Skip to Main Content
Measurement and simulation of evapotranspiration at a wetland site in the New Jersey PinelandsAuthor(s): David M. Sumner; Robert S. Nicholson; Kenneth L. Clark
Source: U.S. Geological Survey Scientific Investigations Report 2012–5118, 30 p.
Publication Series: Miscellaneous
Station: Northern Research Station
PDF: Download Publication (3.26 MB)
Related Research Highlights Impact of Invasive Insects and Fire on Forest Water Resources
DescriptionEvapotranspiration (ET) was monitored above a wetland forest canopy dominated by pitch-pine in the New Jersey Pinelands during November 10, 2004–February 20, 2007, using an eddy-covariance method. Twelve-month ET totals ranged from 786 to 821 millimeters (mm). Minimum and maximum ET rates occurred during December–February and in July, respectively. Relations between ET and several environmental variables (incoming solar radiation, air temperature, relative humidity, soil moisture, and net radiation) were explored. Net radiation (r = 0.72) and air temperature (r = 0.73) were the dominant explanatory variables for daily ET. Air temperature was the dominant control on evaporative fraction with relatively more radiant energy used for ET at higher temperatures. Soil moisture was shown to limit ET during extended dry periods. With volumetric soil moisture below a threshold of about 0.15, the evaporative fraction decreased until rain ended the dry period, and the evaporative fraction sharply recovered. A modified Hargreaves ET model, requiring only easily obtainable daily temperature data, was shown to be effective at simulating measured ET values and has the potential for estimating historical or real-time ET at the wetland site. The average annual ET measured at the wetland site during 2005–06 (801 mm/yr) is about 32 percent higher than previously reported ET for three nearby upland sites during 2005–09. Periodic disturbance by fire and insect defoliation at the upland sites reduced ET. When only undisturbed periods were considered, the wetland ET was 17 percent higher than the undisturbed upland ET. Interannual variability in wetlands ET may be lower than that of uplands ET because the upland stands are more susceptible to periodic drought conditions, disturbance by fire, and insect defoliation. Precipitation during the study period at the nearby Indian Mills weather station was slightly higher than the long-term (1902–2011) annual mean of 1,173 millimeters (mm), with 1,325 and 1,396 mm of precipitation in 2005 and 2006, respectively.
- Check the Northern Research Station web site to request a printed copy of this publication.
- Our on-line publications are scanned and captured using Adobe Acrobat.
- During the capture process some typographical errors may occur.
- Please contact Sharon Hobrla, email@example.com if you notice any errors which make this publication unusable.
- We recommend that you also print this page and attach it to the printout of the article, to retain the full citation information.
- This article was written and prepared by U.S. Government employees on official time, and is therefore in the public domain.
CitationSumner, David M.; Nicholson, Robert S.; Clark, Kenneth L. 2012. Measurement and simulation of evapotranspiration at a wetland site in the New Jersey Pinelands. USGS Scientific Investigations Report: 2012-5118. U.S. Department of the Interior. U.S. Geological Survey; 30 p.
- Effects of invasive insects and fire on energy exchange and evapotranspiration in the New Jersey pine lands
- Comparison of hydrology of two Atlantic Coastal Plain forests
- Energy and water balance of two contrasting loblolly pine plantations on the lower coastal plain of North Carolina, USA
XML: View XML