
NSF Org: |
CMMI Division of Civil, Mechanical, and Manufacturing Innovation |
Recipient: |
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Initial Amendment Date: | November 13, 2018 |
Latest Amendment Date: | November 13, 2018 |
Award Number: | 1902888 |
Award Instrument: | Standard Grant |
Program Manager: |
Jacqueline Meszaros
CMMI Division of Civil, Mechanical, and Manufacturing Innovation ENG Directorate for Engineering |
Start Date: | November 1, 2018 |
End Date: | October 31, 2020 (Estimated) |
Total Intended Award Amount: | $30,000.00 |
Total Awarded Amount to Date: | $30,000.00 |
Funds Obligated to Date: |
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History of Investigator: |
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Recipient Sponsored Research Office: |
1500 SW JEFFERSON AVE CORVALLIS OR US 97331-8655 (541)737-4933 |
Sponsor Congressional District: |
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Primary Place of Performance: |
101 Kearney Hall Corvallis OR US 97331-8507 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): | HDBE-Humans, Disasters, and th |
Primary Program Source: |
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Program Reference Code(s): |
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Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.041 |
ABSTRACT
This Rapid Response Research (RAPID) project examines fundamental issues on the evacuation time estimates associated with earthquake and tsunami hazards by linking social science warning research, transportation engineering, and casualty modeling. This devastating event to Palu and the nearby cities of Donggala and Mamuju, Indonesia is of major scientific relevance to American researchers because it is similar in nature to the predicted M9.0 Cascadia Subduction Zone (CSZ) earthquake. The Palu event has uniquely important implications to the coastal communities in the CSZ. First, the 20-ft tsunami generated by a M7.5 strike-slip earthquake resembles a similar local source of tsunami generation on the Pacific Northwest (PNW) coast. Understanding people's behavioral responses to the Palu earthquake and tsunami can provide unique insights to improve the preparedness of PNW coastal communities and other coastal areas of United States. Second, the Palu event represents a "worst case scenario" (earthquake, tsunami, large inland flows of mud, and liquefaction, where soil failure swallowed 1,400 houses) in which the event happened at the same time a large number of people had congregated on a beach for a festival. It is clear that the densely populated coastal areas took heavy damage because of tsunami-generated large inland flows of mud. Intense ground shaking from the preceding earthquake may have triggered soil liquefaction and lateral spreading. These combined processes are also common near streams and on reclaimed land that can produce destructive mudslides in relatively flat areas on the PNW coast from the predicted CSZ event. Third, the unique geographic location of Palu sitting at the end of a narrow 10km-long finger-like bay likely amplified the fast-moving surge of water and wave energy on the relatively shallower seabed, exacerbating the damaging power of the tsunami on the affected people and communities. There are similar communities on the PNW coast located on this type of bay. Lastly, many PNW coastal communities suffer a similar lack of tsunami preparedness. In the CSZ, the threat of near-field tsunamis has been recognized only recently, so many communities have based their evacuation plans on far-field tsunami scenarios that provide 4-6 hours of forewarning. The difficulty of predicting such events with the current technology for earthquake and tsunami warning makes it essential to learn from the Palu event. In addition, a study of Palu tsunami evacuations will inform evacuation planning for other similar type rapid-onset disasters such as flash floods.
This project uses the Protective Action Decision Model (PADM) as a guide to collecting empirical data on people's behavioral responses to the Palu earthquake and tsunami. Questions include: How many people recognized the earthquake shaking as an environmental cue for a tsunami onset? How many people received warnings from officials, news media, and peers? How did people respond to the threat? This project uses a validated survey procedure previously used in American Samoa (2009), Christchurch (2011), Tohoku (2011), Cook Strait (2013), and Lake Grassmere (2013). Collected data focus on (1) the amount of time it took officials to decide to issue tsunami evacuation warnings; (2) the tsunami warning sources, channels, messages and warning dissemination times; (3) people's evacuation participation rates, preparation times, and departure times; and (4) people's evacuation logistics.
This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
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PROJECT OUTCOMES REPORT
Disclaimer
This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.
The overall objective of this RAPID proposal is to use the Protective Action Decision Model (PADM) as a guide to collecting empirical data on people's behavioral responses to the Palu earthquake and tsunami. Specifically, this project has collected a uniquely valuable dataset to respond the following seven major research objectives (RO): RO 1: Collected data on the amount of time it took officials to decide to issue tsunami evacuation warnings; RO 2: Collected data on tsunami warning sources, channels, messages and warning dissemination times. This will include data on people's ability to recognize earthquake shaking as an environmental cue to tsunami onset; RO 3: Collected data on people's evacuation participation rates (vs. sheltering in-place), preparation times, and departure times; RO 4: Collected data on people's evacuation logistics (e.g., route choices, destination/accommodations choices, evacuation durations, and evacuation costs); RO 5: Assessed the extent to which earthquake/tsunami brochures were distributed or workshops were held before the event and if they predict shorter evacuation preparation and departure times; RO 6: Assessed the ability of physical, social, and household contexts; social and environmental cues; socially-transmitted warnings; demographic characteristics; prior experience; and cultural background to predict warning receipt, risk perception/personalization, evacuation decisions, and evacuation departure times; and RO 7: Assess the ability of demographic data to predict people's evacuation logistics.
This project achieved three interdisciplinary objectives that link social science warning research, transportation engineering, and casualty modeling. First, it extended warning research, which has focused substantially on hurricanes, to tsunamis--thus providing more information on warning response in rapid onset events. Second, it seeked to replicate and extend the findings from the one major earthquake/tsunami, the 2009 American Samoa. Third, it omplemented the recent study of the Uttarakhand India flash flood.
The data on warning dissemination and household preparation times will significantly reduce the uncertainty associated with current estimates of tsunami evacuation departure times that are used in evacuation transportation models. More accurate tsunami ETEs will provide a sound scientific basis for estimating casualty rates under existing terrain and evacuation route system conditions. In turn, this baseline condition can be used to examine the potential effectiveness of hazard education programs that increase recognition of earthquake shaking as an environmental cue to tsunami onset, thus eliminating authorities' decision times and reducing warning dissemination time distributions.
This study used the Protective Action Decision Model (PADM) as a guide to collect about 488 household residents' responses to the 2018 Palu Indonesia M7.5 earthquake and tsunami. The results show that (1) The disparity between the widespread availability of motor vehicles and the transportation mode actually used to evacuate (foot) requires an explanation. Of course, not all respondents had access to motorized vehicles with which to evacuate. Moreover, the research team's interviews and observations indicated the majority of the motor vehicles are motorcycles. Thus, even people with motorcycles might have evacuated by foot because 1) motorcycles were unable to evacuate all family members, 2) motorcycles might have taken more time to prepare to evacuate than evacuating by foot, 3) damage to the road network by liquefaction and collapsed buildings might have impeded vehicular travel. Whatever the explanation is, this result is consistent with the 2004 Thailand tsunami in which 75% of the respondents evacuated by foot and the evacuation expectations survey in Kamakura City Japan, in which 71% of the respondents expected to evacuate by foot. However, these results are quire different from the 53% of the respondents in the American Samoa tsunami who evacuated by car and the 75% of those in the evacuation expectations survey in the CSZ that expected to evacuate by car. Consequently, further research is needed to identify the determinants of tsunami evacuation model choice. (2) Although 43% of the respondents had a motorized vehicle (car, truck or motorcycle) available to them, 67% of them evacuated by foot, 29% in their own motor vehicles, and 4% carpooled in a friend's or neighbor's vehicle. For their evacuation destinations, 31% respondents went to other villages but 69\% stayed within their own village. For their evacuation accommodations, most respondents went to a public location such as a park (37%), but a few went to the home of a relative (6%), a mosque (5%), an official shelter (4%), the home of a friend (2%), or another location (47%). (3) 65% of them left within 5 minutes, 76% within 10 minutes, 84% within 15 minutes, and 95% within 30 minutes. Only 4% took more than 40 minutes to leave.
This study also compared the response behaviors from this study with the past earthquake and tsunami events such as the 2009 American Samoa (M8.0), the 2011 Christchurch (M6.3), the 2011 Hitachi (M9.0). The purpose of this comparison is to identify what are the commonalities and differences.
Last Modified: 07/09/2021
Modified by: Haizhong Wang
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