Sustainable Development Practices Using Geoinformatics. Группа авторов

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      2.4.1 Thematic Layers of GHI

       2.4.1.1 AOT, PWV, and Temperature

An illustration of a map showing spatial distribution of (a) AOT at wavelength of 340nanometer, (b) PWV, (c) temperature, (d) field photographs showing emissions of gases from various sources.

      Water vapor has a significant relationship between various components of the hydrological cycle. The PWV is an important parameter of water vapor, which is a measure of the total water vapor contained in a small vertical column extending from the ground surface to the top of the atmosphere. However, the majority of moisture in the atmosphere is contained approximately within the lowest 10,000 ft. Distribution of PWV is a good indicator of the dynamics of circulation systems in the atmosphere. It is also an imperative physical parameter for characterizing the optical properties of atmospheric aerosols that influence the global radiation budget and climate change. At present, PWV is also measured using MICROTOPS-II Sunphotometer of solar intensity at 936 and 1,020 nm. The PWV in the study area exhibits a range of 0.3 to 1.7 cm (Figure 2.3b). It shows variation with high values in industrial areas and low values in forest areas. The high value in industrial areas shows that the humidity near industrial areas is higher as compared to the coal mining, forest, and urban areas.

      Surface temperature is also playing a major role in increasing AOT in the atmosphere. During day time, temperature over the study area in the winter season varies between 12.3°C and 29.5°C (Figure 2.3c). There are some surface mine fires present in this region, which is responsible for increasing the average temperature of the area (Figure 2.3d). The present study revealed that the temperature is found to be higher in the vicinity of industrial areas as compared to the mining, urban, and forest area (Figure 2.3c).

       2.4.1.2 Land Use/Land Cover

      LU/LC is an important indicator of global environmental change that indicates the influence of human activities on the physical environment [30]. Land use (LU) refers to various anthropogenic activities and practices on land, whereas land cover (LC) measures natural vegetation, water-bodies, rock/soil, and natural cover [6]. LU/LC changes have become a central component in current strategies for managing natural resources and monitoring environmental changes.

An illustration of a map showing the Land use and land cover map of South Karanpura Coalfield region.

      2.4.2 Thematic Layers of SVI

Land use/land cover classes Area (km2) % Area
Built-up land 40.24 10.56

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