Temperature and precipitation biases in CORDEX RCM simulations over South America: possible origin and impacts on the regional climate change signal

被引:4
作者
Blazquez, Josefina [1 ]
Solman, Silvina A. A. [2 ]
机构
[1] Univ Nacl La Plata FCAG UNLP, Fac Ciencias Astron & Geofis, Paseo Bosque Paseo Bosque S-N B1900FWA, La Plata, Argentina
[2] Univ Buenos Aires, CONICET, Fac Ciencias Exactas & Nat, Ctr Invest Mar & Atmosfera CIMA,CNRS,IRD, Ciudad Univ Pabellon 2,Piso 2 C1428EGA, Ciudad Autonoma Buenos A, Argentina
关键词
Systematic errors; Climate change signal; South America; RCM CORDEX models; CLARIS-LPB; MODEL; PROJECTIONS; RESOLUTION; PERFORMANCE; ENSEMBLE;
D O I
10.1007/s00382-023-06727-5
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Precipitation and temperature biases from a set of Regional Climate Models from the CORDEX initiative have been analysed to assess the extent to which the biases may impact the climate change signal. The analysis has been performed for the South American CORDEX domain. A large warm bias was found over central Argentina (CARG) for most models, mainly in the summer season. Results indicate that the possible origin of this bias is an overestimation of the incoming shortwave radiation, in agreement with an underestimation of the relative humidity at 850 hPa, a variable that could be used to diagnose cloudiness. Regarding precipitation, the largest biases were found during summertime over northeast of Brazil (NEB), where most models overestimate the precipitation, leading to wet biases over that region. This bias agrees with models' underestimation of both the moisture flux convergence and the relative humidity at lower levels of the atmosphere. This outcome suggests that the generation of more clouds in the models may drive the wet bias over NEB. These systematic errors could affect the climate change signal, considering that these biases may not be stationary. For both CARG and NEB regions, models with higher warm biases project higher warming levels, mainly in the summer season. In addition, it was found that these relationships are statistically significant with a confidence level of 95%, pointing out that biases are linearly linked with the climate change signal. For precipitation, the relationship between the biases and the projected precipitation changes is only statistically significant for the NEB region, where models with the largest wet biases present the greatest positive precipitation changes during the warm season. As in the case of biases, the analysis of the temperature and precipitation projections over some regions of South America suggests that clouds could affect them. The results found in this study point out that the analysis of the bias behaviour could help in a better interpretation of the climate change signal.
引用
收藏
页码:2907 / 2920
页数:14
相关论文
共 48 条
[1]   Evaluating the Time-Invariance Hypothesis of Climate Model Bias Correction: Implications for Hydrological Impact Studies [J].
Alberto Velazquez, Juan ;
Troin, Magali ;
Caya, Daniel ;
Brissette, Francois .
JOURNAL OF HYDROMETEOROLOGY, 2015, 16 (05) :2013-2026
[2]  
Allen M, 2006, PREDICTABILITY OF WEATHER AND CLIMATE, P391, DOI 10.1017/CBO9780511617652.016
[3]   Projecting climate change in South America using variable-resolution Community Earth System Model: An application to Chile [J].
Bambach, Nicolas E. ;
Rhoades, Alan M. ;
Hatchett, Benjamin J. ;
Jones, Andrew D. ;
Ullrich, Paul A. ;
Zarzycki, Colin M. .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2022, 42 (04) :2514-2542
[4]   Multiscale precipitation variability and extremes over South America: analysis of future changes from a set of CORDEX regional climate model simulations [J].
Blazquez, Josefina ;
Solman Silvina, A. .
CLIMATE DYNAMICS, 2020, 55 (7-8) :2089-2106
[5]   Performance of a high resolution global model over southern South America [J].
Blazquez, Josefina ;
Nunez, Mario N. .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2013, 33 (04) :904-919
[6]   Overestimation of Mediterranean summer temperature projections due to model deficiencies [J].
Boberg, Fredrik ;
Christensen, Jens H. .
NATURE CLIMATE CHANGE, 2012, 2 (06) :433-436
[7]   Bias Correction of Regional Climate Model Simulations in a Region of Complex Orography [J].
Bordoy, Roger ;
Burlando, Paolo .
JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY, 2013, 52 (01) :82-101
[8]   Combined influence of atmospheric physics and soil hydrology on the simulated meteorology at the SIRTA atmospheric observatory [J].
Cheruy, F. ;
Campoy, A. ;
Dupont, J-C. ;
Ducharne, A. ;
Hourdin, F. ;
Haeffelin, M. ;
Chiriaco, M. ;
Idelkadi, A. .
CLIMATE DYNAMICS, 2013, 40 (9-10) :2251-2269
[9]  
Chou S., 2014, Am J Clim Change, V3, P438, DOI [10.4236/ajcc.2014.35039, DOI 10.4236/AJCC.2014.35039]
[10]   Temperature dependent climate projection deficiencies in CMIP5 models [J].
Christensen, Jens H. ;
Boberg, Fredrik .
GEOPHYSICAL RESEARCH LETTERS, 2012, 39