Urban floods have been highly prominent natural disasters occurring in catchments across the globe, causing financial loss and damage to buildings. This necessitates effective and sustainable mitigation mechanisms. In this context, flood-susceptibility-based building risk (FSBR), a combined index for evaluating flood susceptibility and building risk simultaneously to understand the impact of the flood, is proposed by fusing XGBoost (facilitates flood susceptibility) and Hydrologic Engineering Center River Analysis System 2D (enables building risk) in climate change situations. The methodology is applied to Greater Hyderabad Municipal Corporation, India. Six combinations of FSBR, namely, high building risk and high flood susceptibility (HH), high and medium (HM), medium and medium (MM), medium and high (MH), low and medium (LM), and low and high (LH) are employed to study the urban floods. The total affected areas for HH, HM, MH, MM, LH, and LM are 63.40 km2 (52.627%), 28.92 km2 (24%), 9.52 km2 (7.9%), 4.81 km2 (3.99%), 9.26 km2 (7.686%), and 4.56 km2 (3.79%) (totalling 120.47 km2). The number of corresponding buildings is 182,178, 84,136, 46,238, 22,691, 48,092, and 23,781. Waterproofing as a mitigation measure is considered. The total cost of waterproofing is Rs 4,964.60 cr.

  • Machine learning and hydraulic modelling are complemented to derive an indicator, flood-susceptibility-based building risk (FSBR), for the urban catchment.

  • Six combinations of FSBR are employed to study urban floods.

  • Waterproofing as a mitigation measure is studied.

AUROC

area under the receiver operating characteristic

BRT

boosted regression tree

CART

classification and regression tree

Cr

crores

DB

deep boost

DLNN

deep learning neural network

EAC

equivalent annual cost

FSBR

flood-susceptibility-based building risk

FSM

flood susceptibility modelling

GCMs

general circulation models

GEE

Google Earth Engine

GHMC

Greater Hyderabad Municipal Corporation

HEC-RAS 2D

Hydrologic Engineering Center River Analysis System 2D

HH

high building risk and high flood susceptibility

HM

high building risk and medium flood susceptibility

HRB

high-risk buildings

LH

low building risk and high flood susceptibility

LM

low building risk and medium flood susceptibility

LRB

low-risk buildings

MH

medium building risk and high flood susceptibility

ML

machine learning

MM

medium building risk and medium flood susceptibility

MODIS

MODerate Resolution Imaging Spectroradiometer

MRB

medium-risk buildings

NN

neural networks

NRSC

National Remote Sensing Centre

RCPs

representative concentration pathways

RF

Random Forest

SVM

support vector machine

TGPHMED

Telangana Public Health & Municipal Engineering Department

TSDPS

Telangana State Development Planning Society

XGBoost

eXtreme Gradient Boosting

Urban floods have been highly prominent natural disasters occurring in catchments across the globe. Some related factors are low-lying areas, clogged drains, settlements in flood-plain areas, and impervious surfaces. In addition, the widening gap between the increase in urbanization and available infrastructure is a major challenge. This inadequacy, in turn, will not be able to mitigate the impact of urban floods effectively. Another dimension is climate change, evidenced by high-intensity, short-duration, high-frequency rainfall affecting cities significantly (Nkwunonwo et al. 2020). This increases the quantity of water during most of the mentioned situations, which impacts the flooding area and escalates the flood susceptibility (Hammond et al. 2015).

Many floods have occurred in Hyderabad, Mumbai, Chennai, Bengaluru, and Vadodara. These cities have faced substantial financial losses and property damage (Flood Report 2021). In Hyderabad, severe floods occurred in 2000, 2006, 2016, 2018, and 2021. The flood depth range is 1–4 m in many locations (Rangari et al. 2021). Mumbai is another major city affected by urban floods due to climate change, as evidenced by the extreme rainfall of 944 mm for 24 h in 2005 (Sahany et al. 2010; Mumbai floods 2021). The case is similar with cities like Chennai, Bengaluru, and Vadodara, which are highly affected by urban floods (Vadodara floods 2019; Bengaluru floods 2021; Chennai floods 2021).

Literature review

Numerous modelling approaches are employed to compute flood susceptibility. Machine learning (ML) is gaining momentum in classifying flood-susceptible regions due to its flexibility and adaptability (Baghbani et al. 2022; Saha et al. 2022). Shahabi et al. (2021) employed a deep belief–back propagation–genetic algorithm for Iran's Haraz watershed to generate flood susceptibility modelling (FSM). It was compared with other benchmarking ML techniques and found to be superior. Abedi et al. (2022) implemented the classification and regression tree (CART), XGBoost, random forest (RF), and boosted regression trees (BRT) to create an FSM of the Bâsca Chiojdului river basin. RF was found to be the best. Antzoulatos et al. (2022) employed RF, support vector machine (SVM), naive-based RF, and neural networks (NNs) to assess flood susceptibility in the Trieste, Monfalcone, and Muggia municipalities, northeast Italy. The RF model was highly rated with an F1 score of 0.99, followed by SVM, naive-based RF, and NN. Taromideh et al. (2022) reviewed ML applications to flood aspects at length. CART, RF, BRT, and several other models were employed to create an urban flood risk map for a case study in Iran. CART performed better than other ML algorithms.

General circulation models (GCMs) and associated representative concentration pathways (RCPs) are utilized for climate-based study. They help reproduce the historic observed climatic changes. Zennaro et al. (2021) studied the role of ML algorithms in climate change risk assessment and provided future directions. Chakrabortty et al. (2021) assessed flood susceptibility based on artificial neural networks (ANNs), deep boost (DB), and deep learning neural network in a climate change perspective for a case study in West Bengal, India. DB is the most preferred when compared with the others. They also studied flood susceptibility in detail in climate change scenarios. In summary, ML algorithms predict flood susceptibility but not flood depth (or building risk), which only hydraulic models can handle.

A few researchers have considered building risk an essential objective in vulnerability assessment for urban cities (Hossain & Meng 2020). It could be computed with inundation areas and flood depth information at the location. Park et al. (2021) studied flood risk assessment in Ulsan City, South Korea, using Hydrologic Engineering Center River Analysis System 2D (HEC-RAS 2D) for 2016. The inundated area was found to be 0.01–11.71 km2, and the average flood depth for each administrative district was 0.47–1.20 m. A total of 20.6% of buildings were exposed to flood, resulting in high flood damage. Chen et al. (2022) assessed the flood risk map of Taiwan under RCP 8.5. It was concluded that approximately 14% of townships had high-risk buildings (HRBs). Ventimiglia et al. (2020) suggested waterproofing measures for the Mela River in northeastern Sicily, and Alabbad et al. (2022) for Iowa Middle Cedar Watershed to reduce property vulnerability and losses that would minimize building risk.

It is understood from the mentioned literature that both flood susceptibility and building risk are considered individually to judge the effect of flood. In this context, it is felt that by a combined index that considers flood susceptibility and building risk simultaneously, the impact of flood and possible mitigation measures can be understood holistically, which is the primary focus of this article. The authors propose flood-susceptibility-based building risk (FSBR) that addresses the mentioned challenge. Accordingly, the following objectives are formulated in the RCP 2.6 scenario:

  • (i)

    Computation of FSBR

  • (ii)

    Computation of cost of waterproofing that mitigates FSBR

The framework is applied to Greater Hyderabad Municipal Corporation (GHMC), India, due to its high population density and proneness to urban floods. The city has suffered major floods, and related details are presented in Table 1 (Rangari et al. 2021). Details of the case study are presented in the next section.

Table 1

Details of year and rainfall, flood water depth, and damage to the city of Hyderabad

Year and dateDetails of rainfall (mm)Flood water depth (m)Representative impactsReferences
26 August 2000 241.5 2–4 Damage to houses/livelihood/number of people affected/financial loss Hyderabad floods 2000  
8 August 2006 220.7 0–1 Hyderabad floods 2006  
9–10 August 2008 137 2–3 Rangari et al. (2021)  
23 September 2016 165 1–3 Hyderabad floods 2016  
25 September 2019 133 1–2  Hyderabad floods 2019  
14 October 2020 300 1–4  Hyderabad floods 2020  
8 October 2021 150 1–4  Hyderabad floods 2021  
Year and dateDetails of rainfall (mm)Flood water depth (m)Representative impactsReferences
26 August 2000 241.5 2–4 Damage to houses/livelihood/number of people affected/financial loss Hyderabad floods 2000  
8 August 2006 220.7 0–1 Hyderabad floods 2006  
9–10 August 2008 137 2–3 Rangari et al. (2021)  
23 September 2016 165 1–3 Hyderabad floods 2016  
25 September 2019 133 1–2  Hyderabad floods 2019  
14 October 2020 300 1–4  Hyderabad floods 2020  
8 October 2021 150 1–4  Hyderabad floods 2021  

Study area and data collection

The GHMC area is 625 km2 and is divided into various zones and circles (Greater Hyderabad Municipal Corporation 2023). The annual average rainfall is 840 mm and is at the maximum from June to September, leading to heavy flash floods. Average temperatures during winter and summer are 22 and 30 °C. The mean hottest and coldest months are May and December, respectively. The average annual rainy days and dry days are 56 and 265. The average maximum and minimum relative humidities in winter are 79% and 31%, whereas those in summer are 67% and 26%, respectively (TSDPS 2021).

GHMC falls in the Musi River catchment (Figure 1(a)). The altitude ranges from 456 to 637 m, as shown in Figure 1(b). Slope ranges from 0.3 to 19.82°. The slope falls gradually from west to east, leading to the valley near the Musi River. The water bodies in the catchment act as storage reservoirs for drinking water and groundwater recharge. GHMC has three major storage reservoirs: Osman Sagar, Himayat Sagar, and Hussain Sagar, besides a minor one, Mir Alam Tank, as shown in Figure 1(a). These add flora and fauna to the catchment, increasing the catchment's ecology. There was a rapid increase in the impervious percentage from 2006 to 2016. The present research considered climate change aspects based on GCM, GFDL-CM3, and RCP 2.6. Extreme rainfall of 1,740.62 mm, likely to occur in 2040 for RCP 2.6 (three-day event, July 23–25), is considered a high-intensity, short-duration rainfall for this purpose. The following data are used for the modelling (Table 2).
Table 2

Data and its sources

DataSources
GCM and pathway GFDL-CM3 and RCP 2.6 
The future extreme rainfall event 1,740.62 mm (likely to occur over three days in 2040) 
Rainfall data India Meteorological Department and GHMC 
Soil data Directorate of Agricultural Commissionerate, Telangana 
Digital elevation The United States Geological Survey 
Curve number land use data, GHMC, and Open Street maps 
Evapotranspiration, land surface temperature, normalized density vegetative index MODerate Resolution Imaging Spectroradiometer (MODIS) of Google Earth Engine (GEE) 
Flood locations GHMC Disaster Management Cell and National Remote Sensing Centre (NRSC) 
Cost of waterproofing Telangana Public Health and Municipal Engineering Department (TGPHMED 2021
DataSources
GCM and pathway GFDL-CM3 and RCP 2.6 
The future extreme rainfall event 1,740.62 mm (likely to occur over three days in 2040) 
Rainfall data India Meteorological Department and GHMC 
Soil data Directorate of Agricultural Commissionerate, Telangana 
Digital elevation The United States Geological Survey 
Curve number land use data, GHMC, and Open Street maps 
Evapotranspiration, land surface temperature, normalized density vegetative index MODerate Resolution Imaging Spectroradiometer (MODIS) of Google Earth Engine (GEE) 
Flood locations GHMC Disaster Management Cell and National Remote Sensing Centre (NRSC) 
Cost of waterproofing Telangana Public Health and Municipal Engineering Department (TGPHMED 2021
Figure 1

(a) Watershed area of GHMC (modified and adapted from GHMC; numbers indicating storm water zones) and (b) elevation map of GHMC.

Figure 1

(a) Watershed area of GHMC (modified and adapted from GHMC; numbers indicating storm water zones) and (b) elevation map of GHMC.

Close modal

Description of methods employed and modelling ahead

The present article is a logical extension of the previous works of the authors (Madhuri et al. 2021a, 2021b), where information about modelling was discussed in detail for GHMC. Five ML algorithms, SVM, logistic regression (LR), K-nearest neighbour (KNN), AdaBoost, and XGBoost, are applied to understand the flood susceptibility of GHMC for historical data. Eight flood-influencing factors were used for this purpose. The area under the receiver operating characteristic (AUROC) is one of the standard methods for validating the model's performance (Tehrany et al. 2015). It is a graphical approach that describes the change in the algorithm's classification ability, as the probability threshold is altered (Shahabi et al. 2021). It compares and validates ML algorithms.

XGBoost is found to be the best, with a mean AUROC score of 0.83 and a standard deviation of 0.04. It is closely followed by AdaBoost, which has a mean AUROC score of 0.82 with a standard deviation of 0.04. Both algorithms significantly outperformed LR, SVM, and KNN with respective AUROC scores of 0.71, 0.74, and 0.77. Corresponding standard deviations are 0.07, 0.06, and 0.06.

Later, the study was analysed in climate change situations, as mentioned in the study area section. The flood susceptibilities generated from XGBoost for RCP 2.6 are classified into two different ranges, i.e., 30%–70% as moderate (M) and 70%–100% as high susceptibility (H), respectively. The 30% flood susceptibility value indicates a 30% chance of flooding in that location/pixel.

Furthermore, HEC-RAS 2D was employed to compute the submergence area and flood-depth-based building risk. Three levels, namely, low-risk buildings (LRBs), medium-risk buildings (MRBs), and HRBs were categorized. Corresponding flood depths are <0.5 m, ≥0.5 m and <1 m, ≥1 m (Abdulrazzak et al. 2019; Rangari et al. 2019; Rangari et al. 2021). Figure 2 presents the workflow for generating FSBR (Madhuri 2022).
Figure 2

Workflow for generating FSBR.

Figure 2

Workflow for generating FSBR.

Close modal

If building risk due to flood depth obtained by HEC-RAS 2D is high (H) and flood susceptibility obtained by ML algorithm is high (H), it is termed HH in the context of FSBR. It is high-priority combination that needs immediate action for mitigation measures by policy-makers. Suppose two buildings with high risk are situated in medium- and low-susceptibility areas; in that case, the priority is a medium-susceptible area. Six combinations of FSBR, namely, high building risk and high flood susceptibility (HH), high and medium (HM), medium and medium (MM), medium and high (MH), low and medium (LM), and low and high (LH) are employed to study the urban floods. Results related to flood susceptibility, building risk, and FSBR are discussed in the next section.

Flood susceptibility using XGBoost

Table 3 presents zone-wise flood areas of buildings and roads under high, moderate, and low flood susceptibilities. Zones 12, 8, and 15 are highly susceptible, with exposed building areas of 14.61, 7.75, and 7.27 km2, respectively. In the case of roads, zones 12, 5, and 13 are highly susceptible, with areas of 3.52, 3.11, and 2.65 km2, respectively. In moderate susceptibility, buildings in zones 13, 15, and 12 are exposed in areas of 5.97, 4.74, and 4.29 km2, respectively. In the case of roads, exposed zones are 12, 13, and 8, with areas of 6.41, 4.48, and 3.29 km2, respectively. None of the zones have low flood susceptibility. Buildings and roads are highly susceptible in GHMC, with areas of 57.59 and 22.76 km2.

Table 3

Flood-susceptible areas (in km2) for RCP 2.6 (Madhuri et al. 2021a)

Zone number (1)Buildings
Roads
High (2)Medium (3)High (4)Medium (5)
1.9 1.49 1.52 0.44 
0.21 0.49 
1.88 0.41 1.34 0.58 
1.65 2.94 1.23 1.2 
6.29 1.25 3.11 2.38 
0.74 0.4 0.79 1.11 
1.31 0.32 0.55 0.91 
7.75 2.24 2.35 3.29 
0.12 0.09 0.08 0.21 
10 3.54 1.65 1.23 1.84 
11 1.12 0.75 0.43 0.92 
12 14.61 4.29 3.52 6.41 
13 6.84 5.97 2.65 4.48 
14 1.91 0.64 0.79 1.19 
15 7.27 4.74 2.32 2.71 
16 0.45 0.15 0.36 0.21 
Total (GHMC) 57.59 27.33 22.76 27.88 
Zone number (1)Buildings
Roads
High (2)Medium (3)High (4)Medium (5)
1.9 1.49 1.52 0.44 
0.21 0.49 
1.88 0.41 1.34 0.58 
1.65 2.94 1.23 1.2 
6.29 1.25 3.11 2.38 
0.74 0.4 0.79 1.11 
1.31 0.32 0.55 0.91 
7.75 2.24 2.35 3.29 
0.12 0.09 0.08 0.21 
10 3.54 1.65 1.23 1.84 
11 1.12 0.75 0.43 0.92 
12 14.61 4.29 3.52 6.41 
13 6.84 5.97 2.65 4.48 
14 1.91 0.64 0.79 1.19 
15 7.27 4.74 2.32 2.71 
16 0.45 0.15 0.36 0.21 
Total (GHMC) 57.59 27.33 22.76 27.88 

Note: No buildings and roads are in the low-susceptibility category.

Building risk based on HEC-RAS 2D

Information about flood inundation mapping, flood depth, and building risk are presented in Table 4. The most vulnerable locations to flooding are situated near the Hussain Sagar and Musi River.

Table 4

Percentage of flooded and non-flooded zones and zone-wise flood depth ranges and percentage of HRB, MRB, and LRB for RCP 2.6 (Madhuri et al. 2021b)

Zone number (1)% Flooding (2)% Non-flooding (3)Flood depth range (m) (4)% HRB (5)%MRB (6)%LRB (7)
81 19 0.3–5.7 69 23 
71 29 0.1–2.0 42 16 42 
64 36 0.1–1.9 38 18 44 
70 30 0.1–2.1 50 15 35 
75 25 0.2–5.8 70 21 
69 31 0.1–4.6 65 26 
68 32 0.1–4.1 64 28 
61 39 0.1–4.3 49 12 39 
62 38 0.1–2.3 39 12 49 
10 69 31 0.1–2.1 40 15 45 
11 61 39 0.1–1.9 40 16 44 
12 62 38 0.3–8.0 41 15 44 
13 65 35 0.2–6.8 51 14 35 
14 62 38 0.1–1.6 38 17 45 
15 69 31 0.2–5.1 55 12 33 
16 70 30 0.1–1.9 64 10 26 
GHMC 67 33 0.1–8.0 51 13 36 
Zone number (1)% Flooding (2)% Non-flooding (3)Flood depth range (m) (4)% HRB (5)%MRB (6)%LRB (7)
81 19 0.3–5.7 69 23 
71 29 0.1–2.0 42 16 42 
64 36 0.1–1.9 38 18 44 
70 30 0.1–2.1 50 15 35 
75 25 0.2–5.8 70 21 
69 31 0.1–4.6 65 26 
68 32 0.1–4.1 64 28 
61 39 0.1–4.3 49 12 39 
62 38 0.1–2.3 39 12 49 
10 69 31 0.1–2.1 40 15 45 
11 61 39 0.1–1.9 40 16 44 
12 62 38 0.3–8.0 41 15 44 
13 65 35 0.2–6.8 51 14 35 
14 62 38 0.1–1.6 38 17 45 
15 69 31 0.2–5.1 55 12 33 
16 70 30 0.1–1.9 64 10 26 
GHMC 67 33 0.1–8.0 51 13 36 

Zones 1 and 5 have high percentage inundation areas of 81% and 75% as they are near the Musi River and exist in low-lying areas. Zone 11 has the least percentage of inundation area of 61% due to its high elevation level. Zones 12 and 13 have flood depths of 0.3–8 and 0.2–6.8 m. This is due to rapid urbanization in these zones. Zones 1, 5, 8, and 15 are equally vulnerable, with flood depth ranges of 0.3–5.7, 0.2–5.8, 0.1–4.3, and 0.2–5.1 m. This may be due to their proximity to the Musi River and its low elevation of 466–525 m. The ranges of zone-wise percentages of HRB, MRB, and LRB are 38%–70%, 8%–18%, and 21%–49%, respectively. The highest number of HRBs was found in Zone 5, followed by Zone 1. It can be found that there is a greater number of LRB in zones 9, 3, and 14, as these are at relatively higher elevations. Inundated area, flood depth, and percentage of HRB, MRB, and LRB, respectively, GHMC-wise, are 442.53 km2, 0.1–8 m, 51%, 13%, and 36%, respectively. The inundation area is 67%, more than half of the catchment area. This may be due to high-intensity, short-duration rainfall in the catchment.

The vulnerability of buildings due to flooding is assessed using a footprint map (Figure 3). It is the primary information needed to analyse the situation spatially during and after a flood. It is prepared using the images from Open Street maps and case-study-related data (Open Street Maps 2016). The raster images are geo-referenced and are then digitized into a vector format in the form of polygons. Each building has a unique identifier and is represented by a polygon. Identification helps divide the buildings by area, perimeter, location, or zone. The high, medium, and low flood depth data from HEC-RAS 2D are merged with the obtained vectorized building data. This overlaying of the building features provides the exact number of HRB, MRB, and LRB, as shown in Figure 3. It can be observed from Figure 3 that 51% of the buildings which are in red are HRB.
Figure 3

Building footprint map showing LRB–MRB–HRB as inundated with low, medium, and high flood depths.

Figure 3

Building footprint map showing LRB–MRB–HRB as inundated with low, medium, and high flood depths.

Close modal

Flood-susceptibility-based building risk

Efforts were made to study the FSBR regarding the total affected area (summation of rooftop area and surface area) and the number of affected buildings (Figures 4 and 5). It is to be noted that the higher the flood depth, the greater the total affected area and vice versa. Among the 16 zones, only 5, 8, 12, 13, and 15 are found to have high total affected areas as examined here. Other zones have less FSBR/less affected areas than the mentioned zones. The ML algorithm does not identify low flood susceptibility (Table 3). Hence HL, ML, and LL categories are not applicable here.
Figure 4

FSBR for total area affected for RCP 2.6 (numbers on top of bars are zone numbers, where the maximum affected area is observed).

Figure 4

FSBR for total area affected for RCP 2.6 (numbers on top of bars are zone numbers, where the maximum affected area is observed).

Close modal
Figure 5

FSBR for number of buildings affected for RCP 2.6 (numbers on top of bars are zone numbers, where maximum number of affected buildings are observed).

Figure 5

FSBR for number of buildings affected for RCP 2.6 (numbers on top of bars are zone numbers, where maximum number of affected buildings are observed).

Close modal

In the HH category, zones 5, 15, 12, and 3 have affected areas of 13.07, 10.04, 8.50, and 7.64 km2 with the corresponding number of buildings, 27,622, 30,850, 30,462, and 24,159, respectively. In contrast, the number of buildings in zone 9 is significantly less. This may be because of high elevation levels between 561 and 602 m. Zones 5 and 15 together occupied 36% of the total affected area. This may be due to their vicinity to the Musi River. In the HM category, zones 13, 12, 15, and 5 have 18,112, 16,148, 13,476, and 8,313 buildings with affected areas of 5.92, 4.85, 4.05, and 3.94 km2, respectively. Zones 2, 7, 9, and 14 are the least affected.

In the case of MH, zones 12, 13, 15, and 8 have 11,102, 6,353, 5,996, and 6,411 buildings with affected areas of 2.25, 1.28, 1.22, and 1.09 km2, respectively. Zones 12 and 13 have the highest curve number values, leading to high FSBR to flooding. In the MM category, zones 12, 13, 15, and 8 have 5,886, 4,732, 3,257, and 1,714 buildings with total affected areas of 1.36, 0.95, 0.66, and 0.46 km2, respectively. Zones 2, 6, 9, and 16 have fewer buildings affected by floods as they are very far from the Musi River or at high elevation levels. Also, they have fewer pervious areas than zones 12, 13, 15, and 8.

In the LH category, zones 12, 15, 13, and 8 have 12,075, 6,652, 6,288, and 4,445 buildings with total affected areas of 2.28, 1.20, 1.18, and 1.11 km2. Zones 12 and 15 occupy 25.1% and 13.83%, respectively, of the total affected buildings in this category.

Both these zones are more prone to flooding. In the LM category, zones 12, 13, 15, and 8 have total affected areas of 1.34, 0.88, 0.64, and 0.42 km2 with 6,338, 4,794, 3,624, and 1,825 buildings. Almost 26.6% and 20.16% of the total affected buildings are in zones 12 and 13, respectively. In the HH, HM, MH, and MM categories, the maximum total affected areas in zones 15, 13, 12, and 12 are 10.04, 5.92, 2.25, and 1.36 km2. The high slope of 19.13° for zone 15, areas near the Musi River, and the imperviousness of zone 12 are causes of urban flooding.

GHMC: In the case of the HH, HM, MH, MM, LH, and LM categories, the total affected areas are 63.40, 28.92, 9.52, 4.81, 9.26, and 4.56 km2 (totalling 120.47 km2) with 182,178, 84,136, 46,238, 22,691, 48,092, and 23,781 buildings (totalling 407,116). The least number of buildings and flood-affected areas are in the LM category.

Waterproofing for reducing FSBR

Waterproofing is the mechanism to restrain the entry of water into the walls and rooftops of a building (Kubal 2008). In addition, it will increase the life cycle of buildings considerably. It is employed to reduce the FSBR in terms of the total affected area and the number of exposed buildings (TGPHMED 2021). This demands the investment to reduce the affected areas/number of buildings to a minimum (equivalent annual cost (EAC) is computed (refer to Equation (1)):
(1)
where = capital investment, = discount rate, and = life of waterproofing. This provides comprehensive information about the required yearly investment. Here, the capital investment was established on the rooftop waterproofing and surface waterproofing, as presented in Equations (2)–(4):
(2)
(3)
(4)

Only salient points are described here to understand the impact of waterproofing measures on the affected area and exposed buildings.

Zone-wise analysis

Waterproofing costs for zones 5, 15, and 12 for the HH category are 538.71 cr, 413.91 cr, and 350.38 cr; and costs for the corresponding EAC/building are Rs 27,800, 19,100, and 16,400 (refer to column 14, Table 5). Zones 2, 3, and 14 require less EAC/building of 13,900, 12,500, and 12,800 (refer to column 14). EAC/building for zones 13, 15, and 12 in the HM category are 19,200, 17,700, and 17,600 (refer to column 15). These values in the MH category are 11,900, 12,000, and 11,900 (refer to column 16); those in MM are 11,900, 11,900, and 13,600 (refer to column 17); those in LH are 11,000, 10,700, and 11,100 (refer to column 18); and those in LM are 10,800, 10,500, and 12,400 (refer to column 19). A decrease in EAC/building is observed in MH compared with HM due to there being less affected area.

Table 5

Number of buildings, waterproofing cost, and EAC/building for RCP 2.6

Zone no. (1)No. of buildings
Cost (cr) Rs
EAC/building Rs
Total cost (Rs) (cr) (20)EAC/building/() (21)
HH (2)HM (3)MH (4)MM (5)LH (6)LM (7)HH (8)HM (9)MH (10)MM (11)LH (12)LM (13)HH (14)HM (15)MH (16)MM (17)LH (18)LM (19)
10,468 3,743 1,517 207 1,506 224 215.22 84.61 13.21 2.05 12.38 1.82 29,300 32,200 12,400 14,100 11,700 11,600 329.28 26,500 
644 254 278 6.30 0.00 1.93 0.00 1.74 0.00 13,900 10,800 8,900 9.97 12,100 
5,718 1,304 2,659 654 2,595 645 50.00 10.98 18.45 3.91 15.23 3.41 12,500 12,000 9,900 8,500 8,400 7,500 101.98 10,700 
9,353 5,125 2,687 1,490 2,477 1,645 115.30 62.32 21.83 11.95 26.36 12.95 17,600 17,300 11,600 11,400 15,200 11,200 250.71 15,700 
27,622 8,313 3,282 1,147 3,354 1,129 538.71 162.51 24.61 7.57 22.04 6.43 27,800 27,800 10,700 9,400 9,400 8,100 761.88 24,200 
3,394 2,091 418 320 421 229 52.59 28.42 3.51 2.13 3.11 1.42 22,100 19,300 12,000 9,500 10,500 8,800 91.18 18,900 
4,741 1,627 792 73 811 78 95.57 39.20 6.61 0.61 5.79 0.37 28,700 34,300 11,900 11,800 10,200 6,800 148.15 26,000 
17,691 6,411 4,294 1,714 4,445 1,825 252.22 99.89 45.24 18.98 45.74 17.45 20,300 22,200 15,000 15,800 14,700 13,600 479.52 18,800 
381 84 96 43 175 54 3.74 2.36 0.77 0.51 1.24 0.84 14,000 40,000 11,400 17,000 10,100 22,100 9.46 16,200 
10 7,349 3,880 2,951 1,566 3,074 1,538 102.63 48.16 29.96 14.02 25.75 12.29 19,900 17,700 14,500 12,800 11,900 11,400 232.82 16,300 
11 2,985 1,782 1,215 683 1,323 689 31.17 20.14 9.31 6.57 10.01 6.04 14,900 16,100 10,900 13,700 10,800 12,500 83.25 13,700 
12 30,462 16,148 11,102 5,886 12,075 6,338 350.38 199.96 93.07 56.31 94.13 55.41 16,400 17,600 11,900 13,600 11,100 12,400 849.26 14,700 
13 24,159 18,112 6,353 4,732 6,288 4,794 314.96 243.95 53.00 39.40 48.66 36.43 18,600 19,200 11,900 11,900 11,000 10,800 736.40 16,300 
14 5,639 1,900 2,514 900 2,491 944 50.63 16.48 17.46 5.92 16.49 5.36 12,800 12,400 9,900 9,400 9,400 8,100 112.34 11,100 
15 30,850 13,476 5,996 3,257 6,652 3,624 413.91 167.26 50.65 27.31 49.77 26.66 19,100 17,700 12,000 11,900 10,700 10,500 735.57 16,400 
16 722 140 108 19 127 25 18.97 5.37 2.79 1.00 3.34 1.35 37,400 54,600 36,800 75,000 37,500 77,100 32.83 41,000 
Total 182,178 84,136 46,238 22,691 48,092 23,781 2,612.31 1,191.60 392.40 198.24 381.80 188.25       4,964.6  
Zone no. (1)No. of buildings
Cost (cr) Rs
EAC/building Rs
Total cost (Rs) (cr) (20)EAC/building/() (21)
HH (2)HM (3)MH (4)MM (5)LH (6)LM (7)HH (8)HM (9)MH (10)MM (11)LH (12)LM (13)HH (14)HM (15)MH (16)MM (17)LH (18)LM (19)
10,468 3,743 1,517 207 1,506 224 215.22 84.61 13.21 2.05 12.38 1.82 29,300 32,200 12,400 14,100 11,700 11,600 329.28 26,500 
644 254 278 6.30 0.00 1.93 0.00 1.74 0.00 13,900 10,800 8,900 9.97 12,100 
5,718 1,304 2,659 654 2,595 645 50.00 10.98 18.45 3.91 15.23 3.41 12,500 12,000 9,900 8,500 8,400 7,500 101.98 10,700 
9,353 5,125 2,687 1,490 2,477 1,645 115.30 62.32 21.83 11.95 26.36 12.95 17,600 17,300 11,600 11,400 15,200 11,200 250.71 15,700 
27,622 8,313 3,282 1,147 3,354 1,129 538.71 162.51 24.61 7.57 22.04 6.43 27,800 27,800 10,700 9,400 9,400 8,100 761.88 24,200 
3,394 2,091 418 320 421 229 52.59 28.42 3.51 2.13 3.11 1.42 22,100 19,300 12,000 9,500 10,500 8,800 91.18 18,900 
4,741 1,627 792 73 811 78 95.57 39.20 6.61 0.61 5.79 0.37 28,700 34,300 11,900 11,800 10,200 6,800 148.15 26,000 
17,691 6,411 4,294 1,714 4,445 1,825 252.22 99.89 45.24 18.98 45.74 17.45 20,300 22,200 15,000 15,800 14,700 13,600 479.52 18,800 
381 84 96 43 175 54 3.74 2.36 0.77 0.51 1.24 0.84 14,000 40,000 11,400 17,000 10,100 22,100 9.46 16,200 
10 7,349 3,880 2,951 1,566 3,074 1,538 102.63 48.16 29.96 14.02 25.75 12.29 19,900 17,700 14,500 12,800 11,900 11,400 232.82 16,300 
11 2,985 1,782 1,215 683 1,323 689 31.17 20.14 9.31 6.57 10.01 6.04 14,900 16,100 10,900 13,700 10,800 12,500 83.25 13,700 
12 30,462 16,148 11,102 5,886 12,075 6,338 350.38 199.96 93.07 56.31 94.13 55.41 16,400 17,600 11,900 13,600 11,100 12,400 849.26 14,700 
13 24,159 18,112 6,353 4,732 6,288 4,794 314.96 243.95 53.00 39.40 48.66 36.43 18,600 19,200 11,900 11,900 11,000 10,800 736.40 16,300 
14 5,639 1,900 2,514 900 2,491 944 50.63 16.48 17.46 5.92 16.49 5.36 12,800 12,400 9,900 9,400 9,400 8,100 112.34 11,100 
15 30,850 13,476 5,996 3,257 6,652 3,624 413.91 167.26 50.65 27.31 49.77 26.66 19,100 17,700 12,000 11,900 10,700 10,500 735.57 16,400 
16 722 140 108 19 127 25 18.97 5.37 2.79 1.00 3.34 1.35 37,400 54,600 36,800 75,000 37,500 77,100 32.83 41,000 
Total 182,178 84,136 46,238 22,691 48,092 23,781 2,612.31 1,191.60 392.40 198.24 381.80 188.25       4,964.6  

EAC/building for the HM category for zones 3 and 14 are Rs 12,000 and 12,400. These buildings have larger surface areas than those in the MH, MM, LH, and LM categories. Due to this, EAC/building is higher than in the mentioned categories (refer to column 15). Waterproofing costs (summation of all categories) of zones 5, 12, 13, and 15 are 761.88 cr, 849.26 cr, 736.40 cr, and 735.57 cr. The cost of the corresponding EAC/building is 24,200, 14,700, 16,300, and 16,400 (refer to columns 20–21).

GHMC: HH, HM, MH, MM, LH, and LM category buildings require an investment of 2,612.31 cr, 1,191.60 cr, 392.40 cr, 198.24 cr, 381.80 cr, and 188.25 cr (refer to column 8–13) and the total cost of waterproofing is 4,964.6 cr. On average, 17,400 as EAC/ building can be invested in preparedness for urban floods. As a note, HEC-RAS 2D provides limited information on high, medium, and low building risks. On the other hand, the FSBR has three options related to high risk (HH, HM, HL), medium risk (MH, MM, ML), and low risk (LH, LM, LL). This flexibility in decision-making makes FSBR preferable over individual usage of XGBoost and HEC-RAS 2D. A brief discussion to prove the potentiality of FSBR is as follows: HH covers 35% of the submergible building area and requires 2,612.31 cr for waterproofing. These values for HM are 16% and 1,191.60 cr, whereas HRB covers 51% and 3,808.91 cr. This gives an edge to policy-makers even in demarcating HRB into two categories and provides leverage while prioritizing the critical buildings for mitigation measures when the budget is limited. Similar inferences can be drawn for other categories.

There can be different ways for possible funding and its operations to encourage citizens to explore waterproofing measures, which are as follows:

  • The tax benefits for implementing waterproofing measures can be provided to the house owner. This can be 1%–2% of the construction cost. This will encourage an individual to invest in waterproofing measures.

  • Flood insurance/waterproofing bonds can be a better option for encouraging house owners to invest in waterproofing measures. This will enable people to safeguard their houses and families from a catastrophe.

  • Use corporate social responsibility funds to safeguard public buildings against flood risk.

Urban floods have been highly prominent natural disasters occurring in catchments across the globe. This requires effective and sustainable mitigation mechanisms to minimize damage. In this context, a holistic approach, FSBR, is proposed by fusing XGBoost and HEC-RAS 2D (that provides building risk) in climate change situations and is applied to GHMC, India. The following conclusions are drawn:

  • Buildings and roads have high susceptible areas of 57.59 and 22.76 km2.

  • The inundated area is 442.53 km2, with ranges of flood depth being 0.1–8 m.

  • Percentages of HRB, MRB, and LRB, respectively, are 38%–70%, 8%–18%, and 21%–49%.

  • Total affected areas for HH, HM, MH, MM, LH, and LM are 63.40, 28.92, 9.52, 4.81, 9.26, and 4.56 km2 totalling 120.47 km2. Corresponding buildings are 182,178, 84,136, 46,238, 22,691, 48,092, and 23,781, totalling 407,116. The total cost of waterproofing is 4,964.60 cr.

This is the first-time application where ML and hydraulic modelling are complemented to derive an indicator, FSBR, for the urban catchment. The aim of this study is not to replicate the previous research works, but to give a new framework to researchers interested in this research area.

Data cannot be made publicly available; readers should contact the corresponding author for details.

The authors declare there is no conflict.

Abdulrazzak
M.
,
Elfeki
A.
,
Kamis
A.
,
Kassab
M.
,
Alamri
N.
,
Chaabani
A.
&
Noor
K.
2019
Flash flood risk assessment in urban arid environment: case study of Taibah and Islamic universities' campuses, Medina, Kingdom of Saudi Arabia
.
Geomatics, Natural Hazards and Risk
10
(
1
),
780
796
.
Abedi
R.
,
Costache
R.
,
Shafizadeh-Moghadam
H.
&
Pham
Q. B.
2022
Flash-flood susceptibility mapping based on XGBoost, random forest and boosted regression trees
.
Geocarto International
37
(
19
),
5479
5496
.
doi:10.1080/10106049.2021.1920636
.
Alabbad
Y.
,
Yildirim
E.
&
Demir
I.
2022
Flood mitigation data analytics and decision support framework: Iowa Middle Cedar Watershed case study
.
Science of the Total Environment
814
,
152768
.
doi:10.1016/j.scitotenv.2021.152768
.
Antzoulatos
G.
,
Kouloglou
I.-O.
,
Bakratsas
M.
,
Moumtzidou
A.
,
Gialampoukidis
I.
,
Karakostas
A.
,
Lombardo
F.
,
Fiorin
R.
,
Norbiato
D.
,
Ferri
M.
,
Symeonidis
A.
,
Vrochidis
S.
&
Kompatsiaris
I.
2022
Flood hazard and risk mapping by applying an explainable machine learning framework using satellite imagery and GIS data
.
Sustainability
14
(
6
),
3251
.
Baghbani
A.
,
Choudhury
T.
,
Costa
S.
&
Reiner
J.
2022
Application of artificial intelligence in geotechnical engineering: a state of the art review
.
Earth-Science Reviews
228
,
103991
.
Bengaluru floods
2021
Bengaluru rain fury: Lakes overflow, Yelahanka faces the brunt. The Hindu (23 November 2021)
. .
Chakrabortty
R.
,
Pal
S. C.
,
Janizadeh
S.
,
Santosh
M.
,
Roy
P.
,
Chowdhuri
I.
&
Saha
A.
2021
Impact of climate change on future flood susceptibility: an evaluation based on deep learning algorithms and GCM model
.
Water Resources Management
35
(
12
),
4251
4274
.
Chen
Y. J.
,
Lin
H. J.
,
Liou
J. J.
,
Cheng
C. T.
&
Chen
Y. M.
2022
Assessment of flood risk map under climate change RCP 8.5 scenarios in Taiwan
.
Water
14
(
2
),
207
.
Chennai floods
2021
Chennai floods map: Where flooding has hit India and latest weather forecast after record rains. i (10 November 2021)
. .
Flood Report
2021
Report of the Committee Constituted for Formulation of Strategy for Flood Management Works in Entire Country and River Management Activities and Works Related to Border Areas (2021–26)
.
NITI Aayog, New Delhi, India. Available from: https://www.niti.gov.in/sites/default/files/2021–03/Flood-Report.pdf (accessed April 2022)
.
Greater Hyderabad
Municipal Corporation
2023
Greater Hyderabad Municipal Corporation Zones and Circles. Available from: https://www.ghmc.gov.in/Documents/Zones.pdf (accessed 10 February 2023)
.
Hammond
M. J.
,
Chen
A. S.
,
Djordjević
S.
,
Butler
D.
&
Mark
O.
2015
Urban flood impact assessment: a state-of-the-art review
.
Urban Water Journal
12
(
1
),
14
29
.
Hyderabad floods
2000
Hyderabad floods: What caused deluge in 2000 and GSI's suggestions for future prevention
.
Financial Express
.
Hyderabad floods
2006
Explained: Why floods occur in Hyderabad
.
The Times of India
.
Hyderabad floods
2016
India – 11 dead in Telangana floods, dams remain dangerously high. FloodList (28 September 2016)
.
Hyderabad floods
2019
When Musi rose in fury: 111 years later, history serves as a reminder. The Times of India (29 September 2019)
.
Hyderabad floods
2020
Record rainfall of 300mm in 24 hours caused flash floods in Hyderabad, neighbouring districts. News18 (14 October 2020)
.
Hyderabad floods
2021
Major traffic hurdles, low-lying areas inundated with a spell of rain lashed in Hyderabad. Hyderabad News (9 October 2021)
.
Kubal
M. T.
2008
Construction Waterproofing Handbook
, 2nd edn.
McGraw-Hill
,
New York, USA
.
Madhuri
R.
2022
Risk Assessment and Mitigation Strategies for Urban Floods under Climate Change
.
PhD thesis
,
BITS Pilani, Rajasthan
,
India
.
Madhuri
R.
,
Sistla
S.
&
Srinivasa Raju
K.
2021a
Application of machine learning algorithms for flood susceptibility assessment and risk management
.
Journal of Water and Climate Change
12
(
6
),
2608
2623
.
Madhuri
R.
,
Sarath Raja
Y. S. L.
,
Srinivasa Raju
K.
,
Punith
B. S.
&
Manoj
K.
2021b
Urban flood risk analysis of buildings using HEC-RAS 2D in climate change framework
.
H2Open Journal
4
(
1
),
262
275
.
Mumbai floods
2021
Red alert in Mumbai, chances of over 200mm rain in some parts till July 22. Hindustan Times (21 July 2021)
. .
Open Street Maps
2016
GIS Maps Available from Open Street Maps
.
Available from: https://download.geofabrik.de/asia/india.html (accessed July 2017)
.
Park
K.
,
Choi
S.-H.
&
Yu
I.
2021
Risk type analysis of building on urban flood damage
.
Water
13
(
18
),
2505
.
Rangari
V. A.
,
Umamahesh
N. V.
&
Bhatt
C. M.
2019
Assessment of inundation risk in urban floods using HEC RAS 2D
.
Modeling Earth Systems and Environment
5
(
4
),
1839
1851
.
Rangari
V. A.
,
Bhatt
C. M.
&
Umamahesh
N. V.
2021
Rapid assessment of the October 2020 Hyderabad urban flood and risk analysis using geospatial data
.
Current Science
120
(
12
),
1840
1847
.
Saha
S.
,
Gayen
A.
&
Bayen
B.
2022
Deep learning algorithms to develop flood susceptibility map in data-scarce and ungauged river basin in India
.
Stochastic Environmental Research and Risk Assessment
36
(
10
),
3295
3310
.
Sahany
S.
,
Venugopal
V.
&
Nanjundiah
R. S.
2010
The 26 July 2005 heavy rainfall event over Mumbai: numerical modeling aspects
.
Meteorology and Atmospheric Physics
109
(
3
),
115
128
.
Shahabi
H.
,
Shirzadi
A.
,
Ronoud
S.
,
Asadi
S.
,
Pham
B. T.
,
Mansouripour
F.
,
Geertsema
M.
,
Clague
J. J.
&
Bui
D. T.
2021
Flash flood susceptibility mapping using a novel deep learning model based on deep belief network, back propagation and genetic algorithm
.
Geoscience Frontiers
12
(
3
),
101100
.
Taromideh
F.
,
Fazloula
R.
,
Choubin
B.
,
Emadi
A.
&
Berndtsson
R.
2022
Urban flood risk assessment: integration of decision making and machine learning
.
Sustainability
14
(
8
),
4483
.
TGPHMED
2021
Common Schedule of Rates as per TS Standard Data for the Year 2022–23
.
Government of Telangana, Hyderabad, India. Available from: https://publichealth.telangana.gov.in/getInfo.do?dt=2&id=221&oId=222 (accessed 4 April 2021)
.
TSDPS
2021
Weather and Climatology of Telangana
.
Available from: https://tsdps.telangana.gov.in/ (accessed August 2021)
.
Vadodara floods
2019
Cloudburst in Vadodara: 424 mm rainfall in six hours; city flooded, schools closed. weather.com (31 July 2019)
. .
Zennaro
F.
,
Furlan
E.
,
Simeoni
C.
,
Torresan
S.
,
Aslan
S.
,
Critto
A.
&
Marcomini
A.
2021
Exploring machine learning potential for climate change risk assessment
.
Earth-Science Reviews
220
,
103752
.
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