Apr 29, 2026
Daily Reference Evapotranspiration (ETo) in Yuma Valley: What the Seasonal Pattern Means for Irrigation
Reference evapotranspiration, or ETo, is a daily measure of atmospheric water Reference evapotranspiration, or ETo, is a daily measure of atmospheric water demand from a well-watered reference surface. For growers in Yuma Valley, where almost every drop of water a crop receives comes from irrigation, ETo is one of the most useful numbers available for deciding when and how much to irrigate.
How ETo changes over the year
The graph shows daily ETo at the AZMET Yuma Valley station from May 2023 through early 2026 (Figure 1). The pattern repeats each year: ETo is low in winter, climbs through spring, peaks during the hot summer period, and declines again in fall. From June through August, daily ETo often rises into the 0.30 to 0.40 inch per day range, with some peak days approaching 0.44 inch per day. During December through February, daily ETo often falls below 0.10 inch per day. This seasonal swing is much more important for irrigation management than the weak downward trendline.
That is a four- to five-fold difference in daily crop water demand between the peak of summer and the depth of winter. A grower irrigating a full-canopy crop in July is managing a very different situation than the same grower irrigating in January, even if the field looks similar.

Figure 1. Daily reference evapotranspiration (ETo) at the AZMET Yuma Valley station
from May 2023 through early 2026.
What high and low ETo numbers actually mean
Four weather factors drive ETo up or down: solar radiation, air temperature, relative humidity, and wind speed. When all four push in the same direction, bright sun, high heat, dry air, and strong wind- ETo climbs quickly and crop water demand rises with it. When conditions are mild and humid, ETo stays low, and irrigation needs ease off. The table below gives a practical guide to what different ETo ranges mean for a Yuma Valley grower and how to respond:

These ranges are general guides. The actual water use of any specific crop also depends on its growth stage and canopy cover, which is captured by the crop coefficient (Kc). A young transplant with little canopy uses far less water than a mature plant at full cover, even when ETo is the same.
Turning ETo into an irrigation target
Multiply daily ETo by the crop coefficient (Kc) for your crop and growth stage to get estimated crop water use:
Crop ET = ETo × Kc
For example, if ETo is 0.30 inches per day and your crop is at a growth stage with a Kc of 0.80, the crop is using about 0.24 inches of water that day. At a peak summer ETo of 0.40 inches per day with the same Kc, water use climbs to 0.32 inches per day. That difference adds up quickly across a field over a week. Staying current with daily ETo during high-demand periods matters more than it does in the cooler months, when ETo is low and there is more time to respond.
What this means for irrigation management
During warm, sunny, dry, and windy periods, particularly from April through September, check ETo daily and adjust irrigation accordingly. During cooler months, ETo is low enough that there is more flexibility, but it still varies with weather and should not be ignored entirely.
Current daily ETo for Yuma Valley is available from the AZMET network at ag.arizona.edu/azmet. Use the daily ETo value along with your crop’s Kc to estimate how much water to apply. Combining that number with soil moisture information and knowledge of your irrigation system’s output will give you the most reliable basis for scheduling. During peak summer demand, staying close to that daily target is one of the most effective things a grower can do to protect yield and avoid water stress.