The Endless Grind

Still plugging away. One paper done and one to go. Then to Frankenstein the whole thing together into a thesis!

So Long Without An Update

So Ambusten Creek is a tricky one.

Looking at this photo, would you ever have guessed that:

a) effective discharge or greater occurs 32 days per year?
b) bankfull discharge occurs less than one day per 100 years?

Hard at work now. No pretty pictures.

I Wonder What Flow Moves This?

In Norrish Creek. Think it ever moves?

Seasonal Variation

So if a stream fines after a big flood and then coarsens again over time as it winnows... what is the appropriate stage to use to represent it for effective discharge calculations?

The fine stage may represent the Qe in terms of maximum sediment transported, but the coarse stage undoubtedly represents the channel forming discharge as it is this being moved that will reshape the channel itself instead of moving sediment through it.

Photo: channel of Ambusten Creek - large immobile clasts not well represented in the sediment photos.

Playing Catchup

Reworking and rethinking a lot of this stuff in an attempt to get the papers written and out the door. Nash (1994) paper is very useful on second read-through as here is someone who has considered many of the same issues as I am confronting albeit with simpler computational tools from 15 years ago.