unclej, thank you for your assurance that my concerns will be alleviated by the presentations at the meeting. I would like to attend but meanwhile there are some more questions that need to be asked and points to raise.
There are some very high weirs between Bubble Springs and Conksbury bridge. Are you saying that opening the sluices in these allows Trout to migrate through this section? Is this done and has it been done every year, since the weirs were built? Are those deep pools drained completely to produce a natural river flow? Have any studies been carried out to assess how far Trout migrate along the Lathkill? Or even Derwent/Wye/Lathkill? My, educated, guess is that those weirs are a significant if not total barrier to fish migration. Could you state how dependent the Lathkill fishery has been, since the 1850s, on stocking and what proportion of the fish stocks are produced by natural spawning? I am curious too about the "traditional spawning beds" above and below Bateman's House, where the river is entirely man-made. This is not a personal attack but a genuine interest in how high the Trout ascended the river and what conditions they found, bearing in mind that nothing below a point well above Carters Mill is natural.
If the river was to run on the surface from Lathkill Head Cave down to Bubble Springs - and I cannot believe that it ever did "perennially" in historical times, then significant cave systems would be permanently flooded. That 3D mapping would be very useful together with a review of known hydrology.
And back to basics:
To restore 1960s Magpie Sough water levels would mean that the sough would have to be blocked producing a 30'-40' head where it meets the Wye.
To restore 1880s levels the sough would have to be blocked completely at a point which would ensure that all water captured by it was trapped. The ideas of "control" and "access" do not fit in with these scenarios. All the consequences of blocking the sough can be estimated but some, I imagine, only guessed at.
As I have said and others above, the sough being open is one factor and obviously others play a part. In fact, the only consistent factor is the sough being open and the changes that are occurring must be due to other influences.