| Literature DB >> 34352028 |
Toru Miwa1,2, Hidetake Matsuyoshi3, Yasuyuki Nomura4, Ryosei Minoda5.
Abstract
This study aimed to examine the types and causes of dizziness experienced by individuals after a major earthquake. This cross-sectional study enrolled healthy participants who experienced the 2016 Kumamoto earthquakes and their aftershocks. Participants completed a questionnaire survey on their symptoms and experiences after the earthquakes. The primary outcome was the occurrence of dizziness and the secondary outcome was the presence of autonomic dysfunction and anxiety. Among 4,231 eligible participants, 1,543 experienced post-earthquake dizziness. Multivariate logistic regression analysis revealed that age (≥21, P < .001), female sex (P < .001), floor on which the individual was at the time (≥3, P = .007), tinnitus/ear fullness (P < .001), anxiety (P < .001), symptoms related to autonomic dysfunction (P = .04), and prior history of motion sickness (P = .002) were significantly associated with the onset of post-earthquake dizziness. Thus suggesting that earthquake-related effects significantly affect inner ear symptoms, autonomic function, and psychological factors. Earthquake-induced disequilibrium may be further influenced by physical stressors, including sensory disruptions induced by earthquake vibrations, changes in living conditions, and autonomic stress. This study increases our understanding of human equilibrium in response to natural disasters.Entities:
Mesh:
Year: 2021 PMID: 34352028 PMCID: PMC8341659 DOI: 10.1371/journal.pone.0255816
Source DB: PubMed Journal: PLoS One ISSN: 1932-6203 Impact factor: 3.240
Fig 1Map of Kumamoto, 2016.
Blue Xs indicate the epicenters. Magenta to yellow colors indicate earthquake size (Shindo data). Information was reprinted from the Japan Meteorological Agency (https://www.jma.go.jp/jma/indexe.html) under a CC BY license with permission from the Japan Meteorological Agency, original copyright 2016.
Participants’ details.
| PEDS group | |
| People who felt the illusion sway: 1,543 | |
| Non-PEDS group | |
| People who did not feel the illusion sway: 2,113 |
PEDS, post-earthquake dizziness syndrome.
Fig 2PEDS frequency according to sex, age, and earthquake parameters.
a) PEDS was present in 1,543 of the 3,656 participants (42.2%). The incidence of PEDS was higher in female than male participants. b) Female participants in their 30’s were more likely to experience PEDS (73%, asterisk) than female participants of other ages. Male participants in their 40’s were more likely to experience PEDS (60%, asterisk) than male participants of other ages. c) PEDS was most frequently described as a feeling of the ground shaking. d, e) PEDS was felt within one week of the earthquake and lasted up to several weeks. f) PEDS was more commonly experienced in indoor settings. Abbreviation: PEDS, post-earthquake dizziness syndrome.
Results of the multivariate logistic regression analysis of PEDS onset.
| Explanatory variables | OR | 95% CI | |
|---|---|---|---|
| 0.16 | 0.11–0.23 | ||
| 3.00 | 2.41–3.73 | ||
| 1.71 | 1.45–2.01 | ||
| 1.07 | 0.97–1.18 | ||
| 0.97 | 0.81–1.16 | ||
| 1.35 | 1.08–1.67 | ||
| 1.43 | 1.25–1.64 | ||
| 3.05 | 2.56–3.64 | ||
| 1.10 | 1.00–1.21 | ||
| 1.22 | 1.10–1.36 |
*P < .05
**P < .01
***P < .001.
Abbreviations: OR, odds ratio; CI: Confidence interval.
Fig 3Relationship between aftershock number and the likelihood of PEDS.
There was a null correlation between geological conditions/number of aftershocks and prevalence of PEDS (R (3) = - 0.06, P = .28). Abbreviation: PEDS, post-earthquake dizziness syndrome.
Number of aftershocks and PEDS ratio per region.
| Kumamoto Region | PEDS+:PEDS- | Max Shindo | Number of aftershocks |
|---|---|---|---|
| Central | 595:1,031 | 7 | 467 |
| Northern | 103:83 | 7 | 340 |
| Southern | 92:66 | 7 | 461 |
| Western | 89:92 | 7 | 777 |
| Eastern | 551:820 | 7 | 441 |
PEDS, post-earthquake dizziness syndrome.