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Gravity Assist Podcast, Venus with David Grinspoon (1)
Nov. 29, 2017
This global view of the surface of Venus is centered at 180 degrees east longitude. Magellan synthetic aperture radar mosaics from the first cycle of Magellan mapping are mapped onto a computer-simulated globe to create this image. Data gaps are filled with Pioneer Venus Orbiter data, or a constant mid-range value. Simulated color is used to enhance small-scale structure. The simulated hues are based on color images recorded by the Soviet Venera 13 and 14 spacecraft. The image was produced by the Solar System Visualization project and the Magellan science team at the JPL Multimission Image Processing Laboratory and is a single frame from a video released at the October 29, 1991, JPL news conference. Credits: NASA/JPLThe next stop on our virtual tour is Venus, the closest planet to Earth and the hottest planet in our solar system, with surface temperatures scorching enough to melt lead.
NASA’s Jim Green is joined by David Grinspoon of the Planetary Science Institute to discuss Venus’ volcanoes, clouds of sulfuric acid, and runaway greenhouse effect. Was Venus once was like Earth in its distant past and what clues might it provide about the future of our own planet? You’ll also hear about Venus’ backward rotation and “forever sunsets,” plus the remarkable and heroic “Apollo 11”-like story of the Akatsuki spacecraft.
Transcript:
Jim Green: Our solar system is a wondrous place, with a single star, our Sun, and everything that orbits around it-- planets, moons, asteroids, and comets. What do we know about this beautiful solar system we call home? It’s part of an even larger cosmos, with billions of other solar systems.
Hi, I’m Jim Green, director of Planetary Science at NASA, and this Gravity Assist. With me today is David Grinspoon. He’s an astrobiologist, a senior scientist with the Planetary Science Institute, and today we’re talking about Earth’s twin planet, Venus.
David did some early work in his PhD on Venus. What was that like? And, what did you do?
David Grinspoon: Well, when I was in grad school in the 1980s, there was this new idea about large-impact events affecting planets. You know, we had recently discovered this amazing fact that Earth in an event 65 million years ago that knocked out the dinosaurs and caused an extinction.
So, people were starting to wonder, “What else have large impacts done in the solar system?” And, I had a couple of mentors who suggested that I look at some other atmospheres. And, I started just being drawn towards the fact that Venus is so similar to Earth, and yet so different, and wondering what large impacts did to Venus.
And, that led me to work on things like what happens when comets hit Venus and what does that do to the amount of water in such a dry planet? And, what was the early climate of Venus like compared to Earth, under the influence of being pummeled by a lot of impacts?
It’s basically how I learned to do climate modeling, was by considering these sort of weird scenarios of early atmospheres and what might have been happening to them under the influence of violent impacts.
Jim Green: Even though Venus is about the size of the Earth, it’s very different in many ways. What do you think is happening on Venus that makes it so different?
David Grinspoon: Well, that’s one of the very compelling questions about Venus, because it’s so Earth-like in terms of its bulk properties. If you just ask the most basic questions, “What’s the size of it? What’s the mass of it? Where is it located in the solar system?” you’d say, “Wow, it’s just like Earth in all these ways.”
And, then you’d start looking at, what’s the environment like? And, you’d go, “Whoa, that’s not at all like Earth,” because it’s so incredibly hot and so incredibly dry. So, it’s evolved in a different direction.
And, so when you start talking about Venus today and comparing it to Earth, you’re led to these questions of not just what’s happening there now, but how has it evolved, you know, and how did those two planets head down such different paths?
Obviously, for Venus, it’s a story of somehow having lost its oceans and lost what we think of as a more pleasant climate a long time ago in the past, and trying to understand that sort of divergence of conditions away from what we believe was more Earth-like a lot time ago.
Jim Green: So, how does Venus help us understand what Earth’s climate is like?
David Grinspoon: Well, it serves as an interesting laboratory for us to test a lot of our ideas about climate and atmospheric processes on a planet that, again, is somewhat Earth-like in some ways, and somehow very, very different in other ways. But, you know, with climate and the environment, a lot of it has the same physics and chemistry in different situations.
So, you know, everybody knows about the greenhouse effect on Earth and how carbon dioxide is part of that. Well, picture a planet just like Earth, where the atmosphere is almost all carbon dioxide basically, and what would that do to climate? You know, it’s an interesting sort of thought experiment, but it’s also a real experiment because we have this planet next door, Venus, which is basically all carbon dioxide.
And, many other aspects of Earth are sort of almost exaggerated on Venus, too. You’ve heard about acid rain. The clouds on Venus are sulfuric acid, so it’s sort of the extreme case of acid rain. So, that’s also allowed us to study, again, an Earth environmental issue in almost an exaggerated form.
And, so, this is just something that kind of makes us smarter about the problems and the puzzles that we encounter on Earth, by seeing them in an altered, and sometimes exaggerated form, on a nearby planet.
Jim Green: Venus isn’t actually that very far away from us, nor is it very far away from the Sun in the sense that our two planets have evolved, at the moment, very differently. But, what was Venus like early on in its evolution, do you think?
David Grinspoon: Well, that’s a great question, and of course, that’s one of the mysteries that compels us in our research and exploration, is to try to get a more clear picture of the earliest history of Venus. We have a lot of circumstantial evidence that leads us to believe it was a much more Earth-like planet a long time ago.
For instance, there’s the fact that Venus is so incredibly dry today. In fact, if you add up the amount of water on Venus and compare it to what we think is the amount of water on Earth--I say it like that because we don’t actually know how much water is hidden inside the Earth.
But, it’s something like, 100,000 times as much water on Earth than on Venus, which is really strange, because we picture them probably having formed with roughly the same amount, because they formed nearby out of similar materials. So, we think Venus had oceans and we think it had a more sort of pleasant climate, possibly even for life, early on, and we’ve got some other circumstantial evidence about that.
So, my best guess is that it was much more Earth-like early on. I would say an informed guess, but there’s still a lot of mystery there and a lot of experiments we’d like to do and measurements we’d like to make to try to sort of pin down that early history much more clearly.
Jim Green: One of the things that’s fascinated me about Venus is that it rotates in the opposite direction, and it rotates very slowly. How has that affected its evolution, do you think?
David Grinspoon: Yeah, it’s an interesting fact that, you know, almost all the planets rotate in the same direction as Earth does. So, if you’re standing on their surfaces, the Sun rises in the east and sets in the west, like we’re used to.
If you were on the surface of Venus, assuming you could see the Sun, which, you know, would be hard because it’s so cloudy there, but the Sun would actually rise in the west and set in the east. And, it would do so very, very slowly, because the planet rotates incredibly slowly.
So, in fact, if you’re on Venus, you could walk fast enough to keep the sunset in the same place. You could walk as fast as the Sun is moving around the planet. I did that calculation once and I was like, “Wow, well that would be kind of neat. You could watch the sunset forever just by walking.”
But, you know, how that fits into the evolution is a fascinating question. We don’t fully understand the cause of that. We surmise that it’s related, both to the early impact history of Venus, just as Earth’s rotation and Earth’s moon are related to the early impact history of the Earth and setting the Earth spinning in a certain way.
You know, the planets formed by these big collisions and the final few were probably very violent. So, the geometry of those final few collisions, which way they hit, probably really influenced that spin.
But, on Venus, there’s also the fact that we have this incredibly thick atmosphere, 100 times almost as thick as Earth’s, and that can cause a sort of drag on the rotation of the planet through what we call tides, atmospheric and solar tides, which are just these phenomena of the mass of the atmosphere itself can actually pull on the planet’s rotation over a long period of time. So, that might have to do with how slowly it’s rotating.
We’re not sure about its total evolution of the rotation rate over time. But, as far as rotating in the sort of backwards direction, if you will, we think that probably has to do with large impacts early on in its history, when it was still forming.
Jim Green: Yeah, that’s fascinating. You know, maybe that means that over time, Venus will end up being tidally locked with the Sun. And, then, we’re going to have a completely different environment, perhaps, with the extremes in temperature on both sides.
David Grinspoon: Yeah, that’s really an intriguing possibility that Venus, moving so slowly, could be on its way to being tidally-locked, and that at some point, probably in the pretty distant future--I don’t think we have to start revising our models too quickly. But, it could actually become a locked planet, like we think a lot of these exoplanets are, where one side is permanently facing the star.
Jim Green: As you mentioned, Venus has this huge pressure and enormous clouds that are very opaque. But, you know, we have been able to penetrate through those.
One mission was called Magellan. What was the most important set of observations that came from the Magellan spacecraft?
David Grinspoon: Magellan was an amazing mission. It really revolutionized our understanding of this neighboring planet. Before then, we had a couple of pictures of a couple of spots on the surface from these Russian landers, which were amazingly able to operate under those extreme surface conditions briefly in the ‘70s and the ‘80s.
And, we had a couple of sort of vague images from radar of parts of the planet, but with Magellan, we were able to orbit and basically get images of--get maps of the entire surface, almost the entire surface, by using radar, which as you say, penetrates through those clouds. It does sort of flash photography almost, bouncing radar off the surface, and then you see that image and you build up what the planet looks like.
And, that revolutionized our view of Venus in so many ways. One thing we learned was how volcanically interesting Venus is. Its surface is almost completely covered, in one way or another, with volcanic features, these broad plains, flat plains that we think of as flood basalts, like we have some areas on Earth. The Pacific Northwest comes to mind of these big flood basalt areas.
And, then other kinds of volcanoes, these steep shield volcanoes, like Hawaiian style shield volcanoes. So, I think of Venus almost as volcano world. It immediately sharpened the question of, is it still volcanically active?
And, since--ever since Magellan, we’ve been trying to nail that down. Again, we think we have some clues about that, but we don’t have what we sometimes refer to as the smoking gun, telling us it’s definitely volcanically active.
But, now that we know from Magellan there’s volcanoes all over the place, that’s sort of the next question. Are they still going?
Jim Green: Right. I mean, supplying carbon dioxide into the atmosphere, is that believed to be because of the volcanoes?
David Grinspoon: Well, over the long term, yes. I mean, that’s how CO2 gets--the main way CO2 gets supplied to planetary atmospheres. But, we don’t really know if Venus requires an active supply now, because there may be nothing removing CO2 from the atmosphere.
You know, on Earth, we have this cycle where CO2 is supplied by volcanoes and well, now by factories and cars, too, but, historically, by volcanoes. And, then, you know, it’s removed from the atmosphere by these, what we call weathering reactions, that are facilitated by water running over rocks and pulling CO2 out and making carbonate rocks.
Venus has no surface water, so it may not really have any way of removing CO2 from the atmosphere. But, we do see other things in the atmosphere that may require an ongoing volcanic source.
We see all these sulfur gasses, SO2, sulfuric acid, and it may be that chemical reactions are always removing those from--with surface minerals, reacting with surface minerals. So, in fact, the sulfur gasses we see on Venus today may require an ongoing source of volcanic gasses.
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