Smike wrote:
Mike wrote:
Very true Smike. I was waiting for someone to say what you did about discharges to control the upstream progression of the salt line. Forgetting sea level rise for a moment, droughts and the resulting upstream movement of the salt line would not always coincide with ideal timing for coldwater releases into the Lehigh. We have seen low flows at various times of the year over the past decades, even in winter and spring, but they seem to most often occur in mid-summer or late summer through fall. They can also occur for extended periods with no crystal ball for when the end will occur, so I don’t see release of extra water, if it gets that far, designated for salt line control being frittered away for trout management. I would only expect release of such waters (those for salt line control) to be coincidental to trout management, perhaps beneficial at times, but at others not so much.
Absolutely, flow control for salt line issues can at times be diametrically opposed to supporting wild trout. This is why incorporating studying the benefits of building a new selective level release tower is so important. If we can’t be assured of flow levels, at the very least we can be assured it can be cold when used. The where they pull water from (level wise from the lake) will have zero impact on ability to when and how much they need downstream. So it would be an improvement that would not impact water use for the DRBC.
For the study we are working on trying to figure out how we can better survey the wild trout fishery in existence now. Whether that is working with PFAB or getting partnership help from the groups like TU or others. At times there are certain locations on the river which could very well achieve the threshold for Class A, or B biomass. It’s hard to survey given the size, and the fact that brown trout move a lot in and out of the river. Bottom line is having solid data showing this would be huge asset to pushing for flow plans that would help to protect the fishery.