Regional climate effects of irrigation and urbanization in thewestern united states: a model intercomparison
In the western United States, more than 30,500 square miles has been converted to irrigated agriculture and urban areas. This study compares the climate responses of four regional climate models (RCMs) to these past land-use changes. The RCMs used two contrasting land cover distributions: potential natural vegetation, and modern land cover that includes agriculture and urban areas. Three of the RCMs represented irrigation by supplementing soil moisture, producing large decreases in August mean (-2.5 F to -5.6 F) and maximum (-5.2 F to -10.1 F) 2-meter temperatures where natural vegetation was converted to irrigated agriculture. Conversion to irrigated agriculture also resulted in large increases in relative humidity (9 percent 36 percent absolute change). Only one of the RCMs produced increases in summer minimum temperature. Converting natural vegetation to urban land cover produced modest but discernable climate effects in all models, with the magnitude of the effects dependent upon the preexisting vegetation type. Overall, the RCM results indicate that land use change impacts are most pronounced during the summer months, when surface heating is strongest and differences in surface moisture between irrigated land and natural vegetation are largest. The irrigation effect on summer maximum temperatures is comparable in magnitude (but opposite in sign) to predicted future temperature change due to increasing greenhouse gas concentrations.
- Research Organization:
- COLLABORATION - UC Santa Cruz; ScrippsInstitute of Oceanography; USGS; UC Davis
- DOE Contract Number:
- DE-AC02-05CH11231
- OSTI ID:
- 893610
- Report Number(s):
- LBNL-60284; CEC-500-2006-031; R&D Project: G2W020; TRN: US200625%%430
- Country of Publication:
- United States
- Language:
- English
Similar Records
SSP‐Based Land‐Use Change Scenarios: A Critical Uncertainty in Future Regional Climate Change Projections
Strong Influence of Irrigation on Water Budget and Land Surface Temperature in Indian Subcontinental River Basins