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      Quantitative Definition and Spatiotemporal Distribution of Little Water Season (LIWAS) in Korea

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      https://www.riss.kr/link?id=A103801006

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      다국어 초록 (Multilingual Abstract)

      Like other continental climatic regions Korea has a period around the spring when agricultural activities are interrupted frequently by a shortage of available water resources during the season.
      This season, which is termed the Little Water Season (LIWAS) in this study, has important implications for many socio-economic activities but the scientific definition of this season remains vague. In this study, the onset and termination dates, as well as the characteristics of the LIWAS have been defined based on the Available Water Resources Index (AWRI). Based on the proposed definition of LIWAS, the implications on hydrological conditions over a range of geographic scales and their inter-annual variations on the water resource environments in Korea have been assessed. To develop an appropriate index for LIWAS based on AWRI, the criterion value (CV) for LIWAS was set as the lowest 25th percentile of the AWRI values averaged for 30 years (1981-2010). Therefore, the Little Water Season for Korea (LIWAS_K) was considered as the period when the daily averaged AWRIs were successively lower than the CV (143.7 mm). Based on this, the mean onset and end date of LIWAS_K, was 9 February and 11 May which also reflected the period in the spring season when the available water resources are expected to the lowest. Moreover, a number of seasonal characteristics of the water availability during the LIWAS, such as the Little Water Intensity (LWI), Water Deficit Amount (WDA) and Water Deficit Intensity (WDI) have been defined for the particular study region. Based on our results, we aver that the proposed season classification of the LIWAS can be better analyzed using the concept of usable water resources as a classification of dry period instead of using temperature and raw rainfall datasets.
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      Like other continental climatic regions Korea has a period around the spring when agricultural activities are interrupted frequently by a shortage of available water resources during the season. This season, which is termed the Little Water Season (L...

      Like other continental climatic regions Korea has a period around the spring when agricultural activities are interrupted frequently by a shortage of available water resources during the season.
      This season, which is termed the Little Water Season (LIWAS) in this study, has important implications for many socio-economic activities but the scientific definition of this season remains vague. In this study, the onset and termination dates, as well as the characteristics of the LIWAS have been defined based on the Available Water Resources Index (AWRI). Based on the proposed definition of LIWAS, the implications on hydrological conditions over a range of geographic scales and their inter-annual variations on the water resource environments in Korea have been assessed. To develop an appropriate index for LIWAS based on AWRI, the criterion value (CV) for LIWAS was set as the lowest 25th percentile of the AWRI values averaged for 30 years (1981-2010). Therefore, the Little Water Season for Korea (LIWAS_K) was considered as the period when the daily averaged AWRIs were successively lower than the CV (143.7 mm). Based on this, the mean onset and end date of LIWAS_K, was 9 February and 11 May which also reflected the period in the spring season when the available water resources are expected to the lowest. Moreover, a number of seasonal characteristics of the water availability during the LIWAS, such as the Little Water Intensity (LWI), Water Deficit Amount (WDA) and Water Deficit Intensity (WDI) have been defined for the particular study region. Based on our results, we aver that the proposed season classification of the LIWAS can be better analyzed using the concept of usable water resources as a classification of dry period instead of using temperature and raw rainfall datasets.

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      참고문헌 (Reference)

      1 최광용, "현재와 미래 우리나라 겨울철 강수형태 변화" 대한지리학회 43 (43): 1-19, 2008

      2 고정웅, "한반도 우기의 강수 특성과 지역 구분" 한국기상학회 41 (41): 101-114, 2005

      3 최기선, "한반도 여름 강우량의 변화에서 1996년을 중심으로 나타나는 남북진동 패턴" 한국기상학회 20 (20): 91-100, 2010

      4 김고운, "한반도 봄철 강수량의 장기변동과 미래변화" 한국기상학회 22 (22): 449-454, 2012

      5 김성, "한반도 봄철 가뭄과 연관된 북반구 대기순환패턴의 변화" 한국기상학회 41 (41): 571-585, 2005

      6 최기선, "한반도 Warm Season의 시종 및 이와 연관된 기후의 장기 변동" 한국기상학회 41 (41): 301-314, 2005

      7 이승호, "전구 기온 상승이 한국의 적설량 변화에 미치는 영향" 대한지리학회 38 (38): 463-477, 2003

      8 강민구, "수자원의 지속가능성 평가 지수 개발과 구성 요소의 중요도 평가" 한국수자원학회 39 (39): 59-68, 2006

      9 박창용, "기온과 강수특성을 고려한 남한의 기후지역구분" 대한지리학회 44 (44): 1-16, 2009

      10 권진주, "가뭄심도 분류기준의 개선방안 제시" 한국수자원학회 46 (46): 195-204, 2013

      1 최광용, "현재와 미래 우리나라 겨울철 강수형태 변화" 대한지리학회 43 (43): 1-19, 2008

      2 고정웅, "한반도 우기의 강수 특성과 지역 구분" 한국기상학회 41 (41): 101-114, 2005

      3 최기선, "한반도 여름 강우량의 변화에서 1996년을 중심으로 나타나는 남북진동 패턴" 한국기상학회 20 (20): 91-100, 2010

      4 김고운, "한반도 봄철 강수량의 장기변동과 미래변화" 한국기상학회 22 (22): 449-454, 2012

      5 김성, "한반도 봄철 가뭄과 연관된 북반구 대기순환패턴의 변화" 한국기상학회 41 (41): 571-585, 2005

      6 최기선, "한반도 Warm Season의 시종 및 이와 연관된 기후의 장기 변동" 한국기상학회 41 (41): 301-314, 2005

      7 이승호, "전구 기온 상승이 한국의 적설량 변화에 미치는 영향" 대한지리학회 38 (38): 463-477, 2003

      8 강민구, "수자원의 지속가능성 평가 지수 개발과 구성 요소의 중요도 평가" 한국수자원학회 39 (39): 59-68, 2006

      9 박창용, "기온과 강수특성을 고려한 남한의 기후지역구분" 대한지리학회 44 (44): 1-16, 2009

      10 권진주, "가뭄심도 분류기준의 개선방안 제시" 한국수자원학회 46 (46): 195-204, 2013

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      2008-02-05 학술지명변경 외국어명 : 미등록 -> Asia-Pacific Journal of Atmospheric Sciences KCI등재
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