Send Temps: Why You Climb Harder in the Cold (Temperature, Humidity and Friction)
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Last February we drove four hours to a boulder we'd fallen off all autumn. Thirty-eight degrees, a dry north wind, rock so cold it hurt to touch. One of us did it second go after warm-ups. The same move had spat us off eleven times in October. Nothing changed in our fingers between those two dates. Everything changed in the air.
Every boulderer has a version of that story, and it's why send temps is one of the few pieces of climbing slang that crossed over into the weather app. But the folklore around it is half right. The cold isn't what makes the rock sticky. The cold is what stops you from making it slippery.
The 10-second answer
The best temperature for climbing hard boulders sits roughly between 35 and 55°F (2–13°C), with humidity under about 50% and a breeze. That's a climbers' rule of thumb, not a lab result, and the lab results are more interesting: temperature on its own barely moves skin friction. What it moves is sweat. Cool, dry air keeps your fingertips in the narrow band of moisture where skin grips best. Humidity and dew point decide more of your session than the thermometer does. Too cold, and you lose the other half: numb fingers, glassy skin, stiff shoe rubber.
What "send temps" actually means
Ask ten climbers and you'll hear ten numbers, but they all describe the same thing: conditions where friction stops being the limiting factor and strength is. On a warm day, the hard move fails because your fingers slide off a sloper you could otherwise hold. On a send-temps day, it fails because you're not strong enough. That second kind of failure is the honest one, and it's why people drive through the night for a cold front.
It matters most on friction-dependent holds: slopers, rounded rails, slabby feet, polished granite at Bishop or sandstone at Joe's Valley. On a deep crimp or a jug, temperature changes very little. That's why the gym crimp ladder feels the same in July and the Buttermilks don't.
The science: skin, not rock
Here's the part most articles skip. When researchers have actually measured finger friction on rock, temperature hasn't done much. A 2012 study in Sports Biomechanics (Amca and colleagues) measured fingertip friction on limestone and sandstone holds and found chalk raised the friction coefficient by roughly 19–22%, but found no correlation between friction and the room's temperature or humidity. Small sample, controlled lab. Even so, it's a useful reality check.
A review published by Friction Labs (a chalk company, and we're a chalk-adjacent company, so read us both with that in mind) lands in the same place: comparing 50°F and 80°F, finger maximum force didn't change; endurance was lower in the warm. Humidity, at 19% vs 85%, did more damage: lower work capacity, more sweat, slower recovery. Their conclusion, which we agree with: temperature has minimal direct effect on skin friction; humidity is the bigger problem.
So why does cold feel so good?
Because of skin moisture. Tribology research on fingertips describes a bell curve: bone-dry skin grips poorly (hard, less contact), slightly damp skin grips best (softer, more surface in contact), and wet skin grips worst (a film of water between you and the hold). Your sweat glands decide where on that curve you sit, and warm or humid air pushes them toward "wet". Cold, dry air holds you near the top of the curve for longer. That's send temps in one sentence. We went deeper on the moisture mechanics in why climbers use chalk at all.
Your shoes care about temperature, your fingers less
Climbing rubber is a polymer, and polymers stiffen as they cool. On a frozen morning, your edges feel like plastic and your smears skate. That's the one place where the thermometer itself matters, and it's why the best cold sessions start with shoes kept in the car's cabin or inside your jacket, not in the trunk.
Humidity and dew point: the numbers to check first
If you only look at one number before a session, make it the dew point, not the temperature. Dew point is the temperature at which air drops its moisture. When the rock surface cools to the dew point, water condenses on it. You won't always see it; you'll just feel holds that are inexplicably greasy at 7 a.m. and fine by 10.
- Big gap between air temperature and dew point (say 15°F or more): dry air, rock stays dry, you sweat less. Go.
- Small gap (under about 5°F): the air is near saturation. Shaded rock and north faces can be damp to the touch even without rain.
- Relative humidity is easier to find in an app, but it shifts through the day with temperature. Dew point is the steadier read.
Wind is the free bonus. A light breeze strips the moist air off your fingers and off the stone. The same 50°F day can feel like two different crags with and without it.
A rough guide, in Fahrenheit and Celsius
These bands are what we, and most of the boulderers we climb with, use as a starting point. They're not physics; they're accumulated sessions. Your hands sweat at their own rate, so adjust.
| Air temperature | What tends to happen | Best for |
|---|---|---|
| Below 30°F (−1°C) | Numb fingertips, stiff rubber, short tries. Skin goes hard and glassy. | Short warm-ups, one or two hard burns, then leave |
| 30–45°F (−1–7°C) | Peak friction for most people, if dry. Needs a long warm-up and layers between goes. | Slopers, slab, limit projects |
| 45–60°F (7–16°C) | Comfortable and still good if humidity is low. The all-round sweet spot. | Volume sessions, most projects |
| 60–75°F (16–24°C) | Fine in the shade and in dry air; humid days start to feel greasy. | Crimps, steep jugs, shaded walls |
| Above 75°F (24°C) | Sweat wins. Chalk turns to paste between tries. | Early mornings, evenings, or the gym |
How cold is too cold to climb?
When your fingers stop telling you the truth. Below freezing, the problem isn't friction; it's feedback. You can't feel how much skin is on the hold, so you over-grip, pump faster, and get hurt on moves your brain thinks you're holding. Cold tendons and pulleys also tolerate sudden loading worse than warm ones, which is why winter sessions need longer warm-ups, not shorter.
Our rule: if you need to warm your hands between every single attempt and they're still numb on the first move, you're past the useful window. Go home or go to the gym. Nobody ever regretted leaving a frozen boulder for another day.
Send temps by season
Winter: the season itself
In the US, winter is when the desert areas earn their reputation. Hueco Tanks and Red Rocks are winter destinations precisely because their summers are unclimbable, and so is Joshua Tree, where sloper-and-smear climbing makes friction everything. The trap is the opposite of summer: sunny faces can be perfect at noon and frozen at 4 p.m. Chase the sun in the morning, chase the shade only on the warmest days.
One sandstone warning that has nothing to do with friction: don't climb on wet sandstone. It loses strength when soaked and holds break. After rain at Red Rocks, give the stone time to dry out fully before touching it.
Summer: borrow the cold
Summer send temps exist, you just have to find them. Altitude buys you roughly 3–5°F per 1,000 feet. Pre-dawn and late evening sessions on north-facing stone can be genuinely good. And headlamp sessions are a real thing for a reason. If the dew point is high, though, no time of day saves you; that's a training-in-the-gym week.
Spring and fall: the shoulder seasons
Fall is the most reliable window across most of the country: cooler air arriving before the winter storms. That's when Bishop and Joe's Valley fill up. Spring is the same temperatures with more rain, so the dew point check matters twice as much.
Making your own send temps in bad conditions
You don't control the weather. You control what your hands do between attempts:
- Rest longer, and in the shade. Skin temperature drops faster than you think if you get out of the sun.
- Brush every hold before every serious try. Humid days pack chalk into a greasy layer; a good brush resets it.
- Liquid chalk as a base layer. On sweaty days, a coat of liquid chalk before loose chalk lasts longer between tries. We wrote up when liquid chalk beats powder.
- Chalk less, more often. A thick layer becomes paste. A thin layer, refreshed every try, stays dry.
- Cold drink, hands off the thermos. The Friction Labs review mentions a cold drink before sessions to lower core temperature. Holding a hot mug between tries does the opposite for your fingertips.
- Keep your chalk in good shape too. Damp chalk is a different problem from damp air; we covered it in how to store climbing chalk.
Full transparency: we make one product, a bouldering chalk bucket, and this is the part of the session it's built for. A wide opening you can hit with both hands between tries, and a free brush and chalk ball in the box, so the "brush every hold" rule actually happens. We carry it to our own winter sessions; if it doesn't survive a February morning at the boulders, it doesn't ship. It's $49.99 at launch instead of $89.99, the first run ships in November 2026, free shipping, US only. A chalk bag works too; what matters is that re-chalking is fast enough that you actually do it.
Quick answers
What temperature is best for climbing?
For hard bouldering, most climbers aim for roughly 35–55°F (2–13°C) with low humidity. For comfortable volume climbing, 45–65°F (7–18°C) is easier on the body. Humidity often matters more than the exact number.
Is it better to climb in humidity or heat?
Neither, but dry heat is usually easier than humid cool. In dry air, sweat evaporates; in humid air, it stays on your fingers and turns chalk to paste. That's why a 65°F desert day can climb better than a 50°F muggy one.
Does cold rock have more friction?
Not much, by itself. The rock doesn't get stickier; your skin stays drier, which keeps it in its best-gripping range. Your shoe rubber actually loses some grip in the cold.
Do send temps matter in the gym?
Less, but yes. Gym HVAC keeps temperature steady, not humidity. A packed gym on a rainy summer evening is measurably worse for slopers than an empty one on a dry winter morning. If you're moving from the gym to the crag, this is the first variable you'll meet that the gym never taught you.
— CRACX Co-founder
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Cover photo : houssam korichi / Unsplash. Graphics by CRACX.