Evapotranspiration and land cover transitions: long‐term watershed response in recovering forested ecosystems

Abstract

Changes of the land surface affect the water balance components over seasonal, annual and decadal time scales. This study explored the role of vegetation cover transitions on evapotranspiration in forested watersheds of the North American West. We applied empirical time‐recovery functions describing the impact of forest removal and subsequent regrowth on actual evapotranspiration (AET) or runoff. A generalized function (K‐curve) was adapted to the North American West and tested using three different datasets of observed or estimated AET in forest chronosequences: AET from flux towers equipped with eddy covariance sensors, AET estimated from the water balance in experimental paired watersheds and in a set of gauged watersheds with considerable forest cover history dating back to the 18th century. AET from the first two datasets showed a behaviour similar to the K‐curve, although the timing and the magnitude differed substantially. To reconstruct long‐term changes in AET for the gauged watersheds, we applied a transfer function approach linking the K‐curve and the reconstructed forest cover history at the watershed scale. In several watersheds, correlation coefficients between the reconstructed AET changes and the annual water balances suggest that changes in time were driven by the land cover transitions. In watersheds with low correlations, disturbance activities peaked before the 20th century, and the effects of vegetation have phased out in the period of streamflow observations. The findings of this paper suggest that trends in the observed water balance in forested watersheds can be associated to land cover disturbances well before the start of hydro‐climatic observations. Copyright © 2011 John Wiley & Sons, Ltd.

The potential of observed soil moisture dynamics for predicting summer evapotranspiration in a successional chronosequence

“…A second water balance model (Model II, Eq. 2) therefore added an interception threshold value of 0.5 mm/h (Gash, 1979). The water vapor exchange from the canopy to the atmosphere is assumed to be 0.5 mm/h when P (t)≥0.5 mm/h and I(t) = P (t) when P (t)<0.5 mm/h.…”

“…Jassal et al (2009) found that in a Douglas fir succession initially reduced evapotranspiration (AET) recovered 12 years after disturbance. Brena Naranjo et al (2011) detected a recovery effect on AET in forest chronosequences and on the water balance in various watersheds in the North American West. Although changes in AET exhibited a different timing, a gradual recovery was common for at least 60 years after disturbance.…”

Sensitivity of a data-driven soil water balance model to estimate summer evapotranspiration along a forest chronosequence

“…Jassal et al (2009) found that in a Douglas fir succession initially reduced actual evapotranspiration (AET) recovered 12 yr after disturbance. Breña Naranjo et al (2011) detected a recovery effect on AET in forest chronosequences and on the water balance in various watersheds in the North American West. Although changes in AET exhibited a different timing, a gradual recovery was common for at least 60 yr after disturbance.…”