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. 2013 Dec 31;8(12):e85586. doi: 10.1371/journal.pone.0085586

Table 2. Parameter estimates from GLM models of fish ladder passage times in relation to ΔT.

Parameter estimate
Dam Run n Hour Hour2 °C ΔT
Ice Harbor Spring Chinook 1,026 -0.192** 0.010** 0.053* -0.080
Summer Chinook 215 -0.067 0.004 0.119* 0.355**
Fall Chinook 218 -0.170* 0.009** 0.061 0.557*
Steelhead 1,352 -0.239** 0.010** -0.001 0.309**
Lower Monumental Spring Chinook 572 -0.280** 0.012** 0.008 -0.039
Summer Chinook 184 -0.064 0.003 0.125** 0.308**
Fall Chinook 115 -0.118 0.007 -0.044 0.166
Steelhead 987 -0.159** 0.007** 0.035* 0.124*
Little Goose Spring Chinook 880 -0.040 0.002 0.045* -0.122
Summer Chinook 174 -0.082 0.003 0.179** 0.310
Fall Chinook 142 -0.098 0.006 0.218* 0.792
Steelhead 1,048 -0.114** 0.005** 0.066** 0.442**
Lower Granite Spring Chinook 635 -0.130** 0.007** 0.022 0.047
Summer Chinook 174 -0.077 0.003 0.159** 0.207*
Fall Chinook 122 -0.141 0.007* -0.112* 0.797**
Steelhead 911 -0.115** 0.007** -0.001 0.286**

Passage times were calculated for radio-tagged Chinook salmon and steelhead at Snake River dams in 2000-2003. Independent variables included migration year (not uniquely estimable), hour of first detection at a base-of-ladder antenna (quadratic effect), water temperature (°C) at the ladder base at the time of first detection, and ΔT (the °C temperature difference between top-of-ladder and base-of-ladder sites). Positive ΔT parameter estimates indicate slower fish passage as ΔT increases.

* P ≤ 0.05; ** P ≤ 0.005