NH038-0009
Impacts of Atmospheric Pressure on the Annual Maximum of Monthly Sea Levels in the Northeast Asian Marginal Seas

Wednesday, 16 December 2020
Poster
MyeongHee Max Han, Seoul National University, Research Institute of Oceanography/School of Earth and Environmental Sciences, Seoul, Korea, Republic of (South), Yang-Ki Cho, School of Earth and Environmental Sciences/Research Institute of Oceanography, Seoul National University, 1 Gwanak-ro, Gwanak-gu, Seoul, South Korea, Hyoun-Woo Kang, KIOST, Ocean Circulation and Climate Research, Ansan, South Korea, SungHyun Nam, Seoul National University, Research Institute of Oceanography, Seoul, Korea, Republic of (South); Seoul National University, School of Earth and Environmental Sciences, Seoul, Korea, Republic of (South), Do-Seong Byun, Korean Hydrographic and Oceanographic Agency, Busan, South Korea, Kwang Young Jeong, Korea Hydrographic and Oceaographic Agency, Research Div., Busan, South Korea and Eunil Lee, Korea Hydrographic and Oceanographic Agency, Busan, South Korea
Abstract:
Monthly mean sea levels have annual maxima in August in the northeast Asian marginal seas (NEAMS). Based on satellite altimetry data, the rising rate of the August NEAMS sea level (ANS, 4.2 mm yr-1) is greater than those of the NEAMS (3.6 mm yr-1) and global (3.4 mm yr-1) annual mean sea levels. Thus, the interannual variations of ANS are classified as relatively high (period H) and low (period L) years and have been analyzed because of the high risk of sea-level fluctuation to the coastal regions in August. In period H, there are large atmospheric pressure gradients between the high pressure zone in the Kuroshio Extension (KE) and the low pressure zone in the west of Taiwan (WT). In period L, the atmospheric pressure gradients are small between the above-mentioned zones. Large atmospheric pressure gradients induce strong west-northwestward wind stresses and more Ekman transport from the northwest Pacific Ocean into the NEAMS. The correlation coefficient between August NEAMS sea level index (ANSI), which is the difference of atmospheric pressure anomalies between the KE and the WT, and the August NEAMS sea level anomaly (ANSA) is 0.73. Although there is a significant correlation (coefficient: 0.64) between ANSA and the East Asian Summer Monsoon Index, ANSI might be more useful in estimating the variability of ANSA.