Characteristics of Extreme Climate Sequences over Korea Using a Regional Climate Change Scenario

被引:11
作者
Eun-Soon, Im [1 ]
Kwon, Won-Tae [1 ]
机构
[1] KMA, Climate Res Lab, METRI, Seoul 516720, South Korea
关键词
D O I
10.2151/sola.2007-005
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
We investigate the characteristics and potential future change of extreme climate phenomena based on daily statistical properties. To assess the fine-scale climate change projection over Korea, an ECHO-G B2 scenario simulation has been dynamically downscaled by using the RegCM3 nesting system. Two sets of multi-decadal simulations are performed for the present day (1971-2000) and future climate (2021-2050). We analyze four categories of weather spells in terms of the sequences of dry/wet and frost/hot days from the nested domain simulation of 20 km grid spacing. In the validation of the reference scenario, the model shows a reasonable performance of reproducing both observed climatological and distinct characteristics of each spell. Regarding the projected extreme climate events, the results indicate not only a significant change in frequency and intensity, but also substantial change in the fine scale detail of the regional distribution of temperature-based as well as precipitation-based extreme events. A substantial increase of hot spells is found along with increasing of maximum temperature. Longer-period frost spells are projected to decrease, whereas relatively short-period frost spells are likely to increase due to breaks of long spells by greenhouse warming. Wet spells of long periods tend to be more frequent, showing a distinct variation across regions.
引用
收藏
页码:17 / 20
页数:4
相关论文
共 21 条
[11]  
Im ES, 2007, CLIM DYNAM, V28, P759, DOI [10.1007/s00382-006-0203-z, 10.1007/s00382-006-0203-Z]
[12]   Projected Changes in Precipitation Characteristics around Japan under the Global Warming [J].
Kimoto, M. ;
Yasutomi, N. ;
Yokoyama, C. ;
Emori, S. .
SOLA, 2005, 1 :85-88
[13]   Response of the East Asian summer monsoon to doubled atmospheric CO2:: Coupled climate model simulations and projections under IPCC AR4 [J].
Kripalani, R. H. ;
Oh, J. H. ;
Chaudhari, H. S. .
THEORETICAL AND APPLIED CLIMATOLOGY, 2007, 87 (1-4) :1-28
[14]  
Leung LR, 1999, J CLIMATE, V12, P2010, DOI 10.1175/1520-0442(1999)012<2010:PNCSSB>2.0.CO
[15]  
2
[16]   Internal variability in a 1000-yr control simulation with the coupled climate model ECHO-G - I. Near-surface temperature, precipitation and mean sea level pressure [J].
Min, SK ;
Legutke, S ;
Hense, A ;
Kwon, WT .
TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY, 2005, 57 (04) :605-621
[17]   Changes in Extremes Indices over Japan Due to Global Warming Projected by a Global 20-km-mesh Atmospheric Model [J].
Mizuta, Ryo ;
Uchiyama, Takao ;
Kamiguchi, Kenji ;
Kitoh, Akio ;
Noda, Akira .
SOLA, 2005, 1 :153-156
[18]  
Nakicenovic N., 2000, SPECIAL REPORT EMISS
[19]   Regional climate simulation for Korea using dynamic downscaling and statistical adjustment [J].
Oh, JH ;
Kim, T ;
Kim, MK ;
Lee, SH ;
Min, SK ;
Kwon, WT .
JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN, 2004, 82 (06) :1629-1643
[20]   Downscaling of daily rainfall occurrence over northeast Brazil using a hidden Markov model [J].
Robertson, AW ;
Kirshner, S ;
Smyth, P .
JOURNAL OF CLIMATE, 2004, 17 (22) :4407-4424