POTENTIAL CLIMATE CHANGES IN ARIZONA AND U.S. SOUTHWEST​

Heat and drought changes​

Higher average temperatures, increased droughts—including hotter drought periods and more wildfire due to heat and drought.​

Precipitation changes​

Decreases in precipitation of 5% to 10% compared to earlier values, especially in April, May and June—months that are already very dry. Possible more extreme variability in rainfall, with longer periods with no rainfall and more extreme rainfall events when rain does occur. More rain than snow compared to past ratios, but thicker deeper snowfalls when it is cold. ​

​Evaporation changes​

Higher evaporation rates. More water loss from soils. Possible decreased runoff to rivers and less recharge of groundwater.​

​Water demand changes​

Increased outdoor water demand due to heat, drought and less rain. More competition for graywater between individuals and municipal systems. More competition for stormwater flows.​

Water supply changes​

Reduced surface water supplies flowing in the Colorado River, therefore lower flows to the CAP (Central Arizona Project canal) and reduced allocations to CAP water users. Possible rationing of municipal water supplies. Possible reduced groundwater recharge and higher groundwater pumping costs with deeper water levels. More rapid melting of mountain snowpack, shorter snowmelt period in the spring resulting in less runoff to landscapes and surface waters.​

Wind changes​

High winds during intense storms breaking limbs or uprooting trees; more dust storms.​

Additional effects on edible trees​

Stress due to lower rainfall and higher temperatures. Decreasing chill hours but not necessarily fewer freezing nights or less frost risk. Expanded range of insects that attack fruit trees. More competition for and reduced availability of conventional water supplies. Stress due to urban heat island effects in dense urban areas. Higher levels of the greenhouse gas CO2 potentially providing more “plant food.”​