Discrete GIS data refers to geographic data that only exists in specific locations, rather than being continuous across an entire area.
Discrete data is characterized by having well-defined boundaries, particularly for polygon data. This means that the data is constrained within certain limits and does not extend indefinitely.
Examples of discrete GIS data include point and line data, such as the location of trees, rivers, and streets. These data types are inherently discrete because they occur at specific locations and are not continuous across the landscape.
Discrete GIS data can be contrasted with continuous GIS data, which is data that varies smoothly across space without any well-defined boundaries. An example of continuous data might be temperature or elevation measurements.
Discrete GIS data is particularly useful for mapping specific features, such as infrastructure or natural resources, that are present in limited, specific locations. By contrast, continuous data is more useful for identifying patterns and trends across a larger area.
Discrete GIS data can be represented in various ways, including as points, lines, and polygons, depending on the nature of the data and the purpose of the mapping. For example, roads might be represented as lines, while individual trees might be represented as points.
Continuous GIS data is geographic data that varies smoothly across space without any well-defined boundaries, in contrast to discrete data which is constrained to specific locations.
Examples of continuous GIS data include elevation, slope, temperature, precipitation, and other environmental or climatic measurements that vary continuously across the landscape.
Every point on a map made with continuous GIS data will contain a value, indicating the value of the measured variable at that location.
Unlike discrete data, which has well-defined boundaries, continuous data is characterized by a lack of clear limits or borders between different values. Instead, the values vary smoothly across space, with no abrupt changes or discontinuities.
Continuous GIS data is particularly useful for identifying patterns and trends across a larger area, such as mapping the distribution of rainfall or temperature across a region.
Continuous data can be contrasted with discrete GIS data, which is data that only exists in specific locations and is characterized by well-defined boundaries.
Continuous GIS data can be represented in various ways, including as contour lines, heat maps, and color-coded surfaces, depending on the nature of the data and the purpose of the mapping.
GIS analysts use various tools and methods to process, analyze, and visualize continuous GIS data, including statistical methods, interpolation, and spatial analysis techniques.
Most ArcGIS applications use discrete geographic information, which is characterized by well-defined boundaries and specific locations. Examples include landownership, soils classification, zoning, and land use.
Discrete data is typically represented by nominal, ordinal, interval, and ratio values, depending on the nature of the data and the level of measurement.
Nominal data is data that cannot be ranked or ordered, such as landownership or soil type. Ordinal data is data that can be ranked, but the differences between the values are not necessarily equal, such as zoning categories.
Interval data is data where the differences between values are meaningful and can be measured, but there is no true zero point, such as temperature measurements. Ratio data is data where there is a true zero point, such as weight or height.
Surfaces, on the other hand, are continuous data that vary smoothly across space without any well-defined boundaries. Examples of surfaces include elevation, rainfall, pollution concentration, and water tables.
Continuous data can be represented in various ways, such as contour lines, heat maps, and color-coded surfaces, depending on the nature of the data and the purpose of the mapping.
GIS analysts use various tools and methods to process, analyze, and visualize both discrete and continuous GIS data, including statistical methods, interpolation, and spatial analysis techniques.
1. Principles Thermal Infrared Remote Sensing is based on the detection of naturally emitted electromagnetic radiation from objects, rather than reflected solar energy. According to Planck's Radiation Law , all objects with a temperature above absolute zero (0 K) emit electromagnetic radiation. For Earth surface features, the peak emission lies in the Thermal Infrared (TIR) region of 3–14 μm of the electromagnetic spectrum. The amount of radiation emitted is primarily a function of surface temperature and emissivity . Sensors measure the radiant energy flux density (W/m²) , which is later converted to surface temperature using Stefan-Boltzmann's Law . 2. Radiation Properties in TIR Emissivity (ε): Ratio of radiation emitted by a surface to that emitted by a perfect blackbody at the same temperature. Natural surfaces like water (ε ≈ 0.98) have high emissivity, while bare soils and metals have lower values. Blackbody: An idealized object th...
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