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Summer Releases Back in the Old Days

JOE.T

Dry Flies Only
Here are 5 links to the USGS Stilesville Guage.

I ran 1995-1999 to give everyone an idea of what we use to have in the "Summer" -June ,July, and August for Releases on the WB.

You can see that we had a lot more water coming down the WB back than.It had nothing to do with a fisheries plan, it was all about keeping Montaque at 1750.

Than years later we started with Rio dumping water down the Mongaup and Wallenpaupack dumping water down the Lackawaxen to take care of Montaque

The reservoir would often get well below 50% capacity by September but it always filled back up, and NYC always had water to sell.

The Point is now with down river resources satisfying Montaque there is more than enough water to add to the fishery.For now will call that number X.

If you see anything above 1500 cfs that meant that we had a spill from a lot of rain.You can't debate facts like this.


1995 - USGS Current Conditions for USGS 01425000 WEST BR DELAWARE RIVER AT STILESVILLE NY

1996 - USGS Current Conditions for USGS 01425000 WEST BR DELAWARE RIVER AT STILESVILLE NY

1997 - USGS Current Conditions for USGS 01425000 WEST BR DELAWARE RIVER AT STILESVILLE NY

1998 - USGS Current Conditions for USGS 01425000 WEST BR DELAWARE RIVER AT STILESVILLE NY

1999 - USGS Current Conditions for USGS 01425000 WEST BR DELAWARE RIVER AT STILESVILLE NY
 
Hi Joe,

Of course we can debate the data.

Check out the attached graph for one of the years you chose to show.

If there were any trout to start the summer after 40 cfs for most of the month of May, there probably were not many left when the release dropped to less than 30 cfs for most of October and November.

By the way, Rio and Wallenpaupack were in operation through the 1990's. One thing that tends to happen is both of those reservoirs run out of available water during the summer and stop producing power. That is when the Directed releases from Cannonsville really get cranking.

The other complete year profiles have similar killer low flows.

Checkout last years flow profile. The other attached graph. Really nice until the end of the year when things dried up, but only down to 100 cfs. 100 cfs, is not good, certainly, but a bunch better than 45 or 30 cfs.

Jim
 

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Hi Joe,

Of course we can debate the data.

Check out the attached graph for one of the years you chose to show.

If there were any trout to start the summer after 40 cfs for most of the month of May, there probably were not many left when the release dropped to less than 30 cfs for most of October and November.

By the way, Rio and Wallenpaupack were in operation through the 1990's. One thing that tends to happen is both of those reservoirs run out of available water during the summer and stop producing power. That is when the Directed releases from Cannonsville really get cranking.

The other complete year profiles have similar killer low flows.

Checkout last years flow profile. The other attached graph. Really nice until the end of the year when things dried up, but only down to 100 cfs. 100 cfs, is not good, certainly, but a bunch better than 45 or 30 cfs.

Jim

Jim I don't know of any year that has been perfect or close to it for 12 months.

My point of the post was just summer releases.

If you compare the previous 5 years below to the 5 years I pulled from the late 90's it obvious to anyone that we had more water in the summer back than.

I know that the down river water sources have been around a long time, however it wasn't until 2005 when PPL was approved to be re-licensed by FERC that the releases down the Lackawaxen where used to satisfy Montaque ??

The crazy thing is you can't find the data on USGS, it's all been deleted prior to 2007, why would USGS delete or remove all data prior to 07 just for the Lackawaxen and Mongaup?

Check this out ! I mean you can't make this stuff up.

Lackawaxen prior to 07 - USGS Current Conditions for USGS 01432110 Lackawaxen River at Rowland, PA

Mongaup prior to 07 - USGS Current Conditions for USGS 01433500 MONGAUP RIVER NEAR MONGAUP NY

Looks like the MIB at work here.

Any ideas on why USGS would delete info on just those to site's ?


2010 - USGS Current Conditions for USGS 01425000 WEST BR DELAWARE RIVER AT STILESVILLE NY

2011 - USGS Current Conditions for USGS 01425000 WEST BR DELAWARE RIVER AT STILESVILLE NY

2012 - USGS Current Conditions for USGS 01425000 WEST BR DELAWARE RIVER AT STILESVILLE NY

2013 - USGS Current Conditions for USGS 01425000 WEST BR DELAWARE RIVER AT STILESVILLE NY


2014 - USGS Current Conditions for USGS 01425000 WEST BR DELAWARE RIVER AT STILESVILLE NY


I sense a disturbance in the force.Ah yes it was Darth Vader.
 
The crazy thing is you can't find the data on USGS, it's all been deleted prior to 2007, why would USGS delete or remove all data prior to 07 just for the Lackawaxen and Mongaup?

Check this out ! I mean you can't make this stuff up.

Lackawaxen prior to 07 -


-----

Nope.

Rosemary Woods.


rosemary_woods.jpg
 
Hi Joe,

I think these two statements need some clarification:

If you compare the previous 5 years below to the 5 years I pulled from the late 90's it obvious to anyone that we had more water in the summer back than.

This is mostly due to random chance and different weather conditions than because of any sort of flow plan. IF you swapped plans for each five year period, the 1990's would be improved by the FFMP regime. There would be no low dips and the minimum flow would be 400 or 500 instead of the 325 that was in place in the 1990s. You are correct that the Montague releases would be a bit lower on the WB, but NOT for the reason that you give. They would be lower because under FFMP there is already more water coming down the system. More water on the WB as well as more on the EB and Neversink which would also count towards Montague. As a guess, if the Rivermaster needed 1000 cfs, there would already be 740 cfs of water coming down under FFMP, so call for water would be 260 cfs. Under the 1990's plan, there would be 325+95+53= 473 of flow from the plan and the rivermaster would need to call for an additional 527. So, Cannonsville releases would be 92 cfs less under FFMP because that 92 cfs would be made up by the larger EB and Neversink releases.

Also make sure to look at the scale of flow. The last 5 years under FFMP we were seldom under 400 cfs on the WB during the summer.

I know that the down river water sources have been around a long time, however it wasn't until 2005 when PPL was approved to be re-licensed by FERC that the releases down the Lackawaxen where used to satisfy Montaque ??

This is just not true. Lackawaxen power releases have counted towards the 1750 target, I think since their inception. Certainly since 1980.

jim
 
With so much data, you can make almost any case. That's what politicians do with polls.
 
OK... no one's happy with what we had or what we got... Here's the new flow plan....

250CFS Cannonsville release April 1 to May 15th (more if required to keep Hale at least 450 CFS and/or Hancock temp below peak of 65 degrees F).

From May 15 to June 15th, Cannonsville release of 350 CFS (more if required to keep Hale at least 450 CFS and/or Hancock below peak of 65 degrees).

June 15th to August 15th, Cannonsville release of 500 CFS (more if required to keep Hancock below peak of 65 degrees).

August 15th to Nov 15th - 250 CFS (more if required to keep Hale at 350 CFS and/or Hancock below 65 degree peak)

October 15th to December 1 end of year 200 CFS. Winter.. dunno.
 
Fred, I'm totally on board with your plan. It can't be that easy,can it? After reading the ffmp link you posted my brain damn near melted. Your plan sounds much easier. I would like to hear from ny why it can't happen. What is their science behind what they do?
 
Hi Joe,

I think these two statements need some clarification:

If you compare the previous 5 years below to the 5 years I pulled from the late 90's it obvious to anyone that we had more water in the summer back than.

This is mostly due to random chance and different weather conditions than because of any sort of flow plan. IF you swapped plans for each five year period, the 1990's would be improved by the FFMP regime. There would be no low dips and the minimum flow would be 400 or 500 instead of the 325 that was in place in the 1990s. You are correct that the Montague releases would be a bit lower on the WB, but NOT for the reason that you give. They would be lower because under FFMP there is already more water coming down the system. More water on the WB as well as more on the EB and Neversink which would also count towards Montague. As a guess, if the Rivermaster needed 1000 cfs, there would already be 740 cfs of water coming down under FFMP, so call for water would be 260 cfs. Under the 1990's plan, there would be 325+95+53= 473 of flow from the plan and the rivermaster would need to call for an additional 527. So, Cannonsville releases would be 92 cfs less under FFMP because that 92 cfs would be made up by the larger EB and Neversink releases.

Also make sure to look at the scale of flow. The last 5 years under FFMP we were seldom under 400 cfs on the WB during the summer.

I know that the down river water sources have been around a long time, however it wasn't until 2005 when PPL was approved to be re-licensed by FERC that the releases down the Lackawaxen where used to satisfy Montaque ??

This is just not true. Lackawaxen power releases have counted towards the 1750 target, I think since their inception. Certainly since 1980.

jim

if there is one benefit of the low water year of 2015- its that people are starting to dig into and learn the details of the FFMP. Many have declared war against NYC in the past based purely on the fact the fishing was poor- but had no idea why the flows were what they were. Now, people are trying to educate themselves and thats important.
In looking at the charts Joe T is posting for the 1990s and comparing that to current FFMP flows, the summer conditions prior to the FFMP are going to appear far better. They were. The issue here is whats better for the trout? Many fisherman fail to realize how fatal poor winter conditions can be to trout bc they aren't around at that time. Need proof?- Go fish the Ausable River in the adirondacks which has beautiful water all year, but is filled with stocked trout because anchor ice is so lethal there that they are unable to support a strong wild fish population. The FFMP is better than prior plans when it comes to producing conditions on THE TAILWATERS for trout to survive year round.
As I've said many times, the FFMP is not better for the main stem but everyone keeps ducking that argument and isn't addressing it. The main stem is undoubtedly worse off under the FFMP bc it assumes spring conditions will provide freestone flow and on dry years like this one assumes (or completely neglects) the main stem in the name of the OST ,the Cali drought , and climate uncertainty - which are reflected but untold in the non-transparent OST forecasting. The main is fishing as bad as it ever has- bugs are horrible and crowds are as bad as they have ever been because people/guides would rather float dead water than wade good water. Beyond that flows and river conditions have been totally different on the main. U rarely saw the main under 2000 cfs during the 1990s, early 2000s. Now, the main in the 3000s is streamer time and big water for kelly gallop bros trying to break instagram. The FFMP is worse for the main stem and better for the tailwaters. End of Story. This raises a new debate though on what is more important, the tailwaters or the main. The tailwaters were always the crown jewel but crowds and the love of drift boats brought the upper main and buck to long stretch into the lead in terms of angler support. The wb because such a shit show that people decided to go down river in the name of adventure and delaware veteran status. So- lets not forget that in the 1990s the majority of support was for keeping WEST BRANCH conditions at their best because most people preferred fishing that river. 15 years later we have a pro main stem crowd because those same people got pissed the wb got crowded and started casting blind Iso's and smoking weed at dark eddy when the po po and park service wasn't going to snag them (unless u were riding with moose). TR will attest to most of this I'm sure.
 
if there is one benefit of the low water year of 2015- its that people are starting to dig into and learn the details of the FFMP...
[MAJORITY of text snipped due to Park Service surveillance. Drones overhead.] ...15 years later we have a pro main stem crowd because those same people got pissed the wb got crowded and started casting blind Iso's and smoking weed at dark eddy when the po po and park service wasn't going to snag them (unless u were riding with moose). TR will attest to most of this I'm sure.


=============

MOOSE? Ol' Roger?

Now, that brings back memories.

Good synopsis.

JC, go straight to the head of the class.

This guy knows his shit. First, he wins One Bug 2015 running away from the crowd and now a nice well rounded report about the Main Stem vs. the West Branch.

Report Card: A-

You get the minus because you forgot to mention Mr. Lee Kwon Doo of Flushing with a burgeoning tilapia venture on Big Island south of Callicoon on the Main Stem about four years ago where they dug eight pits without any NYS DEC mining permits and strung wire across the pits so eagles and other birds wouldn't eat the fish much to USF&W dismay.

But all in all - a nice recap.

Bring me the stack of bibles.

Tight lines.
 
You get the minus because you forgot to mention Mr. Lee Kwon Doo of Flushing with a burgeoning tilapia venture on Big Island south of Callicoon on the Main Stem about four years ago where they dug eight pits without any NYS DEC mining permits and strung wire across the pits so eagles and other birds wouldn't eat the fish much to USF&W dismay.

Holy shit did this actually happen? Incredible.

JC how could you leave this part out?

Sounds like Mr. Koo was an entrepreneurial visionary way ahead of his time. In a few years when the climate change induced food wars begin in earnest, the entire main stem will be utilized as a tilapia and carp farm providing valuable nutrition for the survivors of the next four superstorms to hit Manhattan, who will be living in tipis that moosekid's hipster army will build in central park and drinking Beetle (C) brand desalinated water out of sheepshead bay. I digress.

For those of us like cdun who get our boots wet like real men, this season has been a godsend. no banana boats and stinktoons lousing up my favorite spots and putting the fish down.:)

Would be nice to be able to catch fish below lordville though...
 
Hi Fly,

I am interested in why you think FFMP is worse for the mainstem. Could you elaborate a bit.

A dry May is going to bad under most plans. I am just not sure how FFMP is worse in a dry year. The releases in May under FFMP are more than any other plan. Certainly not as much as everyone wants, but still better.

Thanks,

Jim
 
Jim,

The FFMP has been tough on the main IMO for several reasons, some of which are not directly flow related but nonetheless have had direct negative consequences on the main. First, the low FFMP spring time flow requirements in an attempt to conserve water for summer flows have really condensed the season on the main because we are seeing warmer springs. Unless the system is chock full of water and a 1500 release/spillage occurs, the wb is going to run under 300 cfs in april and may. This causes the main to rely heavily on freestone flow from the bkill/ebranch and even on a decent water year leaves the main in that 1000-1500 cfs range most springs. A few days in the 80s which is normal for spring now and the main starts creeping up to upper 60s by early/mid may. These early season warmups have really hurt the hatch activity on the main and you see the hatches accelerate and few bugs coming off by late may. This year proves that as have the past few. The bug life on the mainstem is the worst I've ever seen in my time fishing the system.
The common sub 300 cfs springtime flows on the wb have also caused a dramatic increase in pressure on the mainstem because the wb is not floatable or barely floatable most springs. The upper main to buckingham has become a joke the past 5 years, which admittedly is in part due to just an increase in boats in general, but also in part bc the west branch is too low to float for much of the early spring unless we have 100% capacity/spillage. The fish are getting absolutely pounded on the upper main to the point the fish have mouth's that look like the wb no kill fish. Many Guides are going where the water is though and the closest float to town- to shehawken to buck it is.
Also, the summertime flows on the wb are steady under the FFMP, but overall lower most days during the summer months under the FFMP. The main used to actually benefit from the yo yo flows and 750cfs+ flows on the wb during the summer prior to the FFMP and the main would stay cool/have hatches for much of the late spring/early summer and sometimes even late summer. Now, with the 400 release on the wb for much of the summer, the main is consistently low, upper 60s/70s for the whole summer and few hatches because the water is too warm. Daytime summer sulphers are a non-existent thing on the main and I remember hitting them along with cahils for much of the summer and fog coming off the main in july from cool water temps. Yes, sometimes the main would get very low when the yo yo flows caused a sudden drop, but this was usually short lived and the majority of the summer was higher releases out of the wb and better fishing down on the main for a longer portion of the season.

Again- I think the FFMP is the best option we have seen for the wb. It keeps the river in better shape for the entire season(including winter) than past plans. My point is that whats good for wb under the FFMP is not good for the main.The main doesnt have winter flow issues and only runs into issues from may-early sept. Therefore, the wb could be managed like garbage for 9 months of the year and the main would still thrive so long as water was let out at over 500 cfs for most of the Mid May-Early Sept window.Under the ffmp 400 cfs out of the dam for most of the summer(unless we have montague releases like last year)keeps the wb in great shape all summer and doesnt stress the fish with up and down flows in a matter of hours, but keeps the main fairly warm and near 70 just a few pools down from the junction since there will be warm and low flows coming in from the eb just about every summer. The low and consistently low flows for april/may (and this year june) also leave the main susceptible to warmer flows that do not let up for any significant period in a warm spring like this year.
 
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Jim,

The FFMP has been tough on the main IMO for several reasons, some of which are not directly flow related but nonetheless have had direct negative consequences on the main. First, the low FFMP spring time flow requirements in an attempt to conserve water for summer flows have really condensed the season on the main because we are seeing warmer springs. Unless the system is chock full of water and a 1500 release/spillage occurs, the wb is going to run under 300 cfs in april and may. This causes the main to rely heavily on freestone flow from the bkill/ebranch and even on a decent water year leaves the main in that 1000-1500 cfs range most springs. A few days in the 80s which is normal for spring now and the main starts creeping up to upper 60s by early/mid may. These early season warmups have really hurt the hatch activity on the main and you see the hatches accelerate and few bugs coming off by late may. This year proves that as have the past few. The bug life on the mainstem is the worst I've ever seen in my time fishing the system.
The common sub 300 cfs springtime flows on the wb have also caused a dramatic increase in pressure on the mainstem because the wb is not floatable or barely floatable most springs. The upper main to buckingham has become a joke the past 5 years, which admittedly is in part due to just an increase in boats in general, but also in part bc the west branch is too low to float for much of the early spring unless we have 100% capacity/spillage. The fish are getting absolutely pounded on the upper main to the point the fish have mouth's that look like the wb no kill fish. Many Guides are going where the water is though and the closest float to town- to shehawken to buck it is.
Also, the summertime flows on the wb are steady under the FFMP, but overall lower most days during the summer months under the FFMP. The main used to actually benefit from the yo yo flows and 750cfs+ flows on the wb during the summer prior to the FFMP and the main would stay cool/have hatches for much of the late spring/early summer and sometimes even late summer. Now, with the 400 release on the wb for much of the summer, the main is consistently low, upper 60s/70s for the whole summer and few hatches because the water is too warm. Daytime summer sulphers are a non-existent thing on the main and I remember hitting them along with cahils for much for much of the summer and fog coming off the main in july from cool water temps. Yes, sometimes the main would get very low when the yo yo flows caused a sudden drop, but this was usually short lived and the majority of the summer was higher releases out of the wb and better fishing down on the main for a longer portion of the season.

Again- I think the FFMP is the best option we have seen for the wb. It keeps the river in better shape for the entire season(including winter) than past plans. My point is that whats good for wb under the FFMP is not good for the main.The main doesnt have winter flow issues and only runs into issues from may-early sept. Therefore, the wb could be managed like garbage for 9 months of the year and the main would still thrive so long as water was let out at over 500 cfs for most of the Mid May-Early Sept window.Under the ffmp 400 cfs out of the dam for most of the summer(unless we have montague releases like last year) most keeps the wb in great shape all summer and doesnt stress the fish with up and down flows in a matter of hours, but keeps the main fairly warm and near 70 just a few pools down from the junction since there will be warm and low flows coming in from the eb just about every summer. The low and consistently low flows for april/may (and this year june) also leave the main susceptible to warmer flows that do not let up for any significant period in a warm spring like this year.

-------------

This time it's an "A".

File it.

FWIW, after guiding for 21 years, I don't believe I ever saw Serio (when he was a licensed guide) guiding south of Long Eddy to Hankins to Callicoon to Damascus.

Ever.

And for the record, Mr. Serio's co-hort on the FFMP project, Dr. Kolesar, who is not a guide but does fish the Main Stem from time to time, has stated in emails and various publications, that the trout season on the Main Stem south of Lordville effectively ends in early to mid June until the fall.

Tight lines.
 
Hi Jim


What is your take on the economy this year 2015 in Hancock and Deposit.I ask obviously since you live there.

What do think happened to the hatches on the Upper WB and the Main Stem ?

Many of us have actually seen certain Mayflies disappear in certain pools, and other Mayfly species on a big decline.

Have you seen how bad the silt is on the Upper WB?

Thanks

Joe.T
 
Hi Fly,

There is still a bit of a disconnect here, I am afraid.

What were the releases in the "good old days" in May?

Jim
 
Hi Fly,

FFMP in average or wet years has a release of 400 cfs the last part of May and 500 cfs June thru August. That is what we saw last year.

No other plan ever released more water in the summer for the fisheries.

We have yet to have a dry summer under FFMP, except for the tail end of last summer. The Montague releases will still be made as they were before.

Jim
 
Hi Joe,

Economy is down this year for Hancock and I would expect Deposit too. The low flows have certainly hurt the fishing industry. So what is your point? We need more water, we all know that. FFMP is not to blame.

Hatches are down this year. I think contributing factors were the low flows in the winter and the brutal cold. It was a double wammy. My guess is that half of the river bottom was frozen solid this past winter. Silt may be a contributing factor.

Reports of very few 1 and 2 year fish on the upper WB would also indicate a rough winter with little cover.

Silt: Twenty years ago the upper WB was like a spring creek. Lots of grass beds in muddy bottom. The 2006 flood took all of that away. Heck, even the mud flats in front of our house are not mud flats anymore. This may be the river just naturally filling those areas back in, since we have not had any good flushing flows the last couple of years. I do not know. What are your thoughts?

What do you all think a "flushing flow" on the WB needs to be to get rid of the silt? Or do we want to get rid of it?

Jim
 
Hi Tony,

Not sure what your point is about me not fishing much below Long Eddy. That is true.

I probably averaged 10 days a year below Long Eddy.

Never saw much need to go down that way, except occasionally in the Spring.

I seldom had clients that targeted shad or smallies, most of the time the trout fishing was as good or better upstream.

Besides after you drifted through an area down there there were not anymore fish that could be caught!! You and your clients would get most of them!!!

Jim
 
Hi Tony,

I think that Peter K. is just being pragmatic.

Many years the Mainstem below Lordville or Long Eddy becomes inconsistent for trout in the summer.

Jim
 
Hi All,

An interesting exercise:

Look up the lake elevations for Lake Wallenpaupack. These are the elevation targets that Talen Energy (formerly PPL) has to maintain as minimum at the beginning of each month.

If you find those targets, the next step is to calculate how much water they can release during the month to be at or above the next target.

In dry years, there will be summers when Talen will not be able to release due to the elevation targets. This will cause higher directed releases from the WB.

Where do we stand with elevation today and what is the July 1st elevation target.

This will help predict when NYC Directed releases may kick in.

Jim
 
Hi Fred,
OK... no one's happy with what we had or what we got... Here's the new flow plan....

250CFS Cannonsville release April 1 to May 15th (more if required to keep Hale at least 450 CFS and/or Hancock temp below peak of 65 degrees F).

From May 15 to June 15th, Cannonsville release of 350 CFS (more if required to keep Hale at least 450 CFS and/or Hancock below peak of 65 degrees).

June 15th to August 15th, Cannonsville release of 500 CFS (more if required to keep Hancock below peak of 65 degrees).

August 15th to Nov 15th - 250 CFS (more if required to keep Hale at 350 CFS and/or Hancock below 65 degree peak)

October 15th to December 1 end of year 200 CFS. Winter.. dunno.

This is your proposed flow plan.

Has some good points to it.

A couple of questions.

Do you want to maintain this under any conditions? Dry years vs Wet years?

Stop in the office sometime and we will run it in OASIS and see how things look.

One of the problems that is inherent in your plan, WHO is going to run it? NYS DEC wanted out of managing plans for flow and temperature. Do you trust NYC to do it? The DRBC?

Once you figure that out, where does the money come from?

I think that FFMP performed better than your plan would have last year.

There were only a few days that Hancock approached a max temp of 65.

Jim
 

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Jim,

The FFMP has been tough on the main IMO for several reasons, some of which are not directly flow related but nonetheless have had direct negative consequences on the main. First, the low FFMP spring time flow requirements in an attempt to conserve water for summer flows have really condensed the season on the main because we are seeing warmer springs. Unless the system is chock full of water and a 1500 release/spillage occurs, the wb is going to run under 300 cfs in april and may. This causes the main to rely heavily on freestone flow from the bkill/ebranch and even on a decent water year leaves the main in that 1000-1500 cfs range most springs. A few days in the 80s which is normal for spring now and the main starts creeping up to upper 60s by early/mid may. These early season warmups have really hurt the hatch activity on the main and you see the hatches accelerate and few bugs coming off by late may. This year proves that as have the past few. The bug life on the mainstem is the worst I've ever seen in my time fishing the system.
The common sub 300 cfs springtime flows on the wb have also caused a dramatic increase in pressure on the mainstem because the wb is not floatable or barely floatable most springs. The upper main to buckingham has become a joke the past 5 years, which admittedly is in part due to just an increase in boats in general, but also in part bc the west branch is too low to float for much of the early spring unless we have 100% capacity/spillage. The fish are getting absolutely pounded on the upper main to the point the fish have mouth's that look like the wb no kill fish. Many Guides are going where the water is though and the closest float to town- to shehawken to buck it is.
Also, the summertime flows on the wb are steady under the FFMP, but overall lower most days during the summer months under the FFMP. The main used to actually benefit from the yo yo flows and 750cfs+ flows on the wb during the summer prior to the FFMP and the main would stay cool/have hatches for much of the late spring/early summer and sometimes even late summer. Now, with the 400 release on the wb for much of the summer, the main is consistently low, upper 60s/70s for the whole summer and few hatches because the water is too warm. Daytime summer sulphers are a non-existent thing on the main and I remember hitting them along with cahils for much of the summer and fog coming off the main in july from cool water temps. Yes, sometimes the main would get very low when the yo yo flows caused a sudden drop, but this was usually short lived and the majority of the summer was higher releases out of the wb and better fishing down on the main for a longer portion of the season.

Again- I think the FFMP is the best option we have seen for the wb. It keeps the river in better shape for the entire season(including winter) than past plans. My point is that whats good for wb under the FFMP is not good for the main.The main doesnt have winter flow issues and only runs into issues from may-early sept. Therefore, the wb could be managed like garbage for 9 months of the year and the main would still thrive so long as water was let out at over 500 cfs for most of the Mid May-Early Sept window.Under the ffmp 400 cfs out of the dam for most of the summer(unless we have montague releases like last year)keeps the wb in great shape all summer and doesnt stress the fish with up and down flows in a matter of hours, but keeps the main fairly warm and near 70 just a few pools down from the junction since there will be warm and low flows coming in from the eb just about every summer. The low and consistently low flows for april/may (and this year june) also leave the main susceptible to warmer flows that do not let up for any significant period in a warm spring like this year.

Fly... I find your commentary vary interesting and informative. But one question I have is aren't those 750CFS releases connected not to the fishery but rather to meet Montague flow targets? I can't recall any plan that dumped that kind of water down the river for the fishery. We could see those releases this year despite the FFMP. In fact I would argue the reason for the low releases at the moment is do to NYC's fear of an extended Montague release like the one that almost drained Cannonsville about 8 years ago.

Now Long ago there was a thermal release requirement I believe at Hankins. That may have been the reason for the higher flows but I think it's really Montague driving those flows. The difference now is there seems to be the use of more downstream water.

Lastly, I do not think there is a plan that really can cool the Main below Lordville or Buck for that matter with the WB and very upper main being thermally sound and with flow all season long. There is simply not enough water over many years. Again 1000CFS release over 30 days is 20% of the capacity of Cannonsville... Alot of water over 3 months of summer.

It is a good question to ask however... Is it better for the fishery to protect the WB and upper main all season long vs, cooling the main down july and august?
 
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Hi Fred,

I believe you are exactly correct about the higher summer releases. They were directed releases for Montague.

The old thermal bank was a total of about 9000 cfs/days. This was to be used to help keep all four rivers below 75 at certain locations. It was not very much water to work with for an entire year. you could release 750 from WB, 100 from Pep and 50 from the Nev for only ten days. The bank would then be exhausted.

For the record, I have always been in favor of some bank of water for thermal or the unexpected.

Jim
 
Hi Fred,
OK... no one's happy with what we had or what we got... Here's the new flow plan....

250CFS Cannonsville release April 1 to May 15th (more if required to keep Hale at least 450 CFS and/or Hancock temp below peak of 65 degrees F).

From May 15 to June 15th, Cannonsville release of 350 CFS (more if required to keep Hale at least 450 CFS and/or Hancock below peak of 65 degrees).

June 15th to August 15th, Cannonsville release of 500 CFS (more if required to keep Hancock below peak of 65 degrees).

August 15th to Nov 15th - 250 CFS (more if required to keep Hale at 350 CFS and/or Hancock below 65 degree peak)

October 15th to December 1 end of year 200 CFS. Winter.. dunno.

This is your proposed flow plan.

Has some good points to it.

A couple of questions.

Do you want to maintain this under any conditions? Dry years vs Wet years?

Stop in the office sometime and we will run it in OASIS and see how things look.

One of the problems that is inherent in your plan, WHO is going to run it? NYS DEC wanted out of managing plans for flow and temperature. Do you trust NYC to do it? The DRBC?

Once you figure that out, where does the money come from?

I think that FFMP performed better than your plan would have last year.

There were only a few days that Hancock approached a max temp of 65.

Jim

Jim... Thanks for your comments. This was just off the top of my head so I don't have all the answers. I would guess in dry years it might have to be dialed back a bit. Not sure how. Would require more thought. Maybe a bit lower flow at Hale and a bit higher temperature at Hancock? Dunno. Not sure who would twist the value. Maybe the FUDR could pay someone to do it. Dunno.

Not sure why the FFMP would have performed better... perhaps releases to 600 CFS under FFMP?.... have to look and see as I don't frankly recall of course last year ambients were great. Lower East fished end of July for me. This year, my plan would have solved the issues we've had to date. The FFMP.. may work OK with a thermal release added geared to Hancock or Lordville.
 
Hi Joe,

Economy is down this year for Hancock and I would expect Deposit too. The low flows have certainly hurt the fishing industry. So what is your point? We need more water, we all know that. FFMP is not to blame.

Hatches are down this year. I think contributing factors were the low flows in the winter and the brutal cold. It was a double wammy. My guess is that half of the river bottom was frozen solid this past winter. Silt may be a contributing factor.

Reports of very few 1 and 2 year fish on the upper WB would also indicate a rough winter with little cover.

Silt: Twenty years ago the upper WB was like a spring creek. Lots of grass beds in muddy bottom. The 2006 flood took all of that away. Heck, even the mud flats in front of our house are not mud flats anymore. This may be the river just naturally filling those areas back in, since we have not had any good flushing flows the last couple of years. I do not know. What are your thoughts?

What do you all think a "flushing flow" on the WB needs to be to get rid of the silt? Or do we want to get rid of it?

Jim

Hi Jim

I really didn't have a point about the local economy,it's just what I've been hearing and wanted your take on it since you actually live there year round.

I think hatches being down or even gone are from both the silt and I agree this past winter may have been the number 2 punch.

I don't know how a big flush would work since we also have silt coming out of the reservoir.Silt is not a good thing for most mayfly's.

Bottom line is the System needs research and studies done by a Biologist who can confirm or dismiss any educated guessing by guys like us.

I'm working on the Biologist part.

Thanks

JOE.T
 
I defer to the knowledge of people like Jim and Joe and Jeff, and others on the site who have been thinking about these issues for a long time. But I want to put a few points out there. I apologize in advance if these are stupid ideas.

The first point is that this was an abnormally dry and hot spring after an extremely cold winter. Not in any way normal. Anchor ice and snowpack, followed by a rapid heat up and no rain. In April and May of this year, the weather station in Hancock reported .01 inch of precipitation. On average, those months will have at least 2 or 3 inches of rain. (The mean is actually close to 15 inches for those two months, but it's pulled upward by extreme rainstorms.)

Of course the rivers are suffering. Of course the economy is suffering. This is almost a "worst case scenario" for the trout season. As JC and others have pointed out, FFMP is meant to protect the system during times of low flows, i.e. winter and summer, and anticipates some early spring rain, which we did not get at all.

No rainfall whatsoever in March and April is not a "new normal" - it's a test case and an opportunity to show the state and the city what happens when the Upper Delaware system doesn't have enough water in spring. A few emails back, somebody said "you broke it, you bought it" to Jim. The way I read this is that he is now somehow responsible for the weather. Wrong. Bigger releases would have helped this year. Smaller releases would have made things even worse. But you have to keep things in perspective. No flow plan is going to entirely anticipate and moderate the effects of extreme weather.

Second point. There are a couple of possible arguments that FUDR and others could use in pushing for an adjustment to the flow plan. They each have different implications.

The health of the fishery: Seems like the crucial issue here is avoiding really low flows when there are prolonged periods of high ambient temps. These are likely to happen in the summer. The Montague target releases will take care of some of these situations, and the FFMP scheduled releases will take care of others, but not all. Thermal protection releases, which Jim has been arguing for, and which the DEP explicitly said they were open to last week, seem to be the answer. When the reservoirs are above X% full, the rivermaster will release enough water to keep temps below 70 at Y location (Let's say Lordville). This doesn't seem unreasonable to me. And might not require huge amounts of water, though I really have no idea.
The health of the economy:This is related to the health of the fishery but not the same thing. Thermal releases won't make the river floatable during a dry spring like we're having. Recreational boating of all sorts (kayaking, canoeing, pontoons as well as drift boats) has been way, way down this year. And that's what a lot of people come to the Upper Delaware for, not just to hire guides and cast from a drift boat for a rising trout. Keeping more of the system floatable during peak season for the fishing industry up there would require bigger releases during the spring when the freestones are not supplying enough water. Like now. This seems to me like a tougher case to make. The city will want to hold on tight to its water during a dry spring, not knowing what summer will bring.

In my mind, the thermal releases are the low hanging fruit. They might not help the boating, but they'll keep the fish healthy and keep more water fishable longer, which will also help reduce the pressure on some parts of the system and will put money in the pockets of guides who can convince clients to wade from time to time. And the powers that be, whoever they are, seem more likely to agree to an increased release during, say, an occasional five day heat wave, than increased baseline releases.

my two cents as basically an outside observer of this debate.
 
Hi Joe,

The biology is important.

The problem with studying biological systems is you have to study them for many years to be able to figure them out and make conclusions and recommendations.

NYS is supposed to have completed a report every year under FFMP. They are either not complete or there seems no copies exist.

Might be worth your time to dig into that a bit.

jim
 
Hi Mud,

Very good points.

Peter and I have always set our sights and goal on something that we thought the decree parties would buy into and accept.

FFMP was of course the big one and then the improvements suggested by PA Fish and Boat as well as NY DEC was also something that looked to be possible.

Peter has done extensive work on the Thermal Release Protocol. We never called that a permanent plan, but thought that the decree parties would be more willing to accept a plan that was experimental or a trial in nature. We had the perfect opportunity to pass this trial plan this year but could not get any traction from the decree parties.

The decree parties are locked in some other issues and until those are resolved they were not going to consider a thermal plan. Remember, to make a change, it takes all 5 members to agree. All you NJ folks could get on your government to end the stalemate amongst the decree parties!!!! Please!!!

Jim
 
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