English  |  正體中文  |  简体中文  |  Items with full text/Total items : 26988/38789
Visitors : 2359033      Online Users : 51
RC Version 4.0 © Powered By DSPACE, MIT. Enhanced by NTU Library IR team.
Scope Adv. Search

Please use this identifier to cite or link to this item: http://ntour.ntou.edu.tw:8080/ir/handle/987654321/44310

Title: The Sea Surface Temperature Variation during the Spring Tide and Neap Tide in the South China Sea
Authors: Huang, Shih-Jen;Kuo, Nan-Jung;Ho, Chung-Ru;Lo, Yao-Tsai
Contributors: 國立臺灣海洋大學:海洋環境資訊系
Date: 2016-04
Issue Date: 2017-11-21T08:09:31Z
Publisher: EGU General Assembly 2016, held 17-22 April, 2016 in Vienna Austria, id. EPSC2016-13229
Abstract: Abstract:The sea surface temperature (SST) data of MODIS/Terra (Moderate-resolution Imaging Spectroradiometer) are used to analyze the SST difference between the spring tide and the neap tide in the South China Sea (SCS) from 2001 to 2013. The 4 stations from north to south in the SCS are used to investigate the variation of SST. The results show the lowest SST found on January and the highest SST found on June. The standard deviation of SST in shallow regions (St. 1 and St. 4) are larger than the deep regions (St. 2 and St. 3). During the winter and spring the standard deviation of SST at the neap tide are greater than the spring tide period. From the later winter to early summer, the SST during the neap tide period is greater than the spring tide period. They are more obvious in the shallow regions. Meanwhile the influence of tide action in the shallow regions is greater than it in the deep regions.
URI: http://ntour.ntou.edu.tw:8080/ir/handle/987654321/44310
Appears in Collections:[海洋環境資訊系] 演講及研討會

Files in This Item:

There are no files associated with this item.

All items in NTOUR are protected by copyright, with all rights reserved.


著作權政策宣告: 本網站之內容為國立臺灣海洋大學所收錄之機構典藏,無償提供學術研究與公眾教育等公益性使用,請合理使用本網站之內容,以尊重著作權人之權益。
網站維護: 海大圖資處 圖書系統組
DSpace Software Copyright © 2002-2004  MIT &  Hewlett-Packard  /   Enhanced by   NTU Library IR team Copyright ©   - Feedback