‘귤화위지’와 중국의 기후변동
‘The Citrus Change the Trifoliate Orange’ and the Climatic Change of China
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The ebb and flow of Northern limit of Citrus cultivation, represented by ‘the Citrus Change the Trifoliate Orange,’ reflects the history of climatic variation in China. Climate has been changing constantly in the last 5,000 years. The change made the Northern limit of Citrus cultivation go up and down repeatedly. Huai-River was lying on the border of the limitation during the Chunchou-Period. In the second century B. C. the temperature was milder than today, even though the line moved to the southern area, Chang-River area. After the Nanbeichao-Period consisted of cold current, the warm climate during the Xiu·Tang-Period let the line of limit go northward until the Huai-River. The climate warming contributed to make Dongting-Mountain into the largest production region of mandarins. The Song-Period was also warm, because ‘Medieval Warm Period’ maintained until this period. The twelfth century was very cold, in particular, so that the arable boundary of citrus fruits moved back to the south until the Chang-River. In the thirteenth century, it went up and reached Huai-River again. As the Little Ice Age started, the belt of citrus cultivation came south back again. Especially, the seventeenth century was cold, so the changed current became a cause of freezing to death of citrus fruits in areas which located southern parts of Jiangnan - Jiagnxi, Hunan, Anhui, Zhejang. During the Little Ice Age the latitude of the northern limit of citrus cultivation had moved two to three degrees southwards. This demonstrates how much the areas were cold. This also suggests that there was a huge conversion of eco-system at that time. It should be remembered that the human history makes its progress in the context of the overwhelming change.
Abstract
The ebb and flow of Northern limit of Citrus cultivation, represented by ‘the Citrus Change the Trifoliate Orange,’ reflects the history of climatic variation in China. Climate has been changing constantly in the last 5,000 years. The change made the Northern limit of Citrus cultivation go up and down repeatedly. Huai-River was lying on the border of the limitation during the Chunchou-Period. In the second century B. C. the temperature was milder than today, even though the line moved to the southern area, Chang-River area. After the Nanbeichao-Period consisted of cold current, the warm climate during the Xiu·Tang-Period let the line of limit go northward until the Huai-River. The climate warming contributed to make Dongting-Mountain into the largest production region of mandarins. The Song-Period was also warm, because ‘Medieval Warm Period’ maintained until this period. The twelfth century was very cold, in particular, so that the arable boundary of citrus fruits moved back to the south until the Chang-River. In the thirteenth century, it went up and reached Huai-River again. As the Little Ice Age started, the belt of citrus cultivation came south back again. Especially, the seventeenth century was cold, so the changed current became a cause of freezing to death of citrus fruits in areas which located southern parts of Jiangnan - Jiagnxi, Hunan, Anhui, Zhejang. During the Little Ice Age the latitude of the northern limit of citrus cultivation had moved two to three degrees southwards. This demonstrates how much the areas were cold. This also suggests that there was a huge conversion of eco-system at that time. It should be remembered that the human history makes its progress in the context of the overwhelming change.
참고문헌 (120)
- "晏子春秋", ~
- "史記", ~
- "淮南子", ~
- "三國志", ~
- "隋書", ~
- "舊唐書", ~
- "宋史", ~
- "明史", ~
- "純孝章皇帝實錄", ~
- "農桑輯要", ~
- "御定歴代賦彚", ~
- "御定全唐詩", ~
- "古今圖書集成", ~
- "吳都文粹續集", ~
- "朝鮮王朝實錄", ~
- 高似孫, "剡錄", ~
- 顧况, "華陽集", ~
- 郭槖駝, "種樹書", ~
- 歐陽詢, "藝文類聚", ~
- 金友理, "太湖備考", ~
- 羅愿, "爾雅翼", ~
- 李綱, "梁谿集", ~
- 白居易, "白氏長慶集", ~
- 范成大, "吳郡志", ~
- 范仲淹, "范文正集", ~
- 査愼行, "敬業堂詩集", ~
- 蘇軾, "東坡全集", ~
- 宋林希, "考工記解", ~
- 葉夢得, "避暑錄話", ~
- 葉夢珠, "閱世編", ~
- 吳仁傑, "離騷草木疎", ~
- 翁澍, "具區志", ~
- 王士禎, "居易錄", ~
- 王世懋, "學圃雜疏", ~
- 王鏊, "震澤集", ~
- 王鏊, "震澤編", ~
- 姚廷遴, "歷年記", ~
- 韋應物, "韋蘇州集", ~
- 陸友仁, "硏北雜志", ~
- 張世南, "游宦紀聞", ~
- 莊綽, "鷄肋編", ~
- 鄭言紹, "太湖備考續編", ~
- 鄭虎臣, "吳都文粹", ~
- 朱長文, "吳郡圖經續記", ~
- 陳舜兪, "都官集", ~
- 陳元龍, "格致鏡原", ~
- 蔡沈, "書經集傳", ~
- 彭乗, "墨客揮犀", ~
- 韓彦直, "橘錄", ~
- 胡渭, "禹貢錐指", ~
- 嘉慶, "松江府志", ~
- 嘉靖, "寧德縣志", ~
- 嘉靖, "福寧州志", ~
- 嘉靖, "吳邑志", ~
- 嘉靖, "潮州府志", ~
- 嘉靖, "太倉州志", ~
- 康熙, "瓊山縣志", ~
- 康熙, "樂會縣志", ~
- 康熙, "當塗縣志", ~
- 康熙, "文昌縣志", ~
- 康熙, "湘鄕縣志", ~
- 康熙, "遂安縣志", ~
- 康熙, "臨高縣志", ~
- 康熙, "興化府莆田縣志", ~
- 乾隆, "婁縣志", ~
- 乾隆, "安仁縣志", ~
- 乾隆, "連江縣志", ~
- 乾隆, "永興縣志", ~
- 乾隆, "吳江縣志", ~
- 景定, "建康志", ~
- 光緖, "定安縣志", ~
- 光緖, "黃岩縣志", ~
- 道光, "西安縣新志正誤", ~
- 同治, "武岡洲志", ~
- 同治, "宜春縣志", ~
- 萬曆, "宜興縣志", ~
- 民國, "衢縣志", ~
- 民國, "同安縣志", ~
- 崇禎, "吳縣志", ~
- 雍正, "從禾縣新志", ~
- 正德, "瓊台志", ~
- 유소민, "기후의 반역" (2005), 성균관대학교출판부
- 葛全勝, "中國歷朝氣候變化" (2011), 科學出版社
- 滿志敏, "中國歷史時期氣候變化硏究" (2009), 山東敎育出版社
- 牟重行, "中國五千年氣候變遷的再考證" (1996), 氣象出版社
- 文煥然, "中國歷史時期冬半年氣候冷暖變遷" (1996), 科學出版社
- 楊煜達, "淸代雲南季風氣候與天氣災害硏究" (2006), 復旦大學出版社
- 劉昭民, "中國歷史上氣候之變遷" (1982), 臺灣商務印書館
- 張丕遠, "中國歷史氣候變化" (1996), 山東科學技術出版社
- 周開隆, "中國果樹志․柑橘卷" (2010), 中國林業出版社
- 竺可楨, "竺可楨全集 第1~5卷" (2004), 上海科技敎育出版社
- H. H. Lamb, "Climate: Present, Past and Future, Vol.2 Climate History and the Future" (1977), Methuen & Co Ltd
- Wolfgang Behringer, "A Cultural History of Climate" (2010), Polity Press
- 김문기, "명청시기 강남의 기후변동과 동정감귤", 명청사연구, 14 (2001)
- 김문기, "17세기 中國과 朝鮮의 小氷期 氣候變動", 역사와경계, (77), pp.133~194 (2010), 부산경남사학회
- 김문기, "소빙기와 청어: 천․해․인의 관점에서", 역사와경계, 8(89), pp.69~108 (2013), 부산경남사학회
- 김연옥, "한국의 소빙기 기후 : 역사 기후학적 접근의 일시론", 지리학과 지리교육, 14 (1984)
- 이호철, "19세기초 조선의 기후변동과 농업위기", 조선시대사학보, 2 (1997)
- 佳宏偉, "近十年來生態環境變遷史硏究綜述", 史學月刊, 2004(6) (2004)
- 葛全勝, "中國歷史時期溫度變化特徵的新認識: 紀念竺可楨｢中國過去五千年溫度變化初步硏究｣發表30周年", 地理科學進展, 21(4) (2002)
- 高建慧, "中国中世纪暖期气候研究综述", 地理科学, 2006(3) (2006)
- 龔高法, "柑橘凍害" (1983), 農業出版社
- 滿志敏, "歷史時期柑橘種植北界與氣候變化的關係", 復旦學報(社會科學判), 1999(5) (1999)
- 滿志敏, "中國東部十三世紀溫暖期自然帶的推移", 復旦學報(社會科學版), 1990(5) (1990)
- 文煥然, "中國歷史時期冬半年氣候冷暖變遷" (1996), 科學出版社
- 徐道一, "明淸宇宙期", 大自然探索, 1984(4) (1984)
- 宋正海, "中國古代自然災異群發期" (2002), 安徽敎育出版社
- 王紹武, "中世紀暖期與小氷期", 氣候變化硏究進展, 6(5) (2010)
- 林國欽, "從兩宋詩詞看溫州柑橘的發展與影響", 學術探討, 2011(7) (2011)
- 張德二, "我國‘中世紀溫暖期’氣候的初步推斷", 第四紀硏究, 1993(1) (1993)
- 張福春, "氣候變遷和超長期豫報文集" (1977), 科學出版社
- 张娴, "中国小冰期气候研究综述", 南京信息工程大学学报(自然科学版), 2013(4) (2013)
- 鄭景雲, "從中國科擧2000年溫度變化看20世紀增減", 地理學報, 57(6) (2002)
- 左昕昕, "中世纪暖期气候研究综述", 中国沙漠, 2009(1) (2009)
- 周書燦, "20世紀中國歷史氣候硏究述論", 歷史學, 2008(2) (2008)
- 陳橋驛, "浙江古代柑橘栽培業的發展", 農業考古, 1985(2) (1985)
- 鈔曉鴻, "生態環境與明淸社會經濟" (2004), 黃山書舍
- 竺可楨, "中國歷史上氣候之變遷", 東方雜誌, 22(3) (1925)
- 竺可楨, "中國近五千年來氣候變遷的初步硏究", 考古學報, 1972(1) (1972)
- Chu Ko-chen, "A Preliminary Study on the Climatic Fluctuations during the Last 5,000 Years in China", Scientica, 16(2) (1973)