Development of a precipitation–area curve for warning criteria of short-duration flash flood

• Main Authors: D.-H. Bae, M.-H. Lee, S.-K. Moon
• Format: Article
• Language: English
• Published: Copernicus Publications 2018-01-01
• Series: Natural Hazards and Earth System Sciences
• Online Access: https://www.nat-hazards-earth-syst-sci.net/18/171/2018/nhess-18-171-2018.pdf

This paper presents quantitative criteria for flash flood warning that can be used to rapidly assess flash flood occurrence based on only rainfall estimates. This study was conducted for 200 small mountainous sub-catchments of the Han River basin in South Korea because South Korea has recently suffered many flash flood events. The quantitative criteria are calculated based on flash flood guidance (FFG), which is defined as the depth of rainfall of a given duration required to cause frequent flooding (1–2-year return period) at the outlet of a small stream basin and is estimated using threshold runoff (TR) and antecedent soil moisture conditions in all sub-basins. The soil moisture conditions were estimated during the flooding season, i.e., July, August and September, over 7 years (2002–2009) using the Sejong University Rainfall Runoff (SURR) model. A ROC (receiver operating characteristic) analysis was used to obtain optimum rainfall values and a generalized precipitation–area (<i>P</i>–<i>A</i>) curve was developed for flash flood warning thresholds. The threshold function was derived as a <i>P</i>–<i>A</i> curve because the precipitation threshold with a short duration is more closely related to basin area than any other variables. For a brief description of the <i>P</i>–<i>A</i> curve, generalized thresholds for flash flood warnings can be suggested for rainfall rates of 42, 32 and 20 mm h⁻¹ in sub-basins with areas of 22–40, 40–100 and &gt; 100 km², respectively. The proposed <i>P</i>–<i>A</i> curve was validated based on observed flash flood events in different sub-basins. Flash flood occurrences were captured for 9 out of 12 events. This result can be used instead of FFG to identify brief flash flood (less than 1 h), and it can provide warning information to decision-makers or citizens that is relatively simple, clear and immediate.