Why is Evapotranspiration (ET) important?

The primary component of hydrologic budgets, evapotranspiration (ET), the sum of evaporation and transpiration from plants, reflects the degree of water loss into the atmosphere, which is critical information when determining irrigation watering needs, groundwater supply levels, drought patterns, and other environmental impacts related to water budgets.

Superior ET Data to Inform Your Decisions

Whether you're focused on environmental research, agricultural research, or crop production, field-proven HOBO weather stations and sensors provide the accurate and reliable data needed to calculate evapotranspiration to support your water management decisions and understanding, from irrigation to climate impacts on ecosystems. We currently do not support evapotranspiration calculations, but will soon offer this feature on our LI-COR Cloud monitoring platform.

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Farmer looking at data monitoring corn field

Remote Monitoring Stations for Calculating Evapotranspiration (ET)

 

Data Access

Remote access via cellular Remote access via cellular

Memory

32 MB, 2 million measurements, continuous logging 16 MB, 1 million measurements, continuous logging

Internet Connection

Cellular Cellular

HOBOnet Wireless Capability

Yes Yes (RX2106/05 only)

Inputs

10 (wired) + 50 (wireless) 5 (wired) + 50 (wireless)

Mobile Alerts

Yes Yes

Power Options

Solar Solar or Battery

Water Level/Flow

Yes Yes (RX2104/03 only)

 

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River running through a marsh with the outlet in the distance

Frequently Asked Questions

LICOR Cloud provides Reference ET (ETo) for a short canopy, calculated by using the Penman-Monteith equation, which is recommended by the Food and Agriculture Organization (FAO) and the American Society of Civil Engineers (ASCE).

Temperature, Humidity, Wind Speed, and Solar Radiation parameters are all required to calculate Evapotranspiration (ET).

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