原名「台灣學術線上」
包含TAO期刊庫 + TAO書籍庫 + 論文 + 史料文獻
首頁 | 關於TAO | 瀏覽 | 進階查詢 | 參考工具 | 會員服務 | 已購專書 | RSS服務 | 電子報 | FAQ  
查詢範圍:
   
查詢模式:
熱門查詢詞:
老人需求dvdTaiwan vet雞濾泡顆粒細胞
   
   
   
     
   
 
項次 書目
1
題名:STUDY OF THE KUROSHIO CURRENT BETWEEN TAIWAN AND ISHIGAKIJIMA    
臺灣與石垣島間黑潮之研究
著者:Tsu-You Chu(朱祖佑)
出版地區:台灣
出版城市:台北市
學科:地球科學
刊名:Science Reports of the National Taiwan University ACTA Oceanographica Taiwanica
卷期:6期(1976.12)
頁碼:1-24
語言:英語
摘要: 中文摘要PDF ; 英文摘要PDF

本研究之目的有二:1.研究臺灣東面黑潮流量之變化。2.研究黑潮流量與臺灣東岸及石垣島之間海面差之關係,以便利用潮汐資料,推算黑潮流量。 自1974年至1975年,九連號研究船曾實施六個航次,從事水文測量,計算黑潮流量。其結果顯示,每一航次之總流量均不相同。自1974年7月之18×106立方米/秒,增加至1975年9月之42.12×106立方米/秒。逐年變化較大,而季節變化不明顯。 基隆與石垣島1974年及1975年之潮汐資料,經低頻率過濾處理,以兩地之海面差,與黑潮流量相比較。其結果顯示石垣島之平均海平面,均較基陸為高。此與地衡流之原理相符合。北半球海流之流向,指向海面傾斜方向之右側。 六個航次之平均流量為29.3×106立方米/秒。基隆與石垣島二地之平均海面差為93.8毫米。接近臺灣之側站A與接近石垣島之測站0之間,平均動力高度之差為64.4毫米。設吾人假定此值相當於石垣島實際上因黑潮總流量而上昇之高度,則在二地海面差之中,減去此值,則其差值32.4毫米,可認為係二地驗潮儀基準面之差。其中亦可能含有在平均海面差之中未能消除之氣象影響。 因二地驗潮儀基準面之差,應為常數。假定氣象之影響亦為常數,則吾人可在實際上所測基隆與石垣島二地之海面差,減去此值,即可計算臺灣沿海與石垣島間黑潮之流量。 在另一方面,發現在六個航次中,黑潮總流量與A,O兩測站間動力高度差之比,非常接近。其平均比值0.47立方米/秒/毫米,吾人對於此比值如認為適當,則將來僅需在A,O兩測站,同時實施水文測量。以水文資料,即可計算黑潮之流量。
The purpose of the present study is twofold: 1. To study the fluctuations of the Kuroshio Current especially the transport of the current in the sea east of Taiwan. 2. The relation between the geostrophical transport of the current and the difference of mean sea level between Ishigakijima and the coast of Taiwan to asses the general utility of tide gauge data for monitoring the Kuroshio transport. Six cruises were carried out during the year 1974 and 1975 by the R/V CHIU LIEN for hydro-graphic and geostrophic transport of the Kuroshio has been calculated. The results show that the total transport varies from cruise to cruise. It was increasing from 18.69×106M3/sec in July, 1974 to 42.12×106M3/sec in September, 1975. The yearly variation is quite large while the seasonal variation is not clear. Tidal gauge data of Keelung and Ishigakijlma of the year 1974 and 1975 have been processed with the low pass filter CL 121 and their difference are used for comparison with geostrophic transport between Ishigakijima and the coast of Taiwan. The results show that the mean sea levels of Ishigakijima are all higher than that of Keelung. This is quite in accordance with the theory that geostrophic currents are flowing to the right hand side of the slope of sea surface in the northern hemisphere. The average transport of the six curises is 29.3×106M3/sec and the difference of mean sea levels of the two places is 93.8 cm. The mean total difference of dynamic height between the two end stations A and O of six cruises is 61.4 cm (dynamic). If we consider this value as the actual rise in cm of the mean sea level at Ishigakijima due to the total transport of Kuroshio we can subtract this value from the difference of mean sea level and the balance 32.4 cm may be considered as the difference of datumn plane of tide gauge at the two places. This value may also include some meteorological effects upon sea level not eliminated in average. Since the difference of datumn plane must be a constant and if we assume that the meteorological effects not eliminated in average are also constants, then we can subtract this value from the actual measurements of difference of mean sea level of the two places and calculate the total transport of the Kuroshio between Ishigakijima and the coast of Taiwan. On the other hand, we have found that the ratios of geostrophic transport to the difference of dynamic height between the two end stations A and O of six cruises are very close. If we consider the mean ratio of the six cruises 0.47×106M3/sec/cm as a reasonable value, we need only to carry out hydrographic measurements at stations A and O at the same time and calculate the total transport from the hydrographic data.




本卷期目次
Science Reports of the National Taiwan University ACTA Oceanographica Taiwanica 6期 (1976.12)
STUDY OF THE KUROSHIO CURRENT BETWEEN TAIWAN AND ISHIGAKIJIMA/ Tsu-You Chu
ELECTROPHORETIC STUDY OF THE MUSCLE EXTRACTS OF BULLET TUNA (AUXIS ROCHEI) IN WATERS AROUND TAIWAN/ Su-Zan YehRong-Tszong Yang
THE DEMERSAL FISH STOCKS OF THE WATERS OF NORTH AND NORTHWEST AUSTRALIA/ Hsi-Chiang Liu
STUDIES ON ALGIN FROM BROWN ALGAE OF TAIWAN I. ESTIMATION OF YIELD AND QUALITY OF ALGIN/ Hong-Nong ChouYoung-Meng Chiang
ECOLOGICAL AND MORPHOLOGICAL STUDY OF THE FISH-FAUNA FROM THE WATERS AROUND TAIWAN AND ITS ADJACENT ISLANDS 17. A study of sex reversal in a pomacanthid fish, Genicanthus semifasciatus (KAMOHARA)/ Shih-Chieh ShenChen-Hsiang Liu
ECOLOGICAL AND MORPHOLOGICAL STUDY OF THE FISH-FAUNA FROM THE WATERS AROUND TAIWAN AND ITS ADJACENT ISLANDS 20. Study on the goatfishes-Mullidae/ Shih-Chieh Shen
魚類族群仔稚時期餌料的消費和加入量之間的關係/ 王健雄
STRONTIUM DISTRIBUTION IN COASTAL RANGE ANDESITES, EASTERN TAIWAN/ Lu-Chin ChenTung-Wuu Huang
A NOTE ON THE SIGNIFICANT WAVE DERIVED FROM JONSWAP SPECTRUM/ Joe WangNai-Kuang Liang
COMMENT ON M. C. LIN'S PAPER ON INTERNAL WAVES IN A STRATIFIED INCOMPRESSIBLE FLUID
PROCESSES MODIFYING THE ISOTOPIC COMPOSITION OF DISSOLVED OXYGEN/ Woei-Lih Jeng
STUDY ON MERCURY IN THE WATERS, SEDIMENTS AND BENTHONIC ORGANISMS ALONG CHAI-I COASTAL AREA/ Tsu-Chang HungTsung-Tien Lin
TIDAL CURRENTS IN THE OFFSHORE AREA OF SU-AOU IN RELATION TO TIDES OF THE LAND STATION ALONG THE EAST COST OF TAIWAN/ K. ChengT. Y. Chu
ON THE STEADY STATE CURRENTS IN SHALLOW SEAS OR LAKES/ San-Lang Lien
DISTRIBUTION OF Na, Mg, Ca, K, Sr AND Li IN SEA WATERS FROM THE BASHI CHANNEL/ Hsien-Wen LiJu-Chin Chen
GEOCHEMISTRY OF LANHSU ANDESITES/ Ju-Chin Chen
NUMERICAL SIMULATION OF TURBULENT DISPERSION OF FINITE SIZE PARTICLES/ Wei-Chung Chen
ON UPWELLING ALONG THE EASTERN COAST OF TAIWAN: A REVIEW OF HYDROGRAPHIC AND CHEMICAL DATA/ Gudrun M. Bodvarsson
 
   
 
   

與TAO合作 | 隱私與版權聲明 | 聯絡方式 | 下載Adobe Reader
地址:台北市中正區(100)北平東路30-12號3樓
電話:(02)2393-6968 傳真:(02)2393-6877
Email: service@wordpedia.com
Wordpedia Family: 學校、企業版入口 | 遠流影音館
Copyright©2011 Wordpedia Co., Ltd. All Rights Reserved.