2013
DOI: 10.3133/ofr20131133
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Salton Sea ecosystem monitoring and assessment plan

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Cited by 7 publications
(3 citation statements)
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“…Because disamenity damages are a function of distance to the Sea's edge, we measure the distance of single‐family residences from the Sea using tax assessor parcel maps and contour maps delineating the Sea's edge based on its elevation. To avoid the complexity of multiple habitat types and challenges associated with speculating on their relative abundance and function in the future, we follow previous work in estimating wetland acreage and use the sum of a 25‐m buffer around the Sea's edge and a 1‐km buffer inside the Sea's edge (Case et al., 2013; Cohen, 2014).…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…Because disamenity damages are a function of distance to the Sea's edge, we measure the distance of single‐family residences from the Sea using tax assessor parcel maps and contour maps delineating the Sea's edge based on its elevation. To avoid the complexity of multiple habitat types and challenges associated with speculating on their relative abundance and function in the future, we follow previous work in estimating wetland acreage and use the sum of a 25‐m buffer around the Sea's edge and a 1‐km buffer inside the Sea's edge (Case et al., 2013; Cohen, 2014).…”
Section: Methodsmentioning
confidence: 99%
“…To calculate changes in wetland habitat area, we again use contour maps of the bathymetry of the Sea to locate the Sea's edge and iteratively calculate wetland acreage. We follow previous work and sum the acreage of a 25-m buffer around the Sea's edge and a 1-km buffer inside the Sea's edge (Case et al, 2013;Cohen, 2014). Wetland acreage can then be calculated for each year according to Sea elevations under baseline and water delivery reduction scenarios.…”
Section: Transformationsmentioning
confidence: 99%
“…The retreating shoreline leaves behind exposed playa which has the potential to generate dust that is easily mobilized by strong winds in the area from the vast salt flats (King et al 2011) (Figure 2). A model from the US Geological Survey estimated that the decline of 3 feet in elevation will expose over 11,000 acres of saline lakebed sediment (Case et al 2013). A separate study predicts that fugitive wind-blown dust could increase by up to 40 to 80 tons per day after water inflows are reduced in 2018 and the lake will shrink by about 100 square miles by 2030 (Cohen and Hyun 2006).…”
Section: A Crisis In Slow Motion: Disappearing Seas and Air Pollutionmentioning
confidence: 99%