Climatic consequences of adopting drought tolerant vegetation over Los Angeles as a response to California drought utilized a regional climate model to analyze the impacts of drought-tolerant vegetation in Los Angeles. The results revealed that drought-tolerant vegetation contributed to a daytime warming of 1.9 degrees Celsius, largely due to decreases in irrigation, and a nighttime cooling of 3.2 degrees Celsius, due to differences in soil thermodynamics and heat exchange. The report concludes that the greater magnitude of the nighttime cooling could counterbalance the warming effects during the day.
