TY - JOUR
T1 - Hurricanes Irma and Maria post-event survey in US Virgin Islands
AU - Cox, Daniel
AU - Arikawa, Taro
AU - Barbosa, Andre R.
AU - Guannel, Greg
AU - Inazu, Daisuke
AU - Kennedy, Andrew
AU - Li, Yue
AU - Mori, Nobuhito
AU - Perry, Kwasi
AU - Prevatt, David
AU - Roueche, David
AU - Shimozono, Takenori
AU - Simpson, Chase
AU - Shimakawa, Eisuke
AU - Shimura, Tomoya
AU - Slocum, Richard
PY - 2019/4/3
Y1 - 2019/4/3
N2 - Hurricanes Irma and Maria caused catastrophic damages across the Caribbean Islands during the 2017 hurricane season. After the storms, a joint United States–Japanese team investigated coastal impacts in the US Virgin Islands, which are composed of the islands of St. Thomas, St. John, Water Island, and St. Croix. Coastal inundation was dominated by wave run-up in almost all locations, with many locations showing inundation exceeding 4-m elevation from mean sea level. In contrast, maximum elevations recorded at tide gauges did not exceed 1 m at any location. Coastal damage was relatively minor for such strong hurricanes because of the lack of heavy development at low elevations on the most exposed coastlines. Many moored vessels were destroyed, and coastal structures and infrastructure within the inundation region suffered significant damage. However, few large structures experienced catastrophic losses from coastal inundation. In contrast, strong winds caused extensive structural damage throughout the US Territory. Evidence was seen for past inundation of the coastline, but could not be conclusively linked to any particular events.
AB - Hurricanes Irma and Maria caused catastrophic damages across the Caribbean Islands during the 2017 hurricane season. After the storms, a joint United States–Japanese team investigated coastal impacts in the US Virgin Islands, which are composed of the islands of St. Thomas, St. John, Water Island, and St. Croix. Coastal inundation was dominated by wave run-up in almost all locations, with many locations showing inundation exceeding 4-m elevation from mean sea level. In contrast, maximum elevations recorded at tide gauges did not exceed 1 m at any location. Coastal damage was relatively minor for such strong hurricanes because of the lack of heavy development at low elevations on the most exposed coastlines. Many moored vessels were destroyed, and coastal structures and infrastructure within the inundation region suffered significant damage. However, few large structures experienced catastrophic losses from coastal inundation. In contrast, strong winds caused extensive structural damage throughout the US Territory. Evidence was seen for past inundation of the coastline, but could not be conclusively linked to any particular events.
U2 - 10.1080/21664250.2018.1558920
DO - 10.1080/21664250.2018.1558920
M3 - Article (Academic Journal)
SN - 0578-5634
VL - 61
SP - 121
EP - 134
JO - Coastal Engineering Journal
JF - Coastal Engineering Journal
IS - 2
ER -