Journal
JOURNAL OF HYDROMETEOROLOGY
Volume 15, Issue 6, Pages 2558-2585Publisher
AMER METEOROLOGICAL SOC
DOI: 10.1175/JHM-D-14-0082.1
Keywords
Hydrometeorology; Climate models; Hydrologic models; Land surface model; Atmosphere-land interaction; Regional effects
Categories
Funding
- California Energy Commission [CEC-500-10-041]
- USGS through the Southwest Climate Science Center
- NOAA through the California Nevada Climate Applications Project (CNAP)
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A new technique for statistically downscaling climate model simulations of daily temperature and precipitation is introduced and demonstrated over the western United States. The localized constructed analogs (LOCA) method produces downscaled estimates suitable for hydrological simulations using a multiscale spatial matching scheme to pick appropriate analog days from observations. First, a pool of candidate observed analog days is chosen by matching the model field to be downscaled to observed days over the region that is positively correlated with the point being downscaled, which leads to a natural independence of the downscaling results to the extent of the domain being downscaled. Then, the one candidate analog day that best matches in the local area around the grid cell being downscaled is the single analog day used there. Most grid cells are downscaled using only the single locally selected analog day, but locations whose neighboring cells identify a different analog day use a weighted combination of the center and adjacent analog days to reduce edge discontinuities. By contrast, existing constructed analog methods typically use a weighted average of the same 30 analog days for the entire domain. By greatly reducing this averaging, LOCA produces better estimates of extreme days, constructs a more realistic depiction of the spatial coherence of the downscaled field, and reduces the problem of producing too many light-precipitation days. The LOCA method is more computationally expensive than existing constructed analog techniques, but it is still practical for downscaling numerous climate model simulations with limited computational resources.
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