"Natural time" is a new view of time introduced in 2001 that is not continuous, in contrast to conventional time which is in the continuum of real numbers, but instead its values form countable sets as natural numbers.
Definition
In natural time domain each event is characterized by two terms, the "natural time", and the energy. is defined as, where k is a natural number and is the total number of events in the time sequence of data. A related term,, is the ratio, which describes the fractional energy released. The term is the variance in natural time:
Time reversal, in contrast to clock time, is applicable when studying the approach of a system to criticality with natural time analysis. Living systems for example are considered to operate far from equilibrium as there is flow of energy crossing their boundaries, in contrast to deceased organisms where inner driving forces are absent. While time irreversibility is a fundamental property of a living system, the state of death is more time reversible by means of energy flow across the system's boundaries. Thus a critical state of a system can be estimated by applying natural time analysis upon calculating the entropy upon both normal time flow and time reversal and studying the difference of the two results.
Applications
Seismology
Earthquake nowcasting
In seismology, nowcasting is the estimate of the current dynamic state of a seismological system. It differs from forecasting which aims to estimate the probability of a future event but it is also considered a potential base for forecasting. Nowcasting is based on the earthquake cycle model, a recurring cycle between pairs of large earthquakes in a geographical area, upon which the system is evaluated using natural time. Nowcasting calculations produce the "earthquake potential score", an estimation of the current level of seismic progress. When applied to seismicity, natural time has the following advantages:
Declustering of the aftershocks is not necessary as natural time count is evenly valid in any case of aftershock or backgroung seismicity.
Natural time statistics do not depend on the level of seismicity, given that the b value does not significantly vary.
Typical applications are: great global earthquakes and tsunamis, aftershocks and induced seismicity, induced seismicity at gas fields, seismic risk to global megacities, studying of clustering of large global earthquakes, etc.
Earthquake prediction
Natural time analysis has been initially applied to VAN method in order to improve the accuracy of the estimation of the time of a forthcoming earthquake that has been indicated to occur by seismic electric signals. The method deems SES valid when κ1 = 0.070. Once the SES are deemed valid, a second NT analysis is started in which the subsequent seismic events are noted, and the region is divided up as a Venn diagram with at least two seismic events per overlapping rectangle. When κ1 approaches the value κ1 = 0.070 for the candidate region, a critical seismic event is considered imminent, i.e. it will occur in a few days to one week or so.
Cardiology
Natural time analysis has been experimentally used for the diagnosis of heart failure syndrome as well as identifying patients at high risk for sudden cardiac death, even when measuring solely the heart rate, either using electrocardiography or far more inexpensive and portable equipment.
Economy
Due to similarities of the dynamic characteristics between earthquakes and financial markets, natural time analysis, which is primirily used in seismology, was chosen to assist in developing winning strategies in financial markets, with encouraging results.
