Present and future climatologies in the phase I CREMA experiment

被引:48
作者
Coppola, Erika [1 ]
Giorgi, Filippo [1 ]
Raffaele, Francesca [1 ]
Fuentes-Franco, Ramon [2 ]
Giuliani, Graziano [1 ]
LLopart-Pereira, Marta [3 ]
Mamgain, Ashu [4 ]
Mariotti, Laura [1 ]
Diro, Gulilat Tefera [1 ]
Torma, Csaba [1 ]
机构
[1] Abdus Salam Int Ctr Theoret Phys, Trieste, Italy
[2] Ctr Sci Res & Higher Educ Ensenada, Baja, California Cice, Mexico
[3] Univ Sao Paulo, Dept Atmospher Sci, BR-05508090 Sao Paulo, Brazil
[4] Indian Inst Technol Delhi, Ctr Atmospher Sci, New Delhi, India
关键词
REGIONAL CLIMATE-CHANGE; RADIATIVE-TRANSFER; MODEL REGCM2; PRECIPITATION; SIMULATION; TESTS; BIAS; ASIA;
D O I
10.1007/s10584-014-1137-9
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
We provide an overall assessment of the surface air temperature and precipitation present day (1976-2005) and future (2070-2099) ensemble climatologies in the Phase I CREMA experiment. This consists of simulations performed with different configurations (physics schemes) of the ICTP regional model RegCM4 over five CORDEX domains (Africa, Mediterranean, Central America, South America, South Asia), driven by different combinations of three global climate models (GCMs) and two greenhouse gas (GHG) representative concentration pathways (RCP8.5 and RCP4.5). The biases (1976-2005) in the driving and nested model ensembles compared to observations show a high degree of spatial variability and, when comparing GCMs and RegCM4, similar magnitudes and more similarity for precipitation than for temperature. The large scale patterns of change (2070-2099 minus 1976-2005) are broadly consistent across the GCM and RegCM4 ensembles and with previous analyses of GCM projections, indicating that the GCMs selected in the CREMA experiment are representative of the more general behavior of current GCMs. The RegCM4, however, shows a lower climate sensitivity (reduced warming) than the driving GCMs, especially when using the CLM land surface scheme. While the broad patterns of precipitation change are consistent across the GCM and RegCM4 ensembles, greater differences are found at sub-regional scales over the various domains, evidently tied to the representation of local processes. This paper serves to provide a reference view of the behavior of the CREMA ensemble, while more detailed and process-based analysis of individual domains is left to companion papers of this special issue.
引用
收藏
页码:23 / 38
页数:16
相关论文
共 36 条
  • [1] Adjustment of global gridded precipitation for systematic bias
    Adam, JC
    Lettenmaier, DP
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D9)
  • [2] Overestimation of Mediterranean summer temperature projections due to model deficiencies
    Boberg, Fredrik
    Christensen, Jens H.
    [J]. NATURE CLIMATE CHANGE, 2012, 2 (06) : 433 - 436
  • [3] Dynamical downscaling: Assessment of value retained and added using the regional atmospheric modeling system (RAMS)
    Castro, CL
    Pielke, RA
    Leoncini, G
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2005, 110 (D5) : 1 - 21
  • [4] Christensen JH, 2007, AR4 CLIMATE CHANGE 2007: THE PHYSICAL SCIENCE BASIS, P847
  • [5] Potential for added value in temperature simulated by high-resolution nested RCMs in present climate and in the climate change signal
    Di Luca, Alejandro
    de Elia, Ramon
    Laprise, Rene
    [J]. CLIMATE DYNAMICS, 2013, 40 (1-2) : 443 - 464
  • [6] Dickinson R E., 1993, NCAR Technical Note
  • [7] Emanuel KA, 1999, J ATMOS SCI, V56, P1766, DOI 10.1175/1520-0469(1999)056<1766:DAEOAC>2.0.CO
  • [8] 2
  • [9] Updated regional precipitation and temperature changes for the 21st century from ensembles of recent AOGCM simulations
    Giorgi, F
    Bi, X
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2005, 32 (21) : 1 - 4
  • [10] Introduction to the TAC special issue: The RegCNET network
    Giorgi, F.
    Pal, J. S.
    Bi, X.
    Sloan, L.
    Elguindi, N.
    Solmon, F.
    [J]. THEORETICAL AND APPLIED CLIMATOLOGY, 2006, 86 (1-4) : 1 - 4