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우리나라 산지 하천의 하안단구는 매 빙기마다 형성되었는가?

Did Fluvial Terrace of Mountain Streams in Korea Form in Each Glacial Stage?

이광률
한국지형학회 (The Geomorphological Association Of Korea)|2019.09|한국지형학회지 (Journal of The Korean Geomorphological Association)|제26권 제3호|pp. 19-30|DOI 10.16968/JKGA.26.3.19

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참고문헌

키워드

하안단구fluvial terrace기후단구기후단구 모델장기적 기후 변동중·단기적 기후 변동여름 몬순climatic terraceclimatic terrace modellong-term climatic changemedium- and short-term climatic changesummer monsoon
주제분류지리학

초록

This study summarizes domestic and foreign previous works on fluvial terrace with absolute ages to discuss formative process of climatic terrace in Korea. Different from traditional climatic terrace model, approximately three quarters from foreign works have argued that formation of climatic terrace can be attributed to medium- and short-term climatic change or other environmental factors, rather than long-term climatic change of glacial and interglacial cycles. Based on previous works on fluvial terrace in Korea, it can be suggested that fluvial terrace in Korea formed not due to long-term climatic change of 100,000-year cycles related to glacial and interglacial cycles, but due to medium- and short-term climatic change or climatic event of tens of thousands of years related to intensity change in summer monsoon, one of the important factors affecting precipitation in Korea.

Abstract

This study summarizes domestic and foreign previous works on fluvial terrace with absolute ages to discuss formative process of climatic terrace in Korea. Different from traditional climatic terrace model, approximately three quarters from foreign works have argued that formation of climatic terrace can be attributed to medium- and short-term climatic change or other environmental factors, rather than long-term climatic change of glacial and interglacial cycles. Based on previous works on fluvial terrace in Korea, it can be suggested that fluvial terrace in Korea formed not due to long-term climatic change of 100,000-year cycles related to glacial and interglacial cycles, but due to medium- and short-term climatic change or climatic event of tens of thousands of years related to intensity change in summer monsoon, one of the important factors affecting precipitation in Korea.

참고문헌 (53)

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