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The same is true of PO4 and chlorophyll a at Winchester Creek (riverine/freshwater zone). South Slough chlorophyll a concentrations peak in late-spring and summer (Figure 11)(SWMP 2012). The concentrations are generally below the Oregon estuarine water quality criteria standard (15 µg/L) except for a few seasonal peaks at Valino Island and Winchester Creek in 2006 and the Boathouse station in 2007. In this document, we summarize available information on nitrogen, phosphorus, silica, and chlorophyll a concentrations (and their various forms) in the Coos estuary (Figure 1). The forms in which nutrients are found in the Coos estuary are listed in Table 1.
As river discharge rates progressively decrease from winter through summer, the residence time for diatoms lengthens and increases their effect on silica concentrations. ODEQ’s 2007 PO4 Isthmus Slough data follow the opposite seasonal pattern to nitrogen, with peak PO4 concentrations mostly occurring in the dry months and lower concentrations during the rainy season (Figure 18, Table 4). Nutrients in South Slough’s upper watershed are well correlated with precipitation (Cornu et al. 2012). Concentrations of phosphate, ammonium, and silica increased during periods of low rainfall, and declined during the rainy season.
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Historic estimates suggest that Oregon supported approximately 9,000 bears in the 1930s (Bailey 1936). By the 1980s, the estimated size of the Oregon bear population had approximately doubled to reach 18,000 bears (ODFW 1987). This trend has continued in recent decades with the bear population reaching 25,000 in the 1990s and remaining between 25-35,000 statewide in the 2000s. Due to the limitations of survey methods, bear population estimates are not available for individual GMUs (see Chapter Summary for data limitations). Herd composition data for both the Tioga and Sixes unit show that bull ratios have met their management objectives for over 20 years and suggest that local populations are likely increasing (Figure 6)(ODFW 2015b).
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