Influence of warm surface water originating from the East China Sea on surface water temperature off the south coast of Korea in summer

IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY
Jong-Kyu Kim , Byoung-Ju Choi
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引用次数: 0

Abstract

Surface seawater temperature in the southwestern coast of Korea suddenly rose in the summer of 2017. This rapid temperature rise event occurred simultaneously with a change in wind direction in the Korea Strait from northwesterly to southeasterly due to the approach of typhoon Noru. To identify the causes of the abrupt rise in surface temperature, the variations of the surface currents and temperature were investigated using a three-dimensional ocean circulation model. Warm and less saline surface water, a mixed shelf water of the Changjiang Diluted Water and saline water from an onshore branch of the Kuroshio in the East China Sea (ECS), flowed northeastward to the west and south of Jeju Island, proceeding eastward through the Jeju and Korea Straits. While westerly winds prevailed, wind-driven ageostrophic currents flowed southeastward, moving away from the south coast of Korea, due to Ekman transport. The shallow coastal region was occupied by cool and saline surface water (T < 22 °C, S > 32.5 psu). However, after the wind shifted to an easterly direction, the surface ageostrophic currents realigned northwestward, and the warm and less saline water moved into the shallow coastal region. In a passive tracer dispersal experiment, dyes injected from the ECS flowed to the west of Jeju Island and through the Jeju Strait via geostrophic currents. These dyes did not affect the shallow southern coastal region of Korea while the westerly winds dominated. However, during the easterly wind event, the dyes were advected toward the coast by the coastward Ekman transport. An analysis of temperature data observed at Cheongsando over 16 years and the tracer experiment revealed that the abrupt temperature rise in the summer of 2017 was a marine heatwave event generated by the advection of warm and less saline surface water from the ECS to the southwestern coast of Korea through the Jeju Strait.

源自东海的温暖表层水对夏季韩国南海岸表层水温的影响
2017 年夏季,韩国西南海岸的表层海水温度突然上升。在温度迅速上升的同时,由于台风 "诺鲁 "的逼近,朝鲜海峡的风向也从西北风转为东南风。为了查明表层温度突然上升的原因,使用三维海洋环流模型对表层洋流和温度的变化进行了研究。温暖且盐度较低的表层水,即长江稀释水的陆架水和来自东海(ECS)黑潮陆上支流的盐水的混合水,向东北方向流向济州岛西部和南部,向东穿过济州海峡和韩国海峡。在盛行西风的同时,由于埃克曼输送作用,由风驱动的老练流向东南流动,远离韩国南海岸。沿岸浅水区的表层海水(T < 22 °C,S > 32.5 psu)温度较低,含盐量较高。然而,风向转为东风后,表层老熟流重新向西北方向移动,暖水和盐度较低的海水进入浅海沿岸地区。在被动示踪剂扩散实验中,从 ECS 注入的染料通过地转流流向济州岛西部,流经济州海峡。在西风占主导地位时,这些染料没有影响到韩国南部沿海浅水区。然而,在东风事件期间,这些染料被沿岸的埃克曼输送带吹向海岸。对 16 年来在青山岛观测到的温度数据和示踪实验的分析表明,2017 年夏季温度的突然升高是由温暖且盐度较低的表层水从东中部海域通过济州海峡向韩国西南海岸的平流所产生的海洋热浪事件。
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来源期刊
Continental Shelf Research
Continental Shelf Research 地学-海洋学
CiteScore
4.30
自引率
4.30%
发文量
136
审稿时长
6.1 months
期刊介绍: Continental Shelf Research publishes articles dealing with the biological, chemical, geological and physical oceanography of the shallow marine environment, from coastal and estuarine waters out to the shelf break. The continental shelf is a critical environment within the land-ocean continuum, and many processes, functions and problems in the continental shelf are driven by terrestrial inputs transported through the rivers and estuaries to the coastal and continental shelf areas. Manuscripts that deal with these topics must make a clear link to the continental shelf. Examples of research areas include: Physical sedimentology and geomorphology Geochemistry of the coastal ocean (inorganic and organic) Marine environment and anthropogenic effects Interaction of physical dynamics with natural and manmade shoreline features Benthic, phytoplankton and zooplankton ecology Coastal water and sediment quality, and ecosystem health Benthic-pelagic coupling (physical and biogeochemical) Interactions between physical dynamics (waves, currents, mixing, etc.) and biogeochemical cycles Estuarine, coastal and shelf sea modelling and process studies.
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