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PREFACE <br />Our job was supposed to be simple: Run the river, measure the flows, and estimate how much <br />flow would be needed to maintain the river's recreation experiences. But which flows, and which <br />experiences? We were four days into a seven day trip on Alaska's Gulkana River, and already we had <br />encountered -- endured in some cases — a full range of both. <br />Starting out in two overladen rafts and <br />a snap - together vinyl canoe on a bright <br />afternoon, we had learned it was possible to <br />float down the narrow but relatively deep <br />headwaters on a measured 26 cfs, while R <br />even three times that flow didn't allow us — <br />or the spawning king salmon — passage ` <br />through the riffles that appeared <br />downstream as the channel widened. <br />Making little progress pulling our rafts over <br />the bars, we cheered the light rain that A..w► <br />began to fall on our second day, a rain that <br />turned into a full scale downpour by that <br />afternoon. Unfortunately, the added flow "Boat dragging" on Alas 's Middle Fork of the Gulkana <br />did little to help our situation: the river had River at low flows. <br />picked up gradient and now presented a <br />boulder- choked channel. The river was <br />running close to 300 cfs and had plenty of depth -- just enough to fill your hip waders — but only the <br />canoe was managing to find a clear route through. By the time we hit the upper river's only rapid, a <br />short zig -zag gorge, the river was roaring but still couldn't provide a navigable run. We ended up <br />lining the rapid. <br />The rain didn't stop that day, nor for two more, and the river reached its bankfull stage sometime <br />after we had slogged through 35 miles of meandering flat water but before we got to the usually <br />manageable Canyon Rapids, a quarter -mile Class III -IV run. <br />We had almost been flooded out of one camp, and watched <br />in dismay as cutbank after cutbank sloughed off into the <br />river, turning the once clear green water into a muddy soup <br />that killed the fabled salmon and grayling fishing — at least <br />for us. In the long run, of course, the erosion and the soon - <br />to -come deposition were simply part of the dynamic system <br />that nurtures good fish runs, not to mention creating <br />expansive camping beaches for which the river is also <br />known. But as we scouted the suddenly challenging <br />whitewater of the Canyon, looking for a safe route around a <br />huge hole at the end of the run -- and not even thinking <br />about trying to measure the raging flows — we began to <br />fully understand the potential complexity of the instream <br />flow issue. <br />Conceptually simple, determining flow needs for <br />recreation can often be practically challenging. The <br />complexity begins with measuring flows, but extends very <br />quickly to the relationship between different flows and the <br />conditions that create a high quality trip. As an early study <br />of its kind, we could have predicted the Gulkana would <br />have much to teach us. But in the five years and dozen or <br />so studies we have collectively worked on since, there is still <br />much to learn. <br />Canyon Rapids at higher flows. <br />