2013
DOI: 10.3133/ofr20131081
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Final report for sea-level rise response modeling for San Francisco Bay estuary tidal marshes

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Cited by 28 publications
(48 citation statements)
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“…http://www.ecologyandsociety.org/vol21/iss1/art19/ Downscaling of climate projections has resulted in growing concern that sea-level rise may influence California rail survival and habitat suitability (U.S. Fish and Wildlife Service 2013) through the reduction of habitat available as refuge cover for salt marsh-obligate species (Flick et al 2003, NOAA 2009. Approximately 90% of marshland in SF Bay has been lost or converted to other land uses, causing reduction and fragmentation of remaining marshland (San Francisco Bay Area Wetlands Ecosystem Goals Project 1999), and SF Bay may lose the remaining high-marsh habitat that serves as refuge during extreme tides over the next century (Stralberg et al 2011, Takekawa et al 2013), unless sedimentation rates can increase to offset sea-level rise and thereby minimize loss of tidal refugia. Detailed analysis of California rail call-count surveys, habitats, and landscape conditions has increased our understanding of how marsh structure, surrounding landscapes, and restored marshland may influence California rail populations ).…”
Section: Discussionmentioning
confidence: 99%
“…http://www.ecologyandsociety.org/vol21/iss1/art19/ Downscaling of climate projections has resulted in growing concern that sea-level rise may influence California rail survival and habitat suitability (U.S. Fish and Wildlife Service 2013) through the reduction of habitat available as refuge cover for salt marsh-obligate species (Flick et al 2003, NOAA 2009. Approximately 90% of marshland in SF Bay has been lost or converted to other land uses, causing reduction and fragmentation of remaining marshland (San Francisco Bay Area Wetlands Ecosystem Goals Project 1999), and SF Bay may lose the remaining high-marsh habitat that serves as refuge during extreme tides over the next century (Stralberg et al 2011, Takekawa et al 2013), unless sedimentation rates can increase to offset sea-level rise and thereby minimize loss of tidal refugia. Detailed analysis of California rail call-count surveys, habitats, and landscape conditions has increased our understanding of how marsh structure, surrounding landscapes, and restored marshland may influence California rail populations ).…”
Section: Discussionmentioning
confidence: 99%
“…Loss of tidal refugia could be minimized if sedimentation rates can offset sea level rise. However, under all projected climate scenarios, San Francisco Bay is expected to lose high marsh habitat that serves as refuge during extreme tides (Stralberg et al 2011;Takekawa et al 2013).…”
Section: Discussionmentioning
confidence: 99%
“…The remaining natural habitats in San Francisco Bay may not currently provide high quality habitat for clapper rails, and nearly 96 % may convert to mudflat under projected sea-level rise scenarios (Cayan et al 2008;Takekawa et al 2013). Short vegetation, or that which occurs at the lowest elevations of the marsh, may provide suitable habitat for the majority of the year but be unsuitable during critical high tide periods.…”
Section: Discussionmentioning
confidence: 99%
“…LIRA's elevational range across Sanchez, Coyote, and Seal (1.77 to 2.51 m NAVD88, or 0.75 to 1.49 m above MSL) corresponds with the high marsh (0.7 to 1.0 m MSL) and upland transition zone (> 1.0 m MSL) in estuary tidal marshes (Takekawa et al 2012 LIRA was found across a soil salinity gradient that decreased from the high marsh into the transition zone, a salinity pattern consistent with findings in the estuary (Mahall and Park 1976;St. Omer 2004), at Pt.…”
Section: Habitats Susceptible To Invasionmentioning
confidence: 99%
“…We displayed LIRA's vertical range (in NAVD88) as boxplots relative to tidal datums [mean high water (MHW) and mean higher high water (MHHW)] and 100-year flood elevations (USACE 1984) using the R statistical package. Tidal datums have been used to describe the distribution of marsh vegetation in the estuary (Hinde 1954;Atwater et al 1979;Takekawa et al 2012), and the 100-year flood elevation shows the approximate upper reach of tidal inundation. We obtained tidal datum values referenced to mean lower low water (MLLW) from 16 surrounding National Ocean Service (NOS) water level stations from the http://www.noaa.gov website (NOAA CO-OPS 2010), and point locations of 100-year flood elevation data (in NAVD88) from the Pacific Institute website (PI 2011 (Foxgrover et al 2005).…”
Section: Elevational Range Of Lira Relative To Tidesmentioning
confidence: 99%