Upper Ocean Thermal Structure in the Western North Pacificfrom Satellite Altimetry / 利用衛星測高觀測西北太平洋的上層海洋溫度結構

博士 / 國立臺灣大學 / 大氣科學研究所 / 100 / This thesis firstly demonstrates the importance of satellite-derived upper ocean thermal structure (UOTS) in typhoon research. Using a simple two-layer model, UOTS can be roughly derived from satellite altimetry and the intensity change of the Supertyphoon Dianmu (2004) is investigated. It is found that Dianmu’s intensity is very sensitive to the during typhoon SST cooling and upper ocean heat content (UOHC). During 2010, UOTS was estimated on a daily basis from satellites for the use in the large international field experiment, Impact of Typhoons on the Ocean in the Pacific (ITOP), showing the advantage of satellite-derived UOTS in typhoon-ocean research.
Secondly, using >38,000 Argo temperature profiles, a linear regression method for the western North Pacific (i.e., REGWNP) is developed. Then, >7,000 in situ profiles are used to assess accuracy of REGWNP-derived UOTS. The results show that REGWNP is able to produce rather reliable UOTS. During the typhoon season, the rms difference for the depth of 20°C isotherm (D20), depth of 26°C isotherm (D26), UOHC and averaged temperature of the upper 100 m (T100) is less than 30 m, 20 m, 20 kJ cm-2, and 1.5°C, respectively. Also, it is found that REGWNP outperforms the traditional two-layer approach and is comparable to a sophisticated full ocean model for producing real-time UOTS field.
Finally, based on the sea surface height anomaly (SSHA) record between 1993 and 2010, the long-term changes in ocean conditions in the western North Pacific main typhoon intensification region are investigated. It is found that the activity of warm eddies enhanced while cold eddies weakened. In terms of subsurface variability, D20, D26 and UOHC increased by 9-17%, meanwhile, T100 warmed by 0.16-0.35°C over the 18 years period. Furthermore, it is also found that the total area of positive SSHA (≧ 10 cm) features substantially increased while negative SSHA (≦ -10 cm) features deceased. These results suggest that the western North Pacific ocean conditions are becoming more favorable to typhoon intensification.

Identiferoai:union.ndltd.org:TW/100NTU05022038
Date January 2012
CreatorsIam-Fei Pun, 潘任飛
Contributors林依依
Source SetsNational Digital Library of Theses and Dissertations in Taiwan
Languageen_US
Detected LanguageEnglish
Type學位論文 ; thesis
Format173

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