본 연구에서는 2009년 여름 강원도 양구군 해안분지(펀치볼)에 구축한 자동기상관측망 기온자료를 분석하여 여름철 하루 중 시간진행 또는 일기패턴에 따른 산간분지 내 기온감률 변화 특징을 밝히고자 한다. 산정부와 분지 내 사이에 형성되는 여름철 일평균 기온감률은 $-0.53^{circ}C$/100m이나, 일변화에 의해 새벽 6시경에 $-0.25^{circ}C$/100m의 최저, 오후 4~5시경에 $-0.85^{circ}C$/100m의 최고값을 나타낸다. 종관일기 패턴 별 일평균 기온감률은 강수일($-0.63^{circ}C$/100m), 집중호우일($-0.53^{circ}C$/100m), 약간 구름 낀 날($-0.47^{circ}C$/100m), 맑은날($-0.39^{circ}C$/100m) 순으로 높게 나타난다. 여름철 맑은날 새벽에는 분지 내에서 기온역전현상으로 냉기호가 형성되는 반면, 호우일에는 구름에 의한 복사냉각효과 감소로 온기호가 형성된다.
In this study, diurnal and intra-seasonal variations of summertime temperature lapse rate (TLR) by synoptic weather conditions in a mountainous basin are examined based on hourly temperature data observed in 2009 summer at an Automatic Weather Station (AWS) network deployed in Haean basin (called Punch Bowl), Yanggu in the Republic of Korea. Summertime average TLR between the top and bottom of the basin is $-0.53^{circ}C$/100m. Due to its diurnal variations, TLR shows the lowest by $-0.25^{circ}C$/100m at 6AM, while it maximizes up to $-0.85^{circ}C$/100m between 4PM~5PM. Comparisons of daily average TLRs by synoptic weather patterns reveal that the magnitude of TLRs is greatest in the order of rainy days ($-0.63^{circ}C$/100m), heavy rainfall days ($-0.53^{circ}C$/100m), partly cloudy days ($-0.47^{circ}C$/100m), and sunny days ($-0.39^{circ}C$/100m). At dawn on sunny days in summer, strong cooling pools accompanying temperature inversion layers are formed within the basin, while on heavy rainfall days, warming pools are observed due to relatively low TLRs associated with the reduction of surface radiation cooling by clouds.
