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최영은 (2004)
Trends on Temperature and Precipitation Extreme Events in Korea, 39
Young-ho Lee, D. Cha, Dong‐Kyou Lee (2008)
Impact of Horizontal Resolution of Regional Climate Model on Precipitation Simulation over the Korean PeninsulaAtmosphere, 18
L A Vincent X Zhang (2000)
Temperature and precipitation trends in Canada during the 20th centuryAtmos.-Ocean, 38
S. Herrera, L. Fita, Jesús Fernández, J. Gutiérrez (2010)
Evaluation of the mean and extreme precipitation regimes from the ENSEMBLES regional climate multimodel simulations over SpainJournal of Geophysical Research, 115
Dong‐Kyou Lee, D. Cha, Hyun‐Suk Kang (2004)
Regional Climate Simulation of the 1998 Summer Flood over East AsiaJournal of the Meteorological Society of Japan, 82
E. Im, Joong‐Bae Ahn, W. Kwon, F. Giorgi (2006)
Multi-decadal scenario simulation over Korea using a one-way double-nested regional climate model system. Part 2: future climate projection (2021–2050)Climate Dynamics, 30
M. Suh, Seongjin Hong, Jeon‐Ho Kang (2009)
Characteristics of Seasonal Mean Diurnal Temperature Range and Their Causes over South KoreaAtmosphere, 19
Seok-Geun Oh, M. Suh, Jisu Myoung, D. Cha (2011)
Impact of Boundary Conditions and Cumulus Parameterization Schemes on Regional Climate Simulation over South-Korea in the CORDEX-East Asia Domain Using the RegCM4 ModelJournal of The Korean Earth Science Society, 32
David Williamson (1983)
Description of NCAR Community Climate Model (CCM0B)
D. Easterling, R. Stouffer, M. Wehner (2008)
CHAPTER 4. Measures To Improve Our Understanding of Weather and Climate Extremes. Weather and Climate Extremes in a Changing Climate. Regions of Focus: North America, Hawaii, Caribbean, and U.S. Pacific Islands
M. Clark, M. Serreze (2000)
Effects of variations in east Asian snow cover on modulating atmospheric circulation over the North Pacific OceanJournal of Climate, 13
G. Miguez-Macho, G. Stenchikov, A. Robock (2005)
Regional Climate Simulations over North America: Interaction of Local Processes with Improved Large-Scale FlowJournal of Climate, 18
A. Steiner, J. Pal, S. Rauscher, J. Bell, N. Diffenbaugh, A. Boone, L. Sloan, F. Giorgi (2009)
Land surface coupling in regional climate simulations of the West African monsoonClimate Dynamics, 33
Jing-Wei Liu, Li Bo, Tianjun Zhou, Zeng Xian-Feng, Feng Lei (2012)
The Extreme Summer Precipitation over East China during 1982-2007 Simulated by the LASG/IAP Regional Climate ModelAtmospheric and Oceanic Science Letters, 5
Leopoldo Oliveira, A. Piola, M. Mata, I. Soares (2009)
Brazil Current surface circulation and energetics observed from drifting buoysJournal of Geophysical Research, 114
M Wild K Makowski (2008)
Diurnal temperature range over Europe between 1950 and 2005Atmos. Chem. Phys. Discuss., 8
P. Zhai, Xuebin Zhang, Hui Wan, Xiaohua Pan (2005)
Trends in Total Precipitation and Frequency of Daily Precipitation Extremes over ChinaJournal of Climate, 18
M. Kanamitsu, W. Ebisuzaki, J. Woollen, Shi-Keng Yang, J. Hnilo, M. Fiorino, G. Potter (2002)
NCEP–DOE AMIP-II Reanalysis (R-2)Bulletin of the American Meteorological Society, 83
K. Oleson, G. Niu, Zong‐Liang Yang, D. Lawrence, P. Thornton, P. Lawrence, R. Stöckli, R. Dickinson, G. Bonan, S. Levis, A. Dai, Taotao Qian (2008)
Improvements to the Community Land Model and their impact on the hydrological cycleJournal of Geophysical Research, 113
K A Emanuel (1991)
A scheme for representing cumulus convection in large-scale modelsJ. Climate, 48
Feng Jin-ming, Wang Yongli, Fu Congbin (2011)
Simulation of Extreme Climate Events over China with Different Regional Climate ModelsAtmospheric and Oceanic Science Letters, 4
Chansoo Kim, M. Suh, Ki-Ok Hong (2009)
Bayesian Changepoint Analysis of the Annual Maximum of Daily and Subdaily Precipitation over South KoreaJournal of Climate, 22
M. Suh, Dong‐Kyou Lee (2004)
Impacts of land use/cover changes on surface climate over east Asia for extreme climate cases using RegCM2Journal of Geophysical Research, 109
Linling Chen, O. Johannessen, Huijun Wang, A. Ohmura (2011)
Accumulation over the Greenland Ice Sheet as represented in reanalysis dataAdvances in Atmospheric Sciences, 28
T. R. Karl (2008)
Weather and climate extremes in a changing climate-Regions of focus: North America, Hawaii, Caribbean, and U
M. Suh, Seok-Geun Oh, Dong‐Kyou Lee, D. Cha, Suk‐Jin Choi, C. Jin, Song‐You Hong (2012)
Development of New Ensemble Methods Based on the Performance Skills of Regional Climate Models over South KoreaJournal of Climate, 25
E. Im, M. Kim, W. Kwon, D. Bae (2007)
Sensitivity of Recent and Future Regional Climate Simulations to Two Convection Schemes in the RegCM3 Nesting SystemAsia-pacific Journal of Atmospheric Sciences, 43
citation_title=Experts recommend ways coping with increasing droughts, citation_publication_date= (2009)
Experts recommend ways coping with increasing droughts
citation_title=CORDEX Experiment, citation_publication_date= (2009)
CORDEX Experiment
D. Cha, Dong‐Kyou Lee (2009)
Reduction of systematic errors in regional climate simulations of the summer monsoon over East Asia and the western North Pacific by applying the spectral nudging techniqueJournal of Geophysical Research, 114
F. Giorgi, E. Coppola, F. Solmon, L. Mariotti, M. Sylla, X. Bi, N. Elguindi, G. Diro, V. Nair, G. Giuliani, U. Turuncoglu, S. Cozzini, I. Güttler, T. O’Brien, A. Tawfik, A. Shalaby, A. Zakey, A. Steiner, F. Stordal, L. Sloan, Č. Branković (2012)
RegCM4 : model description and preliminary tests over multiple CORDEX domainsClimate Research, 52
K. Trenberth (2011)
Changes in precipitation with climate changeClimate Research, 47
H. Storch, H. Langenberg, F. Feser (2000)
A Spectral Nudging Technique for Dynamical Downscaling PurposesMonthly Weather Review, 128
W. Landman (2010)
Climate change 2007: the physical science basisSouth African Geographical Journal, 92
K. Emanuel (1991)
A Scheme for Representing Cumulus Convection in Large-Scale ModelsJournal of the Atmospheric Sciences, 48
Yuqing Wang, O. Sen, Bin Wang (2003)
A Highly Resolved Regional Climate Model (IPRC-RegCM) and Its Simulation of the 1998 Severe Precipitation Event over China. Part I: Model Description and Verification of Simulation*Journal of Climate, 16
null Kobayashi (2006)
ERA-Interim: New ECMWF reanalysis products from 1989 onwards
T. Halenka, J. Kalvová, Z. Chládová, A. Demeterová, K. Zemánková, M. Belda (2006)
On the capability of RegCM to capture extremes in long term regional climate simulation – comparison with the observations for Czech RepublicTheoretical and Applied Climatology, 86
Dankers Rutger, Hiederer Roland (2008)
Extreme Temperatures and Precipitation in Europe: Analysis of a High-Resolution Climate Change Scenario
A. Dai (2011)
Drought under global warming: a reviewWiley Interdisciplinary Reviews: Climate Change, 2
Dong‐Kyou Lee, D. Cha, Suk‐Jin Choi (2005)
A Sensitivity Study of Regional Climate Simulation to Convective Parameterization Schemes for 1998 East Asian Summer MonsoonTerrestrial Atmospheric and Oceanic Sciences, 16
A. Holtslag, E. Bruijn, H. Pan (1990)
A High Resolution Air Mass Transformation Model for Short-Range Weather ForecastingMonthly Weather Review, 118
Liming Zhou, A. Dai, Yongjiu Dai, R. Vose, C. Zou, Yuhong Tian, Haishan Chen (2009)
Spatial dependence of diurnal temperature range trends on precipitation from 1950 to 2004Climate Dynamics, 32
K. Makowski, M. Wild, A. Ohmura (2007)
Diurnal temperature range over Europe between 1950 and 2005Atmospheric Chemistry and Physics, 8
A. Tank, G. Können (2003)
Trends in Indices of Daily Temperature and Precipitation Extremes in Europe, 1946–99Journal of Climate, 16
Im Eun-Soon, W. Kwon (2007)
Characteristics of Extreme Climate Sequences over Korea Using a Regional Climate Change ScenarioSola, 3
Abstract In this study, the impact of lateral boundary conditions (LBCs) on the simulation skills of the climate model RegCM4 for extreme climate events (ECEs) over South Korea are investigated using two sets of 20-yr (1989–2008) integration with two LBCs (ERA and R-2). The ECEs were defined by a percentile method and an absolute threshold method. In general, RegCM4 successfully reproduces the spatial distribution and the inter-annual variability (R > 0.76) of ECEs indices (precipitation and temperature extreme 5%) irrespective of LBCs. When driven by ERA, RegCM4 shows better simulation skill for ECEs (PR5%, TX5%, hot days, tropical nights, and wet days) than when driven by R-2. The ERA run simulates more than +7 mm day−1 and +1.1°C for PR5% and TX5% than those by the R-2 run, respectively. Although RegCM4’s simulation skills for the ECEs defined by absolute thresholds are significantly different according to LBCs, RegCM4 captured the interannual variability of frost days, hot days, tropical nights, and dry days well. However, the numbers of hot days and dry days are strongly underestimated and overestimated, respectively, compared to the observations, irrespective of LBCs. The large differences in the simulation skill of RegCM4 for ECEs over South Korea between two simulations can be caused by the differences between two LBCs, ERA and R-2. For the mean climate state, ERA simulates more humidity and warmer temperatures than the R-2, especially in the low-to-mid troposphere, resulting in a warmer and more humid troposphere especially at the central region of the model domain.
"Asia-Pacific Journal of Atmospheric Sciences" – Springer Journals
Published: Aug 1, 2013
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