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Spatial-Temporal Dynamics Land Use/Land Cover Change and Flood Hazard Mapping in the Upstream Citarum Watershed, West Java, Indonesia


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Fig. 1

Study area at the upstream Citarum Watershed, West Java, Indonesia. Elevation value from SRTM30 DEM provided by the U.S. Geological Survey (USGS).
Study area at the upstream Citarum Watershed, West Java, Indonesia. Elevation value from SRTM30 DEM provided by the U.S. Geological Survey (USGS).

Fig. 2

3D view of the SRTM30 DEM for the Bandung Basin area (Cekungan Bandung).
3D view of the SRTM30 DEM for the Bandung Basin area (Cekungan Bandung).

Fig. 3

LULC maps were used from various years during the period 1990–2016 (sourced and modified from Yulianto et al. (2018, 2019).
LULC maps were used from various years during the period 1990–2016 (sourced and modified from Yulianto et al. (2018, 2019).

Fig. 4

The dynamics of LULC changes during the period 1990–2016 in the study area. A – estimated area in LULC changes (in hectares), B – Trends and percentages in LULC changes (in per cent).
The dynamics of LULC changes during the period 1990–2016 in the study area. A – estimated area in LULC changes (in hectares), B – Trends and percentages in LULC changes (in per cent).

Fig. 5

The dynamics of LULC changes during 1990–2016 in the eight sub-watersheds in the study area.
The dynamics of LULC changes during 1990–2016 in the eight sub-watersheds in the study area.

Fig. 6

Distribution of urban/built-up area expansion in the eight sub-watersheds in the study area in 1990 (A) and 2016 (B).
Distribution of urban/built-up area expansion in the eight sub-watersheds in the study area in 1990 (A) and 2016 (B).

Fig. 7

Results of the terrain surface classification (TSC) as a micro-landform classification in the study area.
Results of the terrain surface classification (TSC) as a micro-landform classification in the study area.

Fig. 8

Micro-landform classification uses the Bandung Basin as a unit area boundary to focus on classifying potential flood areas, which has been combined with information from the Topographic Position Index (TPI) approach by Yulianto et al. (2019).
Micro-landform classification uses the Bandung Basin as a unit area boundary to focus on classifying potential flood areas, which has been combined with information from the Topographic Position Index (TPI) approach by Yulianto et al. (2019).

Fig. 9

Probability map for flood inundation from 2014 to 2018 in the study area.
Probability map for flood inundation from 2014 to 2018 in the study area.

Fig. 10

The result of flood hazard assessment and mapping based on the integration of TSC as a micro-landform classification approach, probability map for flood inundation and flood depths from field observation.
The result of flood hazard assessment and mapping based on the integration of TSC as a micro-landform classification approach, probability map for flood inundation and flood depths from field observation.

Fig. 11

Areas affected by flooding.A, B – a very high flood hazard area in Baleendah, with TSC class of plains, gentle slope, fine texture, high convexity and a flood depth of more than 5 m. C – a high flood hazard area in Bojongsoang, with TSC class of plains, gentle slope, coarse texture, high convexity and a flood depth of 2–4 m. D – a moderate flood hazard area in Cibiroso, with TSC class of open slopes, moderate slope, coarse texture, high convexity and a flood depth of 1–2 m.
Areas affected by flooding.A, B – a very high flood hazard area in Baleendah, with TSC class of plains, gentle slope, fine texture, high convexity and a flood depth of more than 5 m. C – a high flood hazard area in Bojongsoang, with TSC class of plains, gentle slope, coarse texture, high convexity and a flood depth of 2–4 m. D – a moderate flood hazard area in Cibiroso, with TSC class of open slopes, moderate slope, coarse texture, high convexity and a flood depth of 1–2 m.

LULC descriptions used in this study (sourced and modified from Yulianto et al. (2018, 2019).

ID ClassLULC TypeDescription
1Urban/built-up areaConsists of all built-up area, residential, industrial, commercial area, villages, settlements, transportation infrastructure and others.
2Primary forestConsists of natural forests that have not been disrupted by human exploitation.
3Secondary forest and mixed gardenConsists of industrial plantation forests and some garden planting, coconuts, fruits and others.
4PlantationConsists of conservation land, tea plantation, palm oil and others.
5Wet agricultural landConsists of land that requires much water for its planting patterns: irrigated rice fields, rice terraces and others.
6Dry land farmingConsists of land that requires little water for its cropping patterns: fields, moorland and others.
7Water bodyConsists of all water sources, rivers, reservoirs, ponds and others.

Urban/built-up area size in the eight sub-watersheds in the study area.

Sub-WatershedArea (ha)
199019962000200320092016
Cihaur3,409.73,936.73,986.24,505.25,367.46,486.6
Cikapundung8,414.68,965.79,222.39,702.710,451.012,311.6
Cikeruh1,115.71,481.21,635.01,751.11,961.82,793.9
Ciminyak207.1210.3218.8292.9422.2435.3
Cirasea1,019.81,022.31,194.91,257.61,373.71,788.1
Cisangkuy808.3858.7944.51,111.61,318.91,692.9
Citarik720.9872.81,073.51,129.31,135.61,454.2
Ciwidey391.9392.8405.1459.9586.6753.9

Terrain surface classification (TSC) micro-landform characteristics related to flood conditions in the study area.

NoMicro-landform classificationDescriptionFlood hazard class
1Plains, gentle slope, fine texture, high convexityPlains area with the permissible range less than 9% gradient, dominant positive/concave convexity, fine texture indicates a high proportion of finer particles such as silt and clay. Depth of flooding in excess of 5 mVery high flood hazard 1
2Plains, gentle slope, fine texture, low convexityPlains area with the permissible range less than 9% gradient, dominant negative/concave convexity, fine texture indicates a high proportion of finer particles such as silt and clay. Depth of flooding 4–5 m.Very high flood hazard 2
3Plains, gentle slope, coarse texture, high convexityPlains area with the permissible range less than 9% gradient, dominant positive/concave convexity, coarse texture indicates a high proportion of sand. Depth of flooding 3–4 m.High flood hazard 1
4Plains, gentle slope, coarse texture, low convexityPlains area with the permissible range less than 9% gradient, dominant negative/concave convexity, coarse texture indicates a high proportion of sand. Depth of flooding 2–3 m.High flood hazard 2
5Open slopes, moderate slope, coarse texture, high convexityOpen slope area with a gradient of slope between 10 and 15%, dominant positive/concave convexity, coarse texture indicates a high proportion of sand. Depth of flooding 1–2 m.Moderate flood hazard 1
6Open slopes, moderate slope, fine texture, low convexityOpen slope area with a gradient of slope between 10 and 15%, dominant negative/concave convexity, fine texture indicates a high proportion of finer particles such as silt and clay. Depth of flooding 1–2 m.Moderate flood hazard 2
7Upper slopes, steep slope, fine texture, high convexityUpper slopes area with a gradient of slope between 16 and 30%, dominant positive/concave convexity, fine texture indicates a high proportion of finer particles such as silt and clay. Depth of flooding 0.5–1 m.Low flood hazard 1
8Upper slopes, steep slope, fine texture, low convexityUpper slopes area with a gradient of slope between 16 and 30%, dominant negative/concave convexity, fine texture indicates a high proportion of finer particles such as silt and clay. Flood depth less than 0.5 m.Low flood hazard 2
9Upper slopes, very steep slope, fine texture, high convexityUpper slopes area with a gradient of slope between 31 and 60%, and > 60%, dominant positive/concave convexity, fine texture indicates a high proportion of finer particles such as silt and clay.No flood hazard 1
10Upper slopes, very steep slope, coarse texture, low convexityUpper slopes area with a gradient of slope between 31 and 60%, and > 60%, dominant negative/concave convexity, coarse texture indicates a high proportion of sand.No flood hazard 2

The rate of urban/built-up area expansion in the eight sub-watersheds in the study area.

Sub-WatershedUAER (ha a−1)
1990–19961996–20002000–20032003–20092009–20161990–2016
Cihaur87.812.4173.0143.7159.9118.3
Cikapundung91.964.1160.1124.7265.8149.9
Cikeruh60.938.438.735.1118.964.5
Ciminyak0.52.124.721.51.98.8
Cirasea0.443.120.919.359.229.5
Cisangkuy8.421.555.734.653.434.0
Citarik25.350.218.61.145.528.2
Ciwidey0.13.118.321.123.913.9
eISSN:
2081-6383
Language:
English
Publication timeframe:
4 times per year
Journal Subjects:
Geosciences, Geography