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The characteristics of drought occurrence in North Korea and its comparison with drought in South Korea

机译:朝鲜干旱发生的特征及其与韩国干旱的比较

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摘要

The characteristics of the drought occurrence in North Korea over a period of 56 years (1952-2007) were analyzed by region, compared with those of South Korea, and graphed as a drought map for easy detection of the drought's history. To assess them, the Effective Drought Index (EDI), which was calculated from the daily precipitation data for 109 grids of the Korean Peninsula, was used. The daily precipitation data were extracted from the Asian Precipitation Highly Resolved Observational Data Integration towards Evaluation of Water Resources (APHRODITE). The characteristics of the drought occurrence in North Korea were summed up in the following five points. First, North Korea was divided into four drought sub-regions: the Northeastern region (G1), the Northern region (G2), the Central region (G3), and the Southern region (G4). Second, droughts occurred most frequently in G1 (28) and G4 (28 events) and least frequently in G3 (15 events). Third, in all sub-regions, short-term droughts lasting less than 100 days were the most frequent (53 % or higher) and the longest drought lasted 2,911 days (June 30, 1973 to June 20, 1981), which occurred in G3. Fourth, short-term droughts occurred mainly in spring, mid-term droughts (100-500 days) in spring and summer, and long-term droughts (over 500 days) in summer. Fifth, a dry period (monthly mean EDI <0) appeared in all sub-regions between 1973 and 1981 and between 1990 and 1993, and a strong negative precipitation anomaly appeared during each of these periods. When compared to the droughts in South Korea, those in North Korea were less frequent, but the mean duration was longer. Until 1979, droughts occurred almost at the same time in North Korea as South Korea, but beginning in 1980, the time differences between two regions became larger. Thus, the characteristics of the drought occurrence in North and South Korea differ.
机译:通过地区分析,比较了朝鲜56年间(1952-2007年)干旱的发生特征,并与韩国进行了比较,并绘制了干旱图,以便于了解干旱的历史。为了评估它们,使用了有效干旱指数(EDI),该指数是根据朝鲜半岛109格的每日降水数据计算得出的。每日降水量数据是从亚洲降水高度解析观测数据集成到水资源评估(APHRODITE)中提取的。以下五点总结了朝鲜干旱的特征。首先,朝鲜被分为四个干旱分区:东北地区(G1),北部地区(G2),中部地区(G3)和南部地区(G4)。其次,干旱在G1(28)和G4(28事件)中最频繁发生,而在G3(15事件)中最少。第三,在所有次区域中,持续时间少于100天的短期干旱最为频繁(53%或更高),持续时间最长的干旱持续了2,911天(1973年6月30日至1981年6月20日),发生在G3 。第四,短期干旱主要发生在春季,春季和夏季是中期干旱(100-500天),夏季是长期干旱(超过500天)。第五,1973年至1981年以及1990年至1993年之间的所有次区域都出现了干旱期(月均EDI <0),并且在每个时期都出现了强烈的负降水异常。与韩国的干旱相比,朝鲜的干旱发生频率较低,但平均持续时间更长。直到1979年,朝鲜几乎与朝鲜同时发生干旱,但从1980年开始,两个地区之间的时间差变得更大。因此,朝鲜和韩国的干旱发生特征不同。

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  • 来源
    《Theoretical and applied climatology》 |2015年第2期|199-209|共11页
  • 作者单位

    Korea Meteorol Adm, Natl Inst Meteorol Res, Appl Meteorol Res Div, Seogwipo Si 697845, Jeju Do, South Korea;

    Korea Meteorol Adm, Natl Inst Meteorol Res, Forecast Res Div, Seogwipo Si 697845, Jeju Do, South Korea;

    Pukyong Natl Univ, Dept Environm Atmospher Sci, Busan 608737, South Korea;

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