TY - JOUR
T1 - Thermal structure of hot events and their possible role in maintaining the warm isothermal layer in the Western Pacific warm pool
AU - Wirasatriya, Anindya
AU - Kawamura, Hiroshi
AU - Helmi, Muhammad
AU - Sugianto, Denny Nugroho
AU - Shimada, Teruhisa
AU - Hosoda, Kohtaro
AU - Handoyo, Gentur
AU - Putra, Yoppik Disma Girindra
AU - Koch, Magaly
N1 - Funding Information:
First author would like thanks to Diponegoro University for Postdoctoral/Sabbatical Program of World Class University and the research fund under the scheme of International Publication Research 2016-2018 with contract No 1052-24/UN7.5.1/PG/2016; 276/22/UN7.5.1/PG/2017; and 474-78/UN7.P4.3/PP/2018.
Funding Information:
NGSST-O-Global-V2.0a is produced by Center for Atmospheric and Oceanic Studies, Tohoku University, Japan. Contact for data inquiry and request is Dr. Kohtaro Hosoda (khosoda@gmail.com). OAFLUX data can be downloaded at http://oaflux.whoi.edu/data.html. GLOBAL-REANALYSIS-PHY-001-025 is accessible at http://marine.copernicus.eu/. TAO/TRITON buoy data is provided by GTMBA Project Office of NOAA/PMEL and can be accessed at https://www.pmel.noaa.gov/tao/drupal/disdel/. The 3-h real-time TRMM Multi-satellite precipitation analysis data were provided by the NASA/Goddard Space Flight Center and PPS, which develop and compute the 3-h real-time TRMM Multi-satellite precipitation analysis data as a contribution to TRMM, and archived at the NASA GES DISC.
PY - 2020/6/1
Y1 - 2020/6/1
N2 - The short-lived events of high SST are called hot events (HEs) and can only be generated under the conditions of large daily heat gain due to strong solar radiation and weak wind. We investigated the thermal structure below HEs in the western equatorial Pacific by using in situ data obtained from TAO/TRITON buoys. We found that the occurrence of HEs can be identified by the typical vertical thermal structure within the isothermal layer. During the development stage of a HE, heat is accumulated in the surface layer due to strong solar radiation and weak wind, increasing temperature and creating strong stratification in the upper layer. During the decay stage, strong westerly winds induce current convergence which transports the heat from the upper layer to the deeper layer. Thus, temperature decreases at the surface and increases in the deeper layer. Furthermore, this mechanism indicates the important role of HEs in maintaining the warm isothermal layer in the western Pacific warm pool. The more HEs occur, the more heat in the surface layer gained from solar radiation is transported to the deeper layer. This process makes areas of frequent HE occurrences coincident with areas of warm pool. Since surface winds control the heat accumulation and heat transport in the isothermal layer by influencing current divergence and latent heat flux, surface winds become the key factor for the occurrence of HEs and the formation of the thermal structure in the Pacific warm pool.
AB - The short-lived events of high SST are called hot events (HEs) and can only be generated under the conditions of large daily heat gain due to strong solar radiation and weak wind. We investigated the thermal structure below HEs in the western equatorial Pacific by using in situ data obtained from TAO/TRITON buoys. We found that the occurrence of HEs can be identified by the typical vertical thermal structure within the isothermal layer. During the development stage of a HE, heat is accumulated in the surface layer due to strong solar radiation and weak wind, increasing temperature and creating strong stratification in the upper layer. During the decay stage, strong westerly winds induce current convergence which transports the heat from the upper layer to the deeper layer. Thus, temperature decreases at the surface and increases in the deeper layer. Furthermore, this mechanism indicates the important role of HEs in maintaining the warm isothermal layer in the western Pacific warm pool. The more HEs occur, the more heat in the surface layer gained from solar radiation is transported to the deeper layer. This process makes areas of frequent HE occurrences coincident with areas of warm pool. Since surface winds control the heat accumulation and heat transport in the isothermal layer by influencing current divergence and latent heat flux, surface winds become the key factor for the occurrence of HEs and the formation of the thermal structure in the Pacific warm pool.
KW - Short-term high
KW - TAO/TRITON buoys
KW - Thermal stratification
KW - Western Pacific warm pool
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U2 - 10.1007/s10236-020-01362-8
DO - 10.1007/s10236-020-01362-8
M3 - Article
AN - SCOPUS:85083767158
VL - 70
SP - 771
EP - 786
JO - Ocean Dynamics
JF - Ocean Dynamics
SN - 1616-7341
IS - 6
ER -