scholarly journals Forest thinning may increase water yield from the Sierra Nevada

2015 ◽  
Vol 69 (1) ◽  
pp. 10-11 ◽  
Author(s):  
Jim Downing
2005 ◽  
Vol 25 (1) ◽  
pp. 57-66 ◽  
Author(s):  
J. Tang ◽  
Y. Qi ◽  
M. Xu ◽  
L. Misson ◽  
A. H. Goldstein

2021 ◽  
Vol 3 ◽  
Author(s):  
William D. Burke ◽  
Christina Tague ◽  
Maureen C. Kennedy ◽  
Max A. Moritz

Fuel treatments are a key forest management practice used to reduce fire severity, increase water yield, and mitigate drought vulnerability. Climate change exacerbates the need for fuel treatments, with larger and more frequent wildfires, increasing water demand, and more severe drought. The effects of fuel treatments can be inconsistent and uncertain and can be altered by a variety of factors including the type of treatment, the biophysical features of the landscape, and climate. Variation in fuel treatment effects can occur even within forest stands and small watershed management units. Quantifying the likely magnitude of variation in treatment effects and identifying the dominant controls on those effects is needed to support fuel treatment planning directed at achieving specific fire, water, and forest health goals. This research aims to quantify and better understand how local differences in treatment, landscape features, and climate alter those fuel treatment effects. We address these questions using a mechanistic coupled ecohydrologic model—the Regional Hydro-Ecological Simulation System (RHESSys). We ran 13,500 scenarios covering a range of fuel treatment, biophysical, and climate conditions, for the Southern Sierra Nevada of California. Across fuel treatment type, biophysical, and climate parameters, we find nontrivial variation in fuel treatment effects on stand carbon, net primary productivity, evapotranspiration, and fire-related canopy structure variables. Response variable estimates range substantially, from increases (1–48%) to decreases (−13 to −175%) compared to untreated scenarios. The relative importance of parameters differs by response variable; however, fuel treatment method and intensity, plant accessible water storage capacity (PAWSC), and vegetation type consistently demonstrate a large influence across response variables. These parameters interact to produce non-linear effects. Results show that projections of fuel treatment effects based on singular mean parameter values (such as mean PAWSC) provide a limited picture of potential responses. Our findings emphasize the need for a more complete perspective when assessing expected fuel treatment outcomes, both in their effects and in the interacting biophysical and climatic parameters that drive them. This research also serves as a demonstration of methodology to assess the likely variation in potential effects of fuel treatments for a given planning unit.


2017 ◽  
Vol 53 (7) ◽  
pp. 5364-5381 ◽  
Author(s):  
P. C. Saksa ◽  
M. H. Conklin ◽  
J. J. Battles ◽  
C. L. Tague ◽  
R. C. Bales

Water ◽  
2019 ◽  
Vol 11 (1) ◽  
pp. 94 ◽  
Author(s):  
Natalia Hoyos ◽  
Alexander Correa-Metrio ◽  
Steven M. Jepsen ◽  
Beverley Wemple ◽  
Santiago Valencia ◽  
...  

Droughts constitute natural hazards that affect water supply for ecosystems and human livelihoods. In 2013–2016, the Caribbean experienced the worst drought since the 1950s, and climate projections for the southern Caribbean predict less rainfall by the end of the 21st century. We assessed streamflow response to drought for a watershed in the Colombian Caribbean by analyzing the effects of drought length and land cover on streamflow recovery. We generated a calibrated SWAT model and created annual and monthly drought scenarios from rainfall records. We used our model to predict water yield for selected land covers (wet forest, shade coffee, shrub, and dry forest) under drought conditions. Annual scenarios resulted in water yield reductions of ~15 mm month−1 (wet forest, coffee, and shrub) and 5 mm month−1 (dry forest) for the first month after a two-year drought. Maximum water yield reductions for monthly scenarios occurred after a 10-month drought and were ~100 mm month−1 (wet forest, coffee, and shrub) and 20 mm month−1 (dry forest). Streamflow recovered within nine months (annual scenarios), and two to eight months (monthly scenarios) after drought termination. Drought response seems to be conditioned by climatic factors (rainfall seasonality and spatial variability) and catchment properties.


2016 ◽  
Vol 30 (14) ◽  
pp. 5039-5049 ◽  
Author(s):  
Ferhat Gökbulak ◽  
Kamil Şengönül ◽  
Yusuf Serengil ◽  
Süleyman Özhan ◽  
İbrahim Yurtseven ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document