Responses of coastal waters in the Yellow Sea to Typhoon Bolaven

Effect of Sea Surface Temperature Gradient Induced by the Previous Typhoon's Cold Wake on the Track of the Following Typhoon: Bolaven (1215) and Tembin (1214)

“…선행 태풍에 의한 해수 냉각이 후속 태풍에 미 치는 영향과 관련된 사례연구를 살펴보면 선행 태풍 에위니아가 지나간 후 발생한 해수 냉각 효과로 인 하여 후행 태풍인 빌리스(0604)의 발달을 저해하였 다는 연구 결과가 있었다 (Jeong et al, 2013). 다른 선행연구 결과로는 볼라벤에 영향을 받은 황해 연안 의 반응으로 전라남도 앞바다가 10 o C 가까이 감소되 는 특징이 있었고, 급속하게 냉각된 해수면에 의해 덴빈의 강도가 약해지는 특징이 있었다 (Kim et al, 2014). 하지만 Kim et al (2014) (Lee et al, 2014).…”

Simulation of the extreme waves generated by typhoon Bolaven (1215) in the East China Sea and Yellow Sea

“…Measured H max (Hs) at buoys of KOGA-S1, KOGA-S4 and IORS were 20.7 m (12.3 m), 17.2 m (11.2 m) and 17.3 m (11.1 m) respectively. They are very unusual and record-breaking extreme waves although Bolaven was not the strongest recorded typhoon in the ECS (Kim et al, 2014). The extreme waves generated by this typhoon whose heights were larger than 10 m varied in a small range and continued for more than 6 hours.…”

“…1. It generated record-breaking extreme waves (H max = 20.7 m at KOGA-S1 and 17.3 m at Ocean Tower (OT) stations; http://www.khoa.go.kr/) in the deep-water of the ECS (Kim et al, 2014) , and 11.8 m waves (H s ) at Kang Jung in shallow water (KHOA, 2012;Jeong et al, 2012) (Fig. 2).…”

Effect of Typhoon-Generated Cold Wake on the Subsequent Typhoon Tembin and Its Sensitivity to Horizontal Resolutions

“…This cold wake effect impacts the direction and intensity of other typhoons [28,[34][35][36][37][38]. Jeong et al [34] also considered how the typhoon-induced cold wake of Typhoon Ewiniar (0603; the third typhoon of 2006) inhibited the development of Typhoon Billis (0604; the fourth typhoon of 2006).Typhoon Bolaven (1215) resulted in a decrease of about 10 • C along the coast of Jeollanam-do in the Yellow Sea, and the intensity of Typhoon Tembin (1214) was weakened by the rapidly cooled sea surface [35]. However, Kim et al [35] only noted the weakened intensity of Tembin in response to the cooling from Bolaven without investigating the processes that led to this weakening.…”

“…Jeong et al [34] also considered how the typhoon-induced cold wake of Typhoon Ewiniar (0603; the third typhoon of 2006) inhibited the development of Typhoon Billis (0604; the fourth typhoon of 2006).Typhoon Bolaven (1215) resulted in a decrease of about 10 • C along the coast of Jeollanam-do in the Yellow Sea, and the intensity of Typhoon Tembin (1214) was weakened by the rapidly cooled sea surface [35]. However, Kim et al [35] only noted the weakened intensity of Tembin in response to the cooling from Bolaven without investigating the processes that led to this weakening. Moon et al [37] and Heo et al [38] also studied the change in the track of the following and weakening of Tembin via the cold wake using Bolaven and Tembin and focusing on 10 m wind and changes in the waves caused by a typhoon.…”