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Assessment of Land use and Land Cover Change in Shallabugh Wetland of Kashmir Himalaya using LANDSAT TM and LISS IV Satellite Datasets

Ishrat Bashir1 , Farooq A Lone1 , Shafat A Mir1 , Bilal A Beigh3 * and Ikhlaq A Mir2

1 Division of Environmental Sciences, SKUAST-K, Shalimar, Srinagar, Jammu and Kashmir India

2 Centre for Climate Change and Mountain Agriculture (CCMA), SKUAST-K, Shalimar, Srinagar, Jammu and Kashmir India

3 Department of Environmental Science and Limnology, Barkatullah University, Bhopal, Madhya Pradesh India

Corresponding author Email: bilalbeigh658@gmail.com

DOI: http://dx.doi.org/10.12944/CWE.17.3.6

The increase in human activities has highlighted the need to assess land use and land cover in the Shallabugh wetland using LANDSAT TM and LISS IV satellite datasets over a 28-year period from 1990 to 2018. After ground truthing, the images were visually evaluated on screen and seven land use and land cover classes, viz. macrophytic vegetation, mixed plantation, open water, grazing land, agriculture field, built-up area, and vegetable field, were demarcated using Arc-GIS software. Out of a total area of 2552.62 ha, the maximum area was covered by macrophytic vegetation (33.87% and 32.36%) and the minimum area by vegetable field (0.77% and 1.51%) in both the years 1990 and 2018. Over the 28 year time period, land use land cover pattern showed increase in mixed plantation (2.28%), built-up (86.8%) and vegetable field (96.1%), whereas decrease was observed in macrophytic vegetation (4.4%), open water (10.3%), grazing land (28.6%), and agriculture field (2.6%). These remarkable changes were largely attributed to natural and human activities, viz., siltation, plantation and crop cultivation by local people and the construction of residential houses. Shallabugh wetland plays a role as breeding ground for a variety of waterfowl and serves as an important staging and wintering location for migratory avifauna. Land use and land cover change pose a severe threat to the Shallabugh wetland which is one of the most economically important wetland of Kashmir valley.

Human Activities; Land Use Land Cover; Shallabugh wetland; Satellite Datasets

Copy the following to cite this article:

Bashir I, Lone F. A, Mir S. A, Beigh B. A, Mir I. A. Assessment of Land use and Land Cover Change in Shallabugh Wetland of Kashmir Himalaya using LANDSAT TM and LISS IV Satellite Datasets. Curr World Environ 2022;17(3). DOI:http://dx.doi.org/10.12944/CWE.17.3.6

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Bashir I, Lone F. A, Mir S. A, Beigh B. A, Mir I. A. Assessment of Land use and Land Cover Change in Shallabugh Wetland of Kashmir Himalaya using LANDSAT TM and LISS IV Satellite Datasets. Curr World Environ 2022;17(3).


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Article Publishing History

Received: 2022-06-09
Accepted: 2022-09-22
Reviewed by: Orcid Orcid Bushra Praveen
Second Review by: Orcid Orcid Eman H. Khader
Final Approval by: Rui Alexandre Castanho

Introduction 

The Earth's surface is constantly transforming as a result of numerous factors, many of which are anthropogenic in nature.1 Only a small number of landscapes around the world are still in their natural condition.2 According to the 2019 report of Intergovernmental Panel on Climate Change, anthropogenic utilization has had a direct impact on more than 70% of the world's land surface.3 Changes in land use and land cover (LULC) are rapid, dynamic, and widespread, which in turn have adverse consequences for natural ecosystems on a local, regional, and global scale.LULC is an important tool in describing the environment in relation with both natural processes as well as anthropogenic actions.5,6,7,8 LULC change is considered as an important subject matter to study global-change and sustainable development.9,10,11,12,13,14,15 Pollution, degradation, and a catastrophic reduction of wetland ecosystems have resulted from LULC changes in catchment areas during the last five decades. 16,17 Since 1990, approximately 84% of wetlands have undergone ecological change, with 50% of the existing wetlands being lost.18 The LULC changes have a significant impact on the geography of the earth's surface.19 Human beings have been modifying the natural land cover to meet their increasing human needs, viz. economic, social, political, religious, recreation, etc.20

Increased population and allied human activities, particularly deforestation, rapid growth in industries and urbanization, have been found to be the most dominant factors responsible for causing change in LULC.21 Among these factors, increased population growth is thought to be a major factor for causing changes in LULC around the globe.20,22 Rapid population growth causes people to migrate to fragile ecosystems such as wetlands, lakes, and forests, resulting in the expansion of farmland and towns at the expense of natural land cover.20 These changes have a substantial impact on the physical environment as well as the social and economic situations of the people who live there.23 

Ecologists throughout the world are concerned about the negative effects of shifting land use, especially when it comes to aquatic ecosystems.24 To address pressing environmental issues such as wetlands destruction, loss of agricultural fields and wildlife habitats, and unregulated development practices, it is necessary to assess LULC changes in the natural environment.18,25 The study of LULC not only involves analyzing the existing LULC changes, but may also be used to predict future changes.26 Therefore, information on existing LULC is essential for a better understanding of landscape dynamics, better decision-making, and implementation of management strategies to meet the ever-increasing demand for human requirements.27,28,29 

Most of the studies in the early 1970’s were carried out by using exhaustive ground surveys and through the interpretation of aerial photographs.30 Since the 1970’s, numerous satellite systems have been launched to obtain information on the earth’s resources.31 Over the last five decades,32 remote sensing techniques have become an indispensable tool for mapping, analyzing, and monitoring spatial information about natural resources, particularly aquatic ecosystems. The combination of remote sensing and GIS is an effective and powerful tool for studying the spatial and temporal transformation of land cover, as they provide information in less time, at a lower cost, and with higher precision.33,34,34 Most researchers used satellite data to map land use change because of the multi-temporal availability of satellite imagery and the rapid development of image processing software.35,36,37 

Wetlands in the Kashmir Himalayas face a lack of data on their spatial extent and how they have changed over time.38 LULC changes have occurred in the Kashmir Valley during the last five decades as a result of several anthropogenic activities, providing ample opportunity for multiple environmental challenges.39 An unparalleled rate of uncontrolled and unregulated human activities in the watershed of numerous wetlands in the Kashmir Valley has resulted in serious landscape changes.20 The most notable causes, particularly in the last 30 years, have been rapid population expansion, changes in agricultural techniques, expanding urbanization, deforestation, economic growth, and the implementation of developmental projects, among others.18 Many researchers have stated that the increased population has affected forest, farm, built-up, and horticultural areas, with the first two land uses declining while built-up and horticultural areas increasing.40 A comprehensive land use policy must be established to avoid the unsustainable expansion of multiple land uses at the expense of natural land cover. The landscape changes in the Shallabugh wetland ecosystem have not been monitored yet. The water quality and biotic setup of the Shallabugh wetland ecosystem may be affected by changing LULC patterns in the watershed. Shallabugh wetland serves as habitat for fish, waterfowl, and other wildlife species. Hence, the focus of the study is to detect and quantify the LULC change that has occurred in Shallabugh wetland due to various human activities as mapped through LANDSAT TM and LISS IV satellite images from 1990 to 2018.

Study area

The Shallabugh wetland is located in the Ganderbal district at a distance of about 20 km northwest of Srinagar city. The wetland is located at an altitude of about 1580 m amsl and within the geographical coordinates of 34º10' N latitude and 74º42' E longitude (Fig. 1). The wetland is primarily fed by Anchar Lake and numerous tributaries of Sindh and Jhelum River.41 The wetland is an important staging and wintering base for migratory avifauna. More importantly the ecosystem is a breeding area for different species of waterfowl. The waterbody has extensive macrophyte reed beds of Phragmites communis and Typha angustata, abundant growth of Nymphaea sp. in open water areas and mats of Lemna minor in some areas. Willow plantations and paddy fields can be seen in the nearby locations. As a result, the area is extremely important habitat for waterfowl. The widespread changes in LULC patterns due to siltation, agricultural activities, encroachment, grazing, and pollution have resulted in the selection of the Shallabugh wetland for assessment. 

Figure 1: Map of Shallabugh wetland.

 

Click here to view Figure 

The data and methodology adopted for developing LULC maps 

Satellite images are a principal source of data for mapping LULC change detection over time in any geographical area. The use of satellite images from two or more dates is common in remote sensing approaches for studying and measuring LULC changes. For comparison, at least two multispectral satellite images are necessary. LANDSAT TM (15 September 1990) obtained from Earth Explorer and LISS IV (18 October 2018) acquired from NRSC Hyderabad were used to assess LULC changes in the Shallabugh wetland. Images from the autumn season were used, taking into consideration the vegetative attributes of the location, to minimize the effects of the changing seasons and obtain better results. Table 1 lists the specifications of the satellite data used to evaluate landscape dynamics.

When collecting spatial data from several sources, it is necessary for all datasets to overlap accurately. All of the maps must be geo-referenced to the same projection system. In geo-referencing, an uncorrected, raw image from an arbitrary coordinate system is transformed into a map projection coordinate system. Image pixels are positioned and corrected in order to align and fit into real-world map coordinates. The nearest neighborhood technique was used in the re-sampling process. Ground truthing of doubtful areas was done by acquiring field characteristics from several mapped LC classes and relating them to matching image attributes using GPS (global positioning system). After ground truthing and the development of an interpretation key, the images were visually evaluated on screen and the various classes of LULC were demarcated using Arc-GIS software. To map different LULC classes, false colour composite (FCC) images created from selected bands of satellite data were used for onscreen visual interpretation. The percent change for various LULC classes was obtained by the following formula 42:

Where K represents the %age of LU change, and Ua and Ub represent the LU types at the start and end of a period, respectively. Positive values specify an increase in LU area, while negative values show a decline in LU area compared to the previous year. Figure 2 depicts the flowchart of the methodology used in this investigation.

Table 1: Spatial data used to assess the LULC change of Shallabugh wetland.

 

Data type

Source

Data specifications

Time Period

LANDSAT TM

Spatial

Earth Explorer

30 m resolution (Path 149, Row 36

15 September 1990

LISS IV

Spatial

NRSC Hyderabad

5.8 m resolution (Path 96, Row 50

18 October 2018

Figure 2: Schematic methodology adopted for developing LULC maps

 

Click here to view Figure 

Results 

The LULC map depicts the spatial distribution and extent of several LULC categories. Shallabugh wetland has observed considerable LULC changes. The description of the various LULC classes in the study area is illustrated in Figs. 3, 4 and Table 2, respectively. The LULC maps generated for the Shallabugh wetland for two different years (1990 and 2018), with a gap of 28 years, revealed seven different LULC classes viz. macrophytic vegetation, mixed plantation, open water, grazing land, agriculture field, built-up area, and vegetable field. In years 1990 and 2018, the area occupied by macrophytic vegetation was 33.87% and 32.36%, mixed plantation (28.06% and 28.70%), open water (1.84% and 1.65%), grazing land (2.23% and 1.59%), agriculture (31.17% and 30.35%), built-up (2.05% and 3.83%), and vegetable field (0.77% and 1.51%). Throughout all time periods evaluated in the study, macrophytic vegetation has the highest share and vegetable field have the lowest share of all the defined categories of LULC in the study region.

The information contained in the LULC maps derived from LANDSAT TM (1990) and LISS IV (2018) satellite data has shown many variations in the LULC of Shallabugh wetland from 1990 to 2018. The macrophytic vegetation, open water, grazing land, and agriculture field have registered a decline, while mixed plantation, built-up area, and vegetable field have increased. The area of land under macrophytic vegetation has decreased from 864.60 ha in 1990 to 826.08 ha in 2018, a 38.52 ha (4.4%) decrease, while the area of open water has decreased from 47.00 ha in 1990 to 42.17 ha in 2018, a 4.83 ha (10.3%) decrease. The area of grazing land has declined by about 16.34 ha (28.6%) from 1990 to 2018. The results also show that the area of the agriculture field has been reduced from 795.65 ha in 1990 to 774.74 ha in 2018, a 20.91 ha (2.6%) decrease. The mixed plantation has increased from 716.36 ha in 1990 to 732.80 ha in 2018, a 16.44 ha (2.28%) increase. The built-up has increased from 52.42 ha in 1990 to 97.72 ha in 2018, a 45 ha (86.8%) increase, and the vegetable field has increased from 19.76 ha in 1990 to 38.62 ha in 2018, a 18.86 ha (96.1%) increase.

Figure 3: LULC classes of Shallabugh wetland in 1990.

 

Click here to view Figure

Figure 4: LULC classes of Shallabugh wetland in 2018.

 

Click here to view Figure 

Table 2: Area under different LULC classes and the change in the LULC pattern of Shallabugh wetland between 1990 and 2018.

 

Area (ha)

Area (%)

Area change

1990

2018

1990

2018

ha

%

Macrophytic vegetation

864.60

826.08

33.87

32.36

-38.52

-4.4

Mixed Plantation

716.36

732.80

28.06

28.70

+16.44

+2.28

Open water

47.00

42.17

1.84

1.65

-4.83

-10.3

Grazing Land

56.83

40.49

2.23

1.59

-16.34

-28.6

Agriculture Field

795.65

774.74

31.17

30.35

-20.91

-2.6

Built up

52.42

97.72

2.05

3.83

+45

+86.8

Vegetable Field

19.76

38.62

0.77

1.51

+18.86

+96.1

Discussion

The assessment of the LULC maps of the Shallabugh wetland revealed remarkable changes in almost all the LULC classes during the period from 1990 to 2018. These changes are largely attributed to human activities that drive LULC changes.43 The area under the open water has significantly decreased by 4.83 ha (10.3%) from 1990 to 2018. The main cause behind the decline of the open water area is the nonstop inflow of sediments from Sindh Nallah and its tributaries, which brings an enormous amount of sediments that are deposited directly into the wetland and reduces its water holding capacity.18,44 The macrophytic vegetation area decreased by 38.52 ha (4.4%) due to the transformation into plantation area.20 The depth of the wetland has been reduced considerably, and as such, much of the wetland has been converted into marshland, which has resulted in a decline in macrophytic vegetation cover and open water area. Another significant change observed was a decrease of 20.91 ha (2.2%) in grazing land during the same period. The main reason for the decrease in grazing land was the conversion into agricultural land. A 16.44 ha (2.28%) increase was observed in mixed plantation, which could be attributed to afforestation efforts by the locals and Sind forest division Ganderbal.44 

One of the most significant changes observed during the present study includes the expansion of built-up area by 45 ha (86.8%) and vegetable field by 18.86 ha (96.1%) and a decrease of 20.91 ha (2.6%) of agricultural land. The main reason behind the increase in vegetable field and build-up area indicates the conversion of agricultural land and macrophytic vegetation areas.18,44 The agricultural lands are being transformed into buildings as the need for land is increasing day by day for the construction of commercial, residential, and other infrastructural projects at the cost of agricultural land. Several authors have reported the loss of agricultural lands to rapid urbanization.18,44,45,46,47

Conclusion 

Land use changes are a common and dynamic occurrence on the earth's surface. Change in one land use cover leads to change in another land cover as well. For administration and land use planning tasks, understanding of land use change is very essential. For LULC analysis, remote sensing and GIS technology are widely used. The present study used LANDSAT TM and LISS IV satellite images and Arc-GIS software to demonstrate the pattern of LULC dynamics in the Shallabugh wetland from 1990 to 2018. The study revealed that the Shallabugh wetland has undergone enormous LULC changes over the last 28 years (last three decades). The built-up area, vegetable field, and mixed plantation area showed significant expansion. On the other hand, a reduction was observed in macrophytic vegetation, open water, grazing land, and agriculture field. The impact of population growth and development activities on land use changes is clearly demonstrated in this study. Any change in land use becomes very critical for the ecological beauty of the Shallabugh wetland as it serves as a habitat for fish, waterfowl, and other wildlife species. Therefore, due attention is needed to the enhancement of the ecological balance of Shallabugh wetland.

Conflict of Interests

All contributing authors declare no conflict of interest.

Funding Sources

The authors declare that no funds, grants, or other support 

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