Iceman
2006-02-19, 09:55
Evapoventicondenrespiperspitransporation; (I have been working on this one for a bit, so please bear with me.) Evapoventicondenrespiperspitransporation is the point at which the .75 to 1.5liter of perspiration, the .5 liter of respiration transport thru your sleeping bag and condensate at, within or on any given insulative material. For the porposes of this discussion, affected by ventilation, Evapoventicondenrespiperspitransporation is the exact point at which moisture vapors condensate on or in your sleeping bag reducing it's insulative value and causing a moist bag. (Don't even try to abbreviate this as I have found it is impossible, and, besides we all need the exercise.)
Please remember, it is important to consider Evapoventicondenrespiperspitransporation when purchasing a sleeping bag, or selecting a sleeping bag for any given trip. In mild or warm conditions, too warm of a sleeping bag causes the sleeper to get a clammy / sweaty feeling inside of the bag. This example illustrates the importance of considering Evapoventicondenrespiperspitransporation, because (as in this example) the Evapoventicondenrespiperspitransporation point is next to the skin of the sleeper. No evaporative-cooling effect is felt by the sleeper until the bag is opened allowing ventilation of said vapors, and thus moving the Evapoventicondenrespiperspitransporation point to a place further from the skin of the sleeper. The Evapoventicondenrespiperspitransporation point has now been moved from the sleeper, to a point further into the insulative materials of the bag, possibly even completely thru and off of the sleeping bag. Moisture in this case can sometimes be seen condensating on other surfaces of the tent, bivy or hammock, or not at all.
In colder conditions, Evapoventicondenrespiperspitransporation can be noted at the surface of a sleeping bag. The vapors associated with a sleeping human are found to appear either on the surface of the sleeping bag, or at some (Evapoventicondenrespiperspitransporation) point within the layer of insulation. This in essence is Evapoventicondenrespiperspitransporation. When we pick the proper sleeping bag for colder conditions, we should consider Evapoventicondenrespiperspitransporation so that Evapoventicondenrespiperspitransporation occurs at the proper location. Too cold of a bag and the sleeper is uncomfortably cold, and may become, well... a "non-sleeper". Too warm of a bag and, um, .................................................. ......................., I am sure there was a reason not to have too warm of a bag for cold conditions, but I cannot seem to remember what it was right now. More on this later. A sleeping bag which is warm enough for cold conditions may place the Evapoventicondenrespiperspitransporation at the surface of the bag. This can be seen as moisture droplets or ice crystals on the surface. This is actually optimal, in this case the Evapoventicondenrespiperspitransporation allows for the owner of said bag to allow the bags surface to dry. By hanging the sleeping bag out in the sun for a short while, all moisture which had accumulated on the surface due to Evapoventicondenrespiperspitransporation can naturally evaporate and dry. In frigid conditions, the bag can be simply shaken and brushed off, as the ice crystals will simply fall off. Worse is the condition (now I remember) where the sleeper has way too warm of a sleeping bag for the cold conditions that they are experiencing. In this case, Evapoventicondenrespiperspitransporation occurs at mid layer of the given insulative thickness. Moisture here which condensates in the middle of insulative layer is difficult to dry while in the field. Moisture accumulated at this level causes the bag to lose insulative properties, and to gain weight, although slight.
As we can see, proper sleeping bag choices are truly impossible without consideration for Evapoventicondenrespiperspitransporation. It should be considered fool hardy and dangersous to even consider sleeping in a sleeping bag without a thorough study of Evapoventicondenrespiperspitransporation.
One variable which was left out of this discussion which dramatically alters Evapoventicondenrespiperspitransporation is noted below.
If you pee your sleeping bag, and then all bets are off.
Stay tuned for squishysockblisterpop.
Please remember, it is important to consider Evapoventicondenrespiperspitransporation when purchasing a sleeping bag, or selecting a sleeping bag for any given trip. In mild or warm conditions, too warm of a sleeping bag causes the sleeper to get a clammy / sweaty feeling inside of the bag. This example illustrates the importance of considering Evapoventicondenrespiperspitransporation, because (as in this example) the Evapoventicondenrespiperspitransporation point is next to the skin of the sleeper. No evaporative-cooling effect is felt by the sleeper until the bag is opened allowing ventilation of said vapors, and thus moving the Evapoventicondenrespiperspitransporation point to a place further from the skin of the sleeper. The Evapoventicondenrespiperspitransporation point has now been moved from the sleeper, to a point further into the insulative materials of the bag, possibly even completely thru and off of the sleeping bag. Moisture in this case can sometimes be seen condensating on other surfaces of the tent, bivy or hammock, or not at all.
In colder conditions, Evapoventicondenrespiperspitransporation can be noted at the surface of a sleeping bag. The vapors associated with a sleeping human are found to appear either on the surface of the sleeping bag, or at some (Evapoventicondenrespiperspitransporation) point within the layer of insulation. This in essence is Evapoventicondenrespiperspitransporation. When we pick the proper sleeping bag for colder conditions, we should consider Evapoventicondenrespiperspitransporation so that Evapoventicondenrespiperspitransporation occurs at the proper location. Too cold of a bag and the sleeper is uncomfortably cold, and may become, well... a "non-sleeper". Too warm of a bag and, um, .................................................. ......................., I am sure there was a reason not to have too warm of a bag for cold conditions, but I cannot seem to remember what it was right now. More on this later. A sleeping bag which is warm enough for cold conditions may place the Evapoventicondenrespiperspitransporation at the surface of the bag. This can be seen as moisture droplets or ice crystals on the surface. This is actually optimal, in this case the Evapoventicondenrespiperspitransporation allows for the owner of said bag to allow the bags surface to dry. By hanging the sleeping bag out in the sun for a short while, all moisture which had accumulated on the surface due to Evapoventicondenrespiperspitransporation can naturally evaporate and dry. In frigid conditions, the bag can be simply shaken and brushed off, as the ice crystals will simply fall off. Worse is the condition (now I remember) where the sleeper has way too warm of a sleeping bag for the cold conditions that they are experiencing. In this case, Evapoventicondenrespiperspitransporation occurs at mid layer of the given insulative thickness. Moisture here which condensates in the middle of insulative layer is difficult to dry while in the field. Moisture accumulated at this level causes the bag to lose insulative properties, and to gain weight, although slight.
As we can see, proper sleeping bag choices are truly impossible without consideration for Evapoventicondenrespiperspitransporation. It should be considered fool hardy and dangersous to even consider sleeping in a sleeping bag without a thorough study of Evapoventicondenrespiperspitransporation.
One variable which was left out of this discussion which dramatically alters Evapoventicondenrespiperspitransporation is noted below.
If you pee your sleeping bag, and then all bets are off.
Stay tuned for squishysockblisterpop.