Using climate impacts indicators to evaluate climate model ensembles: temperature suitability of premium winegrape cultivation in the United States

被引:0
作者
Noah S. Diffenbaugh
Martin Scherer
机构
[1] Stanford University,Department of Environmental Earth System Science, Woods Institute for the Environment
[2] Purdue University,Department of Earth and Atmospheric Sciences, Purdue Climate Change Research Center
来源
Climate Dynamics | 2013年 / 40卷
关键词
Climate change; Climate impacts; CMIP3; NARCCAP; RegCM3; Winegrape;
D O I
暂无
中图分类号
学科分类号
摘要
We explore the potential to improve understanding of the climate system by directly targeting climate model analyses at specific indicators of climate change impact. Using the temperature suitability of premium winegrape cultivation as a climate impacts indicator, we quantify the inter- and intra-ensemble spread in three climate model ensembles: a physically uniform multi-member ensemble consisting of the RegCM3 high-resolution climate model nested within the NCAR CCSM3 global climate model; the multi-model NARCCAP ensemble consisting of single realizations of multiple high-resolution climate models nested within multiple global climate models; and the multi-model CMIP3 ensemble consisting of realizations of multiple global climate models. We find that the temperature suitability for premium winegrape cultivation is substantially reduced throughout the high-value growing areas of California and the Columbia Valley region (eastern Oregon and Washington) in all three ensembles in response to changes in temperature projected for the mid-twenty first century period. The reductions in temperature suitability are driven primarily by projected increases in mean growing season temperature and occurrence of growing season severe hot days. The intra-ensemble spread in the simulated climate change impact is smaller in the single-model ensemble than in the multi-model ensembles, suggesting that the uncertainty arising from internal climate system variability is smaller than the uncertainty arising from climate model formulation. In addition, the intra-ensemble spread is similar in the NARCCAP nested climate model ensemble and the CMIP3 global climate model ensemble, suggesting that the uncertainty arising from the model formulation of fine-scale climate processes is not smaller than the uncertainty arising from the formulation of large-scale climate processes. Correction of climate model biases substantially reduces both the inter- and intra-ensemble spread in projected climate change impact, particularly for the multi-model ensembles, suggesting that—at least for some systems—the projected impacts of climate change could be more robust than the projected climate change. Extension of this impacts-based analysis to a larger suite of impacts indicators will deepen our understanding of future climate change uncertainty by focusing on the climate phenomena that most directly influence natural and human systems.
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页码:709 / 729
页数:20
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共 138 条
[1]  
Annamalai H(2007)The South Asian summer monsoon and its relationship with ENSO in the IPCC AR4 simulations J Clim 20 1071-1092
[2]  
Hamilton K(2007)Assessing uncertainties in crop model simulations using daily bias-corrected regional circulation model outputs Climate Res 34 211-222
[3]  
Baigorria GA(1990)Global climate change and intensification of coastal ocean upwelling Science 247 198-201
[4]  
Jones JW(2003)Climate modelling: severe summertime flooding in Europe Nature 421 805-806
[5]  
Bakun A(2006)The community climate system model version 3 (CCSM3) J Clim 19 2122-2143
[6]  
Christensen JH(2000)High-quality spatial climate data sets for the United States and beyond Transactions of the ASAE 43 1957-1962
[7]  
Christensen OB(2005)Global high resolution versus limited area model climate change projections over Europe: quantifying confidence level from PRUDENCE results Clim Dyn 25 653-670
[8]  
Collins WD(2010)Intensification of hot extremes in the United States Geophys Res Lett 37 L15701-32
[9]  
Bitz CM(2004)Could CO2-induced land cover feedbacks alter near-shore upwelling regimes? Proc Nat Acad Sci 101 27-15778
[10]  
Daly C(2005)Fine-scale processes regulate the response of extreme events to global climate change Proc Nat Acad Sci USA 102 15774-20198