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Temporal and spatial variability of rainfall and climate trend on Jeju Island

机译:济州岛降雨和气候趋势的时空变化

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The temporal and spatial analyses of rainfall and temperature were conducted for understanding spatial variability and climate trend on Jeju Island. Rainfall data from 1992 to 2009 were used for the spatial analyses, and missing data were adjusted on Mt. Halla and along the northeast coast to reduce uncertainty of spatial variability. In addition, rainfall time series data of both Jeju City and Seogwipo City from 1961 to 2009 were analyzed for a long-term trend and identification of droughts. Mean annual rainfall for the period 1992-2009 shows an area of maximum rainfall centered around Mt. Halla where maximum annual rainfall reaches more than 4,300 mm and mean island rainfall is 2,082 mm. Upward trends in rainfall intensity, magnitude, and dryness conditions at the Jeju City and Seogwipo City from 1961 to 2009 suggest that rainfall has intensified with greater quantities of rainfall occurring over shorter durations, with longer dry periods between storm events. The annual cycle shows a distinct monsoon signature with peak rainfall typically occurring in August. Rainfall seasonality shows a shift in peak rainfall from June, July, and August, to July, August, and September. The most severe droughts in the period 1961-2009 were identified using a 12-month composite SPI. Three severe droughts each lasting around two years were identified over a relatively short nine-year period from 1964-1972.
机译:进行了降雨和温度的时空分析,以了解济州岛的空间变异性和气候趋势。对1992年至2009年的降雨数据进行了空间分析,对缺失的数据进行了调整。汉拿和东北沿海一带减少了空间变异性的不确定性。此外,还分析了济州市和西归浦市1961年至2009年的降雨时间序列数据,以了解长期趋势并确定干旱。 1992-2009年期间的年平均降雨量显示了一个最大降雨量集中在Mt周围的区域。汉拿(Halla)年最大降雨量超过4,300毫米,平均岛屿降雨量为2,082毫米。 1961年至2009年期间,济州市和西归浦市的降雨强度,强度和干燥条件的上升趋势表明,降雨加剧,在较短的持续时间内出现了更多的降雨,而两次暴风雨之间的干旱时间更长。年周期显示出明显的季风特征,通常在八月出现峰值降雨。降雨季节变化表明峰值降雨量从6月,7月和8月到7月,8月和9月发生了变化。使用12个月的综合SPI确定了1961-2009年期间最严重的干旱。在1964年至1972年的短短9年内,确定了三场严重干旱,每次干旱持续两年左右。

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