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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 林卉婷(Huei-Ting Lin) | |
| dc.contributor.author | Chao-Yuan Yang | en |
| dc.contributor.author | 楊朝源 | zh_TW |
| dc.date.accessioned | 2021-05-20T00:49:09Z | - |
| dc.date.available | 2020-09-02 | |
| dc.date.available | 2021-05-20T00:49:09Z | - |
| dc.date.copyright | 2020-09-02 | |
| dc.date.issued | 2020 | |
| dc.date.submitted | 2020-08-20 | |
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/8134 | - |
| dc.description.abstract | 聖嬰/南方震盪是全球海洋與大氣最顯著的變動模式之一，現代觀測結果指示發生在低緯度赤道太平洋的聖嬰/南方震盪與阿留申低壓之間具有遠距離的海洋與大氣遙相關，然而這樣的現象是否在千年的時間尺度之下亦有發生，目前尚未有確切的觀察數據。北海道地區的降雨受控於阿留申低壓影響，因而本研究採集了北海道地區洞穴(43°14’12” N, 142°13’09” E)中生長於十一萬兩千年至七萬兩千年之間的石筍，並利用其碳同位素與微量元素鎂、鍶和鋇之組成，重建了當時的降雨紀錄。結果顯示在千年尺度下，北海道降雨與東、西部赤道太平洋之間的海水溫度異常有共同變化的趨勢，代表在過去本時間段之中，阿留申低壓狀態的改變與太平洋赤道地區的海水溫度變化有遙相關性，彰顯低緯度與中緯度地區海洋與大氣環境遠距離連結的重要性。 | zh_TW |
| dc.description.abstract | El Niño–Southern Oscillation (ENSO) is one of most important global climate modes. In modern day, an ENSO-Aleutian Low (AL) teleconnection was suggested. Whether similar teleconnection had occurred over a multi-millennial scale is not yet available. Here, we present stalagmite-inferred hydroclimate records covering the interval of 112 - 72 ka (kiloanni, age before 1950 C.E.) from Oku-Ashibetsu cave in Hokkaido (43°14’12” N, 142°13’09” E), northern Japan, where the rainfall pattern is influenced by the AL. Records of the stalagmite δ13C, a proxy reflecting changes in temperature and precipitation, covary with the trace elements (Mg, Sr and Ba), proxies for hydrological variation. During 112 - 72 ka, millennial scale covariation was found between the proxies-inferred Hokkaido regional precipitation and the Pacific long-term ENSO-like states reconstructed by the marine sediments. Our results suggest that the hydrology in the western Hokkaido region is possibly coupled with Pacific Ocean hydrodynamics via the AL, emphasizing the teleconnection between low and mid latitudes in the past. | en |
| dc.description.provenance | Made available in DSpace on 2021-05-20T00:49:09Z (GMT). No. of bitstreams: 1 U0001-1808202015065700.pdf: 5451944 bytes, checksum: 92fde57da31737978e78f5a85e00e5ee (MD5) Previous issue date: 2020 | en |
| dc.description.tableofcontents | 論文口試委員審定書 I 致謝 II 摘要 III Abstract IV Contents V List of figures VII List of tables VIII Chapter 1- Introduction 1 Chapter 2- Regional settings and methods 7 2.1 Oku-Ashibetsu cave and regional settings 7 2.2 Material and Methods 12 2.2.1 Subsampling and age model 12 2.2.2 Labwares for U-Th dating chemical procedure 14 2.2.3 Uranium and Thorium purification procedures 15 2.2.4 Uranium and –Thorium isotope analysis 16 2.2.5 Age model 17 2.2.6 Stable oxygen and carbon isotope analysis 18 2.2.7 Trace element analysis 19 Chapter 3- Results 20 3.1 U-Th dating results and age model 20 3.2 Trace element records 24 3.3 Oxygen and carbon stable isotope records 26 3.3.1 Hendy test 26 3.3.2 Oxygen and carbon isotope time series 28 Chapter 4- Discussion 30 4.1 Dating point selecting 30 4.2 Interpretation of the trace elements 32 4.2.1 Sr/Ca and Ba/Ca interpretation 32 4.2.2 Mg/Ca interpretation 37 4.3 Interpretation of the stable isotopic signals 40 4.3.1 Kinetic effect 40 4.3.2 Carbon isotopes 42 4.3.3 Oxygen isotope 44 4.4 Hokkaido hydro-climate and Pacific paleotemperature 46 4.4.1 Proxies comparison in the YB15-1 and YB15-2 46 4.4.2 Multi-proxy derived hydroclimate in the northwest Pacific region 51 Chapter 5- Conclusions 56 References 57 Appendix 1 – Hendy test data 67 Appendix 2 – δ18O δ13C records 68 Appendix 3 – Trace element records 91 | |
| dc.language.iso | en | |
| dc.title | 北海道石筍指示之過去十一萬至七萬年中低緯度間海洋與大氣遙相關紀錄 | zh_TW |
| dc.title | Mid-low latitude ocean-atmosphere teleconnection records during 112-72 ka: Stalagmite-inferred hydroclimate in Hokkaido, Japan | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 108-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.advisor-orcid | 林卉婷(0000-0003-3754-6739) | |
| dc.contributor.coadvisor | 沈川洲(Chuan-Chou Shen) | |
| dc.contributor.coadvisor-orcid | 沈川洲(0000-0003-2833-2771) | |
| dc.contributor.oralexamcommittee | 米泓生(Horng-sheng Mii),賀詩琳(Sze-Ling Ho) | |
| dc.contributor.oralexamcommittee-orcid | 米泓生(0000-0002-0702-3307),賀詩琳(0000-0002-4898-9036) | |
| dc.subject.keyword | 石筍,同位素,古氣候,聖嬰現象,遙相關,微量元素,阿留申低壓,鈾釷定年, | zh_TW |
| dc.subject.keyword | stalagmite,isotope,paleo-climate,ENSO,teleconnection,trace element,Aleutian low,U-Th dating, | en |
| dc.relation.page | 96 | |
| dc.identifier.doi | 10.6342/NTU202003978 | |
| dc.rights.note | 同意授權(全球公開) | |
| dc.date.accepted | 2020-08-20 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 海洋研究所 | zh_TW |
| 顯示於系所單位： | 海洋研究所 | |
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