Journal Pre-proof Disaster awareness in three low risk coastal communities in Puerto Princesa City, Palawan, Philippines Ven Paolo B. Valenzuela, Miguel Esteban, Hiroshi Takagi, Nguyen Danh Thao, Motoharu Onuki PII:
S2212-4209(19)30137-2
DOI:
https://doi.org/10.1016/j.ijdrr.2020.101508
Reference:
IJDRR 101508
To appear in:
International Journal of Disaster Risk Reduction
Received Date: 2 February 2019 Revised Date:
2 September 2019
Accepted Date: 25 January 2020
Please cite this article as: V.P.B. Valenzuela, M. Esteban, H. Takagi, N.D. Thao, M. Onuki, Disaster awareness in three low risk coastal communities in Puerto Princesa City, Palawan, Philippines, International Journal of Disaster Risk Reduction (2020), doi: https://doi.org/10.1016/j.ijdrr.2020.101508. This is a PDF file of an article that has undergone enhancements after acceptance, such as the addition of a cover page and metadata, and formatting for readability, but it is not yet the definitive version of record. This version will undergo additional copyediting, typesetting and review before it is published in its final form, but we are providing this version to give early visibility of the article. Please note that, during the production process, errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. © 2020 Published by Elsevier Ltd.
1
Disaster Awareness in Three Low Risk Coastal Communities in Puerto Princesa City,
2
Palawan, Philippines
3 4
Ven Paolo B. Valenzuela, Graduate Program in Sustainability Science Global Leadership Initiative, The University of Tokyo, Tokyo, Japan
5
Miguel Esteban, Waseda University, Tokyo, Japan
6
Hiroshi Takagi, Tokyo Institute of Technology, Tokyo, Japan
7 8
Nguyen Danh Thao, Ho Chi Minh City University of Technology, Ho Chi Minh City, Vietnam
9 10
Motoharu Onuki, Graduate Program in Sustainability Science Global Leadership Initiative, The University of Tokyo, Tokyo, Japan
11 12
ABSTRACT
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The Philippines as a country is at high risk of suffering from natural hazards and has an
14
extensive national hazard database on the different types of risk. However, some
15
communities are in relatively low risk zones, such as those in Puerto Princesa City in
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Palawan (with many inhabitants of the city believing it to be safe). The present research seeks
17
to ascertain how disaster risk is understood in coastal areas that are only slightly susceptible
18
to natural hazards, in order to provide strategies that can improve disaster risk governance.
19
The study validated national data on hazard risks through a topographical survey,
20
questionnaire surveys, and group interviews (in March 2016 and 2017) to understand whether
21
residents understood the actual risks they are exposed to. The research found that the national
22
data reflects well local conditions, though community members do not have a clear
23
understanding of the risks, particularly coastal hazards. Moreover, the research found that
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there has been a recent disaster event, though it was not properly archived and transmitted to
25
the next generation. Thus, there is a need to raise awareness and correctly explain and
26
transmit knowledge about potential hazards even in communities that have relatively lower
27
disaster risk.
28 29
1. INTRODUCTION
30
Due its geographical location, the Philippines is one of the most disaster-prone countries
31
in the planet, being exposed to both seismic activity and intense tropical cyclones [1–4].
32
Within the country, the island of Palawan is usually believed by most people to be the safest
33
area from disasters [5–7]. Tropical cyclone tracks in the Philippines have two distinctive
34
patterns: (a) those moving westward in a course that is nearly parallel to the equator, and (b)
35
moving westward and then turning north-eastward due to the influence of westerlies blowing
36
around N30° [8]. Palawan is on the outskirts of the former group, and thus is almost free
37
from the influence of strong typhoons.
38
However, historical storm tracks and tsunami maps from IBTrACS and the United
39
States of America’s NGDC/WDS Global Historical Tsunami Database show that Palawan
40
has experienced storms and is at risk to nearby tsunami sources [9,10]. A study using 2013
41
Typhoon Haiyan scenarios found that if a similar event occurs in Palawan, coastal areas
42
would be at high risk of suffering from storm surges [11]. While the area is free from seismic
43
activity, it is still exposed to tsunamis. These hazards may impact Puerto Princesa City,
44
Palawan’s capital and only urban area. PHIVOLCS stated that the city is at risk from a
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nearby fault that can generate a 4 m tsunami wave [12]. This is summarized in Figure 1,
46
along with population density data from the 2015 national census [13].
47
This study adopts the findings of previous research and assumes that, under the right
48
conditions, Puerto Princesa City can be at risk to coastal hazards. On the other hand, the
49
authors acknowledge that most people outside the academe perceive that the area is safe. This
50
contradiction between science and societal perception is the focus of this research. In areas
51
that are perceived not to be particularly at risk to storm surges and tsunamis (despite studies
52
that say otherwise), how do communities understand their local risk and implement disaster
53
preparedness activities? This is particularly crucial when it comes to extreme events, as their
54
effects on coasts have a high degree of uncertainty, and areas currently at low risk might
55
become more hazardous in the future due to the influence of climate change. This risk is
56
further exacerbated by potential development opportunities in coastal areas.
57
Disaster experience promotes disaster awareness [14]. For tropical cyclones with shorter
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return periods, experience often leads to higher preparedness, including increased information
59
and safer infrastructure against future events [15–17]. For tsunamis, disaster experiences
60
suffered by previous generations are an integral component of present disaster preparedness,
61
particularly when correlating an earthquake with a tsunami [18–20]. Moreover, major
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disasters such as the 2004 Indian Ocean Tsunami, the 2011 Tohoku Earthquake and Tsunami
63
and the 2013 Typhoon Haiyan have increased awareness on coastal hazards [21,22]. However,
64
studies on disaster awareness have yet to been carried out in communities that have no
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disaster experience.
66
Increased population density can result in settlements encroaching into hazard prone areas,
67
increasing exposure [23–25]. Lack of pre-impact awareness of hazards by residents in such
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communities may lead them to underestimate their severity or impact [26,27]. Hazard
69
knowledge through media can sometimes be inadequate as it does not directly influence
70
planning and evacuation [28,29]. People without disaster experience can often misunderstand
71
the risks they are exposed to, and typically the most devastating hazards have return periods
72
that are beyond a person’s lifetime.
73
Understanding disaster risk must consider how hazards interconnect and compound
74
existing socio-economic and environmental vulnerability [30,31]. Countries that emphasize
75
disaster risk reduction also address low probability hazards (1 in 1000 or more years events)
76
to protect development gains. Japan invests heavily in preventative structures to protect
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people against tsunamis that can occur in a lifetime (typically 1 in 60 to 100 years), while
78
encouraging preparedness for those that occur once every 1000 years [18,32]. Essentially,
79
disaster prevention addresses frequently occurring hazards, while disaster preparedness aims
80
to prevent deaths from rarer but more devastating disasters. Following the 2011 tsunami,
81
emphasis on how physical infrastructure and emergency management should complement
82
each other has been highlighted, as communities realized the importance of participatory
83
governance [18]. Lindell and Prater (2010) argue that in coastal areas at risk to disasters,
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emergency management should focus on “agency notification and mobilization, protective
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action selection and timing, warning and evacuation, and risk communication and perception”
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[33]. These can be enabled through community-based disaster risk management, which
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enables communities to engage different internal and external stakeholders to invest in
88
disaster risk reduction [34].
89
The Sendai Framework for Disaster Risk Reduction highlights rapid urbanization as an
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underlying risk driver [35]. Coastlines are identified as high risk areas, as they enable access
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to resources and trade, which increases exposure to coastal hazards [36,37]. Frequent hazards
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can focus attention, but current low risk coastal areas might become increasingly hazardous
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in the future as the population density increases [37,38]. However, disaster studies are often
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biased towards high probability events in highly populated areas. This has led to a preference
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in physical infrastructure and relocation solutions that are inadequate when addressing the
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rapidly changing socio-economic dynamics of urban communities [39]. There is a need to
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understand how disaster risk management can be improved in all areas, taking into
98
consideration unplanned development.
99
The present research seeks to ascertain how disaster risk is understood in areas that are
100
only slightly susceptible to natural hazards but may be potentially be at risk in the future,
101
with the aim to facilitate disaster risk governance and reduce risks. The study was conducted
102
in three informal settlements of Puerto Princesa, which served as representations of the
103
consequences of rapid urbanization.
104
The 3 communities are in varying locations within the bay, which could be affected by
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storm surges and tsunamis, though the extent of exposure may be different. Barangay
106
Pagkakaisa is deep inside the bay area, north of the town proper, while Barangay Mandaragat
107
is also in the bay but west of the town. Barangay Bagong Sikat is at the mouth of the bay,
108
south of the main part of the town. Wind-induced surges may affect Barangay Bagong Sikat
109
more, though pressure induced surges will affect all communities. Tsunamis may also affect
110
all communities, with Barangay Bagong Sikat being the first to experience it.
111
The research thus attempted to compare the existing local disaster risk profile of the three
112
coastal communities (as also shown in Figure 1) by determining the hazards and exposure
113
through an analysis of historical storms in the area, a topographical survey, a questionnaire
114
survey of residents, and the use of GIS tools. To validate and assess local government and
115
community response capability to rarely experienced hazards, group interviews with
116
government officials and community leaders were also conducted.
117 118 119 120
Figure 1. Location of Puerto Princesa City and the 3 communities studied. Storm surge inundation levels 1-4, corresponding wave heights, and tsunami inundation scenarios are also shown
121
2. RESEARCH METHODOLOGY
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2.1. TOPOGRAPHICAL SURVEY
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A topographical survey was conducted at the three barangays (the smallest administrative
124
division in the Philippines) where the questionnaire surveys were distributed, in order to
125
establish their relative height and how high a storm surge would reach in them. [40,41]. The
126
survey measured ground elevation and/or the level of houses at each point, using a GPS
127
[GPSMAP; Garmin Ltd.], a laser ranging instrument [TruPulse 360; Laser Technology, Inc.]
128
and prism (see Figure 2). Each survey started at the sea and proceeded towards the nearest
129
highest ground. Tide levels were corrected using the XTIDE software.
130 131
Figure 2. Topographical survey conducted by the authors in March 2016.
132
A topographic map of the community was also generated using ArcGIS 10.5, which was
133
overlaid with the storm surge and tsunami scenario inundation scenarios gathered. The GPS
134
points from the topographical surveys were then plotted on the map.
135
136
2.2. QUESTIONNAIRE SURVEY
137
The research employed five local enumerators to conduct structured questionnaire
138
surveys with residents amongst the three coastal barangays to ascertain their awareness of
139
tsunamis and storm surges. The surveys were conducted on 15-16th March 2016, which
140
resulted in a sample of 155 respondents (n=155), from 155 completed questionnaires. The
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questionnaire was drafted in English and then a modified version (in both English and
142
Filipino) was administered to individuals randomly encountered at the survey locations on an
143
opportunistic basis (typically those enjoying their free time outdoors, and who were willing to
144
participate in the survey). The questionnaire survey took about 10 minutes per individual to
145
complete. The survey questions were closed-ended, in order to rapidly appraise their
146
awareness to hazards. The data was encoded into the Statistical Package for the Social
147
Sciences (SPSS) to provide descriptive statistical analysis of the results. A chi-square test, a
148
one-way analysis of variance (ANOVA) or a Kruskal-Wallis Test, whenever applicable, were
149
used to determine statistical significance. A significance level of 0.05 was adopted for this
150
study. The information generated was then validated through group interviews with
151
government officials and community leaders.
152
2.3. GROUP INTERVIEWS
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Group interviews were conducted during two different time periods: 17 March 2016, and
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15-16 March 2017 (see Figure 3). The first interview was conducted the day after the
155
topographical surveys were carried out, and only involved members of the City Disaster Risk
156
Reduction and Management Office (CDRRMO). The second set of interviews were
157
conducted a year after, and involved the remaining stakeholders listed in Table 1 below.
158
During these set of interviews, preliminary findings from the questionnaire surveys with
159
residents were discussed with the informants for validation. The group interviews were
160
designed in order to provide narratives of the survey results, as well as to understand the
161
perception of disaster risk by residents and authorities.
162
Table 1. List of Group Interviews Stakeholder Provincial Government City Government
Office Provincial Disaster Risk Reduction and Management Office Puerto Princesa City Disaster Risk Reduction and Management Office
Community Leaders
Barangay Pagkakaisa
Community Leaders
Barangay Mandaragat
Community Leaders
Barangay Bagong Sikat
Affected Community
Barangay Bagong Sikat
Position of Informants Media and Officer
Information
City Disaster Risk Reduction and Management Officer Research and Training Officer Barangay Captain Barangay Councilor Barangay Secretary Barangay Treasurer Barangay Councilors Barangay Secretary Barangay Treasurer Barangay Captain Barangay Councilor Barangay Secretary Barangay Treasurer Residents
Number of Informants 2
3
4
4
4
5
163
164 165 166
Figure 3. Group interviews. Discussions with City Disaster Management Officials (left) and interviews with local community leaders (right)
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The group interviews followed a semi-structured format to ensure that participants could
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express their thoughts in a free-flowing manner. The following is a list of the guide questions
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employed:
170
•
Are you aware of your community being at risk to storm surges or tsunamis?
171
•
Has your community experienced coastal disasters in the past?
172
•
What is the primary hazard that your community is concerned with?
173
•
How do you provide residents with hazard information?
174
•
Do you have an emergency management system in place?
175
In addition to the above, the following questions were also asked during the group
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interview with the residents of Barangay Bagong Sikat:
177
•
Have you experienced a disaster before? What was it and when did it happen?
178
•
Where were you during the event?
179
•
Can you describe the sequence of events during the disaster?
180
•
How did you respond to these events?
181 182 183
3. RESULTS 3.1. TOPOGRAPHICAL SURVEY 3.1.1. BARANGAY PAGKAKAISA
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Barangay Pagkakaisa has a population of 1,131 people. The field survey started in the
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morning on 16th March 2016. Figure 4 shows a summary of the points surveyed, and a
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diagrammatic representation of their elevation.
187 188 189 190 191
Figure 4. Map of Brgy Pagkakaisa, showing areas at risk of storm surge and a diagrammatic representation of its cross-sectional elevation profile. Basemap Sources: Esri, DigitalGlobe, GeoEye, i-cubed, USDA FSA, USGS, AEX, Getmapping, Aerogrid, IGN, IGP, swisstopo, and the GIS User Community
192
Houses in Points C and D are 2.26 m above sea level when corrected by XTIDE. If the
193
Highest High-Water Level (HHWL) is considered (which was +1.8 m in 2016, the year the
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topographical survey was conducted) the houses are only 0.46 m above sea level. All
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surveyed points are within all hazard zones, and even small storm surges or tsunamis would
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flood them. Point E, the highest elevation surveyed, is still at risk to a 4 m storm surge or
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tsunami.
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3.1.2. BARANGAY MANDARAGAT
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Barangay Mandaragat is the most populous amongst the 3 communities surveyed, with
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9,210 residents. The survey was carried out on the 16th March 2016, with Figure 5 detailing
201
its outcome.
202 203 204 205 206
Figure 5. Map of Brgy Mandaragat, showing areas at risk of storm surge and a diagrammatic representation of its cross-sectional elevation profile. Basemap Sources: Esri, DigitalGlobe, GeoEye, i-cubed, USDA FSA, USGS, AEX, Getmapping, Aerogrid, IGN, IGP, swisstopo, and the GIS User Community
207
Point D, the best representative of the floor level of the houses in this community, is 1.5
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m above sea level (when corrected by XTIDE). The community would be at risk in the event
209
of a 2 m storm surge. When considering the HHWL, the houses would be at an elevation of -
210
0.3 m, which means that high tides may inundate the houses each year. The houses in this
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community are therefore at risk to storm surges and tsunamis, with points F and G being the
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only safe areas (in the nearest hill to the community).
213
3.1.3. BARANGAY BAGONG SIKAT
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Barangay Bagong Sikat has 7,497 residents and is located to the south of the city proper,
215
near the opening of the bay. Figure 6 outlines the summary of the points surveyed and its
216
cross-sectional diagrammatic representation. The survey started at 16th March 2016 at 16:48.
217 218 219 220 221
Figure 6. Map of Brgy Bagong Sikat, showing areas at risk of storm surge and a diagrammatic representation of its cross-sectional elevation profile. Basemap Sources: Esri, DigitalGlobe, GeoEye, i-cubed, USDA FSA, USGS, AEX, Getmapping, Aerogrid, IGN, IGP, swisstopo, and the GIS User Community
222
Point C represents the floor level of the houses in this community. It is in the middle of
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the settlement and is 2.78 m above sea level when corrected by XTIDE. Considering HHWL,
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the houses are at 0.96 m above sea level. The houses in this community can be inundated by a
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storm surge and tsunami of more than 3 m high in normal circumstances. During the highest
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tide of the year, a weak storm surge of 2 m may inundate the houses (to a depth of 1.04 m).
227
This community was affected by a storm surge event in 2008, though data on the exact
228
inundation height could not be found by the authors. Inferring from group interviews, the
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waves should have been more than 1 m, but less than 3 m. Points A, B, C, and D are all
230
within the storm surge and tsunami inundation areas. Point E is located at the edge of the area
231
that could be potentially flooded by a tsunami. Traversing from Point D to Point E requires a
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sudden uphill climb which may hinder mobility during an actual evacuation. Fishing boats
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are anchored along the coastline, which explains why many of these were damaged during
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the disaster event in 2008.
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3.1.4. EXPOSED POPULATION IN THE 3 COMMUNITIES
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The topographical survey indicates that the communities would be exposed to even weak
237
storm surges and tsunamis, and there is thus a need to determine the population at risk. To do
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so, the authors determined that the population of each community would be equally spread
239
over its area (from the 2015 Census of Puerto Princesa City, see Table 2), and then
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determined the exposure to each inundation level through GIS (see Table 3). Table 2. Total Population and Total Land Area of the 3 Communities Community Pagkakaisa
241 242
Mandaragat
Bagong Sikat
Total Population
1131
9210
7497
Total Land Area (in km2)
0.11
0.619
0.367
Table 3. Exposure to storm surge and tsunami scenarios in each community Community Pagkakaisa Coastal Hazards
Mandaragat
Bagong Sikat
Area (km2)
% of Area*
# of persons exposed
Area (km2)
% of Area
# of persons exposed
Area (km2)
% of Area
# of persons exposed
Level 1
0.039
35.45%
401
0.163
26.33%
2425
0.030
8.17%
613
Level 2
0.049
44.55%
504
0.227
36.67%
3377
0.037
10.08%
756
Level 3
0.067
60.91%
689
0.278
44.91%
4136
0.042
11.44%
858
Level 4
0.072
65.45%
740
0.344
55.57%
5118
0.047
12.81%
960
0.110
100.00%
1131
0.314
50.73%
4672
0.075
20.44%
1532
Storm Surge
Tsunami *Represents the percentage of the total land area of the community that may be inundated by each coastal hazard scenario
243
3.2. QUESTIONNAIRE SURVEY
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The results of the questionnaire surveys are outlined below.
245
3.2.1. DEMOGRAPHICS
246
The study surveyed 155 respondents in 3 coastal communities (Barangays) in Puerto
247
Princesa City, Palawan. There were 57 respondents in Barangay Pagkakaisa, 52 in Barangay
248
Mandaragat, and 46 in Barangay Bagong Sikat. 101 (65.2%) respondents were female, 52
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(33.5%) were male, and 2 (1.3%) did not indicate any gender. A chi-square test indicated that
250
the gender does not vary by location (p-value = 0.58). Table 4 outlines the gender distribution
251
per community. Table 4. Distribution of Male and Female Respondents by Community
Male Location
Barangay Pakakaisa Barangay Mandaragat Barangay Bagong Sikat Total
Count Count Count Count Subtable N %
23 15 14 52 33.5%
Gender No Answer 34 0 36 1 31 1 101 2 65.2% 1.3%
Female
Total 57 52 46 155 100.0%
252 253
Part of the reason for the gender imbalance may be due to the survey being conducted
254
during daytime. Most respondents were housewives or store owners in the area, whereas the
255
men were either at sea or at work. Figure 7 shows that respondents were mostly women
256
within the working age bracket of 20 to 59 years old. 35 30
Count
25 20 15 10 5 0 No Answer
19 and below
20 to 29
30 to 39
40 to 49
50 to 59
60 to 69
70 to 79 Above 80
Age of Respondents Female
Male
No Answer
257 258
Figure 7. Distribution of respondent's age according to gender
259
This emphasizes the role of women in disaster preparedness, as they are more exposed to
260
disasters in these areas. As the questionnaire survey was conducted during daytime, the high
261
number of female respondents indicates that they are less likely to have an occupation that
262
requires travel outside of the community. Figure 8 shows the gender distribution per
263
occupation of the respondents.
Count
Distribution of Occupation by Gender 50 45 40 35 30 25 20 15 10 5 0
Occupation
264 265
Female
Male
No Answer
Figure 8. Distribution of occupation by gender
266 267
Most of the respondents indicated that they were housewives (27.7%), self-employed or
268
small store owners (19.4%), fisherfolk (16.1%), and unemployed (11.6%). Aside from fishing,
269
the next 3 top occupations in the community were dominated by women (who usually
270
contribute to their families by engaging in home-based businesses [42]. This is typical of an
271
informal settler community, which are typically characterised by the high number of women
272
dominating the local economy [43]).
273
3.2.2. DISASTER EXPERIENCE
274
Respondents were asked about their experiences regarding flooding from the nearby coast
275
or a river. While the researchers were not able to determine whether respondents could
276
discern the difference between coastal or fluvial flooding, most perceived that their area was
277
at little to no risk to floods (See Table 5). A Kruskal-Wallis test determined that the
278
perception of the possibility of flooding was the same across gender and age (asymptotic p-
279
values = 0.330 and 0.441, respectively). During the group interviews participants stated that
280
Palawan rarely experienced strong storms, as it was outside the usual typhoon paths.
281
Table 5. Respondent's perception of possibility of flooding from seas or rivers per Barangay Pakakaisa
Mandaragat
Bagong Sikat
Total
Barangay’s name Count Perception of Possibility of Flooding from Seas or Rivers
No Answer Not at all Little Moderate Strongly Very Strongly Total
0 30 19 5 0 3 57
% Count 0.0% 2 52.6% 29 33.3% 16 8.8% 2 0.0% 2 5.3% 1 100.0%
52
% Count 3.8% 1 55.8% 13 30.8% 18 3.8% 8 3.8% 2 1.9% 4 100.0%
46
% Count 2.2% 3 28.3% 72 39.1% 53 17.4% 15 4.3% 4 8.7% 8 100.0%
155
% 1.9% 46.5% 34.2% 9.7% 2.6% 5.2% 100.0%
282 283
However, there is a significant difference (p= 0.004) amongst communities when it
284
comes to the perception of possibility of flooding. Table 5 shows that more respondents in
285
Bagong Sikat answered that there was a moderate to very strong threat of flooding in their
286
vicinity (though overall most respondents had never experienced any prior damage, see
287
Figure 9). This was clearly higher than in the other 2 barangays.
Stacked Bar of Percentage of Respondents per Community with Previous Disaster Experience
3%
35%
62%
288 289 290 291
Previous Disaster Experience Yes No No Answer
% Respondents per Community
Previous Disaster Experience (N=155)
100% 90% 80% 70% 60% 50% 40% 30% 20% 10% 0% Barangay Pakakaisa (n=57)
No Answer
Barangay Mandaragat (n=52) Community No
Barangay Bagong Sikat (n=46)
Yes
Figure 9. Pie chart of previous disaster experience with stacked bar of percentage of respondents per community
292
An ANOVA test yielded there is a highly significant difference (p-value = .000) on past
293
disaster experience amongst communities. Figure 9 also shows that most respondents who
294
responded positively were from Barangay Bagong Sikat. Respondents who have previous
295
disaster experience were asked about the extent of the damage (see Table 6). Most of those
296
who reported total damage were from Barangay Bagong Sikat. Residents stated that a storm
297
surge event occurred in the area, as will be discussed later in the section regarding the group
298
interview findings.
299
Table 6. Extent of damage from previous disaster experience by community (n=54) Extent of Damage Minor (small cracks, Major (large cracks, slightly torn roofs, slightly torn walls, Total (Totally etc.) etc.) Destroyed) Barangay Count % Count % Count % Pakakaisa 5 26.3% 6 42.9% 1 4.8% Mandaragat 9 47.4% 0 0.0% 1 4.8% Bagong Sikat 5 26.3% 8 57.1% 19 90.5% Total 19 100.0% 14 100.0% 21 100.0%
Total Count 12 10 32 54
% 22.2% 18.5% 59.3% 100.0%
300 301 302
3.2.3. STORM SURGE AND TSUNAMI RISK PERCEPTION Respondents were also asked about their perception of storm surge and tsunami risk (see
303
Table 7).
304
Table 7. Storm surge and tsunami knowledge by community Storm Surge Knowledge Yes Barangay Pakakaisa
No
Tsunami Knowledge
No Answer
Yes
No
No Answer
Count % Count % Count % Count % Count % Count % 41 71.9% 16 28.1% 0 0.0% 52 91.2% 5 8.8% 0 0.0%
Mandaragat
30 57.7%
21 40.4%
1 1.9%
45 86.5%
6 11.5%
1 1.9%
Bagong Sikat
36 78.3%
9 19.6%
1 2.2%
42 91.3%
3 6.5%
1 2.2%
107 69.0%
46 29.7%
2 1.3%
139 89.7%
14 9.0%
2 1.3%
Total
305 306
69% of the respondents knew what a storm surge is, while 89.7% knew what a tsunami is.
307
The reason for such relatively high level of awareness probably resides in media coverage of
308
the 2011 Tohoku Earthquake and Tsunami and 2013 Typhoon Haiyan, respectively (as
309
reported during the interviews). ANOVA tests indicate that there is no significant difference
310
between locations about knowledge of storm surges (p-value = 0.095) and tsunamis (p-value
311
= 0.677). It is interesting to note that the understanding on storm surge (69%) among
312
population in the study site is higher than that in previous studies in neighbouring countries,
313
such as Jakarta, Indonesia (46%) and Mekong delta, Vietnam (55%) [26,44]. Thus, it appears
314
that the term ‘storm surge’ became more prevalent in the aftermath of the 2013 typhoon,
315
which destroyed large sections of the eastern part of the Philippines [21,45].
316
Table 8 shows the perceived level of danger that storm surges represent. The total
317
percentage of those who answered from “not at all” to “moderate” (64.5%) and the sum of
318
the percentages of those who answered from “moderate” to “very strongly” (64.5%) are
319
roughly equal. This means that, overall, respondents are not clear about the threat posed by
320
storm surges. When asked during the interviews informants stated that while storm surges are
321
dangerous, they do not represent a serious threat to them as tropical storms do not regularly
322
pass close to Palawan.
323
Table 8. Count and percentage of perceived storm surge danger by community
No Answer Not at all Little Moderate Strongly Very Strongly Total
Pakakaisa Count % 0 0.0% 12 21.1% 12 21.1% 20 35.1% 5 8.8% 8 14.0% 57 100.0%
Community Mandaragat Count % 1 1.9% 4 7.7% 17 32.7% 13 25.0% 8 15.4% 9 17.3% 52 100.0%
Bagong Sikat Count % 1 2.2% 1 2.2% 7 15.2% 14 30.4% 5 10.9% 18 39.1% 46 100.0%
Total Count % 2 1.3% 17 11.0% 36 23.2% 47 30.3% 18 11.6% 35 22.6% 155 100.0%
324 325
Figure 10 shows that a majority (80.4%) of those from Barangay Bagong Sikat responded
326
that storm surges represent at least a moderate danger to them, compared with much lower
327
percentages in Barangay Pagkakaisa (57.9%) and Barangay Mandaragat (57.7%). A
328
Kruskall-Wallis Test between communities and their perception of storm surge danger
329
yielded a statistically significant result (asymptotic p-value = 0.003). Group interviews
330
revealed that residents in this community recognize that they are at risk of suffering from
331
these events due to this relatively recent disaster experience. However, conducting the same
332
test on age and gender does not yield any significant difference (asymptotic p-values of 0.580
333
and 0.456 respectively). 100% 90%
% Respondents
80% 70%
No Answer
60%
Not at all
50%
Little
40%
Moderate
30%
Strongly
20%
Very Strongly
10% 0% Barangay Pakakaisa
Barangay Mandaragat Barangay Bagong Sikat Community
334 335
Figure 10. Perceived level of storm surge threat by community
336
The perceived threat that tsunamis present, on the other hand, is different (see Table 7).
337
Respondents emphasize that the sudden nature of the hazard is what makes it dangerous.
338
According to interviews with the local disaster managers and village leaders, warnings from
339
national government agencies about the possible risks of a tsunami taking place have been
340
provided to them.
341
342
Table 9. Count and percentage of perceived tsunami danger by community
Perception of No Answer Tsunami Danger Not at all Little Moderate Strongly Very Strongly Total
Pakakaisa Count % 1 1.8% 6 10.5% 5 8.8% 14 24.6% 9 15.8% 22 38.6% 57
100.0%
Community Mandaragat Count % 1 1.9% 5 9.6% 5 9.6% 9 17.3% 15 28.8% 17 32.7% 52
100.0%
Bagong Sikat Total Count % Count % 1 2.2% 3 1.9% 0 0.0% 11 7.1% 5 10.9% 15 9.7% 6 13.0% 29 18.7% 4 8.7% 28 18.1% 30 65.2% 69 44.5% 46
100.0%
155
100.0%
343 344
More than half of respondents stated that they strongly feel that a tsunami would be
345
dangerous for their community (See Figure 11). Despite this higher overall perception of
346
danger (compared to storm surges), a Kruskall-Wallis test determined that there is also
347
statistically significant difference amongst the communities (asymptotic p-value = 0.014).
348
Again, Barangay Bagong Sikat’s higher perception of tsunami danger is probably also a
349
reflection of their increased level of awareness as a result of a relatively recent disaster
350
experience. 100% 90%
% Respondents
80% 70%
No Answer
60%
Not at all
50%
Little
40%
Moderate
30%
Strongly
20%
Very Strongly
10% 0% Barangay Pakakaisa
Barangay Mandaragat Barangay Bagong Sikat Community
351 352
Figure 11. Perceived level of tsunami danger by community
353 354
3.2.4. MONITORING AND WARNING Respondents detailed their sources of hazard information by choosing from several
355
possible responses (multiple choices were allowed, with Table 10 summarizing the answers).
356
Table 10. Count of disaster information and warning source by community
Barangay Pakakaisa Disaster Information and Warning Source
TV, Radio Print Media (Newspapers, Pamphlets, Brochures) Public Address System (Fixed Loudspeakers, Mobile Loudspeakers, etc.) Internet Family, relatives Neighbors Authority Figures (Village Leaders, Police, Firefighters, etc.)
Community Barangay Barangay Mandaragat Bagong Sikat 52 50 44 4
6
3
4
0
1
6 5 11 16
2 4 11 3
4 7 14 11
NGOs and other aid organizations Self-taught or understood by observation (after seeing or hearing the sea)
3
1
2
3
0
1
Others No Answer
0 3
0 1
0 2
357 358
Almost all respondents (146) rely on TV and Radio as their source of disaster information,
359
as they are convenient and readily available. It is also through this that the Philippine Public
360
Storm Warning System (PPSWS) is relayed, which provides relevant information regarding
361
tropical cyclones such as track, wind speed, possible time of earliest impact, and recently,
362
storm surges (shown in Table 11) [46,47]. Despite the proliferation of personal mobile
363
phones, the dependency on the internet, including SNS, is still far below that of traditional
364
media.
365
366
Table 11. The Philippine Public Storm Warning System [46,47] Storm Signal Number Wind Speed 30 km/h to 60 km/h 1 60 km/h to 100 km/h 2 100 km/h to 185 km/h 3 185 km/h to 220 km/h 4 Above 220 km/ 5
Hours before Earliest Impact 36 24 12 12 12
367 368 369
Respondents were also asked whether they have knowledge of any existing local tsunami warning system in the area (see Figure 12).
3%
37%
60%
Yes
No
No Answer
370 371
Figure 12. Knowledge of existing tsunami warning systems in the area
372
While the majority stated that they have no knowledge of any local tsunami warning
373
system, 37% answered that they believe that there is one installed in their community.
374
However, interviews with local disaster managers indicate that there are no tsunami early
375
warning systems in the area. Tsunami Detection and Early Warning Systems are only
376
installed in a few selected areas of the Philippines, and this does not include Palawan [48,49].
377
3.2.5. EMERGENCY MANAGEMENT
378
The respondents were asked if they had participated in any evacuation drill in the last 5
379
years, as well as their knowledge on where to evacuate in the case of storm surges and
380
tsunamis. Figure 13 shows the respondent’s reported participation in evacuation drills,
381
indicating how most (65% of all respondents, n=155) had not participated in any evacuation
382
drill in the past 5 years.
Yes (5 or more times) Barangay Bagong Sikat
Yes (4 times) Yes (3 times)
Barangay Mandaragat
Yes (2 times) Yes (1 time)
Barangay Pakakaisa No 0%
20%
40%
60%
80%
% of respondents
100%
No, but I know the evacuation route No Answer
383 384 385 386
Figure 13. Bar chart of participation of respondents to evacuation drills and stacked bar percentage of respondents per communities who participated in evacuation drills in the last 5 years
387
50% of the respondents from Barangay Bagong Sikat stated that they participated in at
388
least 1 evacuation drill in the last 5 years, compared to around 30% in the other communities.
389
Kruskal-Wallis Test determined that participation in these drills is significantly different
390
according to location (asymptotic p-value = 0.022), and previous disaster experience clearly
391
resulted in a higher participation in evacuation drills.
392
Evacuation drills provide those participating with knowledge of where, when, and how to
393
evacuate. The respondents were asked whether they know where to evacuate to for each of
394
the hazards (See Table 12).
395
Table 12. Knowledge of storm surge and tsunami evacuation area by community
Storm Surge Evacuation Knowledge Tsunami Evacuation Knowledge
Community Pakakaisa Mandaragat Bagong Sikat Totals Count % Count % Count % Count Total % Yes 47 82.5% 34 65.4% 35 76.1% 116 74.8% No 10 17.5% 17 32.7% 10 21.7% 37 23.9% No Answer 0 0.0% 1 1.9% 1 2.2% 2 1.3% Total 57 100.0% 52 100.0% 46 100.0% 155 100.0% Yes 46 80.7% 33 63.5% 37 80.4% 116 74.8% No 10 17.5% 17 32.7% 8 17.4% 35 22.6% No Answer 1 1.8% 2 3.8% 1 2.2% 4 2.6% Total 57 100.0% 52 100.0% 46 100.0% 155 100.0%
396
About three quarters of the respondents stated that they do know where to evacuate to in
397
the event of a storm surge or tsunami. Interestingly, this knowledge level is almost the same
398
for storm surge and tsunamis, implying that they could perceive that these two coastal
399
hazards are similar types of physical phenomenon. However, it is important to note that for
400
most Filipinos an evacuation shelter is typically the nearest Barangay Hall, Church, or school,
401
which are not necessarily safe during a disaster, and the physical impact due to a tsunami and
402
storm surge is not necessarily the same.
403 404
3.3. GROUP INTERVIEWS AND THE CASE OF TROPICAL STORM NUOL (2008)
405
Respondents from Barangay Bagong Sikat had experienced damage during a previous
406
disaster but could not identify the year in which it occurred. The range of responses was
407
between 2007 and 2010, which the group interviews narrowed to an event in 2008: tropical
408
depression Nuol, (locally known as “Tonyo”, which affected the Philippines from 13 – 16
409
November 2008). At its peak, it was a tropical storm with 75 km/h (45 mph) 10-min
410
sustained winds and a central pressure of 994 hPa, though this was after it had passed the
411
country. For the Philippines, this was a relatively weak storm. Authorities did provide
412
warnings about the storm (which passed 60 km south of Puerto Princesa City) and the
413
possibility of landslides, flash flooding, and storm surges [50,51].
414
Respondents confirmed that Barangay Bagong Sikat experienced a storm surge event.
415
Three large waves slammed into the community, destroying houses and boats. Residents also
416
feared that the fire that broke out in the community could be carried by winds towards a
417
nearby petroleum depot. Barangay leaders indicated that 600 families were affected, 150
418
small fishing boats were destroyed, and 100 houses were destroyed or sustained damage.
419
However, interviews yielded different interpretations of the phenomena. The respondents
420
were confused as to what had caused the disaster. Most informants stated that it was caused
421
by a weather system that affected the Philippines, though many believed that it was in
422
mainland Luzon.
423
Further literature review found that the disaster was not archived properly. The event
424
happened in 2008, when most local news did not have their own websites, though
425
information was detailed in blogs by local journalists. According to them, 2 barangays were
426
hit, 1050 families were affected, 600 houses were destroyed and 278 partially damaged
427
[52,53]. One of these communities was Barangay Bagong Sikat. The event was also reported
428
nationally, though there was some discrepancy in the information published. ABS-CBN
429
News (2008) quotes an unnamed Red Cross report that the storm damaged 4 barangays, with
430
3 people reported missing, and 213 families being evacuated [54]. They further reported that
431
a fire and a storm surge had affected Purok Sampaguita and a couple of other communities
432
within Barangay Bagong Sikat. Puerto Princesa City declared a state of calamity as a
433
response to this event [55]. There was thus a discrepancy in the number of communities
434
affected, with local news stating 2 while the national news indicated 4. The news sites also
435
stated that the residents affected evacuated within and outside the affected community [54].
436
4. DISCUSSION
437 438
4.1. EXPOSURE TO COASTAL HAZARDS IN URBAN COASTAL COMMUNITIES RESIDING IN “LOW RISK” AREAS
439
The topographical survey showed that the highest elevation amongst the houses in the
440
three communities is +2.68 m, and the lowest is at +1.5 m. All houses are significantly below
441
the worst tsunami or storm surge scenario (potentially up to 4.0 m – 5.0 m in height). If
442
corrected by HHWL, which was 1.8 m in 2016, the lowest houses are -0.3 m below HHWL,
443
meaning they could experience tidal flooding. Thus, even in the minimum 2.0 m scenario for
444
storm surges the communities would clearly be flooded. Based just on this physical
445
assessment, the communities surveyed are exposed to even weak coastal hazards.
446
The Puerto Princesa City case can be compared to other urban communities in Southeast
447
Asia that are experiencing the effects of rapid development and urbanization. Impoverished
448
communities in Jakarta, for instance, would experience potential increased flooding in the
449
next few decades and will be challenged to cope with these hazards [26,56,57]. Communities
450
in Vietnam would likewise be at a higher risk in the future [44,58,59]. Moreover, given that
451
there is a prevailing perception that Puerto Princesa is at low risk, there is no immediate need
452
to invest in physical defences against coastal flooding, potentially exposing their inhabitants
453
to future danger.
454 455
4.2. DISASTER AWARENESS AND EXPERIENCE IN LOW RISK COASTAL COMMUNITIES
456
Coastal disaster events reported in the news, mainly the 2013 Typhoon Haiyan and the
457
2011 Tohoku Earthquake and Tsunami, were identified during the group interviews as the
458
primary examples of storm surge and tsunami events. Clearly, media reports on major coastal
459
disaster events have had an impact on local people’s knowledge about different types of
460
hazards [21,32,60]. This is despite the prevailing perception in 2 out of 3 communities that
461
their settlements are not at risk. While tsunamis are viewed by the communities as
462
threatening (due to the limited warning that precedes them), the inaccurate perception that
463
storms do not pass through the province creates a miscalculation their exposure to storm
464
surges. This is similar to the case of Typhoon Haiyan, were residents did not know what a
465
storm surge was, which clearly had an impact on casualty rates [16,17,21]. Thus, there is a
466
limit to the amount of awareness that the media can create, highlighting the importance of
467
disaster experience (and its transmission across generations).
468
As stated earlier, only residents of Barangay Bagong Sikat appeared to have a different
469
opinion, due to a prior disaster experience, even though respondents were not exactly sure
470
when this had taken place. The group interviews highlighted this prior disaster experience,
471
though the event was neither properly explained to the community members nor archived
472
properly for local transmission of knowledge from one generation to another, or to other parts
473
of the city.
474
Disaster awareness decays over time, with those who experienced it having high
475
awareness about future events, while if there are no programs to keep the memory of the
476
disaster alive then it will be forgotten by the 3rd generation [21]. Low understanding of
477
previous events lead to a lack of basic disaster awareness, as in the case of four communities
478
in Trinidad and Tobago [61]. The storm surge event in Barangay Bagong Sikat is now in its
479
2nd generation, as 10 years have passed since the disaster, though this information is not being
480
transmitted effectively, and that awareness is now decaying. The narratives and the
481
information gathered from secondary sources is thus important in preserving the memory of
482
the disaster event alive. Moreover, the fact that this event took place in an area that is thought
483
of to be safe from coastal disasters can be important to raise disaster awareness in Puerto
484
Princesa City.
485
When communities are aware of previous disasters, it will be more likely that individuals
486
will attempt to seek information regarding the potential hazards that could affect them. At
487
present, communities in Puerto Princesa City mostly rely on the TV and radio to obtain
488
information, as information regarding storms is mostly transmitted using such medium. On
489
the other hand, for the case of tsunamis most respondents stated that they do not know
490
whether there is a tsunami warning system in the vicinity. Effective disaster governance
491
requires a multi-stakeholder engagement in decision making, which in turn, requires multiple
492
sources of reliable information [62,63]. The lack of multiple sources of information and the
493
lack of awareness about coastal hazards can undermine preparedness efforts, as in the case of
494
Typhoon Haiyan in 2013 [16]. This is reflected in participation in evacuation drills where
495
most respondents had not participated in any in the past 5 years, and thus few knew where to
496
evacuate to in the event of a storm surge or tsunami.
497
4.3. CHALLENGES AND OPPORTUNITIES FOR DISASTER GOVERNANCE
498
IN COASTAL COMMUNITIES THAT CONSIDER THEMSELVES TO BE
499
AT LOW RISK
500
Puerto Princesa City is susceptible to coastal hazards, though they have a lower
501
probability of happening than in other parts of the Philippines. Nevertheless, while the
502
possibility is low, there is still the need to inform residents about the risks, as many live very
503
near or directly above the shoreline. This increases exposure to even weak coastal hazards,
504
that would not otherwise result in a disaster (if people lived in areas that were higher or
505
further away from the coast).
506
Disaster awareness is vital for effective disaster governance, and low awareness will
507
undermine efforts to improve disaster risk reduction. In order to protect development gains,
508
the case of the three communities in Puerto Princesa City highlights the need to increase
509
disaster awareness in areas with a perception low susceptibility to natural hazards. Thus,
510
awareness is a component that may initiate investments towards implementing effective
511
disaster governance strategies.
512
5. CONCLUSION
513
The research sought to ascertain how disaster risk is understood in areas that are only
514
slightly susceptible to natural hazards, in order to improve disaster risk governance in coastal
515
areas that may be potentially at risk in the future. The three communities studied in Puerto
516
Princesa City were used as a representative of communities that are at lower risk of suffering
517
from natural hazards than other parts of a disaster-prone country. The authors found that
518
incomplete understanding of risks, particularly the interplay of hazard, exposure and
519
vulnerability, increases the possibility of disasters happening in areas where the population
520
has the perception that they have a low susceptibility to certain types of events. As population
521
increases and takes up residence in coastal areas, exposure to the hazard also increases. This
522
means that beyond the threat of the loss of life due to disasters, livelihoods and other
523
economic opportunities can also be affected.
524
In order to address this and potentially decrease hazard exposure, there is a need to
525
increase disaster awareness by properly looking at an area’s disaster history. Disaster risk
526
managers must learn about previous events within their region and use these as examples for
527
the communities they oversee, in conjunction with using case studies of larger events
528
elsewhere. Media coverage of the 2011 Tohoku Earthquake and Tsunami and 2013 Typhoon
529
Haiyan has already increased the awareness about storm surges and tsunamis in many
530
communities around the planet. This knowledge can further be solidified with a local
531
example, as residents who have experienced a previous coastal disaster typically show a
532
higher participation in disaster preparedness activities.
533
Finally, disaster risk assessments, especially at the local level, should be retrospective,
534
introspective, and prospective. The case of 2008’s Tropical Storm Nuol represents an event
535
that can be used to illustrate the point that disasters can take place in areas that rarely
536
experiences coastal hazards. This exemplifies the problem that disasters typically affect most
537
those who are least prepared and most vulnerable. Such events should be taken into
538
consideration in current planning and preparedness activities, and long-term plans on disaster
539
prevention should consider increased exposure and vulnerability due to urban development.
540
6. ACKNOWLEDGMENTS
541
The authors would like to acknowledge the assistance of the AUN/SEED-Net for their
542
support of this research through the “Coastal disasters and climate change in Southeast Asia:
543
An assessment and countermeasures for sustainable development of the fast-growing coastal
544
areas” project. Also, the Global Program on Sustainability Science, Graduate Leadership
545
Initiative, supported by the Japanese Ministry of Education (MEXT) provided support for the
546
questionnaires that were conducted. A part of the present work was performed as a part of
547
activities of Research Institute of Sustainable Future Society, Waseda Research Institute for
548
Science and Engineering, Waseda University. HT was also funded by the grant for Tokyo
549
Institute of Technology (Japan Society for the Promotion of Science, 16KK0121).
550
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