Recent trends of mean and extreme precipitation in Korea

International Journal of Climatology - Tập 31 Số 3 - Trang 359-370 - 2011
Il‐Won Jung1, Deg‐Hyo Bae1, Gwangseob Kim2
1Department of Civil & Environmental Engineering, Sejong University, 98 Kunja-Dong, Kwangjin-Gu, Seoul, 143-747, Korea
2Department of Civil Engineering, Kyungpook National University, Sankyuk-Dong, Buk-Gu, Daegu 702-701, Korea

Tóm tắt

AbstractThe spatial and temporal variability of precipitation in Korea were investigated using 183 weather station data for 1973–2005. A set of 16 indices that represent mean and extreme values of precipitation data were estimated using daily precipitation data, linear and spatial trend relationships of the indices were analysed using the Mann–Kendall test and Moran's I test statistic, respectively. Results demonstrate that annual precipitation data have a significant positive trend and there is a strong spatial relationship in their variability. The increase of annual precipitation is mainly associated with the increase of frequency and intensity of heavy precipitation during summer season. However, precipitation during spring and winter seasons had a decreasing trend. This variation of precipitation is likely to increase flood and drought risk. It means that the increase of annual precipitation should not be helpful for water resources management but could be a burden to river management and dam operation in Korea. Copyright © 2010 Royal Meteorological Society

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Tài liệu tham khảo

Alexander LV, 2007, Trends in Australia's climate means and extremes: a global context, Australian Meteorological Magazine, 56, 1

10.1111/j.0016-7363.2005.00671.x

10.1002/hyp.6861

10.3354/cr00704

10.3741/JKWRA.2005.38.2.111

10.1007/s00477-006-0036-7

10.1029/2005GL023378

10.1088/1748-9326/2/4/045012

Choi Y, 2004, Trends in temperature and precipitation extreme events in Korea daily precipitation events and their extremes in the southern region of Korea, Journal of the Korean Geographical Society Environmental Impact Assessment, 1139, 711

10.1023/B:CLIM.0000043141.54763.f8

Chung YS, 1999, Recent climate change and related factors observed in Korea, Journal of Korean Meteorological Society, 35, 309

10.2307/2287063

10.1002/hyp.300

10.1175/JCLI3339.1

10.1029/2006WR005099

10.1002/joc.1303

10.1007/s003820050185

10.1007/s003820050186

10.1029/WR018i001p00107

10.1002/joc.864

10.1016/j.jhydrol.2005.07.003

10.1007/s00382-007-0282-5

IPCC, 2001, Climate Change 2001: The Physical Science Basis

IPCC, 2007, Climate Change 2007: The Physical Science Basis

10.1002/hyp.5873

10.1002/joc.797

Kendall MG, 1975, Rank Correlation Methods

KundzewiczZW RobsonA.2000.Detecting Trend and Other Changes in Hydrological Data. World Climate Programme. Water World Climate Programme Data and Monitoring WCDMP‐45 WMO/TD. No. 1013. Geneva May 2000.

10.1023/A:1023694115864

Lee S, 2004, A variation of summer rainfall in Korea, Journal of Korean Geographical Society, 39, 819

10.1111/j.1752-1688.1988.tb00900.x

10.1002/env.507

10.1002/hyp.5534

10.2307/1907187

10.1029/2006JD007103

10.1002/joc.1404

10.1023/A:1005495627778

10.1175/JCLI4262.1

Qinglong Y, 2007, Climate change over the Yarlung Zangbo river basin during 1961–2005, Journal of Geographical Sciences, 17

10.1016/j.pce.2006.02.062

O'Sullivan D, 2003, Geographic Information Analysis

10.1002/hyp.5993

10.1002/joc.1694

PetersonTC FollandC GruzaG HoggW MokssitA PlummerN.2001.Report on the Activities of the Working Group on Climate Change Detection and Related Rapporteurs 1998‐2001. International CLIVAR Project Office Southampton: UK;143.

10.1175/1520-0442(1993)006<2298:IACUBI>2.0.CO;2

10.1002/joc.1838

10.1007/s00382-003-0365-x

10.1002/joc.1639

10.1002/joc.995

StepanekP.2007.Software Package for Processing Climatological Data (Complex Solution). Available athttp://www.klimahom.com/software/index.html.[accessed December 30 2009].

10.1007/s00704-005-0139-y

10.1002/joc.1576

10.5194/hess-12-207-2008

10.1002/hyp.5846

10.1175/JCLI-3318.1

10.1029/2007JD008393