Wetland has been substantially decreased by anthropogenic activities worldwide, requiring urgent conservation action. The present study aimed to analyze the effects of land use land cover change on wetland dynamics from 1992 to 2022 in Jimma City, Southwestern Ethiopia. Landsat TM of 1992, ETM+ of 2000, ETM+ of 2009 and OLI/TIRS of 2022 were used in this study. Landsat images were classified by using supervised classification with maximum likelihood algorithm. The results revealed that grassland, wetland and vegetation land cover classes declined by 2,304.9 ha, 1410.2 ha and 820.5 ha, respectively whereas farm land, settlement and bare land increased by 2,199 ha, 2,111 ha and 225.4 ha, respectively. Results show that the normalized difference water index (NDWI) has positive and negative strong relationship with normailized difference vegetation index (NDVI) and normalized difference built up index (NDBI) with the coefficent determination (R2) of 0.96 and 0.98, respectively. Due to rapid urbanization and declining vegetation cover in the study area, about 98% of wetland land cover in the study area has been lost over the past decades. Therefore, the governmental and non-governmental organizations should give special attention to wetland restoration and management in the study area.

  • Rapid human population and informal settlement accelerate the rate of LULC change.

  • Supervised classification method with maximum likelihood algorithm was applied.

  • Wetland declined by the rate of 47 ha/year from 1992 to 2022.

  • Due to rapid urbanization and declining vegetation cover, about 98% of wetland land cover in the study area was lost over the past decades.

Wetlands are commonly defined as areas that are transitional land between terrestrial and aquatic environments (Tooth & Van Der Waal 2019; Tadese et al. 2020; Mandishona & Knight 2022). They are also defined as the units of the landscape that are found on the interface between land and water bodies (Ray et al. 2022; Wang et al. 2022a; Fang et al. 2023). Wetland ecosystems are important for ecological, economic and other social values (Assefa et al. 2021; Donatti et al. 2022; Takavakoglou et al. 2022; Xu et al. 2023). Ecologically, wetland is used for water purification, soil erosion control, global climate change mitigation, recharging and discharging of ground water and habitat for biodiversity, especially as suitable ecosystems for migratory bird species (Kumari et al. 2020; Yang et al. 2022c; Li et al. 2023b; Qu et al. 2023; Rizal et al. 2023).

The local communities that live around the wetland ecosystems harvest aquatic resources such as medicinal aquatic vegetation, fishes and other importance aquatic organisms as sources of food and for income-generating purposes (Jackson et al. 2012; Dobbs et al. 2016). In addition, wetlands have been viewed as potential sites for nature-based ecotourism and leisure sites for local communities (Chan et al. 2022; Margaryan et al. 2022; Xu et al. 2022). Wetland is under pressure due to uncontrolled anthropogenic activities that deteriorate the wetland ecological balance (Angessa et al. 2019; Degife et al. 2019; Das et al. 2020). The high demand for more open space for commercial, industrial, and residential purposes driven by rapid urbanization growth significantly contribute to wetland degradation. The share of urban green spaces, vegetation and wetlands are in decline as a result of land conversion (Kadhim et al. 2022; Yang et al. 2022a; Yin et al. 2022a).

The expansion of modernized agricultural practices for the maximization of agricultural products to feed the human population has highly accelerated wetland degradation (Li et al. 2021; Ayyad et al. 2022; Wang et al. 2022a; Yang et al. 2023). For the improvement of agricultural yields, utilization of artificial fertilizers, pesticides, herbicides and modernized machine can degrade wetland ecosystems (Zou et al. 2018; Wang et al. 2022b). According to Hu et al. (2017), about 33% of wetlands globally have been lost including 4.58 million km2 of non-water wetlands and 2.64 million km2 of open water in 2009.

In Ethiopia, about 13,700 km2 of the total land area was covered by wetland (Teferi et al. 2010; Menbere & Menbere 2018). However, wetland resources have been degraded due to inappropriate land use such as deforestation, uncontrolled grazing, mining, irrigation activities, dam and canal construction and expansion of agricultural land (Berhanu et al. 2021; Dixon et al. 2021; Zekarias et al. 2021). Several studies have been conducted to evaluate the impacts of land use/land cover (LULC) change on wetland ecosystem dynamics (Chen et al. 2022; Wang et al. 2022c; Yin et al. 2022b; Liu et al. 2023). According to Moisa et al. (2023b), due to expansion of agricultural lands, wetland area has declined at a rate of 4.2 km2/year in Abay Choman and Jimma Geneti watersheds. Consequently, wetlands and water bodies have severely declined by 1,618 ha due to expansion of built-up areas and cultivation areas in and around Bahir Dar City (Assefa et al. 2021).

Some studies have been conducted, including exploring spatio-temporal patterns of informal settlements, urban heat island dynamics in response to LULC changes, and effects of LULC changes on surface temperature in Jimma city (Moisa et al. 2022a, 2022b). However, previous studies have not considered the impacts of changes in urban LULC on wetland ecosystem degradation in relation to uncontrolled urban growth and expansion in and around Jimma city. Wider areas of wetlands have been converted to bare land, urban agriculture, and human settlement, which negatively impact the biological significance of the wetland ecosystem.

Urban expansion has also exacerbated the loss of wetland vegetation, accompanied by a significant reduction in wetland ecosystems. Beside this, other parts of the city's wetlands are used as landfills and waste disposal sites due to lack of information about and attention to the contribution of wetland ecosystems. This and other related information gaps put the wetland ecosystem under threat, which requires research attention to restore the degraded wetland and improve the wetland resource management system. Analyzing the relationship between wetland and other land cover classes such as built-up area and vegetation cover is essential for determining their negative impacts on wetland loss. Geospatial technology was used to map the spatial distribution, as the extent of wetland and its relation to other LULC classes is important for decision makers. Therefore, this study aims to fill the existing research gaps by analyzing the impacts of LULC changes on wetland degradation through correlation and regression of wetland (normalized difference water index, NDWI) with vegetation cover (normalized difference vegetation index, NDVI) and built-up area (normalized difference built-up index, NDBI) by using geospatial techniques in Jimma city, southwestern Ethiopia.

Description of the study area

Jimma is the capital city of Jimma zone which is located in the southwestern part of Ethiopia, 352 km away from Addis Ababa city. Geographically, it is situated between 7°37′30″N and 7°43′30″N and 36°48′0″E and 36° 52′30″E with a topographic variation range from 1,700 m to 2,000 m above sea level (Figure 1). The mean annual rainfall of the study area is 1,523 mm and mean annual temperature is 19.5 °C (Abebe et al. 2019; Moisa et al. 2022b). According to the 2013 Ethiopian Central Statistical Agency report, the city has a total population of 155,434 (Getachew 2022). Populations of Jimma city are characterized by diverse ethnic groups, with the Oromo ethnic group being very dominant. Other ethnic groups such as Amara, Dawro, Gurage, and Kafficho also live in the city.
Figure 1

Location of the study area.

Figure 1

Location of the study area.

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Data sources and descriptions

Landsat images TM of 1992, Landsat ETM + of 2000, Landsat ETM + of 2009 and Landsat OLI/TIRS of 2022 were used for this study (Table 1; Figure 2). The Landsat images were downloaded from the USGS EarthExplorer website (https://earthexplorer.usgs.gov/) which is freely available to users. All Landsat images were downloaded with little cloud cover (<10%) and during the dry season (January, February). The Landsat images were used for LULC change analysis and calculation of NDWI, NDVI and NDBI.
Table 1

Data sources and descriptions

Date of acquisitionLandsat imagerySensorPath/RowMultispectral bandSpatial resolutionSources
20 Jan 1992 Landsat 5 TM 169 & 055 1 to 5 and 7 30*30 https://earthexplorer.usgs.gov/ 
15 Feb 2000 Landsat 7 ETM + 169 & 055 1 to 5 and 7 30*30 https://earthexplorer.usgs.gov/ 
25 Jan 2009 Landsat 7 ETM + 169 & 055 1 to 5 and 7 30*30 https://earthexplorer.usgs.gov/ 
20 Feb 2022 Landsat 8 OLI/TIRS 169 & 055 1 to 5 and 9 30*30 https://earthexplorer.usgs.gov/ 
Date of acquisitionLandsat imagerySensorPath/RowMultispectral bandSpatial resolutionSources
20 Jan 1992 Landsat 5 TM 169 & 055 1 to 5 and 7 30*30 https://earthexplorer.usgs.gov/ 
15 Feb 2000 Landsat 7 ETM + 169 & 055 1 to 5 and 7 30*30 https://earthexplorer.usgs.gov/ 
25 Jan 2009 Landsat 7 ETM + 169 & 055 1 to 5 and 7 30*30 https://earthexplorer.usgs.gov/ 
20 Feb 2022 Landsat 8 OLI/TIRS 169 & 055 1 to 5 and 9 30*30 https://earthexplorer.usgs.gov/ 
Figure 2

Methodological flowchart of study.

Figure 2

Methodological flowchart of study.

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Data analysis

Land use land cover classification

Landsat images of multispectral bands from 1992, 2000, 2009 and 2022 were used for LULC classifications. Landsat images were classified by using supervised classification with maximum likelihood algorithm (Simelane et al. 2021; Dibs et al. 2023). The LULC types of the study area were classified as: bare land, farmland, grassland, settlement (built-up area), vegetation and wetland. The detailed information on LULC types is provided in Table 2.

Table 2

Details of land use/land cover classes

LULC classesDescription
Settlement The area occupied by residential, industrial and commercial complexes, road networks, communication and utilities (airport and bus station) 
Bare land Areas with little or no vegetation cover, open lands, eroded gullies and exposed rocks 
Grassland Land covered with small trees, bushes and shrubs, in some cases mixed with grasses; less dense than forests 
Vegetation Areas covered with green trees, woodland, dense shrub land and plantations such as eucalyptus tree 
Farmland Arable agricultural land, areas used for grazing, partially wet lands 
Wetlands Includes areas that are permanent and seasonal muds, waterlogged, marshy, swampy, and water bodies especially during the rainy season 
LULC classesDescription
Settlement The area occupied by residential, industrial and commercial complexes, road networks, communication and utilities (airport and bus station) 
Bare land Areas with little or no vegetation cover, open lands, eroded gullies and exposed rocks 
Grassland Land covered with small trees, bushes and shrubs, in some cases mixed with grasses; less dense than forests 
Vegetation Areas covered with green trees, woodland, dense shrub land and plantations such as eucalyptus tree 
Farmland Arable agricultural land, areas used for grazing, partially wet lands 
Wetlands Includes areas that are permanent and seasonal muds, waterlogged, marshy, swampy, and water bodies especially during the rainy season 

Classification of accuracy assessment

The reality and quality of LULC classification was evaluated by accuracy assessment. This is performed by collecting ground control points (GCPs) from each LULC type by using GPS and Google Earth Pro. GPS was used in collecting GCPs for the 2022 LULC class accuracy evaluation, and Google Earth Pro was used to collect GCPs for the 1992, 2000, and 2009 LULC class accuracy assessments. The LULC classes comprising six major classes were distinguished for each time period. To calculate accuracy assessment for each LULC type, the collected GCPs were used. By using the random stratified method, 72 samples were collected for each LULC class. In addition, overall accuracy (Equation (1)) and kappa coefficient (Equation (2)) were calculated in realization of pixel based classification of LULC types (Merga et al. 2022; Moisa & Gemeda 2022).
(1)
(2)
where OAC is overall accuracy, Khat is kappa statistics, N is total number of samples, Xij is diagonal values, Obs represents accuracy reported in error matrix, and Exp is correct classification.

Land use/land cover change detection

Trends and rate of LULC change
Trends of LULC classes were the main indicator of how much LULC types had changed in the study area over time (Moisa et al. 2023a). Trends of LULC types of the study area were calculated by using the final and initial year of LULC classes (Equation (3)). The greater values of final LULC classes were related to positive trends and vice versa.
(3)
where X1 is initial year, X2 is the final year.
Rate of LULC change
The extent and degree of LULC change during the study period at the study area were assessed using the rate of LULC change. In this study, LULC types of 1992, 2000, 2009 and 2022 were applied to assess the rate of LULC change in Jimma city (Equation (4)). According to Moisa & Gemeda (2021), the rate of LULC change was calculated to evaluate the degree of LULC change in Addis Ababa city from 1990 to 2020.
(4)
where Y1 and Y2 are the area coverage of LULC at initial year (Y1) and final year (Y2), Z is time interval between two years.
Land use and land cover change matrix

In the present study, the LULC change detection for Jimma city was applied by using the land use transfer matrix from 1992 to 2022. The rate change, losses and gain of LULC within the study period were calculated by using the change matrix in the study area (Pal & Ziaul 2017; Zhang et al. 2021).

Normalized Difference Water Index (NDWI)

According to Delbart et al. (2005), NDWI was used to identify and analyze the moisture status of vegetation canopies which often have important thermal changes across wide areas. In this study, green and near infrared (NIR) bands were used to calculate NDWI. Green band (band 2 for Landsat 5 and 7, band 3 for Landsat 8) and NIR (band 4 for Landsat 5 and 7, band 5 for Landsat 8) reflectance measurements were used to build the formula (Equation (5)).
(5)

Normalized Difference Vegetation Index (NDVI) estimation

NDVI is used for monitoring the growth and health of vegetation as well as to detect any stress or damage. In addition to mapping and categorizing different vegetation types, NDVI values can be used to evaluate changes in vegetation cover over time (Halder et al. 2022; Zhu et al. 2022). Consequently, it has been used to calculate the abundance of vegetation cover on the Earth's surface (Alam et al. 2022). The NDVI value was calculated by using multispectral bands from Landsat images taken in 1992, 2000, 2009, and 2022. Bands 4 and 3 of Landsat 5 and 7 were utilized to measure NIR and red, respectively. Furthermore, in Landsat 8, bands 5 and 4 were employed to assess NIR and red, respectively (Equation (6)).
(6)
where R is red.

Normalized Difference Built-up Index (NDBI)

NDBI emphasizes built-up areas by using the NIR and short wave infrared (SWIR) bands to mitigate the impact of variations in terrain illumination and atmospheric effects (Ghosh et al. 2022). It was determined using Landsat 5 and 7 multispectral bands computed from bands 4 and 5, and Landsat 8 computed from bands 5 and 6. In addition, it is the method that was applied to map built-up area with 92% accuracy (Zhou et al. 2014) (Equation (7)). The idea is that the NDVI was taken as an indicator of vegetation coverage whereas the NDBI was used in extraction of the built-up area. Both NDVI and NDBI were thought to have a strong relationship with land surface temperature (LST) (Aslam et al. 2021).
(7)

Correlation and regression analysis of NDWI, NDVI and NDBI parameters

Correlation and linear regression are the two techniques most commonly employed for examining the relationship between dependent (NDWI) and independent (NDVI, NDBI) variables (Miss 2020). In this study, linear regression determines the relationship as an equation, whereas correlation assesses the strength of the linear relationship between two variables (Hopkins & Ferguson 2014; Yang et al. 2022b). This analysis was used to realize the reliability impacts of NDVI and NDBI variables as major causes and effects for wetland (NDWI) degradation. ArcGIS environment and Microsoft Excel were used to analyze regression and correlation in this study.

Land use and land cover classes of 1992

Results show that grassland and farmland were the most dominant LULC types with an area of 3,909 ha (37.2%) and 2,876 ha (27.4%), respectively. In addition, vegetation and wetland covered areas of 1,621.8 ha (15.4%) and 1,512 ha (14.4%), respectively. However, settlement and bare land were the least dominant LULC types with 514 ha (4.9%) and 82 ha (0.8%) out of the total study area in 1992 (Table 3). The spatial distribution of vegetation and grassland were concentrated in the eastern and northern parts, while settlement and wetlands dominated the central and southeastern parts of the study area (Figure 3(a)). The results of this study are consistent with previous studies (Yan et al. 2022; Duan et al. 2023).
Table 3

Land use land cover classes of 1992

S/noLULC typeArea (ha)Area (%)
Bare land 82 0.8 
Farmland 2,876 27.4 
Grassland 3,909 37.2 
Settlement 514 4.9 
Vegetation 1,622 15.4 
Wetland 1,512 14.4 
 Total 10,515 100 
S/noLULC typeArea (ha)Area (%)
Bare land 82 0.8 
Farmland 2,876 27.4 
Grassland 3,909 37.2 
Settlement 514 4.9 
Vegetation 1,622 15.4 
Wetland 1,512 14.4 
 Total 10,515 100 
Figure 3

LULC map of (a) 1992; (b) 2000; (c) 2009 and (d) 2022.

Figure 3

LULC map of (a) 1992; (b) 2000; (c) 2009 and (d) 2022.

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Land use and land cover classes of 2000

The LULC classes of 2000 show the domination of farmland (4,611.5 ha, 43.9%) followed by grassland (3,258 ha, 31%) and wetland (1,072.2 ha, 10.2%) in Jimma city. However, vegetation (809.7 ha, 7.7%), settlement (612.4 ha, 5.5%) and bare land (146.4 ha, 1.4%) were the least dominant land cover types, respectively (Table 4). Geographically, northern and eastern parts of the study area were mostly occupied by vegetation and wetland land cover types while built-up areas highly dominated the central parts of Jimma city. However, larger parts in the southwest of the study area were dominated by extensive farmland, whereas some of the northern parts were covered by bare land (Figure 3(b)).

Table 4

Land use land cover classes of 2000

S/noLULC typeArea (ha)Area (%)
Bare land 146.4 1.4 
Farmland 4,611.5 43.9 
Grassland 3,258.0 31.0 
Settlement 612.4 5.8 
Vegetation 809.7 7.7 
Wetland 1,072.2 10.2 
 Total 10,510.2 100 
S/noLULC typeArea (ha)Area (%)
Bare land 146.4 1.4 
Farmland 4,611.5 43.9 
Grassland 3,258.0 31.0 
Settlement 612.4 5.8 
Vegetation 809.7 7.7 
Wetland 1,072.2 10.2 
 Total 10,510.2 100 

Land use and land cover classes of 2009

Farmland and grassland of LULC types in 2009 were highly dominant with 4,120.8 ha (39.2%) and 3,639.5 ha (34.6%), respectively. Besides this, vegetation and settlement occupied 1,678.8 ha (16%) and 674.9 ha (6.4%) of the total area. However, wetland was the least dominant LULC class with an area of 221 ha (2.1%) in the study period (Table 5). Except for the central and some southeastern parts of Jimma city, farmland, grassland, and vegetation covered the vast majority of the study area. Additionally, the central and southern parts of the study area were occupied with settlements and bare land (Figure 3(c)). According to Malede et al. (2023), rapid human population growth was the main cause of deforestation in the Birr river watershed of Abay basin, Ethiopia.

Table 5

Land use land cover classes of 2009

S/NoLULC typeArea (ha)Area (%)
Bare land 180.0 1.7 
Farmland 4,120.8 39.2 
Grassland 3,639.5 34.6 
Settlement 674.9 6.4 
Vegetation 1,678.8 16.0 
Wetland 221.0 2.1 
 Total 10,515 100 
S/NoLULC typeArea (ha)Area (%)
Bare land 180.0 1.7 
Farmland 4,120.8 39.2 
Grassland 3,639.5 34.6 
Settlement 674.9 6.4 
Vegetation 1,678.8 16.0 
Wetland 221.0 2.1 
 Total 10,515 100 

Land use and land cover classes of 2022

Land use and land cover classes of 2022 indicate that both farmland and settlement dominate wider parts of the study area with an extent of 5,075.4 ha (48.3%) and 2,625 ha (25%), respectively. Consequently, vegetation and bare land cover an area of 801.6 ha (7.6%) and 307.4 ha (2.9%), whereas wetland covers 101.8 ha (1%) of the total study area (Table 6). Geographically, settlement and farmland dominated the central, southern, some western and northeastern parts of the study area, respectively. Consequently, vegetation and wetland occupied some eastern, northern and southern parts of Jimma city, respectively (Figure 3(d)). Urban expansion has had a negative impact on water bodies and wetland degradation in and around Bahir Dar City (Assefa et al. 2021).

Table 6

Land use land cover classes of 2022

S/NoLULC typeArea (ha)Area (%)
Bare land 307.4 2.9 
Farmland 5,075.4 48.3 
Grassland 1,604.1 15.3 
Settlement 2,625.0 25.0 
Vegetation 801.3 7.6 
Wetland 101.8 1.0 
 Total 10,515 100 
S/NoLULC typeArea (ha)Area (%)
Bare land 307.4 2.9 
Farmland 5,075.4 48.3 
Grassland 1,604.1 15.3 
Settlement 2,625.0 25.0 
Vegetation 801.3 7.6 
Wetland 101.8 1.0 
 Total 10,515 100 

Accuracy assessment

The overall classification exactness of the LULC precision appraisals for 1992, 2000, 2009, and 2022 was 87.5%, 89.4%, 90.7%, and 92.3%, respectively. As a result, for the think about periods 1992, 2000, 2009, and 2022, the kappa coefficients were 0.88, 0.87, 0.81 and 0.85.

Trends of land use land cover from 1992 to 2022

In this study, positive values indicate an increase and negative values indicate a decrease in LULC type in the study area during the study period. The results revealed that grassland, wetland and vegetation land cover declined by 2,304.9 ha, 1,410.2 ha and 820.5 ha, respectively, from 1992 to 2022. Farmland, settlement and bare land increased by 2,199 ha, 2,111 ha and 225.4 ha, respectively (Figure 4). The calculated trend values demonstrate that rapid expansion of built-up areas and farmland causes dramatic reduction of wetland and vegetation land cover. Abebe et al. (2019) stated that rapid population growth and increasing urbanization lead to informal settlement in Jimma city. The degradation of wetland and vegetation cover were the main causes of the urban heat island and increment of land surface temperature (Moisa et al. 2022a, 2022b; Li et al. 2023a).
Figure 4

Trends of LULC types in the study area.

Figure 4

Trends of LULC types in the study area.

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Rate of land use land cover change

The rate of LULC change was used to evaluate speed of increase or decrease in LULC types in the study area. The results show that farmland, settlement and bare land increased at a rate of 216.9, 21.3 and 8.1 ha/year and caused the reduction of vegetation, grassland and wetland cover at a rate of 101.5, 81.4 and 55 ha/year respectively from 1992 to 2000. However, farmland, settlement and bare land increased at a rate of 73.3, 70.4 and 7.5 ha/year and were responsible for a reduction in grassland, wetland and vegetation cover at the rate of 76.8, 47 and 27 ha/year, respectively from 1992 to 2022 (Table 7). The finding of this study was in agreement with the study conducted by Moisa et al. (2023b) in Abay Choman and Jimma Geneti watershed, which indicated that the extent of wetland and forest land declined at a high rate due to expansion of cultivated land. In addition, forest and grassland experienced a high rate of change due to expansion of the settlement area in Anger river sub basin from 1991 to 2020 (Moisa et al. 2022c).

Table 7

Rate of change of land use land cover types in the study area

LULC type1992–20002000–20092009–20221992–2022
(ha/year)(ha/year)(ha/year)(ha/year)
Bare land 8.1 3.7 9.8 7.5 
Farmland 216.9 −54.5 73.4 73.3 
Grassland −81.4 42.4 −156.6 −76.8 
Settlement 12.3 6.9 150.0 70.4 
Vegetation −101.5 96.6 −67.5 −27.4 
Wetland −55.0 −94.6 −9.2 −47.0 
LULC type1992–20002000–20092009–20221992–2022
(ha/year)(ha/year)(ha/year)(ha/year)
Bare land 8.1 3.7 9.8 7.5 
Farmland 216.9 −54.5 73.4 73.3 
Grassland −81.4 42.4 −156.6 −76.8 
Settlement 12.3 6.9 150.0 70.4 
Vegetation −101.5 96.6 −67.5 −27.4 
Wetland −55.0 −94.6 −9.2 −47.0 

Land use land cover change matrix from 1992 to 2022

In this study, conversions of LULC classes from 1992 to 2022 were analyzed. The results revealed that farmland, wetland and vegetation were converted to settlement (built-up area) with an area of 79.1 ha, 16.9 ha and 6.4 ha, respectively from 1992 to 2022. Bare land was gained from wetland and grassland by an area of 2.4 ha and 16.9 ha, respectively. However, 2,961.8 ha was unchanged out of the total study area from 1992 to 2022 (Table 8; Figure 5). Rapid population and informal settlement were causes for decline of vegetation cover and agricultural land in the study area (Abebe et al. 2019). The losses of vegetation cover and wetland were causes of climate change variability and ecological disturbance which related to reduction of urban thermal comfort level. According to Moisa et al. (2022d), the main cause of the decrease in urban thermal comfort level for the local community is decline of vegetation cover in Addis Ababa City.
Table 8

LULC conversion in the study area from 1992 to 2022

2022
LULCBare landFarmlandGrasslandSettlementVegetationWetlandTotal
1992 Bare land 7.7 63.4 61.6 5.5 19.5 19.3 176.9 
Farmland 30.1 1,451.9 2,232.3 79.1 738.7 664.6 5,196.8 
Grassland 16.9 437.0 593.7 27.9 253.1 275.0 1,603.6 
Settlement 114.6 838.2 639.8 375.4 134.1 399.5 2,501.6 
Vegetation 0.5 52.2 215.9 6.4 451.1 74.5 800.5 
Wetland 2.4 49.1 63.3 16.9 21.8 82.0 235.6 
Total 172.1 2,891.8 3,806.7 511.1 1,618.4 1,514.9 10,515.0 
2022
LULCBare landFarmlandGrasslandSettlementVegetationWetlandTotal
1992 Bare land 7.7 63.4 61.6 5.5 19.5 19.3 176.9 
Farmland 30.1 1,451.9 2,232.3 79.1 738.7 664.6 5,196.8 
Grassland 16.9 437.0 593.7 27.9 253.1 275.0 1,603.6 
Settlement 114.6 838.2 639.8 375.4 134.1 399.5 2,501.6 
Vegetation 0.5 52.2 215.9 6.4 451.1 74.5 800.5 
Wetland 2.4 49.1 63.3 16.9 21.8 82.0 235.6 
Total 172.1 2,891.8 3,806.7 511.1 1,618.4 1,514.9 10,515.0 
Figure 5

LULC conversion (post classification) from 1992 to 2022 in Jimma city.

Figure 5

LULC conversion (post classification) from 1992 to 2022 in Jimma city.

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Analysis of NDWI from 1992 to 2022

Wetland status in Jimma city was evaluated by calculating the value of NDWI from 1992 to 2022. The result revealed that the maximum values of NDWI were 0.6, 0.3, 0.2 and 0.12 in 1992, 2000, 2009 and 2022, respectively. A dramatic decline of NDWI is associated with wetland degradation due to urban expansion and reduced vegetation cover. In 1992, wetland was the most dominant class in all parts of the study area (Figure 6(a)), while northern and eastern parts of the study area were dominated by wetland in 2000 (Figure 6(b)). Wetland was highly degraded in larger parts of the study area except in eastern and southern parts between 2009 and 2022 (Figure 6(c) and 6(d)). According to Abebe et al. (2019), the built-up area was highly expanded due to rapid population growth, which aggravated degradation of wetland cover from 1997 to 2017 in Jimma city. A study by Dessu et al. (2020) reported that wetland dramatically declined due to rapid expansion of the built-up area from 1957 to 2018 in Jimma city (Dessu et al. 2020).
Figure 6

NDWI map of (a) 1992; (b) 2000; (c) 2009 and (d) 2022.

Figure 6

NDWI map of (a) 1992; (b) 2000; (c) 2009 and (d) 2022.

Close modal

Analysis of NDVI from 1992 to 2022

The status of vegetation cover determines the greenness and non-greenness, which was evaluated based on the calculated value of NDVI. The calculated NDVI values within the study area were 0.7, 0.49, 0.47 and 0.38 in 1992, 2000, 2009 and 2022, respectively. Results revealed that the dense vegetation cover substantially declined with a maximum NDVI of 0.32 from 1992 to 2022. Dense vegetation cover dominated in the northern and eastern parts of the study area in 1992 and 2000 (Figure 7(a) and 7(b)). Consequently, some northern and eastern parts of the study area were captured by vegetation cover with low vegetation cover in western and southern parts in 2009 (Figure 7(c)). However, highly vegetated areas were diminished except in some northern parts in 2022 due to rapid expansion of built-up area and farmland (Figure 7(d)). The main cause of the decline in vegetation cover was the expansion of built-up area and bare land which resulted from rapid human population growth and informal settlement. Increasing human population resulted from continual local community migration from rural to urban areas for changing livelihoods, which contributes to high demand for housing and is correlated with expansion of the built-up area and decline of vegetation in Jimma city (Abebe et al. 2019; Dessu et al. 2020; Moisa et al. 2022a).
Figure 7

NDVI map of (a) 1992; (b) 2000; (c) 2009 and (d) 2022.

Figure 7

NDVI map of (a) 1992; (b) 2000; (c) 2009 and (d) 2022.

Close modal

Analysis of NDBI from 1992 to 2022

The calculated NDBI was used to determine the status of the built-up area in Jimma city over the study period. The result shows that the maximum NDBI values were 0.17, 0.18, 0.38 and 0.6 in 1992, 2000, 2009 and 2022, respectively. The calculated value shows an increasing trend of 0.43 from 1992 to 2022. This dramatic change of NDBI was caused by rapid urban expansion due to human population growth within the three decades. As a result, the increased value of NDBI was the main reason for the substantial decline of wetland and vegetation cover. Geographically, the built-up area was expanded from central to southern and eastern parts of the study area (Figure 8(a)–8(d)). The result is consistent with previous studies (Dessu et al. 2020; Liu et al. 2020; Moisa et al. 2022a, 2022b), which found that the built-up area was highly expanded due to rapid urban growth which resulted in the decline of green vegetation and wetland in Jimma city.
Figure 8

NDBI map of (a) 1992; (b) 2000; (c) 2009 and (d) 2022.

Figure 8

NDBI map of (a) 1992; (b) 2000; (c) 2009 and (d) 2022.

Close modal

Correlation analysis of NDWI with NDVI and NDBI

Correlation analysis was used to determine positive or negative strong relationships between two variables. In this study, correlated variables were expressed as NDWI with NDVI, NDWI with NDBI, NDVI with NDBI. From the calculated value, the results showed that NDWI has a positive strong relationship with NDVI with a coefficient determination (R2) of 0.97. However, the correlation NDWI with NDBI (R2 = 0.99) and NDVI with NDBI (R2 = 0.99) showed a strong negative relationship (Table 9). The negative correlation between NDWI and NDBI shows that expansion of built-up area (NDBI) was the main reason for the decline of wetland (NDWI) and green vegetation cover (NDVI). A study by Guha & Govil (2022) in Raipur City, India reported that NDWI has a strong negative relationship with NDBI and strong positive relationship with NDVI.

Table 9

Correlations between NDWI, NDVI and NDBI

CorrelationNDVINDWINDBI
NDVI   
NDWI 0.96688  
NDBI −0.9942 −0.9855 
CorrelationNDVINDWINDBI
NDVI   
NDWI 0.96688  
NDBI −0.9942 −0.9855 

Regression analysis for land surface temperature of Jimma city

Linear regression analysis was used to forecast the cause and effects of one dependent variable based on two or more independent variables. In this study, causes and effect of wetland (NDWI) was determined by expansion of built-up area (NDBI) and decline of vegetation cover (NDVI). The P value shows that NDBI is a better predictor of NDWI than NDVI. Our results show that substantial decline of NDWI was the primary cause of the increasing trend of NDBI. Expansion of the built-up area was another cause for the decline of vegetation cover in the study area. Calculated adjusted R2 shows that expansion of built-up area and reduction of vegetation cover contributes to 98% of wetland degradation. The remaining percentage may be affected by other factors (Table 10). According to Moisa et al. (2022a), surface temperature of Jimma city increased by 96.6% due to increasing NDBI and decreasing NDVI over the study period.

Table 10

Correlation coefficients between LST, NDVI and NDBI

CoefficientsStandard errort statP-valueLower 95%Upper 95%
NDWIa −0.061023227 0.049061485 −1.2438 0.0024878 −0.17416 0.0521128 
NDVI −1.138767718 0.39597174 −2.8759 0.002064 −2.05188 −0.225655 
NDBI −2.465513987 0.458735012 −5.3746 0.00067 −3.52336 −1.407669 
CoefficientsStandard errort statP-valueLower 95%Upper 95%
NDWIa −0.061023227 0.049061485 −1.2438 0.0024878 −0.17416 0.0521128 
NDVI −1.138767718 0.39597174 −2.8759 0.002064 −2.05188 −0.225655 
NDBI −2.465513987 0.458735012 −5.3746 0.00067 −3.52336 −1.407669 

Coefficient is statistically significant at P < 0.01.

aDependent variable: NDWI.

Rapid human population growth was the main cause of urban expansion. This settlement may be informal or formal due to migration from rural to urban areas for changing livelihoods, which increases demand for housing in Jimma city. Anthropogenic activities, farmland, built-up area (settlement) and bare land dramatically increased. However, vegetation, grassland and wetland substantially declined over the study period. The results revealed that settlement, farmland and bare land showed increasing trends with an area of 2,111 ha, 2,199.4 ha and 225.4 ha, respectively, from 1992 to 2022, whereas grassland, wetland and vegetation showed decreasing trends with an area of 2,304.9 ha, 1,410.2 ha and 820.5 ha, respectively from 1992 to 2022.

From the calculated LULC types, farmland, settlement (built-up area) and bare land increased at a rate of 73.3 ha/year, 70.4 ha/year and 7.5 ha/year, respectively, from 1992 to 2022. However, grassland, wetland and vegetation decreased at a rate of 76.8 ha/year, 47 ha/year and 27.4 ha/year, respectively. Results show that the decline of wetland, grassland and green vegetation in Jimma city were caused by rapid expansion of built-up area and increasing urban agriculture.

From the calculated LULC change matrix, farmland, wetland and vegetation were converted to settlement (built-up area) with an area of 79.1 ha, 16.9 ha and 6.4 ha, respectively from 1992 to 2022. Bare land gained an area of 2.4 ha and 16.9 ha from wetland and grassland, respectively. However, about 2,961.8 ha was unchanged out of the total study area from 1992 to 2022 in Jimma city. The degradation of wetland in the study area was determined by NDWI, NDVI and NDBI. The parameters had strong negative and positive relationships to each other with coefficient determination (R2) of 0.98. The result indicated that wetland (NDWI) declined due to increasing built-up area (NDBI) and degradation of vegetation cover (NDVI). The linear regression analysis, cause and effect dependent variable (NDWI) and independent variables (NDBI and NDVI) were analyzed. The result shows that wetland was degraded by 98% due to the increase in built-up area and decline of vegetation cover. Based on this study, we suggest that environmental experts and natural resources managers must educate the public and promote the responsible use of natural resources, with a special emphasis on the conservation and protection of wetlands to ensure wise urban development. In addition, the impacts of precipitation and temperature on urban wetland ecosystems and the analysis of urban expansion should be studied using high-resolution satellite imagery.

The authors acknowledge Wollega University Shambu Campus, Kotebe University of Education and Jimma University College of Agriculture and Veterinary Medicine for the existing facilities to carry out this study.

YWB and DAN participated in research design, data collection, Landsat image and document analysis. TWB, BCW and GYJ participated in methodology, data analysis and interpretation. MBM, MMG and DOG participated in research design, literature review, data analysis and manuscript writing. All authors read and approved the final manuscript for publication.

All relevant data are included in the paper or its Supplementary Information.

The authors declare there is no conflict.

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