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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 曾于恒(Yu-Heng Tseng) | |
| dc.contributor.author | Kuan-Ting Lin | en |
| dc.contributor.author | 林冠廷 | zh_TW |
| dc.date.accessioned | 2022-11-23T08:57:02Z | - |
| dc.date.available | 2022-01-17 | |
| dc.date.available | 2022-11-23T08:57:02Z | - |
| dc.date.copyright | 2022-01-17 | |
| dc.date.issued | 2021 | |
| dc.date.submitted | 2022-01-04 | |
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/79268 | - |
| dc.description.abstract | 蜂蜜在台灣扮演非常重要的環境、生態與經濟角色，然而近十年蜂蜜產量卻逐漸下降，並在2019年來到最低點，本研究探討蜂蜜年產量與周遭環境因子(如溫度、降雨、日照週期)和大尺度海洋與大氣變異的關係，冀望能減少氣候變遷下環境變異對蜂農及消費者的衝擊。過去大多相關的研究聚焦在採收季節環境因子與蜜蜂飛行狀態之間的關係，然而我們的分析發現蜂蜜年產量都與台灣冬季所有地區的月平均氣溫有顯著的相關性，而其他因子皆無顯著的關聯。本研究推測可能原因為台灣最主要的蜜源植物如龍眼在冬季的花芽分化對於環境溫度相當敏感，溫度太高會限制花芽的分化數量，影響到兩個月後蜜源植物花期的泌蜜量，連帶造成了蜂蜜年產量的波動。本研究進而探討1982-2019年冬季海洋與大氣變異對於冬季氣溫年際震盪的影響，特別是台灣冬季氣溫變化到底是由海洋或大氣主導?了解變化機制主導的過程便能夠增加蜂蜜產量的可預報性，我們發現在台灣冬季時，北太平洋上大尺度大氣氣壓與環流的影響對台灣氣溫影響非常直接，特別是北太平洋上海面氣壓距平第二模態(North Pacific Oscillation)的空間分布特徵可能是影響台灣地區氣溫與海溫的重要變異，並連帶波動台灣上空的氣壓以及東亞沿岸背景風場，進而影響台灣冬季氣溫與蜜源植物花芽分化的狀態，並間接主導著蜂蜜年產量，而海洋中的重要變異如黑潮海溫鋒面以及海溫距平對氣溫的影響較不顯著，最後利用區域海氣耦合模式驗證大氣與海洋分別的影響，在三十天的海氣耦合模式中也顯示出冬季時大氣對氣溫的影響較直接。 | zh_TW |
| dc.description.provenance | Made available in DSpace on 2022-11-23T08:57:02Z (GMT). No. of bitstreams: 1 U0001-2912202117332200.pdf: 4976314 bytes, checksum: bb590a7329f0ebbf61640a3bab98e457 (MD5) Previous issue date: 2021 | en |
| dc.description.tableofcontents | 致謝 I 中文摘要 II Abstract III 目錄 V 圖片目錄 VII 表格目錄 X 第一章：前言 1 1-1 台灣養殖蜜蜂簡介 1 1-2 大環境因子與台灣冬季溫度變化 3 1-3 蜂蜜產量與冬季溫度研究議題 7 第二章：資料與方法 9 2-1 台灣養殖蜂蜜產量資料 9 2-2 環境資料 9 2-3 台灣冬季溫度(TWSAT) 10 2-4 氣候指標定義 11 a. 西太平洋遙相關模態指數(WP pattern index; WP) 11 b. 北太平洋震盪(North Pacific Oscillation; NPO) 11 c. 黑潮海溫鋒面指數SST front index 11 2-3 研究方法 12 2-4 區域耦合模式 13 第三章：單位蜂箱產量與環境因子分析結果 18 3-1 影響單位蜂箱產量的環境因子 18 3-2 一月溫度與單位蜂箱產量 19 第四章：台灣一月溫度與環境變異分析結果 26 4-1 台灣冬季溫度與環境變異的相關性 26 4-2 台灣一月溫度與海溫鋒面(SST Front) 29 4-3 東亞海溫PC1與環境變異的相關性 30 4-4 遙相關指標與溫度/海溫的領先-滯後相關分析 33 4-5 TWZ500相關的表層環流 35 4-6 分析結果總結 36 第五章：台灣一月溫度與環境變異分析結果 46 5-1 COAWST海氣耦合模式 46 a. 移除海洋反饋組(No ocean case) 46 b. 減弱海溫鋒面實驗組(Smooth front case) 47 5-2 COAWST模式結果 47 5-2.1 移除海洋反饋實驗結果 47 5-2.2 移除海洋鋒面實驗結果 48 第六章：物理機制討論與總結 55 參考資料 60 | |
| dc.language.iso | zh-TW | |
| dc.title | 影響台灣冬季溫度變化的大氣與海洋變異-應用在蜂蜜產量 | zh_TW |
| dc.title | Impacts of Ocean and Atmosphere Variabilities on Winter Temperature in Taiwan-Application in the Honeybee Production | en |
| dc.date.schoolyear | 110-1 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 盧孟明(Hsin-Tsai Liu),許晃雄(Chih-Yang Tseng),許哲源 | |
| dc.subject.keyword | 蜂蜜產量,冬季溫度,北太平洋震盪,東北季風,黑潮海溫鋒面,COAWST海氣耦合模式, | zh_TW |
| dc.subject.keyword | Taiwan Honeybee Production,Winter Temperature,North Pacific Oscillation,Sea Surface Temperature Front,COAWST coupled model, | en |
| dc.relation.page | 64 | |
| dc.identifier.doi | 10.6342/NTU202104596 | |
| dc.rights.note | 同意授權(全球公開) | |
| dc.date.accepted | 2022-01-04 | |
| 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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