SSP-Based Land-Use Change Scenarios: A Critical Uncertainty in Future Regional Climate Change Projections

被引:17
|
作者
Bukovsky, Melissa S. [1 ]
Gao, Jing [2 ,3 ]
Mearns, Linda O. [1 ]
O'Neill, Brian C. [4 ,5 ]
机构
[1] Natl Ctr Atmospher Res, Reg Integrated Sci Collect, Computat & Informat Syst Lab & Res Applicat Lab, POB 3000, Boulder, CO 80307 USA
[2] Univ Delaware, Dept Geog, Newark, DE USA
[3] Univ Delaware, Spatial Sci & Data Sci Inst, Newark, DE USA
[4] Univ Denver, Pardee Ctr Int Futures, Denver, CO USA
[5] Univ Denver, Josef Korbel Sch Int Studies, Denver, CO USA
关键词
CORDEX; land‐ use change; regional climate; SSP; COVER CHANGES; MODEL; IMPACTS; PRECIPITATION; ENERGY; WATER; CLM;
D O I
10.1029/2020EF001782
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
To better understand the role projected land-use changes (LUCs) may play in future regional climate projections, we assess the combined effects of greenhouse-gas (GHG)-forced climate change and LUCs in regional climate model (RCM) simulations. To do so, we produced RCM simulations that are complementary to the North-American Coordinated Regional Downscaling Experiment (NA-CORDEX) simulations, but with future LUCs that are consistent with particular Shared Socioeconomic Pathways (SSPs) and related to a specific Representative Concentration Pathway (RCP). We examine the state of the climate at the end of the 21st century with and without two urban and agricultural LUC scenarios that follow SSP3 and SSP5 using the Weather Research and Forecasting (WRF) model forced by one global climate model, the MPI-ESM, under the RCP8.5 scenario. We find that LUCs following different societal trends under the SSPs can significantly affect climate projections in different ways. In regions of significant cropland expansion over previously forested area, projected annual mean temperature increases are diminished by around 0.5 degrees C-1.0 degrees C. Across all seasons, where urbanization is high, projected temperature increases are magnified. In particular, summer mean temperature projections are up to 4 degrees C-5 degrees C greater and minimum and maximum temperature projections are increased by 2.5 degrees C-6 degrees C, amounts that are on par with the warming due to GHG-forced climate change. Warming is also enhanced in the urban surroundings. Future urbanization also has a large influence on precipitation projections during summer, increasing storm intensity, event length, and the overall amount over urbanized areas, and decreasing precipitation in surrounding areas.
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页数:18
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