scholarly journals Contribution of the Yellow Sea bottom cold water to the abnormal cooling of sea surface temperature in the summer of 2011

2016 ◽  
Vol 121 (6) ◽  
pp. 3777-3789 ◽  
Author(s):  
Joon-ho Lee ◽  
Ig-Chan Pang ◽  
Jae-Hong Moon
Keyword(s):  
Surface Temperature ◽  
Sea Surface Temperature ◽  
Yellow Sea ◽  
Cold Water ◽  
Sea Surface ◽  
The Yellow Sea ◽  
Sea Bottom ◽  
Bottom Cold Water

scholarly journals Seasonal migration of the Yellow Sea Bottom Cold Water

2014 ◽  
Vol 119 (7) ◽  
pp. 4430-4443 ◽  
Author(s):  
Bin Wang ◽  
Naoki Hirose ◽  
Boonsoon Kang ◽  
Katsumi Takayama
Keyword(s):  
Yellow Sea ◽  
Cold Water ◽  
Seasonal Migration ◽  
The Yellow Sea ◽  
Sea Bottom ◽  
Bottom Cold Water

scholarly journals Influence of Sea Surface Temperature on a Mesoscale Convective System producing Extreme Rainfall over the Yellow Sea

2021 ◽  
Author(s):  
Yunhee Kang ◽  
Jong-Hoon Jeong ◽  
Dong-In Lee
Keyword(s):  
Surface Temperature ◽  
Sea Surface Temperature ◽  
Yellow Sea ◽  
Extreme Rainfall ◽  
Sea Surface ◽  
The Yellow Sea ◽  
Convective System ◽  
Mesoscale Convective ◽  
Upper Level ◽  
Convective Cells

AbstractAn extreme rainfall-producing linear mesoscale convective systems (MCSs) occurred over the Yellow Sea, Korea, on 13 August 2012, producing 430 mm of rainfall in less than 12 h, causing devastating flash floods and landslides. To understand the causative processes underlying this event, we examined the linear MCSs formation and development mechanisms using observations and cloud-resolving models. The organized linear MCSs produced extreme rainfall at Gunsan in a favorable large-scale environment. The synoptic environment showed the stationary surface front elongating from China to Korea; a southwesterly low-level jet transported the warm, moist air from low latitudes towards the front. In the upper-level synoptic environment, the trough and entrance regions of the upper-level jet were north of the heavy rainfall, promoting the development of convection. The extreme rainfall over the Gunsan area resulted from the back-building mode of the MCSs, in which new convective cells continued to pass over the same area while the entire convective system was nearly stationary. The sea surface temperature (SST) during the extreme rainfall events was abnormally 1°C higher than the 30-year climatological mean, and a local warm pool (>28.5°C) existed where the convective cells were continuously initiated. Cloud-resolving models simulated the low-level convergence, and the latent heat flux was large in the local warm SST field. These induced MCSs formation and development, contributing to a significant rainfall increase over the Yellow Sea. The terrain’s influence on the large rainfall amount in the area was also noted.

High resolution unsaturated alkenones sea surface temperature records in the Yellow Sea during the period of 3500–1300 cal. yr BP

2017 ◽  
Vol 441 ◽  
pp. 107-116 ◽  
Author(s):  
Qingyun Nan ◽  
Tiegang Li ◽  
Jinxia Chen ◽  
Xuefa Shi ◽  
Xinke Yu ◽  
...  
Keyword(s):  
High Resolution ◽  
Surface Temperature ◽  
Sea Surface Temperature ◽  
Yellow Sea ◽  
Sea Surface ◽  
The Yellow Sea ◽  
Temperature Records
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