Walter & Group...
From Elie Beerten, on "Boatfishing". His diagram in the attachment. My comments in his text in red italics. G. :
Paul,
As I mentioned “ this way of flyfishing is
asking a lot of concentration and continuous
counting”.
“Concentration” to duplicate the method immediately when
you are successfully.
“Counting” 21, 22, 23, … instead of using a stopwatch.
I use the "count method", too. G.
Of course I fully agree on the angle and I would like to add even more.
What
I see during lake fishing lot of fishermen fish just blind. You can increase
your chances a lot if you use the right
angle.
It is very simple and logically and you probally know this a long time.
Facts:
- Mostly trout on lakes are swimming around to find food. On rivers the food is brought to the trout.
Same with most salt water fish. They are usually moving to find food or for whatever other reasons such as moving from area to area in search of better feeding areas, food fish which are also moving, migration patterns, or tidal situations. G.
-
Brown trout are more locked to a certain area then
rainbows.
- Food on lakes can be brought to the trout by wind (small currents).
Conclusion:
If trout move upwind they have a bigger opportunity to find food. Second, if they swim straight behind each other, the first will have all the food and the one behind will have nothing. A reason they swim sideways, next to each other.
This is also one reason it is not easy to tempt a tarpon to take the fly.... because when they are swimming one behind the other in a "string" they are not usually feeding. G.
Knowing this; the best way to meet a trout is to cast sideway. This way you will have much more change to meet a trout and you are always casting to new fish.
Different than with many salt water fish.... With tarpon, for example, the idea is to have your fly moving in the direction the fish is moving so he finds himself already chasing it. The wider the angle between the retrieve and the path of the fish, the less likely you will get a strike. If the angle is SO wide that the fly is more or less coming toward the fish, most salty fish won't take. As Lefty once said, "FLIES DON'T ATTACK FISH"..... an unnatural event. G.
When
you cast right in front you will
only meet the same fish a couple of times. He will get scared.
If you add the third dimension and think about the different feeding levels you will understand that when you use 3 flies your changes are increasing again.
I made a few quick sketches to clarify the above.
If you look carefully you see that one angler (right hand casters, left hand casters, a mix ) is always having a greater change to catch fish.
Well done, Elie ! Helps a lot if both anglers have experience with this method and are used to fishing with one another.
When very windy, this is NOT easy ! On my skiff, I have a little "rule" : The angler in the bow, has the duty to always be aware of the stern angler's fly line position.
In high winds, sometimes the bow angler gains advantage by keeping his back cast very low. If anchored, he can accidentally catch the anchor rode and foul. When that is a risk, I place a 3 lb. lead trolling ball on a carabiner clipped to the rode so it hangs straight down. G.
Regards,
Elie
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
THERMOCLINE
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~`
More from Elie ... on Thermoclines :
Hi Gordy,
I like to do all kinds of flyfishing: salt, fresh, lakes, rivers, …
Yes, the thermoclyne is one of the causes that trout can
feed at a certain level. This has to do with the stratification of water layers
in lakes. The stratification is happening on the deeper lakes due to temperature
and wind. During summer the temperature of the top layers of water are
increasing and the amount of dissolved oxygen is decreasing. Trout need a
certain amount of dissolved oxygen in water to survive. So, they will seek for
the deeper cold water levels.
The stratification divides the water in 2 levels (to keep
it simple) a top layer and bottom layer with in between the thermoclyne. Wind blowing over the water will bring
fresh oxygen in the water. Due to the thermoclyne only the top layer will be
foreseen with fresh oxygen and in the bottom layer the dissolved oxygen will
decrease. This is the reason that
you will find most of the trout around the thermoclyne during hot spells.
Yes, also midges can hover around the thermoclyne. Even
more important when midges are merging to the surface they don’t make their way
straight from the bottom to the surface. They will take pauses at certain
levels. An other reason that trout can feed at a particular
level.
We have also big clouds of daphnia in the water. This
daphnia is like a big protein soup for trout. Trout can get very locked on them.
The daphnia is mostly found at a certain depth. But they can hover through the
water layers by influence of the sun. A cloud in front of the sun can let them
merger a few meters. This means change
flyline!!!
(To be complete: There is a summer stratification and a winter stratification (ice). In spring and in autumn the whole water turns upside down)
Regards,
Elie
```````````````````````````````````````````````````````````````````````````````````````````````````````````````````````````````````````````
Elie... While a true thermocline is a horizontal temperature gradient at a particular depth, there are also sharp temperature divisions in some waters which are VERTICAL. This can happen in fresh water at seams where one body of water flows into another. One glaring example in salt water is the Gulf stream flowing in juxtaposition to waters on either side of it. These vertical temperature lines also hold plankton, forage, and pelagics.
The temperature gradient is one of many things which can collect flotsam and jetsam .... and, therfore the fish which feed on them . In both fresh and salt waters, "scum lines" and "scud lines" can appear when its windy as the result of spiral currents at and near the surface in long lines usually at an angle to the wind of about 45 degrees. Oceanographers tell us that this is caused by the wind coupled with the Coriolis effect which is also partly related to the Earth's rotation. This phenomenon is described in simple terms by Gary Borger. *
* PRESENTATION, Gary Borger, pp. 76-77.
All this may seem to some like information we really don't need. I assure you, however, that this kind of knowledge can make a big difference in one's fishing success !
Gordy
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
SINKING LEADERS & SINKING LINES
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
From Mack Martin:
Attachment:
Bootfishing.xls
Description: Binary data