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re: NYT: Editorial on Climate Change and Louisiana

Posted on 3/5/18 at 1:34 pm to
Posted by Midtiger farm
Member since Nov 2014
5047 posts
Posted on 3/5/18 at 1:34 pm to
Tear down the levees and see if in climate change can stop the Miss from creating land.

It sure hasn't stooped the Atchafalya from depositing a bunch of sediment at its mouth and creating more land.
Posted by kingbob
Sorrento, LA
Member since Nov 2010
67196 posts
Posted on 3/5/18 at 2:01 pm to
quote:

It sure hasn't stooped the Atchafalya from depositing a bunch of sediment at its mouth and creating more land.



This. What's happened at Wax Lake over the past 30 years is a clear proof of concept.

The other problem with the Mississippi River is the fact that it doesn't carry near the amount of sediment it did 100 years ago. Upriver locks and dams on tributaries have resulted in it carrying possibly as little as 10% of the sediment it used to.

Even if we completely unleashed the river, it might not carry enough sediment to save all that has been lost and is being threatened with imminent loss, but no one can deny it wouldn't help tremendously, just at what cost. What costs are we willing to pay in terms of flooding of populated areas and navigation issues for shipping and industry relying on the river.
Posted by NYNolaguy1
Member since May 2011
20919 posts
Posted on 3/5/18 at 2:09 pm to
quote:

It sure hasn't stooped the Atchafalya from depositing a bunch of sediment at its mouth and creating more land.


The river gradient from ORCS to the Wax Outlet is twice that from Red River Landing to Head of Passes.

In other words, its a hell of a lot steeper, and will continue to get steeper until the river eventually changes course. A lot of the new soil in the Wax Outlet has come from the former river bottom.

Meanwhile, the Miss River has the opposite problem, leading to sometimes unpredictable flooding like in 2011.
Posted by LSUgusto
Member since May 2005
19224 posts
Posted on 3/5/18 at 9:26 pm to
quote:

It sure hasn't stooped the Atchafalya from depositing a bunch of sediment at its mouth and creating more land.
I've read reports that say the Mississippi un-leveed wouldn't create land like it used to because it doesn't carry nearly the amount of silt it used to. But, as said, if the Atchafalaya is building land, why wouldn't the Mississippi?

Here's the other thing. You know the dead zone in the Gulf? It's caused by fertilizers from the river concentrating in the gulf and creating algae blooms.

Now, my question is, what would happen to marshes if they were flooded with these fertilized waters? Wouldn't accelerated vegetation growth perhaps overcompensate for the absence of silt coming downriver? I love the concept of these fertilized waters nourishing marsh grass growth and, in the process, reducing the dead zone problem in the Gulf.

Never seen any science discuss this, though.
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