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UA PTYS 206 - Venus

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Slide 1VenusSlide 3Slide 4Slide 5Slide 6Slide 7Slide 8Slide 9Slide 10Slide 11Slide 12Slide 13Slide 14Slide 15Slide 16Slide 17Slide 18Slide 19Slide 20Slide 21Slide 22Slide 23Slide 24Slide 25Slide 26Slide 27Slide 28Slide 29Slide 30Slide 31Slide 32Slide 33Slide 34Slide 35Slide 36PYTS/ASTR 206 – Venus1AnnouncementsTA change for HW3 and HW4Use Priyanka Sharma[email protected]Office hours: Tuesday 10.30am-12.30pmRoom 316, Kuiper BuildingKevin will return after becoming Dr. KevinHW3 available on the website todayDue in a weekPYTS/ASTR 206 – Venus2PTYS/ASTR 206 – The Golden Age of Planetary ExplorationShane Byrne – [email protected]/ASTR 206 – Venus3In this lecture…In this lecture…IntroductionRecap on Venus and its atmosphereSuper-rotationTides and retrograde rotationExploring VenusSurface landersRadar instrumentsSurface of VenusGeography and topographyVolcanoes everywhereCraters (or the lack of them)Wind actionInterior of VenusThin crusts Magnetic fieldsHistory of Venus – controlled by waterA habitable start…Where it all went horribly wrong…Why the Earth escaped the fate of VenusPYTS/ASTR 206 – Venus4One of the largest terrestrial planetsIntroductionIntroductionPYTS/ASTR 206 – Venus5Comparison to the EarthA sister planet?VenusSize 95% of the EarthMass 82% of the EarthDensity 5243 kg m-3About the same as EarthSolar Distance 0.72 AUYear 225 days, 62% of the EarthEccentricity 0.007 (almost zero)Circular orbit, like the EarthRoughlyThe SameInternalStructureRoughlyThe SameOrbitPYTS/ASTR 206 – Venus6You can see Venus for up to 3 hours after sunset or before sunriseThe brightest planet It’s covered in very reflective cloudsIt’s close to the SunIt’s close to usPYTS/ASTR 206 – Venus7Comparison with the Earth IIHow much solar radiation does Venus receive?Remember:Venus is 0.72 AU from the Sun: R=0.72So:Solar power at Venus is 2637 W m-2 (about twice that of Earth)…but Venus reflects 59% of this sunlight – thick cloud coverVenus actually absorbs only: 0.41*2637 W m-2 = 1082 W m-2 Not that different than a clear day at Earth’s equator!People thought that Venus might be some sort of tropical paradise…Nobody could see the surface though…Solar power = 1367 W m-2 / R2Solar power = 1367 W m-2 / 0.722PYTS/ASTR 206 – Venus8Differences from the EarthA sister planet? – not reallyVenusAtmosphere Mostly CO2 (Earth = Mostly nitrogen)Pressure 90 bars(Earth = 1 bar)Surface Temp. 750K(Earth = 300 K)(Molten rock ~ 1000 K)Clouds Sulfuric acid(Earth = water vapor)Rotation period 224 Days - retrograde(Earth = 1 day)Magnetic field None(Earth has a strong field)Surface All volcanic rock(Earth = mix of rock types)VeryDifferentAtmosphereVeryDifferentSurfaceVeryDifferentSpinPYTS/ASTR 206 – Venus9So Earth and Venus started off with similar compositions and positions in the solar systemWhat went wrong for Venus??The answer is in front of you…PYTS/ASTR 206 – Venus10So Earth and Venus started off with similar compositions and positions in the solar systemWhat went wrong for Venus??The answer is in front of you…WATER! – History of Venus depends on the history of its waterPYTS/ASTR 206 – Venus11The greenhouse effectBoth Earth and Venus are warmed by the greenhouse effectGreenhouse gases stop thermal radiation escaping to spaceEarth has ~0.01 bars of CO2 – Temperature boosted by ~30° CVenus has 86 bars of CO2 – Temperature boosted by ~400° CAtmosphere - recapAtmosphere - recapPYTS/ASTR 206 – Venus12Super-rotationClouds on Venus rotate in 4 days!People were surprised to learn later that the solid planet rotates only every 224 daysAtmosphere rotates faster than the planetPYTS/ASTR 206 – Venus13Venus’s weird rotation….Most planets rotate (and orbit) anti-clockwise(when viewed from above the North Pole)Venus rotates ‘backwards’Theories?Giant impactSolar tidesPYTS/ASTR 206 – Venus14Tidal effects on Spin?Venus has a huge massive atmosphere……and is close to the sunSolar tides can slow Venus’s rotationTidal bulge raised by SunRotation of Venus carries the bulge around the planetAttraction between the bulge and the Sun slows down Venus’s rotationEffects of tides - View from the sideSolar tides slow down Venus’s rotation, but don’t explain why it’s retrogradePYTS/ASTR 206 – Venus15Atmosphere is very heavy and rotates very quickly in a retrograde directionDrag of atmosphere on the solid planet might have reversed its spin directionThis only works because….The atmosphere is very massive and has lots of momentum…Solar tides already did most of the work…We have billions of years to get this done…The other possibility is a giant impact reversed Venus’s rotationSurfaceAtmospheric motionFriction from atmospheric dragon rough surfacePYTS/ASTR 206 – Venus16Clouds are very opaqueOrbiters use radar to see the surfaceNASA Magellan mission did the most complete mapping (1992-1994)Pioneer Venus (late 1970’s)Venera 15 and 16 (1980’s)Radar looks off to the sideLight/Dark tones don’t correspond to albedoStrong radar return from:Terrain that has roughness on the scale of the radar wavelength Large-scale slopes facing the spacecraftExploring VenusExploring VenusPYTS/ASTR 206 – Venus17Vertical radar system gathers topographySend radar pulses to surface – timed echoesConverted time delay to distance to figure out where the mountains and valleys arePYTS/ASTR 206 – Venus18Landed spacecraft hard to do on VenusOnly glimpse of the surfaceSoviets had 4 successful Venera landings on VenusOnboard experiments found basaltic surfaceDark surface, albedo of 3-10%Surface winds of ~ 0.3-1.0 m/sSurface temperatures of 740 KLanders lasted 45-60 minutesVenera 14 – 13 S, 310 E – March 1982PYTS/ASTR 206 – Venus19Spherical images can be unwraped into a low-res perspective viewSmooth-ish basaltic rock – low viscosity magmasVenera 9 – A Blockier AppearanceVenera 13PYTS/ASTR 206 – Venus20Earth has obvious topography dichotomyHigh continentsLow ocean floorsVenus has a unimodal hypsogramNo plate tectonicsSeveral volcanic plainsSeveral crustal plateaus Surface of VenusSurface of


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UA PTYS 206 - Venus

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