Evapotranspiration Seasonal Summary (in)

Data Last Updated: 2/27/2025 @ 2:50 PM



Northern Hemisphere Meterological Seasons
Winter: December, January, February
Spring: March, April, May
Summer: June, July, August
Fall: September, October, November

 Daily DetailMonthly SummarySeasonal Summary 




 Evapotranspiration
DateWinterSpringSummerFallYear
Dec 2024 / Nov 2025---0.809* 2.265 less than the Spring average.------0.809* 3.53 less than the yearly average.
Dec 2023 / Nov 20241.265*  5.339* 2.265 more than the Spring average.------6.604* 2.265 more than the yearly average.
Dec 2022 / Nov 2023------------0.000* 4.339 less than the yearly average.
Dec 2021 / Nov 2022------------0.000* 4.339 less than the yearly average.
Dec 2020 / Nov 2021------------0.000* 4.339 less than the yearly average.
Dec 2019 / Nov 2020------------0.000* 4.339 less than the yearly average.
Dec 2018 / Nov 2019------------0.000* 4.339 less than the yearly average.
Dec 2017 / Nov 2018------------0.000* 4.339 less than the yearly average.
Dec 2016 / Nov 2017------------0.000* 4.339 less than the yearly average.
Dec 2015 / Nov 2016------------0.000* 4.339 less than the yearly average.
Dec 2014 / Nov 2015------------0.000* 4.339 less than the yearly average.
Dec 2013 / Nov 2014------------0.000* 4.339 less than the yearly average.
Dec 2012 / Nov 2013------------0.000* 4.339 less than the yearly average.
Dec 2011 / Nov 2012------------0.000* 4.339 less than the yearly average.
 
Max1.265 5.339 ------6.604
Avg1.265 3.074 ------4.339
Min1.265 0.809 ------0.000
 
* Denotes incomplete data for the month/year.Script Developed by Murry Conarroe of Wildwood Weather.
 
Color Key
< 3.000 3.000 - 6.000 6.000 - 9.000 9.000 - 12.000 12.000 - 15.000 15.000 - 18.000 18.000 - 21.000 21.000 - 24.000 24.000 - 27.000 27.000 - 30.000 30.000 - 33.000 33.000 - 36.00036.000>

Evapotranspiration (ET) is a term used to describe the sum of evaporation and plant transpiration from the Earth's land surface to the atmosphere. Evaporation accounts for the movement of water to the air from sources such as the soil, canopy interception, and water bodies. Transpiration accounts for the movement of water within a plant and the subsequent loss of water as vapor through stomata in its leaves.