Time is a fundamental concept in geography and many other disciplines. This article introduces time at three levels. At the philosophical level, the article reviews various notions on the nature of time from early mythology to modern science and reveals the dual nature of reality: external (absolute, physical) and internal (perceived, cognitive). At the analytical level, it introduces the measurement of time, the two frames of temporal reference: calendar time and clock time, and the standard time for use globally. The article continues to discuss time in GIS at the practical level. The GISystem was first created as a “static” computer-based system that stores the present status of a dynamic system. Now, GISystems can track and model the dynamics in geographical phenomena and human-environment interactions. Representations of time in dynamic GISystems adopt three perspectives: discrete time, continuous time and Minkowski’s spacetime, and three representations: ordinal, interval, and cyclical. The appropriate perspective and representation depend on the observed temporal patterns, which can be static, oscillating, chaotic, or stochastic. Recent progress in digital technology brings us opportunities and challenges to collect, manage and analyze spatio-temporal data to advance our understanding of dynamical phenomena.
Song, Y. (2019). Time. The Geographic Information Science & Technology Body of Knowledge (4th Quarter 2019 Edition), John P. Wilson (ed.). DOI: 10.22224/gistbok/2019.4.7.
This topic considers time in three different levels. At the conceptual level, we review various notions on the nature of time from early mythology to modern science. At the analytical level, we discuss the measurement of time and introduces the common and universal frames of temporal references. At the practical level, we cover the representation and use of time in GIS to monitor and model the “dynamics” in geographical phenomena and human-environment interactions. Considering recent advance in digital technology, we consider collection, management, and analysis of spatio-temporal data in GIS and highlights the role and significance of time.
Time is a fundamental concept in geography and many other disciplines. However, the nature of time has long been an open question. Peuquet (2002) in her Representation of Space and Time has reviewed the notions on the nature of time from early mythology to modern science. In sum, these notions are either phenomenological or mathematical, and they are tightly related to human exploration and interpretation of the universe. This section selects and summarizes some notions to advance our understanding of modern representations of time.
The earliest notions on time is from Greek mythology and everyday life. In Greek myth, time is so important that it is personified as Kronos in Hesiod’s Theogony (a.k.a. the god of time, Father Time) (Hesiod 1999). Human sense and perceive time through generation and power successions and an overall forward-moving revolution from Chaos to Cosmos. In this case, time is embedded in multiple linear processes and referenced by discrete events. Hence, time has a discontinuous and sequential nature. During the same periods, human also develop the cyclical view of time to reflect their observations of the nature and their everyday life. In Hesiod’s Works and Days, time is perceptible at various scales: human activities during days and nights, natural events across the seasons, different stages of life, and the repetition of historical events (Richardson 1877, Tandy and Neale 1996). This cyclical, non-linear notions on time are also evidenced in Indian and East Asian philosophy. For instance, Radhakrishnan and Moore (2014) in the book A Source Book in Indian philosophy discusses the movement of the world and argues that “All the systems accept the view of the great world rhythm. Vast periods of creation, maintenance and dissolution follow each other in endless succession”. Chinese philosophy, and Taoist in particular, is deeply rooted in cyclical view of time and considers the universe as an infinity of nesting time cycles (Schipper and Hsiu-huei 1986). These earliest notions on time are phenomenological, primarily relying on the believes or observations of existences and evolutions of the universe (Peuquet 2002).
During the Presocratic period, there has been an increasing interest in mathematics and physics, including questions surrounding divisibility of space, time and matter. Anaxagoras introduce the infinite divisibility through his conception of unlimited smallness: “For of the small there is no smallest, but always a smaller” (Curd 2015). In contrast, atomism decomposes everything into infinitely small and separate partials (atoms) with space as their container (void). Built upon the atomism, Plato regarded time as the moving image of eternity and then distinguished Being and Becoming (Cornford 2014). In Plato’s view, the world of Becoming is the world we perceive through our senses, and this sensible world is always changing. The world of Being is absolute and never changes, yet it causes the essential nature of things (forms) we apprehend in the world of Becoming. Hence, Plato’s notion indicated the numerical and discrete nature of time: time can be measured through the perceived revolution of the universe (at the moment, now and here).
Aristotle, a student of Plato, developed the famous conception of “space as place”: objects are located in some place; therefore, place coexists together with objects and is a necessary condition for the existence of objects (Markosian 2016). Based on this conception, Aristotle agreed with the continuous views on time and rejected the notion of atoms and void that may lead to gaps and emptiness. In Aristotle’s view, a moment was not an element of discontinuity. Instead, a moment linked the successive temporal durations and preserved the continuity of time. Beside, Aristotle developed a cosmological model that consists a finite space with two levels – the earthly and the celestial (Peuquet, 2002). The time in the Aristotelian model is infinite and, just like the space, is equally present everywhere. Aristotle’s notions on space have been dominated for 2,000 years.
The realization of the Earth as an ellipsoid can date to the 17th century, as described by Newton in his Principia (Newton 1962). Here, Newton’s notions on space and time are similar to Plato’s notions because they both distinguished the absolute and relative space and time. The Principia distinguished “absolute and relative, true and apparent, mathematical and common” time:
Based on the notions on absolute space and time, Newton developed laws of motion that connect space, time and bodies (objects) and described the motion of bodies (Friedman 2014). Although the laws of motion were originated from Physics, they have much broader impacts: they lead to a move from the cognitively centered view that relies merely on the abstraction of observations to the positivistic view that relies on the objective descriptions through the process of measurement and mathematical formulation.
During 1880s and 1890s, several experiments on light (an electromagnetic phenomenon) showed that light always traveled with the same speed, regardless how fast the light source moves. These experiments conflicted with Newton’s laws of motion and were the basis for Einstein’s theory of relativity. In Einstein’s view, space and time are relative, and they depend on the motion of the observer who measures them. Light is more fundamental than space and time: the speed of light in a vacuum is the same for all observers, regardless of the observer’s motion or of the motion of the light source. Consequently, space and time are no longer absolute and independent: “matter tells spacetime how to curve, and curved spacetime tells matter how to move”. (Friedman 2014)
In 1908, Minkowski proposed the concept of four-dimensional spacetime that integrated space and time (Stein 1968). In this topic, the terms spacetime, space-time, and spatio-temporal indicate the integration of space and time, terms used here based on existing literatures. In the spacetime, as a flash of light passes from the past to the future, the “present” is defined. All physical reality must be contained within “future” and “past” spacetime, and the “outside” is inaccessible because bodies must travel faster than light to reach it (which is impossible). A moving trajectory of an observer results in a “worldline” inside the future and past spacetime. The spacetime later becomes an essential foundation to Einstein’s theory of general relativity discussed above.
The acquisition and arrangement of knowledge are inevitably relied on our sensory experiences. Despite the debates on absolute or relative, and continuous or discrete nature of space and time, space and time lay the innate and intuitive basis for us to sense and perceive the world. In other words, cognitive interpretations of space and time are built upon the awareness of their existence. This view was first proposed by Kant in his principle of “subjective a prior” (Kant 1955) and has been extensively studied later in the field of cognitive psychology. It agreed with the dual nature of reality: both external (absolute, physical) and internal (perceived, interpreted, cognitive), and considered space and time as the context for us to perceive, understand and represent the reality.
This section considers time as an essential part of reference frames for us to observe and measure the reality. First, this section introduces calendar time and clock time as the two most commonly used frames in accord with two distinct ways we observe and measure the external physical time. Then, this section introduces the standard time as the universal reference for used internationally.
3.1 Calendar Time and Clock Time
The calendar is a measurement system that organizes intervals of time at various levels and give them names for social, religious, commercial and administrative purposes. Calendars are based on the perceived motions of the Moon and the Sun in relate to the Earth, the rotation of the Earth, and the interpreted cyclitic view of time. The basic measurement units include:
The clock is a physical mechanism that measure duration and elapsed time that are shorter than natural units in calendars. For instance, a sundial uses a gnomon to cast a shadow of sunlight on a set of markings to indicate local time (in hours) within one day. The water clock, the hourglass and the pendulum clock are all driven by the gravity of the Earth and used to indicate hours in a day and even minutes in an hour. The most accurate device nowadays are atomic clocks that use the frequency of electronic transitions in certain atoms as the basis to define the second (within a minute). The International System of Units (SI) defines second based on the 133Cs atom and has used it as the basic unit of time since 1967. Beyond second, the smallest time interval that can be measured directly, as of Nov. 2016, is on the order of 850 zeptoseconds (850×10−21 seconds).
3.2 Standard Time
Since the industrial evolution, a universal understanding and agreement on the measurement of time has become increasingly necessary. In 1847, Greenwich Mean Time (GMT) was developed as the first standard time for use by the British railways, navy, and shipping industry. GMT was defined by the mean solar time at the Royal Observatory, Greenwich in the UK. Using GMT as the foundation, 41 nations officially agreed to a universal time at the 1884 International Meridian Conference. Meanwhile, the Greenwich meridian was commonly used as the Prime Meridian.
In 1963, the Coordinated Universal Time was first officially adopted as the standard time, and its abbreviation UTC was first officially adopted in 1967. Since then, the system has been adjusted several times. The current version of UTC is based on Temps Atomique International (TAI) and adjusted by leap seconds considering that Earth’s rotation is slowing. Here, days are identified by the Gregorian calendar, seconds are SI seconds, and minutes and hours are adjusted to reflect the irregular day lengths. Time zones are regions with the same standard time used locally for legal, commercial and social purposes. Hence, these time zones tend to follow the country boundaries and the subdivisions of each country. The time zones are described as positive or negative offsets from UTC in whole hours (e.g. UTC+08:00, UTC-06:00) and may have some other conventional names (e.g. Beijing Time, Chicago Time). Some of the time zones located at higher latitudes also adopt Daylight Saving Time (DST).
The Global Positioning System (GPS) time is implemented by atomic clocks that started timing at midnight on Jan. 6th, 1980 (UTC00:00). The GPS time is transmitted as the number of weeks spent since the start time and the number of seconds since the beginning of the current week. The GPS time is always 19 seconds behind the TAI time; and conversions between the GPS time and the UTC time need to account for the leap seconds (TAI=GPS+19s=UTC+LS).
The discussions in this section reveal that (1) the temporal frames of reference are either cyclical or linear; (2) some universal measurement units of time include second, minute, hour, day, week (weekdays), month, and year, (3) the smallest time interval that can be measured directly exists and determined the precision of measurement, and (4) the time intervals have various temporal relationships to describe their relative “locations” in time (e.g. the TAI time is 19 seconds after the GPS time). The next section will adopt these views and discuss how time is conceptualized, represented and used in Geographic Information Systems (GISystems) and GIScience.
The first GISystem was known as the Canada Geographic Information System (CGIS) developed by Dr. Roger Tomlinson in 1968 to collect, store, analyze and distribute the data collected for the Canada Land Inventory. The information in the system may be added to or modified over time, but these changes may not be necessarily maintained. Therefore, the CGIS is “static” per se and focuses only on the world in the Present (Here and Now). However, the world is ever-changing, and our knowledge of the world is evolving. This requires us to choose appropriate perspective and representation of time in order to investigate the dynamics of geographical phenomena and human-environment interactions. This section introduces the three perspectives on time, the three representations of time, and the four types of temporal patterns in the dynamical GISystems. The section also discusses how the observed temporal patterns determine the appropriate perspective and representation of time. Please note that the perspectives and representations of time are built upon conceptual notions and analytical measurements on time discussed earlier.
4.1 Discrete Time, Continuous Time, and Spacetime
The dynamics of geographical phenomena are results from changes in locations, entities, or both. A change is considered as an event if it is perceivable, measurable and significant for the field of study (e.g. a change in the ownership of a land parcel). The representation of changes and events relies on different views on time and its relationship to space as well as the practical needs. The three main views on time (conceptually) are discrete time, continuous time and spacetime.
As discussed in Section 3, time was treated as a dimension independent from space and viewed as discrete or continuous before Minkowski. In the discrete view, we observe a phenomenon and its state at given points in time and then compare the observed states at different time (points) to understand the process. In the continuous view, we observe and compare a phenomenon and its state at the start and end of each period of time, which is usually associated with the lifetime of an entity/event. For instance,
The third view on time adopts Minkowski’s four-dimensional spacetime. In the spacetime view, we observe changes in space and time simultaneously instead of changes over time. For instance,
Figure 1. Space-time paths with constraints of three family members in a weekday. Source: author; after Ellegård and Lenntorp (1993).
4.2 Ordinal, Interval, and Cyclical Time
While observing dynamic phenomena, we can adopt different representations of time. The most common three representations are ordinal time, interval time and cyclical time. They reflect how we perceive time and temporal relationships.
Figure 2. Temporal relationships between time intervals. Source: author, after Allen (1984).
4.3 Static, Oscillating, Chaotic, and Stochastic Temporal Patterns
The world is a dynamic system that is changing and evolving, and so are the natural systems and our interactions with them. Behaviors of these dynamic systems lead to the temporal patterns we observe and affect how we conceptualize and represent time. The behaviors of dynamic system can be categorized into four classes (Wolfram 1984), and this section discusses the appropriate views and representations of time for each class.
4.4 Spatio-Temporal Data Collection, Management, and Analysis
Advances in digital technology allow us to collect massive spatio-temporal data, derive useful information and advance our knowledge about the “dynamics” in geographical phenomena and human-environment interactions. This section focuses on the temporal aspect and discusses the collection, management, and analysis of spatio-temporal data.
Beside satellite images, location-aware devices such as smartphone can collect geographical locations of mobile objects at discrete time stamps. The temporal resolution of data collected by these devices is determined by the navigation satellite system that sends signals (e.g. GPS, Galileo, BeiDou). For instance, navigation messages of the Global Positioning System (GPS) have a resolution of 1.5 seconds. The devices (receivers) also have their own frequencies to receive or transmit signals. For instance, Automatic Vehicle Location (AVL) systems usually track vehicles locations every 30 seconds to 2 minutes to support the management of transit fleet and the evaluation of transit performance (Tilocca et al. 2016).
Other types of spatio-temporal data such as census and land-use survey usually have much lower temporal resolution, which are determined by how frequent the data is collected and published by the corresponding agencies. For instance, the U.S. Constitution requires that a census of the population should be taken every 10 years, while the American Community Survey (ACS) provides 1-year, 3-year and 5-year estimates within the 10 years. For human mobility at higher temporal resolutions (e.g. hourly, daily), recent studies have applied data collected by mobile devices and location-based services (e.g. Gonzalez et al. 2008, Hasan et al. 2013, Greenblatt and Shaheen 2015).
Modeling Approaches | Modeling Approaches | Modeling Approaches |
---|---|---|
Snapshot method | Semantic-based | Moving Objects |
Time-stamping | Event-based | Graphs-based |
Base state amendment vectors | Process-based | Lifespan-based |
Space-time composite model | Ontology-based | Agents-based |
Domain-based modeling | Feature-based (entity-based) | Kinematics |
Object-oriented | Identify-based | Ontological foundations |
Conceptual modeling extensions |
Visual exploratory analysis can provide some preliminary knowledge about dynamic patterns and support further quantitative analysis and modeling of the temporal patterns. Statistics and data mining are two common approaches. Statistics focus on hypothesis test and goodness of fit from mathematical perspective, while machine learning focuses on algorithms and models from computational perspective. Cressie and Wikle (2015) introduce existing spatio-temporal statistical methods in their book Statistics for Spatio-Temporal Data. Some of these methods are exploratory such as spatio-temporal LISA (Local Indicator of Spatial Association). Some methods examine the spatio-temporal covariance (e.g. Taylor’s frozen turbulence hypothesis that relates temporal to spatial fluctuations in the turbulent flows). And some methods rely on the hierarchical modeling of time series, which are known as hierarchical dynamical spatio-temporal models (DSTM) (e.g. reduced-dimension DSTM for long-lead forecasting of tropical pacific sea surface temperatures).
Compared to statistical analysis and modeling, data mining focuses on extracting interesting patterns and associations instead of investigating the correlation/causality, and contains three phases: training, test and validation (Fayyad et al. 1996). For data with spatial and temporal components, the multi-dimensional nature of the data, the underlying spatial dependencies, and the potential spatio-temporal correlations bring new challenges for spatio-temporal data mining (Shekhar et al. 2010). Studies have developed many data mining methods to advance our understanding of dynamics in physical environments (see, e.g., review by Lausch et al 2015) and human mobility (see, e.g., review by Lin and Hsu 2014). And many programming languages also include packages for data mining such as Scikit-learn in Python (Pedregosa et al. 2011), Weka for Java (Hall et al. 2009), and CLARANS in R (Ng et al. 2002).