exponents reveal persistent
long-range correlations. In the most eastern analyzed areas, larger scales
exhibit higher persistence than smaller scales, which suggests a relationship
between persistence and the highest exposure to the trade winds. Stronger
conclusions can be drawn from multifractal spectra, which indicate that most
rainfall series have a multifractal nature with higher complexity and degree of
multifractality at the smallest scales. Furthermore, a clear dependence of
multifractal nature on the latitude is revealed.Comment: 43 pages. 11 figure
Improving graph-based detection of singular events for photochemical smog agents
Recently, a set of graph-based tools have been introduced for the
identification of singular events of O3, NO2 and temperature time series, as
well as description of their dynamics. These are based on the use of the
Visibility Graphs (VG). In this work, an improvement of the original approach
is proposed, being called Upside-Down Visibility Graph (UDVG). It adds the
possibility of investigating the singular lowest episodes, instead of the
highest. Results confirm the applicability of the new method for describing the
multifractal nature of the underlying O3, NO2, and temperature. Asymmetries in
the NO2 degree distribution are observed, possibly due to the interaction with
different chemicals. Furthermore, a comparison of VG and UDVG has been
performed and the outcomes show that they describe opposite subsets of the time
series (low and high values) as expected. The combination of the results from
the two networks is proposed and evaluated, with the aim of obtaining all the
information at once. It turns out to be a more complete tool for singularity
detection in photochemical time series, which could be a valuable asset for
future research.Comment: 35 pages, 7 figure
Visibility graphs of ground-level ozone time series: A multifractal analysis
A recent method based on the concurrence of complex networks and multifractal
analyses is applied for the first time to explore ground-level ozone behavior.
Ozone time series are converted into complex networks for their posterior
analysis. The searched purpose is to check the suitability of this
transformation and to see whether some features of these complex networks could
constitute a preliminary analysis before the more thorough multifractal
formalism. Results show effectively that the exposed transformation stores the
original information about the ozone dynamics and gives meaningful knowledge
about the time series. Based on these results, the multifractal analysis of the
complex networks is performed. Looking at the physical meaning of the
multifractal properties (such as fractal dimensions and singularity spectrum),
a relationship between those and the degree distribution of the complex
networks is found. In addition to all the promising results, this novel
connection between time series and complex networks can deal with both
stationary and non-stationary time series, overcoming one of the main
limitations of multifractal analysis. Therefore, this technique can be regarded
as an alternative to give supplementary information within the study of complex
signals.Comment: 34 pages, 8 figures, 1 graphical abstrac
Can complex networks describe the urban and rural tropospheric O3 dynamics?
Tropospheric ozone (O3) time series have been converted into complex networks
through the recent so-called Visibility Graph (VG), using the data from air
quality stations located in the western part of Andalusia (Spain). The aim is
to apply this novel method to differentiate the behavior between rural and
urban regions when it comes to the ozone dynamics. To do so, some centrality
parameters of the resulting complex networks have been investigated: the
degree, betweenness and shortest path. Some of them are expected to corroborate
previous works in order to support the use of this technique; while others to
supply new information. Results coincide when describing the difference that
tropospheric ozone exhibits seasonally and geographically. It is seen that
ozone behavior is fractal, in accordance to previous works. Also, it has been
demonstrated that this methodology is able to characterize the divergence
encountered between measurements in urban environments and countryside. In
addition to that, the promising outcomes of this technique support the use of
complex networks for the study of air pollutants dynamics. Particularly, new
nuances are offered such as the identification and description of singularities
in the signal.Comment: 27 pages, 7 figures, 1 graphical abstrac
Multiplex Visibility Graphs as a complementary tool for describing the relation between ground level O3 and NO2
The usage of multilayer complex networks for the analysis of correlations
among environmental variables (such as O3 and NO2 concentrations from the
photochemical smog) is investigated in this work. The mentioned technique is
called Multiplex Visibility Graphs (MVG). By performing the joint analysis of
those layers, the parameters named Average Edge Overlap and Interlayer Mutual
Information are extracted, which accounts for the microscopical time coherence
and the correlation between the time series behavior, respectively. These
parameters point to the possibility of using them independently to describe the
correlation between atmospheric pollutants (which could be extended to
environmental time series). More precisely the first one of them is considered
to be a potential new approach to determine the time required for the
correlation of NO2 and O3 to be observed, since it is obtained from the
correlation of the pollutants at the smallest time scale. As for the second
one, it has been checked that the proposed technique can be used to describe
the variation of the correlation between the two gases along the seasons. In
short, MVGs parameters are introduced and results show that they could be
potentially used in a future for correlation studies, supplementing already
existing techniques.Comment: 29 pages, 7 figure
Joint multifractal analysis of air temperature, relative humidity and reference evapotranspiration in the middle zone of the Guadalquivir river valley
Previous works have analysed the relationship existing between reference
evapotranspiration (ET0) and other climatic variables under a one-at-a-time
perturbation condition. However, due to the physical relationships between
these climatic variables is advisable to study their joint influence on ET0.
The box-counting joint multifractal algorithm describes the relations between
variables using relevant information extracted from the data singularities.
This work investigated the use of this algorithm to describe the simultaneous
behaviour of ET0, calculated by means of Penman-Monteith (PM) equation, and
relative humidity (RH) and air temperature (T), influencing on it in the middle
zone of the Guadalquivir river valley, Andalusia, southern Spain. The studied
cases were grouped according to the fractal dimension values, which were
related to their probability of occurrence. The most likely cases were linked
to smooth behaviour and weak dependence between variables, both circumstances
were detected in the local multifractal analysis. For these cases, the rest of
Penman Monteith (PM) equation variables, neither the T nor the RH, seemed to
influence on ET0 determination, especially when low T values were involved. By
contrast, the least frequent cases were those with variables showing high
fluctuations and strong relationship between them. In these situations, when T
is low, the ET0 is affected by the rest of PM equation variables. This fact
confirmed T as main driver of ET0 because the higher T values the lesser
influence of other climate variables on ET0. Joint multifractal analysis shows
some limitations when it is applied to large number of variables, the results
reported are promising and suggest the convenience of exploring the
relationships between ET0 and other climatic variables not considered here with
this framework such as wind speed and net radiation.Comment: 40 pages, 10 figure