Future intensity-duration-frequency curves of Edmonton under climate warming and increased convective available potential energy

被引:6
作者
Kuo, Chun-Chao [1 ,2 ]
Gan, Kai Ernn [3 ,4 ]
Yang, Yang [2 ]
Gan, Thian Yew [2 ]
机构
[1] Govt British Columbia, River Forecast Ctr, Victoria, BC, Canada
[2] Univ Alberta, Dept Civil & Environm Engn, Edmonton, AB T6G 1H9, Canada
[3] Univ Penn, Dept Comp & Informat Technol, Philadelphia, PA 19104 USA
[4] McMaster Univ, Dept Civil Engn, Hamilton, ON L8S 4L7, Canada
关键词
Annual maximum precipitation; Air temperature; Convective available potential energy (CAPE); Regional climate model (RCM); Global Climate Model (GCM); PRECIPITATION EXTREMES; REGIONAL CLIMATE; PARAMETERIZATION SCHEMES; BIAS CORRECTION; ANNUAL MAXIMUM; MODEL; TEMPERATURE; WEATHER; CANADA; WRF;
D O I
10.1007/s10584-021-03250-6
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A regional climate model called WRF (Weather Research and Forecasting) was set up in a two-way, three-domain nested framework to simulate future May to August precipitation of central Alberta, Canada. WRF is forced with climate outputs from four Global Climate Models (GCMs) for the baseline period 1980-2005, and for 2041-2100 based on the Representative Concentration Pathways (RCP) 4.5 and 8.5 climate scenarios of the Intergovernmental Panel on Climate Change (IPCC). A quantile-quantile bias correction method and a regional frequency analysis were applied to acquire future grid-based IDF curves for the city of Edmonton. Future trends of air temperature and convective available potential energy (CAPE) are investigated. Future IDF curves are expected to have higher intensities because of projected higher air temperature and atmospheric water vapor, and projected increase in CAPE by 2071-2100. Our results likely mean that under the impact of climate change, the future risk of flooding in Edmonton would increase.
引用
收藏
页数:23
相关论文
共 90 条
[1]   Global Precipitation: Means, Variations and Trends During the Satellite Era (1979-2014) [J].
Adler, Robert F. ;
Gu, Guojun ;
Sapiano, Matthew ;
Wang, Jian-Jian ;
Huffman, George J. .
SURVEYS IN GEOPHYSICS, 2017, 38 (04) :679-699
[2]   Global observed changes in daily climate extremes of temperature and precipitation [J].
Alexander, LV ;
Zhang, X ;
Peterson, TC ;
Caesar, J ;
Gleason, B ;
Tank, AMGK ;
Haylock, M ;
Collins, D ;
Trewin, B ;
Rahimzadeh, F ;
Tagipour, A ;
Kumar, KR ;
Revadekar, J ;
Griffiths, G ;
Vincent, L ;
Stephenson, DB ;
Burn, J ;
Aguilar, E ;
Brunet, M ;
Taylor, M ;
New, M ;
Zhai, P ;
Rusticucci, M ;
Vazquez-Aguirre, JL .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2006, 111 (D5)
[3]   Atmospheric warming and the amplification of precipitation extremes [J].
Allan, Richard P. ;
Soden, Brian J. .
SCIENCE, 2008, 321 (5895) :1481-1484
[4]  
[Anonymous], 1948, RANK CORRELATION MET
[5]  
[Anonymous], 2007, Eos, Trans. Amer. Geophys. Union, DOI DOI 10.1029/2007EO470006
[6]   Parameterization-Induced Error Characteristics of MM5 and WRF Operated in Climate Mode over the Alpine Region: An Ensemble-Based Analysis [J].
Awan, Nauman K. ;
Truhetz, H. ;
Gobiet, A. .
JOURNAL OF CLIMATE, 2011, 24 (12) :3107-3123
[7]   Strong increase in convective precipitation in response to higher temperatures [J].
Berg, Peter ;
Moseley, Christopher ;
Haerter, Jan O. .
NATURE GEOSCIENCE, 2013, 6 (03) :181-185
[8]   Future increases in Arctic precipitation linked to local evaporation and sea-ice retreat [J].
Bintanja, R. ;
Selten, F. M. .
NATURE, 2014, 509 (7501) :479-+
[9]   Do Downscaled General Circulation Models Reliably Simulate Historical Climatic Conditions? [J].
Bock, Andrew R. ;
Hay, Lauren E. ;
McCabe, Gregory J. ;
Markstrom, Steven L. ;
Atkinson, R. Dwight .
EARTH INTERACTIONS, 2018, 22 (10) :1-22
[10]   Statistical and dynamical downscaling of the Seine basin climate for hydro-meteorological studies [J].
Boe, J. ;
Terray, L. ;
Habets, F. ;
Martin, E. .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2007, 27 (12) :1643-1655