Evapotranspiration (ET)

Overview

Most of the precipitation that falls on the Colorado River Basin returns to the atmosphere via evapotranspiration (ET), a term which encompasses evaporation of moisture from soils and open water, transpiration from plants and crops, and sublimation from the snowpack. Since ET is such a large component of the water budget from the field scale to the basin scale, ET can strongly influence the moisture status (dryness/wetness) of the land surface and ultimately, the volume of runoff.

Strictly speaking, ET refers to the actual loss of water (depth per unit time) from the land surface. ET is driven by the atmosphere's evaporative demand (E₀)--its "thirst" for surface moisture--but the amount of ET (water loss) is necessarily limited by the available water at the surface. So cumulative ET over an extended period (e.g., one year) cannot exceed precipitation (plus irrigation water, in the case of irrigated cropland).

Figure 1. Cumulative (actual) evapotranspiration (ET) during 2021 over the northwest portion of the Grand Valley, far western Colorado, as estimated by an ensemble of satellite-based methods. (Inset shows a real-color satellite image of the same area.) The highest ET values (about 50"; dark blues) are seen over reservoirs and the surface of the Colorado River, while the extensive irrigated fields (greens and blues) have ET values from 20"-40". ET is lowest (orange; about 5") over the unvegetated "badlands" north and west of the Grand Valley. The estimated Reference ET (ET₀) over this area during 2021 was 45"-52", and precipitation was 6"-10". (Source: ET and satellite images from [OpenET Data Explorer]; design by Jeff Lukas.)

Evaporative demand (E₀) is not limited by available water at the surface, and is often greater than than precipitation (+ irrigation) and ET. Evaporative demand is functionally equivalent to Potential ET (PET). Reference ET (ET₀) is closely related to E₀ and PET; it is an estimate of the upper bound of ET losses (i.e., consumptive water use) from irrigated cropland. In principle, with a fully watered crop, Reference ET would be the same as (actual) ET, but in practice, Reference ET is often greater.

Reference ET and PET can be estimated using an equation that inputs meteorological variables (ideally: temperature, solar radiation, humidity, winds), or derived from remote sensing data using a land-surface model. Direct in-situ measurements of PET and Reference ET (e.g., pan evaporation) are very sparse across the CRB. Actual ET is more challenging to quantify. ET can be estimated using a land-surface (hydrology) model with meteorological inputs, or by assimilating satellite observations of land-surface temperature into an energy-balance model. More direct measurements of ET can be made using Eddy Covariance methods, which requires multiple instrumentation packages arranged vertically on a single tower.

ET and related variables have large seasonal variability relative to their annual variability, with a maximum in summer and minimum in winter. ET and related variables are subject to long-term trends driven by warming temperatures.

Relevance

In the Colorado River Basin, estimates of ET and evaporative demand (Reference ET, PET) are used in reservoir operations, irrigation scheduling, and demand and consumptive use modeling. Estimates of watershed-scale ET are also used to validate the water budget simulations in hydrologic models, such as those used by the CBRFC for streamflow forecasting. Estimates of monthly reservoir evaporation and consumptive use by agriculture are also important terms in the Reclamation operations and planning models, and in Reclamation's calculations of natural flows.

Data and tools

Reference ET (in-situ)

Several weather-station networks in the basin states, mainly serving the agricultural sector, have instrumentation for all of the variables (temperature, solar radiation, humidity, winds) needed for real-time calculations of Reference ET. Typically, Reference ET is calculated hourly and daily, to the nearest 0.01".

CoAgMET

Colorado; 90 active stations in agricultural areas.

AZMET

Arizona; 27 active stations in agricultural and urban areas.

UT AgWeather

Utah and adjacent areas in ID, WY, CO, NM; 130 active stations in agricultural and urban areas.

California Irrigation Management Information System (CIMIS)

California; 150 active stations in agricultural and urban areas.

Evaporative Demand Drought Index (EDDI)

EDDI is based on Reference ET (calculated from gridded NLDAS-2 meteorological data, using the same method as for the in-situ data above) and standardized relative to historical Reference ET for each gridpoint over the time window (2 weeks to 1 year) of interest. EDDI can offer early warning of agricultural and hydrologic drought by providing near-real-time information on the emergence or persistence of anomalous evaporative demand.

OpenET

OpenET is an open-source platform and data viewing tool that brings together several satellite-based ET estimation methods to provide daily, monthly, and annual ET estimates at the field scale. The methods currently in the OpenET ensemble include ALEXI/DisAlexi, eeMETRIC, geeSEBAL, PT-JPL, SIMS, and SSEBop. Free registration required to view data.

Additional resources

State of the Science Report

Chapter 5 of the State of the Science report, Section 5.5 describes ET and evaporative demand, and sources of data, in greater detail.

OpenET - Methodologies page

This section of the OpenET website provides more detail the several remote-sensing-based ET methods that make up the OpenET ensemble, as well as other datasets (such as Reference ET based on gridded climate data) that inform the Open ET ensemble values.