What Actually Happens If You Try To Land On Venus — Transcript
Full transcript
- 0:00You are falling toward Venus at roughly
- 0:0211 km per second and from up here the
- 0:04planet looks calm. That is the first
- 0:07lie. There is no surface to see, just a
- 0:09smooth cream yellow shell, soft and
- 0:12unbroken, like something poured rather
- 0:14than built. No coastlines, no mountain
- 0:17ranges.
- 0:18No storm you can point at and name. It
- 0:21looks frosted. It looks honestly quite
- 0:23pleasant. You are about to find out what
- 0:26is under the frosting. The trouble
- 0:28starts before you touch anything. Your
- 0:30capsule meets the top of the atmosphere
- 0:31and instantly stops behaving like a
- 0:33spacecraft. It becomes a meteor. The air
- 0:36out there is thin, but you are moving so
- 0:38fast that thin does not help. It piles
- 0:40up in front of your heat shield,
- 0:41compresses, and turns white hot. The
- 0:44Soviet landers that did this survived
- 0:46deceleration forces that would turn a
- 0:48person into a smear on the back wall.
- 0:50You cannot take that ride, so your entry
- 0:52has to be shallower and slower, which
- 0:55sounds like a mercy and absolutely is
- 0:56not because Venus punishes anyone who
- 0:59lingers. A gentler entry means a longer
- 1:01entry. A longer entry means more minutes
- 1:04spent inside the thing you are trying to
- 1:05cross. Your shield glows. The capsule
- 1:08shakes hard enough that the instrument
- 1:10panel blurs and then, sooner than you
- 1:12expect, the roar fades. That is because
- 1:15the atmosphere here is thick, absurdly
- 1:18thick. It slows you down so efficiently
- 1:20that you go from meteor to falling
- 1:22object in a couple of minutes. The
- 1:24parachute opens somewhere above 60 km
- 1:27and for a short while Venus is
- 1:28beautiful. You are hanging in a pale
- 1:30golden sky. The light is soft and
- 1:33sourceless. Below you is an ocean of
- 1:35cloud that goes on forever in every
- 1:37direction and it is genuinely lovely
- 1:39right up until you remember what the
- 1:41clouds are made of.
- 1:42You drop into them. It is not water
- 1:44vapor out there. It is sulfuric acid
- 1:47suspended in droplets thick enough to
- 1:49swallow the view completely. The window
- 1:51goes yellow, then dim. Streaks crawl
- 1:54across the glass and stay there. This is
- 1:56a substance that eats metal for a living
- 1:59and treats human skin as a formality.
- 2:01Your parachute is not made of normal
- 2:03fabric because normal fabric would be
- 2:05gone by now.
- 2:06And then, somewhere around 55 km up,
- 2:09something genuinely strange happens.
- 2:12The pressure gauge settles at about one
- 2:13Earth atmosphere.
- 2:15The thermometer reads something like a
- 2:16warm summer afternoon. You are at this
- 2:19exact altitude, sitting in the most
- 2:21Earth-like conditions anywhere in the
- 2:22solar system outside Earth itself. Same
- 2:25squeeze on the hull, same temperature
- 2:27you would complain about at a bus stop.
- 2:29If you could somehow strain out the acid
- 2:31and the carbon dioxide, a person could
- 2:33stand here in ordinary clothes.
- 2:36You cannot stay. You are on a parachute
- 2:38and parachutes go down. So, you keep
- 2:41falling and the gauges begin to move in
- 2:43the wrong direction. Not suddenly. That
- 2:45is the unnerving part.
- 2:47There is no alarm, no dramatic breach.
- 2:50The temperature just climbs steadily,
- 2:53kilometer after kilometer. The way a
- 2:55number climbs when nothing is going to
- 2:56stop it. 50 km, warm. 40, uncomfortably
- 3:01hot. 30, hot enough to bake bread and
- 3:04still falling.
- 3:06At this point, you do something that
- 3:07feels insane. You cut your parachute
- 3:09away on purpose. The reason is simple
- 3:12and grim. The air below you is so dense
- 3:14that you will drift down slowly whether
- 3:15you want to or not and every extra
- 3:17minute spent descending is another
- 3:19minute of heat creeping through the
- 3:20hull. Hanging around under a canopy is
- 3:23not caution here. It is suicide by
- 3:25delay. So, you release the chute, drop
- 3:28onto a small drag ring, and let the
- 3:30atmosphere itself hold you up while you
- 3:32sink toward the floor of the world. The
- 3:35air stops behaving like air. Down here,
- 3:37it acts more like a fluid, something
- 3:39between gas and liquid, and it starts
- 3:41bending light. The horizon curls upward
- 3:44at the edges. Distant ground appears to
- 3:46lift toward you as though you are
- 3:48descending into an enormous shallow
- 3:50bowl. Nothing out there is where your
- 3:52eyes say it is.
- 3:54You are not really falling anymore. You
- 3:56are sinking. The last stretch of the
- 3:58descent takes close to an hour, and it
- 4:00feels less like a drop than like
- 4:02settling through deep water. Because
- 4:04down here the carbon dioxide has been
- 4:05squeezed into something that is not
- 4:07properly a gas and not properly a liquid
- 4:10either. It has weight. It has current.
- 4:12It shoves slowly against the hull, and
- 4:14you can feel the capsule shift as it
- 4:16pushes through.
- 4:18If you are enjoying this video, please
- 4:20hit the subscribe button. It genuinely
- 4:22helps keep the channel alive. And then
- 4:24the drop ends.
- 4:25There is a thud, a small shove into your
- 4:28seat, and a puff of fine dust that does
- 4:30not billow the way dust does at home. It
- 4:32slumps. It sinks back down almost
- 4:35immediately because the air is too heavy
- 4:37to keep anything floating for long.
- 4:39You have landed on Venus.
- 4:41Congratulations. The clock has started,
- 4:43and it is not a long clock.
- 4:45The capsule is not sitting level. It
- 4:47came down on a broken slab and settled
- 4:49at an angle, and there is nothing to be
- 4:51done about that. No wheels, no legs that
- 4:54adjust, nowhere to drive to.
- 4:57Wherever this thing stopped is where it
- 4:58stays for the rest of its very short
- 5:00life.
- 5:01Look out of the window.
- 5:03This is the part almost nobody expects.
- 5:05It is not dark. The surface of Venus is
- 5:08lit in a dim orange glow, like the last
- 5:1020 minutes of a very overcast sunset,
- 5:13and you can see for a surprising
- 5:14distance. The ground is flat and cracked
- 5:17into broad dark slabs,
- 5:19dull plates of volcanic rock stretching
- 5:21off toward that warped uplifted horizon.
- 5:24There are no plants, no water, no ice,
- 5:26no shadows worth the name because the
- 5:29light has been scattered so many times
- 5:30on its way down that it arrives from
- 5:32everywhere at once.
- 5:34The landscape is not dramatic. It is
- 5:36worse than that. It is boring in the way
- 5:39a furnace floor is boring. There is wind
- 5:41out there, but only a gentle one, a slow
- 5:44shuffle of a meter or two per second. On
- 5:46Earth you would barely notice it. Here,
- 5:48that breeze is moving air about 50 times
- 5:50denser than the air in your lungs, which
- 5:53means it carries real force, like a lazy
- 5:55current in a river. The dust it pushes
- 5:57around does not blow, it creeps. And if
- 6:00you could somehow open the hatch and
- 6:02speak, your voice would come out wrong.
- 6:04Deep, buzzing, oddly loud, then
- 6:07swallowed fast. The atmosphere is so
- 6:09thick that sound moves differently
- 6:10through it. Even the acoustics of this
- 6:13place are off.
- 6:14Now, the actual killer gets to work, and
- 6:16it is not the acid, and it is not the
- 6:18pressure. It is the heat and the fact
- 6:21that you have nowhere to put it. The
- 6:22surface temperature here sits at roughly
- 6:24460° C.
- 6:26That is hot enough to melt lead and tin
- 6:28outright. Hot enough that anything
- 6:30organic simply stops being organic. Your
- 6:32capsule is a thermos, packed with
- 6:34insulation and a block of material
- 6:36designed to absorb heat rather than
- 6:38fight it, because fighting is not an
- 6:40option.
- 6:41On any spacecraft near Earth, you dump
- 6:43excess heat by radiating it into cold
- 6:45space. Here, there is no cold anything.
- 6:48The outside is hotter than the inside.
- 6:51There is no direction to push the heat
- 6:53toward. Every cooling system you know
- 6:55how to build works on the assumption
- 6:56that somewhere nearby is colder than
- 6:58you, and on the floor of Venus, that
- 7:00assumption is simply false.
- 7:02So, you are not cooling, you are
- 7:03counting.
- 7:04You try the obvious thing first. You
- 7:06turn the cabin fan up, and all it
- 7:08achieves is moving hot air around
- 7:10faster, while adding its own small
- 7:12contribution to the heat. You check the
- 7:14insulation readings, and they are doing
- 7:16exactly what they were built to do,
- 7:17which is nothing except buy minutes.
- 7:20There is no switch in here that makes
- 7:21Venus colder.
- 7:23Heat pushes in through every seam and
- 7:24every bolt, degree by degree, and all
- 7:26your insulation can do is slow the
- 7:28arithmetic.
- 7:29The Soviet landers that survived this
- 7:31the longest managed a little over 2
- 7:33hours before the readings went silent.
- 7:35That was the record, and it was
- 7:37considered a triumph.
- 7:38Most did far less.
- 7:40Your instruments go first. Electronics
- 7:42hate heat long before metal does. So,
- 7:45the failures arrive in a sequence. A
- 7:47sensor drops out, a display flickers and
- 7:49stays dark, a fan starts making a sound
- 7:52it has never made before. Air inside the
- 7:54cabin turns thick and oven dry. Every
- 7:57surface you touch is warmer than the
- 7:58last time you touched it. Metal buckles
- 8:01get hot enough to mark you. The seat
- 8:03warms through the padding. And then, if
- 8:05a seal finally gives, the ending is
- 8:07quick. 92 times Earth's atmospheric
- 8:10pressure is standing outside that hole,
- 8:12and it is not gentle air.
- 8:14Your body does not crush like a tin can
- 8:17because you are mostly water and water
- 8:18does not compress.
- 8:20What arrives instead is a flood of
- 8:21searing dense carbon dioxide at a
- 8:23pressure your lungs were never designed
- 8:25to face, and it takes the inside of you
- 8:27apart faster than you can register what
- 8:29happened.
- 8:30Nobody is coming. The nearest help is
- 8:33millions of kilometers away, and a radio
- 8:35call from here takes minutes to arrive,
- 8:37then minutes more for the answer.
- 8:40By the time anyone on Earth hears you,
- 8:42the situation they are hearing about is
- 8:44already history. No rescue vehicle can
- 8:46descend to a place that destroys
- 8:48machines in under 2 hours. And here is
- 8:50the strangest part of the whole trip.
- 8:52You will still be there.
- 8:54Venus does not decompose things. There
- 8:56is no liquid water, no bacteria, no
- 8:59weather that erodes the way rain does.
- 9:01Acid rain falls from those beautiful
- 9:03clouds, but it evaporates in the heat
- 9:05long before it reaches the ground. So,
- 9:07your capsule stays where it settled,
- 9:09slowly corroding, slowly sagging,
- 9:12sitting on a plane of volcanic rock that
- 9:14was resurfaced by something planet-wide
- 9:16hundreds of millions of years ago, and
- 9:18has essentially been waiting ever since.
- 9:20There's a small piece of Venus history
- 9:22that says everything about this place.
- 9:24One of the Soviet landers popped off its
- 9:26camera lens cap after touchdown, and the
- 9:28cap landed on exactly the one patch of
- 9:31ground the probe's soil tester was about
- 9:32to poke. So, the first ever measurement
- 9:35of the Venusian soil strength was, in
- 9:37fact, a measurement of a camera lid. The
- 9:39probe had roughly an hour to live and
- 9:41spent part of it studying its own
- 9:42rubbish. That is the tone of the entire
- 9:45planet. It does not rage at you. It just
- 9:47quietly ruins everything, then keeps
- 9:49going.
- 9:50Which leaves one obvious question, and
- 9:52it deserves an answer.
- 9:54If 55 km above the surface is mild and
- 9:56calm, why land at all? Why not simply
- 9:59stay up there?
- 10:00And the honest answer is that you could.
- 10:02Breathable air is a lifting gas in an
- 10:04atmosphere that heavy. So, a sealed
- 10:06habitat full of ordinary oxygen and
- 10:08nitrogen would float in the Venusian sky
- 10:10like a balloon, drifting through acid
- 10:12clouds at shirt sleeve temperature.
- 10:14People have designed exactly that.
- 10:16But, floating is not landing. The moment
- 10:19you go looking for solid ground, you are
- 10:21trading the one hospitable layer of this
- 10:23planet for the least hospitable surface
- 10:25anyone has ever reached. So, that is
- 10:27what actually happens if you try to land
- 10:29on Venus. You survive the fall. You
- 10:32touch down softly. You get a clear view
- 10:34of an orange, silent, slab-covered plain
- 10:37that no human eye was built to see.
- 10:40And then you sit in a cooling metal ball
- 10:42that is not cooling, watching the
- 10:43numbers go up on the only world we know
- 10:46of where the sky is kinder than the
- 10:47ground.
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