Evapotranspiration Seasonal Summary (in)

Data Last Updated: 6/23/2017 @ 07:00 AM



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 2016 / Nov 20173.474 1.151 more than the Winter average.8.288 1.014 more than the Spring average.3.756* 6.365 less than the Summer average.---15.518* 8.242 less than the yearly average.
Dec 2015 / Nov 20161.302 1.021 less than the Winter average.4.435 2.839 less than the Spring average.15.946 5.825 more than the Summer average.7.331 3.289 more than the Fall average.29.014 5.254 more than the yearly average.
Dec 2014 / Nov 20151.780 0.543 less than the Winter average.6.557 0.717 less than the Spring average.8.513 1.608 less than the Summer average.3.715 0.327 less than the Fall average.20.565 3.195 less than the yearly average.
Dec 2013 / Nov 20142.747 0.424 more than the Winter average.6.551 0.723 less than the Spring average.8.097 2.024 less than the Summer average.3.051 0.991 less than the Fall average.20.446 3.314 less than the yearly average.
Dec 2012 / Nov 20132.313 0.01 less than the Winter average.10.541 3.267 more than the Spring average.14.291 4.17 more than the Summer average.5.928 1.886 more than the Fall average.33.073 9.313 more than the yearly average.
Dec 2011 / Nov 2012---------0.187* 3.855 less than the Fall average.0.187* 23.573 less than the yearly average.
 
Max3.474 10.541 15.946 7.331 33.073
Avg2.323 7.274 10.121 4.042 23.760
Min1.302 4.435 3.756 0.187 0.187
 
* 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.