Gear & Kit
Layering that works when you are moving hard
The classic three-layer model was designed for standing around. Aerobic mountain travel produces enormous amounts of moisture, and managing that is a different problem.

The three-layer system — base, insulation, shell — is taught everywhere and it is a reasonable starting point. It is also built around a scenario that does not describe what most of us do, which is move uphill hard for hours, generating serious heat and a remarkable volume of sweat, then stop, in wind, and cool very fast.
Once you frame it as a moisture problem rather than a warmth problem, the sensible choices change.
You will sweat. Plan for where it goes
Someone skinning uphill at a decent pace produces heat comparable to hard running and loses a substantial amount of water through the skin. That moisture has to go somewhere. It either evaporates through your clothing to the outside, or it condenses inside your layers and sits there.
Wet insulation loses most of its value. Wet clothing against skin in wind cools you at a rate that is genuinely dangerous. Nearly every case of someone getting cold on a mountain in adequate clothing traces back to moisture that had nowhere to go.
Start cold
The most useful and least followed piece of advice in winter travel. At the trailhead you should feel slightly underdressed and mildly uncomfortable. Within ten minutes of moving you will be right.
Start warm and you will sweat through the first climb, and everything after that is damage control.
This costs a small amount of discomfort at the start of the day and it removes the single largest source of problems later.
Vent before you shed
Adjusting temperature does not require stopping and unpacking. Open the pit zips. Drop the hood. Take the hat off — a large fraction of heat regulation is available through the head and hands alone. Open the front zip.
Learn to make these adjustments while walking. The people who overheat are usually the people who do not want to stop, and venting means they do not have to.
The base layer, and the wool-versus-synthetic argument
Synthetics move moisture faster and dry faster. Merino manages odour far better, feels less clammy when damp, and retains a bit more warmth when wet. Blends split the difference and are what most people end up preferring for multi-day trips.
Cotton is the one genuine mistake. It absorbs many times its weight in water, holds it against the skin, and dries extremely slowly. It is the classic mechanism of hypothermia in mild conditions.
Fit matters more than fabric. A base layer needs skin contact to wick; a loose one is just a thin jumper.
Active insulation is the real improvement
This is the piece the classic model misses. A traditional insulating layer — a thick fleece or a puffy — is designed to trap air while you are still, and it is far too warm and far too slow to breathe while you are working.
Active insulation is a light, air-permeable piece — grid fleece, or a thin synthetic fill in a highly breathable face fabric — designed to be worn while moving. It provides modest warmth and passes moisture readily, so you stay in a comfortable band without the on-off cycle.
For most winter days, a base layer plus an active mid, with a shell in the pack, will carry you the whole way uphill without stopping to change.
The belay jacket lives in the pack
Separately, carry a genuinely warm insulated jacket, oversized enough to go over everything else, and put it on the moment you stop. Not after you get cold — immediately, at every transition, every belay, every long break.
Synthetic fill for wet conditions and for wearing over damp layers; down for cold and dry, where it wins on warmth for weight. Down that gets wet from the inside is a common and avoidable failure.
This jacket is also your emergency insulation if someone is injured and everything stops. That alone justifies carrying it on days you think you will not need it.
Shells and the limits of breathability
A waterproof membrane can only move vapour when there is a gradient across it — warmer and wetter inside, cooler and drier outside. In warm, humid rain, that gradient is small and even the best shell will feel clammy. That is physics, not a defective jacket.
Practically: wear the hardshell for actual precipitation and serious wind, not as a default outer. On dry cold days a light windproof breathes far better and is enough. Big pit zips are worth more than the marketing rating on the fabric.
Extremities and the bit people forget
Two pairs of gloves minimum: thin ones for tasks, warm ones for standing. Keep spares dry inside the jacket. A wet pair of gloves in a cold wind stops your hands working, and hands that do not work cannot operate a transceiver, tie a knot, or open a pack.
Eat and drink. Insulation slows heat loss; food is what produces heat in the first place. A well-dressed person who has not eaten for six hours will still get cold.


