Keywords

1 Introduction

Located by Nha Be River and within 30 km from the South China Sea, Nha Be District is one of the outer districts of Ho Chi Minh City (HCMC) that has undergone severe urban flooding caused by multiple factors such as its topography (Asian Development Bank 2010; Tran TN 2011), a large and growing impervious area due to urban expansion (Vietnam Climate Adaptation Partnership 2013), and so on. In the context of climate change, Nha Be is highly vulnerable to sea-level rise, tides from rivers, and ground subsidence (Nguyen 2016). It is necessary to understand the frequency, intensity, and impacts of the floods on living quality, commuting, and housing quality for residents, as well as the solutions implemented by homeowners, the community, and the local government. On that basis, the following research proposes solutions for how best to adapt to climate change and flooding.

This paper summarizes certain findings from a quantitative study on the frequency, intensity, and impacts of floods on the locals and local housing, as well as the multi-scale responses from various stakeholders. Among the methods, a survey was used to collect data from one town and six communes (wards) of Nha Be District with the participation of 30 households in each ward. The research objectives are to understand urban flooding in Nha Be District in the context of climate change and support further suggestions and recommendations for this urban area. Also, this research aims to help communities and local authorities take initiative and adapt to climate change and urban flooding.

2 Study Area

Located in the southeast of HCMC, Nha Be District spreads out over an area of 100 km2 and includes one town (Nha Be) and six wards (Hiep Phuoc, Long Thoi, Nhon Duc, Phu Xuan, Phuoc Kien, and Phuoc Loc). Among them, Nha Be Town is the administration and business center that is the most urbanized. Situated near several industrial zones, export processing zones, and on the main gate to the city, Nha Be, Hiep Phuoc, Phuoc Kien, and Phu Xuan are the most populated areas in the district.

Due to its topography, this district consists of low-lying terrain that partly helps drain water out of the city center (Tran TN 2014). However, the recent rapid urbanization has transformed this outer district significantly, reducing its capacity for water storage and drainage. Since its infrastructure has not been well developed, the development of Nha Be has resulted in several issues for the district, including flood inundation. This entire district is estimated to be at risk of flooding due to the backfill projects along Sai Gon, Dong Nai, and Soai Rap River (Bui and Nguyen 2015). Additionally, due to the various impacts of climate change, housing in Nha Be District has suffered, seriously threatening people’s safety and quality of life. Within the district, the most intense flooding has been recorded in the neighborhoods located along Le Van Luong, Huynh Tan Phat, and Nguyen Binh Street (Ngo et al. 2019; Vietnam Climate Adaptation Partnerships 2013).

Due to these impacts, several projects have been implemented involving flood reduction and mitigation efforts at multiple scales. Besides the efforts from the government, people living in Nha Be District have used various approaches to respond to floods. However, due to the mentioned topographic characteristics, the complexity of climate change, flooding, and other factors, still threatens harmful damage to the area.

3 Methodology

Data was collected by questionnaire and in-depth interviews conducted in one town and six communes (wards) of Nha Be District. The questionnaire was structured with four main parts (See Appendix). Part 1 aimed to collect the background information of respondents who imply their knowledge of the studied area, their houses, the flood situation, and their desires. Part 2 asks for their housing details relating to physical attributes such as, construction, renovation, and their evaluation of the house condition as it relates to their accommodation demands. Part 3 consists of questions regarding flood situations with information about frequency, intensity, sea-level rise, causes, and effects. Part 4 includes concerns about the previous solutions suggested by multi-stakeholders at housing and neighborhood scales. This study focuses on analyzing the results of Part 3 and 4 and uses the information attained from Part 1 and 2 for reference if necessary. The in-depth interviews mainly discussed the actions taken by the local governments, through the perspectives of community representatives and land management officers, to deal with floods over time. There were 210 survey respondents from households and 14 in-depth interviews from community representatives and land management officers at the mentioned administration units. Regarding the sampling size, Nha Be District's population is about 76,985 people (According to the data of the 2019 Census). The sampling size is calculated with a confidence level of 93%, and the tolerance is within 7%. The number of questionnaires is calculated by the formula for calculating sample size as follows:

$$n = \frac{N}{{1 + N*e^{2} }}$$

Note:

n: the number of units of the sample population.

N: the number of general units (N = 76,985).

e: the tolerance.

The tolerance (e) was chosen is 7%, the result for n = 203.5 samples. Rounded out 210 samples for one town and six communes (wards) of Nha Be District.

Besides a questionnaire, a guided observation was also used to record the related information in the survey by taking photos.

Data evaluation and analysis were implemented by descriptive statistical methods with support from IBM SPSS software (Ngo 2020). Multiple percentage calculation was mainly used to process data from the questionnaire that included a percentage of identical answers among the sample size and accumulative percentage.

4 Results

4.1 Frequency and Intensity

The findings in Fig. 4 show that flooding is a phenomenon that has been occurring in all wards of Nha Be District for more than ten years. In general, approximately 50% of the surveyed population reported that floods frequently take place in Nha Be District, while nearly half of the respondents just experienced floods at a specific time of the year, mainly during the rainy season. In addition, the study found that there are differences in flood frequency in different wards. Figure 4 provides the whole picture of floods taking place in Nha Be District; in which Nha Be town, which has the highest rate of urbanization, has the most frequent flooding (86.2%), followed by Nhon Duc, Phuoc Kien, and Phuoc Loc (57.2%, 55.6%, and 52%, respectively). Flooding happens more frequently in the rainy season, especially in Hiep Phuoc and Long Thoi, where flooding was found in approximately 80% of the surveyed households. Although flooding was reported by only 14.3% and 8% of respondents in Nhon Duc and Phu Xuan as an abnormal event, it still raises a concern about the capacity of drainage in such areas in case heavier rain comes in the years to come.

Fig. 1
2 maps of Ho Chi Minh City highlight the elevation and drainage system and the flooded areas at tide levels. The maps depict city boundaries, flood-causing, and non-causing rivers, and elevation in meters.

Studied area (the red marked zone) in the maps of elevation and the drainage system (left) and flooded areas at tide levels (right) in Ho Chi Minh City (Tran TN 2014)

Fig. 2
A map of Nha Be District locates the communes and the river. The communes include Phuoc Kein, Phuoc Loc, Nha Be, Phu Xuan, Nhon Duc, Long Thoi, and Hiep Phuoc.

(Source This figure is created by the first author, 2019)

Nha Be District map which shows a town and six communes (wards)

Fig. 3
A photo displays 2 men standing on the boundary wall and inspecting the erosion of the road. The muddy water is below the wall.

Housing was eroded in Nhon Duc Ward, Nha Be District (Authors, 2019)

Fig. 4
A bar graph of the frequency of flood versus wards in the Nha Be district illustrates the frequency is highest in Nha Be and that the occurrence of flood at a specific time of the year is highest in Hiep Phuoc.

Frequency of flood occurring in Nha Be District (Authors, 2019)

With regards to flood status, generally, there is a variation of flood depth among the surveyed households; the average depth is recorded at 23.72 cm. Some households are experiencing serious 70 cm-deep floods. Specifically, flooding severely occurs in the wards with a high urbanization rate, namely, Nha Be and Phuoc Kien with 29.7 cm and 26 cm in depth, respectively, followed by Nhon Duc (20.8 cm), Phu Xuan (17.6 cm), and Long Thoi (17.1 cm). The smallest flood depth was found in Hiep Phuoc and Phuoc Loc with roughly 15 cm (Fig. 5).

Fig. 5
A satellite map of Ho Chi Minh City highlights the communes according to the average flood height. Phuoc Kien records the maximum average flood height.

Intensity of flooding reflected by the flood depth (Authors, 2019)

There is no doubt that there is a strong association between the rising sea levels and flooding. In this chapter, exploring the perception of households regarding sea level was included to examine not only the view of the locals to the climate variation, but also their knowledge about sea-level rise in relation to flooding issues in such areas. Generally, 57.15% of the surveyed households have perceived water variation as abnormal, while 30% and 11.9% of them see a slight increase and significant rise, respectively, in flooding over the last 10 years (2009–2019). There is a variation of perceptions of residents’ viewpoint among the wards of Nha Be District (Fig. 6). Inhabitants living in Nha Be Town, Nhon Duc, Phu Xuan, Phuoc Kieng, and Phuoc Loc are aware of the water variation from sea-level rise over time, which is reflected by the results in more than 50% of the surveys.

Fig. 6
A table has 3 columns and 5 rows. The columns are titled intensity, number, and percentage. A bar graph of the responses versus wards of Ho Chi Minh displays the highest variation in Phu Xuan.

Fluctuation of sea-level rise by year, taken from residents’ viewpoints between 2009 and 2019 (Authors, 2019)

Characterized by a complex waterway system, Nha Be District respondents stated that flooding was mostly due to tides and heavy rains, as their frequencies are 43.5 and 31.9% among all causes, while the operation of water drainage system accounts for only 15.4%. Sea-level rise and landslides, along with dams, are the other rare causes, with roughly 3% of frequency (Table 1).

Table 1 Causes of flood in Nha Be District (Authors, 2019)
Table 2 Impact of floods on residents in Nha Be District (Authors, 2019)

4.2 Impacts

Flooding has negative impacts on several aspects of the studied area. 30.5% of respondents found the effects of floods on traffic, namely making it inconvenient in commuting. A similar number of people (approximately 25%) saw damage to housing and a reduction in their quality of life caused by the seasonal floods. Noticeably, despite a small percentage of the flooding impacts, negative impacts on local business and land loss should be taken into account in flood response and adaptation, especially for the houses located by the main roads and along the river. Figure 7 shows that the houses situated in Le Van Luong Street are considerably vulnerable to be re-flooded because most of them are small retailers and are just slightly higher than the main road elevation.

Fig. 7
A satellite map highlights a road in Phuoc Kien in Nha Be district. A photo displays a general store and 2 people in front of the store.

(Source This photo was taken by the first author, 2019)

House with business activity located on the main road in Nha Be District

4.3 Solutions

To cope with flooding, there are many possible solutions (Table 3). Raising the ground level of the houses is the most referenced household-based solution among inhabitants, accounting for 53.7% of responses. However, nearly 37% of households suggested no solution in Nha Be District. A reason for this may be the dominance of low-income households that have limited to no financial capacity to apply renovation techniques. Only 0.5% of the respondents have applied concrete-based reinforcement. Some households have still coped with flooding with temporary measures such as leveling up furniture and investing in individual pumps for their self-drainage.

Table 3 Selective solutions to cope with floods in Nha Be District (Authors, 2019)

Local governments have taken certain measures to counteract the negative impacts of flooding as well. Based on in-depth interviews with community leaders, because of severe floods taking place on Huynh Tan Phat Street (from the joint with Tran Xuan Soan Street to Phu Xuan Bridge), the local government, with contributions from the residents, has upgraded alleys, namely 1716, 1806, and 1897. This project has partly reduced the flooding issue in the area. Plus, the local government has adopted soft measures such as cleaning sluice and sewage frequently, contributing to the increased efficiency of waterway function, especially when tides and rain take place. This includes dredging the Ba Lao Canal to foster drainage of water during high tide. However, with limited financial resources, the local government has been challenged by the efficiency of the drainage system, which is still poorly aligned between the main roads and narrow alleys. Thus, the participation and engagement of the community are important mechanisms for coping with climate change in Nha Be District. In this way, the effort to raise awareness via communication, propaganda of environmental protection, and trainings has been carried out.

5 Discussion and Conclusion

The study found, conclusively, that flooding has impacted multiple aspects of Nha Be District. Without early protection, it harms the existence of the community in the future. The findings reflect the frequency, intensity, and causes of flooding from the perspectives of the residents, which may contribute to further assessment and analysis of the flood risk in the area. However, to propose appropriate approaches for combating floods, more analysis and mitigation strategies are suggested, i.e., mapping, modeling, and simulation as well as further questionnaires for the area. All of these strategies, as well as those used in this study, can help residents deal with the complexity of climate change.

In conclusion, the study finds that floods occur all around Nha Be District, with the highest intensity and frequency recorded in Nha Be Town. Respectively, tide, precipitation, inadequate drainage systems, and sea-level rise are considered the primary causes of flooding. For people living in the district, floods have negatively impacted traffic and housing conditions as well as their quality of life. In response to the floods, the government has leveled up certain roads and improved the drainage system, while survey respondents prefer to elevate the floors in their homes. Since these measures are still limited, the findings of this chapter imply a need for further actions to deal with flooding in this area. These measures can be proposed and carried out from multiple stakeholders at various scales. Further strategies are recommended to integrate top-down with bottom-up and short-term with long-term solutions. Besides a discussion on flood impact measures, this chapter also contributes to the flood risk assessment, which may support the government in finding proper approaches for this area at the district level. The findings of the chapter can be used as a source of reference for other areas with a similar context in topographic and socio-economic features, such as the other coastal cities, in the developing countries in South and Southeast Asia.