TY - JOUR
T1 - Using a statistical preanalysis approach as an ensemble technique for the unbiased mapping of GCM changes to local stations
AU - Chadwick, Cristián
AU - Gironás, Jorge
AU - Vicuña, Sebastián
AU - Meza, Francisco
AU - Mcphee, James
N1 - Publisher Copyright:
© 2018 American Meteorological Society.
PY - 2018
Y1 - 2018
N2 - Accounting for climate change, GCM-based projections and their uncertainty are relevant to study potential impacts on hydrological regimes as well as to analyze, operate, and design water infrastructure. Traditionally, several downscaled and/or bias-corrected GCM projections are individually or jointly used to map the raw GCMs' changes to local stations and evaluate uncertainty. However, the preservation of GCMs' statistical attributes is by no means guaranteed, and thus alternative methods to cope with this issue are needed. This work develops an ensemble technique for the unbiased mapping of GCM changes to local stations, which preserves local climate variability and the GCMs' statistics. In the approach, trend percentiles are extracted from the GCMs to represent the range of future long-term climate conditions to which local climatic variability is added. The approach is compared against a method in which each GCM is individually used to build future climatic scenarios from which percentiles are computed. Both approaches were compared to study future precipitation conditions in three Chilean basins under future climate projections based on 45 GCM runs under the RCP8.5 scenario. Overall, the approaches produce very similar results, even if a few trend percentiles are adopted in the GCM preanalysis. In fact, using 5-10 percentiles produces a mean absolute difference of 0.4% in the estimation of the probabilities of consecutive years under different precipitation thresholds, which is ~60% less than the error obtained using the median trend. Thus, the approach successfully preserves the GCM's statistical attributes while incorporating the range of projected climates.
AB - Accounting for climate change, GCM-based projections and their uncertainty are relevant to study potential impacts on hydrological regimes as well as to analyze, operate, and design water infrastructure. Traditionally, several downscaled and/or bias-corrected GCM projections are individually or jointly used to map the raw GCMs' changes to local stations and evaluate uncertainty. However, the preservation of GCMs' statistical attributes is by no means guaranteed, and thus alternative methods to cope with this issue are needed. This work develops an ensemble technique for the unbiased mapping of GCM changes to local stations, which preserves local climate variability and the GCMs' statistics. In the approach, trend percentiles are extracted from the GCMs to represent the range of future long-term climate conditions to which local climatic variability is added. The approach is compared against a method in which each GCM is individually used to build future climatic scenarios from which percentiles are computed. Both approaches were compared to study future precipitation conditions in three Chilean basins under future climate projections based on 45 GCM runs under the RCP8.5 scenario. Overall, the approaches produce very similar results, even if a few trend percentiles are adopted in the GCM preanalysis. In fact, using 5-10 percentiles produces a mean absolute difference of 0.4% in the estimation of the probabilities of consecutive years under different precipitation thresholds, which is ~60% less than the error obtained using the median trend. Thus, the approach successfully preserves the GCM's statistical attributes while incorporating the range of projected climates.
KW - Hydrologic cycle
KW - Hydrology
KW - Risk assessment
KW - Statistical techniques
KW - Time series
UR - http://www.scopus.com/inward/record.url?scp=85055038966&partnerID=8YFLogxK
U2 - 10.1175/JHM-D-17-0198.1
DO - 10.1175/JHM-D-17-0198.1
M3 - Article
AN - SCOPUS:85055038966
SN - 1525-755X
VL - 19
SP - 1447
EP - 1465
JO - Journal of Hydrometeorology
JF - Journal of Hydrometeorology
IS - 9
ER -