Phuket is a tropical island in Thailand that is famous for tourism. The COVID-19 pandemic resulted in the number of tourists reducing to almost zero. Since tourism contributes around one-half of the gross provincial product of Phuket, the impact was so severe that even the numbers of people employed and registered as locals decreased. Analysing the data from January 2015 to March 2021, we found that the total, residential and non-residential monthly consumptions dropped significantly after Thailand's State of Emergency was declared in March 2020. Unlike other studies that reported residential consumption increasing when people were required to stay home for a prolonged period, Phuket's residential consumption decreased by more than 10% from the pre-COVID-19 level, possibly due to the drop in peer-to-peer accommodation bookings. To study the impact on consumption in detail, we modelled using cascade regression analysis by dividing the predictors into three groups, namely socioeconomics, weather and calendar period. The results showed that the number of guest arrivals was the most statistically significant in all types of consumption and should be used as a predictor for water demand forecasting models in tourism areas.

  • The first study on the impact of COVID-19 on water consumption on a tropical island.

  • The reduction of tourists impacted residential and non-residential consumptions.

  • Residential consumption decreased during the outbreak, opposite to other reports.

  • The study used the recent data, and the models can estimate consumptions during the outbreak.

  • The weather and calendar impacts were also included in the models.

On January 17, 2020, Thailand reported the first COVID-19 patient outside China. During the first wave of the pandemic, a maximum daily peak of 188 new COVID-19 cases associated with a boxing stadium and drinking venue was confirmed on March 22, 2020. Consequently, a nationwide curfew was enforced on April 3, 2020 (Dechsupa et al. 2020). Abiad et al. (2020a) evaluated the effects of the outbreak on developing Asian economies by comparing the COVID-19 outbreak with the economic impact of the severe acute respiratory syndrome (SARS) outbreak in 2003. The impacts included lower tourism numbers and business activity, as tourist arrivals from China contributed approximately 28% to total arrivals to Thailand in 2018. Tourism provides the main income for Thai residents, where the total and international tourism receipts were around 18% and 13.5% of the gross domestic product in 2017. Later, Abiad et al. (2020b) updated the impact of the COVID-19 pandemic as it extended into 2021. Revised tourism losses reflect extended travel restrictions and the latest passenger survey results. The protracted halt in global tourism, coupled with increased travel aversion, implied substantial tourism losses into 2021 and bode ill for many tourism-dependent economies in developing Asia.

Bhowmick et al. (2020) presented a COVID-19 contamination scenario in the urban and rural water cycle with potential human exposure. They suggested that contaminated raw water and leaky water distribution networks can lead to COVID-19 transmission. The World Health Organization (WHO 2020) published a guideline to provide safe water, sanitation and waste management and hygienic conditions essential for preventing illness and protecting human health during the COVID-19 outbreak. WHO recommended that the residual concentration of free chlorine should be ≥0.5 mg/l after at least 30 min of contact time at pH < 8.0 for effective centralized disinfection. García-Ávila et al. (2021) developed a drinking water distribution network model for a part of Azogues City, Ecuador, using EPANET software (Rossman 2000) and found that about 45% of the model nodes did not comply with the WHO recommendation. Thus, it is important to assess and optimize the quantity of chlorine in water distribution networks, e.g., Javadinejad et al. (2019), Lipiwattanakarn et al. (2021).

Recent studies showed the impact of the COVID-19 pandemic on potable water demand. For example, Bich-Ngoc & Teller (2020) investigated the changes in outbound tourism on daily water demand in Liège, Belgium. The water demand was mainly from residential use (more than 80%). Instead of a regular multiple linear regression, they used a cascade model by dividing predictors into four groups, namely trend, holiday, weather and calendar. Although their available outbound tourism data were limited to December 2018 before the outbreak, they concluded that the threat due to dry and hot weather on increased water demand was higher than the threat from fewer outbound tourists. Balacco et al. (2020) studied the effect of restriction measures due to the COVID-19 spread on water demand in Ruglia, Italy. Using the instantaneous flow data of water consumption from January 1 to April 30 for 2019 and 2020, they highlighted the influence of the change in lifestyle on the daily water demand pattern, such as the shift in the morning peak by a delayed wake up by about two hours and the absence of a classic water peak demand during lunchtime. Kalbusch et al. (2020) used water consumption data collected using telemetry representing 17% of the total consumption from February 21 to April 12, 2020, in Joinville, Southern Brazil. They found that the restrictive actions caused a decrease in water consumption in the non-residential category, but an increase in the residential category. Dzimińska et al. (2021) used a cluster analysis to study the change in hourly water consumption in three apartment buildings in Bydgoszcz, Poland, between May 16, 2019, and October 6, 2020. They found increasing water consumption during the day and night, between 2:00 and 4:00 during the pandemic. Lüdtke et al. (2021) analysed hourly and daily water consumption in Wasserbeschaffungsverband WBV Harburg, northern Germany, from January 1, 2006, until June 28, 2020, using linear mixed models. They found 14.3% higher residential water consumption per day with higher morning and evening demand peaks. Shrestha et al. (2021) reported an increase in residential water consumption and a decrease in commercial consumption during the nationwide lockdown in Nepal during March–April 2020. Abu-Bakar et al. (2021) analysed data from 11,528 households over 20 weeks from January 2020 in the southern and eastern regions of England and found that the average household consumption was 284 litres per household per day (l/h/d) before the COVID-19 lockdown and increased to 411 l/h/d in week four in May (46% above pre-lockdown average). Rizvi et al. (2021) analysed a domestic consumption profile for selected customer meters up to June 2020 and found a 30% increase in consumption during the month of Ramadan and the COVID-19 crisis.

Most of the previous studies were in Europe and limited to 2020. There has been no study in detail of a tourism island in tropical Asia. Thus, this study aimed to fill a research gap by investigating the impact of the COVID-19 pandemic on water consumption in Phuket, southern Thailand. Phuket is one of the most famous tourism islands in Asia, with on average approximately one million guest arrivals at accommodation establishments per month and the resultant tourism activity earning over THB 450 billion in 2019 (48.13% of gross provincial product). In 2020, the average number of guest arrivals reduced to about 300,000 people per month, and tourism earnings fell to THB 100 billion (Ministry of Tourism & Sports 2021). Phuket was one of the first provinces that confirmed COVID-19 patients in Thailand (Department of Disease Control 2021), and its water demand was greatly impacted by the tourism loss due to the outbreak. Tantrakarnapa et al. (2020) found that the number of infected cases was significantly associated with the number of tourists and their activities in Thailand. Bakker & Twining-Ward (2018) studied the emergence of peer-to-peer (P2P) accommodation in the tourism industry, driven by technology such as Airbnb. P2P accommodation gives new opportunities for ordinary residents to offer rooms or entire homes to a global marketplace of consumers (Priporas et al. 2017). It is broadly known today as the sharing economy, and its growth is accelerating at a faster rate in emerging markets. This may result in water consumption in some registered residential properties being used by tourists instead of the real residents. Thus, in this study, we investigate the COVID-19 impact on total, residential and non-residential monthly water consumptions in Phuket, Thailand, up to March 2021.

Data

Phuket is a province in the southern part of Thailand. It consists of the island of Phuket, the largest island in Thailand, and 32 other small islands surrounded by the Andaman Sea. Phuket Island has an area of 543 km2 with a registered population of approximately 400,000 people. There are two weather stations on the Island, as shown in Figure 1. The Provincial Waterworks Authority (PWA), Phuket Branch, delivers a potable water supply to customers on the Island with a service area of 398 km2. The consumption volume and the production capacity are around 2,000,000 and 3,000,000 m3/month, respectively. In March 2021, the number of customers was 65,123 consisting of 52,235 residential meters and 12,888 non-residential meters.

Figure 1

Map of Phuket with locations of Provincial Waterworks Authority (PWA), Phuket branch, and weather stations. The small insert shows a map of Thailand, with Phuket located in the south (red star). The background map is taken from Google Street Map.

Figure 1

Map of Phuket with locations of Provincial Waterworks Authority (PWA), Phuket branch, and weather stations. The small insert shows a map of Thailand, with Phuket located in the south (red star). The background map is taken from Google Street Map.

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Table 1 shows a list of the data from this study. The data were divided into three categories: water consumption, socioeconomics and weather. The water consumption data were from the PWA on a monthly basis, consisting of total water consumption (DT), residential water consumption (DR) and non-residential water consumption (DN). The socioeconomic data consisted of the number of guest arrivals at accommodation establishments (NG), the number of people employed (NE) and the number of people in the registered population (NP) from two sources, the Ministry of Tourism and Sports (MTS) and the National Statistical Office (NSO). Since the data from MTS and NSO were collected at different time scales, we interpolated the NE and NP data to a monthly time scale. However, NP was extrapolated for three months during January–March 2021. The weather data on a monthly basis consisted of mean temperature (T), rainfall (R), mean wind speed (W) and mean humidity (H) from the two weather stations of the Thai Meteorological Department (TMD). The data were used to investigate the total, residential and non-residential water consumption patterns on a monthly time scale in the period January 2015–March 2021, covering the period before and after the Thailand's State of Emergency due to the COVID-19 pandemic.

Table 1

Overview of available data in categories

DataTime scalePeriodSource
Water consumption    
Total water consumption (DTMonthly 2015/01–2021/03 PWA 
Residential water consumption (DRMonthly 2015/01–2021/03 PWA 
Non-residential water consumption (DNMonthly 2015/01–2021/03 PWA 
Socioeconomics    
Guest arrivals (NGMonthly 2015/01–2021/03 MTS 
People employed (NEQuarterly 2014/Q4–2021/Q1 NSO 
Registered population (NPYearly 2014–2020 NSO 
Weather    
Mean temperature (TMonthly 2015/01–2021/03 TMD 
Rainfall (RMonthly 2015/01–2021/03 TMD 
Mean wind speed (WMonthly 2015/01–2021/03 TMD 
Mean humidity (HMonthly 2015/01–2021/03 TMD 
DataTime scalePeriodSource
Water consumption    
Total water consumption (DTMonthly 2015/01–2021/03 PWA 
Residential water consumption (DRMonthly 2015/01–2021/03 PWA 
Non-residential water consumption (DNMonthly 2015/01–2021/03 PWA 
Socioeconomics    
Guest arrivals (NGMonthly 2015/01–2021/03 MTS 
People employed (NEQuarterly 2014/Q4–2021/Q1 NSO 
Registered population (NPYearly 2014–2020 NSO 
Weather    
Mean temperature (TMonthly 2015/01–2021/03 TMD 
Rainfall (RMonthly 2015/01–2021/03 TMD 
Mean wind speed (WMonthly 2015/01–2021/03 TMD 
Mean humidity (HMonthly 2015/01–2021/03 TMD 

The impact of the COVID-19 pandemic appeared to be clear after January 2020 with steep drops in DT and DN, as shown in Figure 2(a). In January 2020, DT and DN were 2,102,518 m3/month and 1,170,338 m3/month, respectively, but in May 2020, they reduced to 1,331,493 m3/month (−36.7%) and 522,727 m3/month (−55.3%), respectively. For DR, many studies reported that residential consumption increased due to a work-from-home policy during the COVID-19 outbreak. However, DR in this study surprisingly decreased along with DT and DN but at a milder rate. DR in January 2020 was 932,180 m3/month and dropped to 808,766 m3/month (−13.2%) in May 2020. Phuket's main industries are tourism and hospitality. Wannasuth & Wichasin (2021) indicated that before the pandemic, the sharing economy (P2P accommodation) had grown rapidly so that even foreigners came to conduct this business in Thailand. Boros et al. (2020) studied the effects of COVID-19 on Airbnb in 15 cities around the world and found that Airbnb had experienced a rapid drop in bookings. Thus, we hypothesize that a decrease in booking P2P accommodation affected the drop in DR during the COVID-19 outbreak. After May 2020, the values of DT, DR and DN did not change much. Comparing Figure 2(a) and 2(b), the monthly pattern of NG was similar to those for DT, and DN. The maximum NG value of 1,524,977 arrivals in January 2020 dropped to the minimum NG value of 3,621 arrivals (−99.8%) in May 2020. The impact can be seen in NE and NP as well, where the general trends of NE and NP were increasing before the pandemic. NE reduced from 322,774 people in Q4 2019 to 296,070 (−8.27%) in Q4 2020, and NP also reduced from 416,582 people in 2019 to 414,471 (−0.51%) in 2020.

Figure 2

Time series of (a) water consumption data and (b) socioeconomic data.

Figure 2

Time series of (a) water consumption data and (b) socioeconomic data.

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Phuket has a tropical monsoonal climate. The southwestern monsoon from the Indian Ocean during May–October brings a stream of warm moist air towards Phuket and causes heavy rain (rainy season). The northeastern monsoon draws cold air from the South China Sea during November–April (dry season), which is thus the best time for tourists to visit Phuket due to cool breezes and blue skies. Figure 3 shows the variation of monthly meteorological data from January 2015 to December 2020. Phuket is warm year-round with monthly mean temperature in the range 27–31 °C (Figure 3(a)). Its location avoids most typhoons and tropical storms. The monthly rainfall is in the range 0–600 mm/month (Figure 3(b)). The monthly mean wind speed is quite steady (1–4 knots), with August having the strongest winds (Figure 3(c)). Figure 3(d) shows the yearly pattern of monthly mean humidity with little variation, similar to the rainfall pattern.

Figure 3

Weather patterns of (a) mean temperature, (b) rainfall, (c) mean wind speed and (d) mean humidity.

Figure 3

Weather patterns of (a) mean temperature, (b) rainfall, (c) mean wind speed and (d) mean humidity.

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Figure 4

Cascade of transformations of prediction models for total, residential and non-residential water consumptions (DT, DR and DN).

Figure 4

Cascade of transformations of prediction models for total, residential and non-residential water consumptions (DT, DR and DN).

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Bich-Ngoc & Teller (2020) applied a cascade model of regression analysis to investigate the daily water demand in Liège, Belgium, because of the high multicollinearity among the predictors. Their statistical model was adapted from Wong et al. (2010) and Maidment & Parzen (1984). In the current study, we followed the cascade model concept used by Bich-Ngoc & Teller (2020). However, our predictors were divided into three groups, namely socioeconomics, weather and calendar period, and we predicted three types of consumption: total, residential and non-residential.

The cascade method for total, residential and non-residential monthly water consumptions (, , ) used in this analysis (Figure 4) consists of three transformations. A first transformation is applied in the linear regression analysis using the socioeconomic data (), considered as base water use components. Then the residuals from the first transformation () are passed to the second linear regression analysis using the weather data () as seasonal water use components. Finally, the residuals from the second transformation () are used for the third linear regression analysis based on the calendar data () as calendrical water use components. The residuals from the third transformation () are considered as random error series (). Thus, the cascade method can be expressed as:
(1)
(2)
(3)
(4)
where the subscripts T, R and N denote total, residential and non-residential consumptions, respectively, and the subscripts 1, 2 and 3 denote the first, second and third transformations, respectively. The base water use components , the seasonal water use components and the calendrical water use components are:
(5)
(6)
(7)
where represents model intercepts, represents vectors of model coefficients, is the socioeconomic data having three predictors (NG, NE, NP), is the weather data having four predictors (T, R, W, H), and is the calendar data (months of the year).
To assess the efficiency of each transformation, each cascade model for each type of water consumption was divided into three sub-models as follows:
(8)
(9)
(10)

There are options regarding selecting the predictors of the models. The model of Bich-Ngoc & Teller (2020) included every input piece of data as a predictor, regardless of whether or not its significance level of the p-value was below the threshold of 0.05. On the other hand, Wong et al. (2010) used trial-and-error analyses to examine the holiday effect on water consumption, divided the model into seven sub-models with all chosen predictors having p-values below 0.05 and then selected the most suitable sub-model. In the current study, we followed the approach of Wong et al. (2010) and applied trial-and-error analyses using the Statsmodels library in Python (Seabold & Perktold 2010). The criterion for choosing the suitable models was to have predictors with p-values below 0.05 as much as possible, because the efficiency should then be the highest and our models were monthly-based models with the possible maximum number of predictors being only 22. The data were divided into a training set from January 2015 to September 2020 (69 months) and a validation set from October 2020 to March 2021 (six months). We chose the data during the COVID-19 outbreak for the validation set to investigate the efficiency of our models in predicting consumptions during the pandemic.

Model parameters

Table 2 shows the intercepts, coefficients and associated p-values of the cascaded regression analysis for the DT,p, DR,p and DN,p models (8)–(10). Although the observed DT value was always equal to DR+DN, the predicted DT,p was not necessarily equal to the predicted DR,p+DN,p. Thus, the value of each parameter in the DT,p model was not equal to the sum of the values of each parameter in the DR,p and DN,p models. The first transformation based on socioeconomics showed that NG was significant in every model with p-values less than 0.0001. As described earlier, the emergence of P2P accommodation in the tourism industry may result in residential water consumption being used by tourists instead of the real residents. Thus, guest arrivals influenced all types of water consumption in our Phuket case study. While NE was significant in the DT,p and DN,p models, NP was significant in the DT,p and DR,p models. These NE and NP results could be easily explained by the people being employed influencing non-residential water consumption while the registered population certainly consumed residential water.

Table 2

Parameters with p-values for total consumption (DT,p), residential consumption (DR,p) and non-residential consumption (DN,p) models, where consumption unit is m3/month

ParameterUnitDT,p model
DR,p model
DN,p model
Coefficientp-ValueCoefficientp-ValueCoefficientp-Value
First transformation based on socioeconomics 
Intercept 1 – −3,384,014 0.0003 −797,787 <0.0001 −2,179,866 0.0018 
NG person 0.34144 <0.0001 0.05562 <0.0001 0.27318 <0.0001 
NE person 9.02590 0.0025   9.30365 0.0001 
NP person 5.09675 0.0004 3.89252 <0.0001   
Second transformation based on weather 
Intercept 2 – −1,945,197 0.0015 −522,670 0.0031 −1,392,504 0.0050 
T °C 66,093 0.0017 17,703 0.0035 47,458 0.0053 
R mm 243.078 0.0098 72.703 0.0079 154.869 0.0421 
W knot       
H       
Third transformation based on calendar period 
Intercept 3 – −56,147 0.0018 −27,694 <0.0001   
Jan –   48,912 0.0002   
Feb – 100,400 0.0270 34,815 0.0056   
Mar –       
Apr – 120,176 0.0087 55,505 <0.0001   
May – 101,765 0.0253 40,908 0.0013   
Jun –   35,058 0.0053   
Jul –       
Aug – 115,700 0.0114 34,417 0.0062   
Sep – 113,867 0.0127 26,743 0.0313   
Oct –       
Nov – 112,542 0.0223 50,553 0.0003   
Dec –       
ParameterUnitDT,p model
DR,p model
DN,p model
Coefficientp-ValueCoefficientp-ValueCoefficientp-Value
First transformation based on socioeconomics 
Intercept 1 – −3,384,014 0.0003 −797,787 <0.0001 −2,179,866 0.0018 
NG person 0.34144 <0.0001 0.05562 <0.0001 0.27318 <0.0001 
NE person 9.02590 0.0025   9.30365 0.0001 
NP person 5.09675 0.0004 3.89252 <0.0001   
Second transformation based on weather 
Intercept 2 – −1,945,197 0.0015 −522,670 0.0031 −1,392,504 0.0050 
T °C 66,093 0.0017 17,703 0.0035 47,458 0.0053 
R mm 243.078 0.0098 72.703 0.0079 154.869 0.0421 
W knot       
H       
Third transformation based on calendar period 
Intercept 3 – −56,147 0.0018 −27,694 <0.0001   
Jan –   48,912 0.0002   
Feb – 100,400 0.0270 34,815 0.0056   
Mar –       
Apr – 120,176 0.0087 55,505 <0.0001   
May – 101,765 0.0253 40,908 0.0013   
Jun –   35,058 0.0053   
Jul –       
Aug – 115,700 0.0114 34,417 0.0062   
Sep – 113,867 0.0127 26,743 0.0313   
Oct –       
Nov – 112,542 0.0223 50,553 0.0003   
Dec –       

In the second transformation based on weather, four predictors were available, namely T, R, W and H. However, only T and R were significant in every model. In addition, the p-values of T were smaller than those of R. Makpiboon et al. (2020) studied the total water demand in three provinces (Bangkok, Nonthaburi and Samutprakarn) in Thailand using three different time scales (daily, monthly and seasonal) based on T and R. They found that both weather predictors were significant with the p-values of T smaller than those of R. Thus, our results agreed with their research results. Finally, 12 predictors (months of the year) were selected in the third transformation based on calendar period. For the DT,p and DR,p models, six months and eight months, respectively, were chosen. However, surprisingly, no month predictor was valid for the DN,p model due to the p-values being higher than the threshold value of 0.05. April had the highest coefficients with the lowest p-values in both the DT,p and DR,p models. This may have been due to the Thai New Year festival in the middle of April, when people in Thailand celebrate the holiday with traditional water ceremonies such as pouring water in ceremonies and in widespread public water splashing and more raucous events.

Predicted monthly water consumption

The comparisons between the observed water consumption and the final predicted values for the training and validation periods are shown in Figure 5. Figure 5(a) shows two types of DT estimation, the final DT model (DT,p3) and the combination of two final models of DR and DN (DR,p3+DN,p2). Both models do not give the same results because the values of the model parameters are slightly different, as shown in Table 2. The results for the DR,p3 and DN,p2 models compared with the observed values are shown in Figure 5(b) and 5(c), respectively. In the training period before the COVID-19 pandemic affected NG, all model results matched reasonably well with the observations. However, during the early period of the pandemic when water demand plunged, our models overestimated consumption, especially between March and June 2020. There was a better fit to water demand in the validation period between October 2020 and March 2021.

Figure 5

Observed (line) and predicted (circle and plus markers) monthly consumption for (a) total consumption, (b) residential consumption and (c) non-residential consumption. The training and validation periods are before and after, respectively, the black vertical dashed line.

Figure 5

Observed (line) and predicted (circle and plus markers) monthly consumption for (a) total consumption, (b) residential consumption and (c) non-residential consumption. The training and validation periods are before and after, respectively, the black vertical dashed line.

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Table 3 shows the detailed performance of the prediction models at each transformation, where R is the coefficient of correlation, RMSE is the root-mean-square error, and MAE and MAPE are the mean absolute error and mean absolute percentage error, respectively. Generally, an increase in transformations led to better efficiency of prediction in this study. In particular, the third transformation based on the calendar period increased the R values in both the training and validation periods. The DR models had the best performance followed by the DT and DN models, respectively. Thus, the residential water demand was better estimated compared with the non-residential demand in this study. The DT,p3 model and the DR,p3+DN,p2 model had similar performance levels. Although the performance based on the values for RMSE, MAE and MAPE was slightly lower in the validation period, the R values dropped substantially. This could be explained by the validation period we chose being during an abnormal situation (the COVID-19 outbreak). However, the RMSE, MAE and MAPE results indicated that our models could satisfactorily predict water demand during the outbreak. Recently, the Thai government has officially endorsed measures for Phuket to reopen for fully vaccinated international travellers without quarantine requirements from July 1, 2021, under the so-called ‘Phuket sandbox’ initiative. The Tourism Authority of Thailand (TAT) estimated that the sandbox would attract 100,000 international tourists in Q3 2021 (TAT 2021). Thus, our models could be helpful in estimating the increase in water demand after the reopening.

Table 3

Performance of prediction models for each transformation

IndicatorDT,p1DT,p2DT,p3DR,p1DR,p2DR,p3DN,p1DN,p2DR,p3+DN,p2
Training period (2015/01–2020/09) 
R (–) 0.812 0.849 0.900 0.796 0.831 0.904 0.830 0.855 0.870 
RMSE (m3/month) 120,041 110,079 95,014 34,614 31,937 24,553 95,920 89,953 104,243 
MAE (m3/month) 95,652 86,787 73,558 27,610 26,278 19,884 75,065 69,245 79,093 
MAPE (%) 5.29 4.85 4.18 3.40 3.25 2.45 7.84 7.38 4.44 
Validation period (2020/10–2021/03) 
R (–) −0.824 −0.759 −0.371 −0.959 −0.370 0.201 −0.772 −0.817 −0.603 
RMSE (m3/month) 104,967 102,245 115,197 51,067 47,945 40,862 64,288 70,458 94,887 
MAE (m3/month) 96,669 90,290 100,655 43,647 44,525 29,764 62,368 59,236 85,135 
MAPE (%) 7.23 6.64 7.36 5.68 5.73 3.85 10.80 10.07 6.21 
IndicatorDT,p1DT,p2DT,p3DR,p1DR,p2DR,p3DN,p1DN,p2DR,p3+DN,p2
Training period (2015/01–2020/09) 
R (–) 0.812 0.849 0.900 0.796 0.831 0.904 0.830 0.855 0.870 
RMSE (m3/month) 120,041 110,079 95,014 34,614 31,937 24,553 95,920 89,953 104,243 
MAE (m3/month) 95,652 86,787 73,558 27,610 26,278 19,884 75,065 69,245 79,093 
MAPE (%) 5.29 4.85 4.18 3.40 3.25 2.45 7.84 7.38 4.44 
Validation period (2020/10–2021/03) 
R (–) −0.824 −0.759 −0.371 −0.959 −0.370 0.201 −0.772 −0.817 −0.603 
RMSE (m3/month) 104,967 102,245 115,197 51,067 47,945 40,862 64,288 70,458 94,887 
MAE (m3/month) 96,669 90,290 100,655 43,647 44,525 29,764 62,368 59,236 85,135 
MAPE (%) 7.23 6.64 7.36 5.68 5.73 3.85 10.80 10.07 6.21 

The total, residential and non-residential monthly water consumptions (DT, DR and DN) on Phuket Island were investigated before and during the COVID-19 pandemic. After Thailand's State of Emergency was declared (in January and then extended in May 2020), the number of guest arrivals at accommodation establishments (NG) plunged 99.8%, and DT, DR and DN dropped 36.7%, 13.2% and 55.3%, respectively. While reductions in DT and DN are common as business slows down or stops, the reduction in DR was surprisingly the opposite according to many reports. We hypothesize that the COVID-19 pandemic hit the tourism and hospitality industries hard, including the P2P accommodation service in Phuket. If many residential properties participated in that service, DR would strongly depend on the tourism and hospitality industries. The COVID-19 impact can be seen in other socioeconomic parameters, namely the number of people employed (NE) and the registered population number (NP). The general trends in NE and NP were increasing before the pandemic. However, NE reduced 8.27% between the fourth quarters of 2019 and 2020, and NP decreased 0.51% from 2019 to 2020.

The cascade models of regression analysis for DT, DR and DN were established using three predictor groups: socioeconomics, weather and calendar period. We trained our models using data from before and during the outbreak between January 2015 and September 2020 and validated the models using data from October 2020 to March 2021. NG was the most important predictor and should be used as a predictor for water demand forecasting models in tourism areas. Monthly mean temperature and rainfall were also significant in all models. In our case study, calendar predictors (months of the year) were not significant in the DN model. Our final models provided satisfactory estimations for DT, DR and DN during the abnormal COVID-19 situation.

The Provincial Waterworks Authority (PWA) and the Thai Meteorological Department (TMD) provided the datasets used in this study. Praewa Jowwongsan and Tas Surasanwong were supported by M.Eng. scholarships from the Faculty of Engineering, Kasetsart University, Bangkok, Thailand, by grant numbers 64/01/WE/M.Eng and 2565/M.Eng, respectively.

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

Abiad
A.
,
Arao
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