tides on earth, in the solar system and beyond….....rosetta_cd\pr\what_is_rs.ppt, 10.06.2011...

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Rosetta_CD\PR\what_is_RS.ppt, 10.06.2011 12:36AM, 1 483rd WE-Heraeus Seminar Extrasolar Planets: Towards Comparative Planetology beyond the Solar System Tides on Earth, in the Solar System and Beyond….. Martin Pätzold Rheinisches Institut für Umweltforschung an der Universität zu Köln Abteilung Planetenforschung Köln

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Page 1: Tides on Earth, in the Solar System and Beyond….....Rosetta_CD\PR\what_is_RS.ppt, 10.06.2011 12:36AM, 1 483rd WE-Heraeus Seminar Extrasolar Planets: Towards Comparative Planetology

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483rd WE-Heraeus SeminarExtrasolar Planets:

Towards Comparative Planetology beyond the Solar System

Tideson Earth,

in the Solar System and Beyond…..

Martin Pätzold Rheinisches Institut für Umweltforschung

an der Universität zu KölnAbteilung Planetenforschung

Köln

Page 2: Tides on Earth, in the Solar System and Beyond….....Rosetta_CD\PR\what_is_RS.ppt, 10.06.2011 12:36AM, 1 483rd WE-Heraeus Seminar Extrasolar Planets: Towards Comparative Planetology

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tide levels for Hamburg, Sankt Pauli:

Tuesday, 7th June 2011 (CEST)

Low tide 04:03 0.3 m

High tide 09:07 3.9 m

Low tide 16:07 0.4 m

High tide 21:16 4.3 m

Bundesamt für Seeschifffahrt und Hydrographie

Page 8: Tides on Earth, in the Solar System and Beyond….....Rosetta_CD\PR\what_is_RS.ppt, 10.06.2011 12:36AM, 1 483rd WE-Heraeus Seminar Extrasolar Planets: Towards Comparative Planetology

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Mont St. Michel, Bretagne

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, 11 The tidal force is a differenced force!

Page 12: Tides on Earth, in the Solar System and Beyond….....Rosetta_CD\PR\what_is_RS.ppt, 10.06.2011 12:36AM, 1 483rd WE-Heraeus Seminar Extrasolar Planets: Towards Comparative Planetology

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, 12 The formation of the tidal bulge is

usually known as the (high) tide

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Revolution without rotation

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Revolution without rotation But the Earth rotates!

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• The Earth rotates faster than the Moon revolves

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• The Earth rotates faster than the Moon revolves

• The tidal bulge is advancing the direct LOS

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• The Earth rotates faster than the Moon revolves

• The tidal bulge is advancing the direct LOS

• Torques try to pull the tidal bulge back into LOS

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• The Earth rotates faster than the Moon revolves

• The tidal bulge is advancing the direct LOS

• Torques try to pull the tidal bulge back into LOS

• Consequence is a slow down of Earth rotation (tidal friction)

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chan

gein

LO

D re

lativ

e to

864

00 s

average change in LOD due to lunar tides:2.3 ms/cy

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• The Earth rotates faster than the Moon revolves

• The tidal bulge is advancing the direct LOS

• Torques try to pull the tidal bulge back into LOS

• Consequence is a slow down of Earth rotation (tidal friction)

• another consequence from conservation of angular momentum: the Moon recedes from the Earth

Page 21: Tides on Earth, in the Solar System and Beyond….....Rosetta_CD\PR\what_is_RS.ppt, 10.06.2011 12:36AM, 1 483rd WE-Heraeus Seminar Extrasolar Planets: Towards Comparative Planetology

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The first extraterrestrial applied space geophysicist

seismometer Lunar Laser RangingReflector

Buzz Aldrin, Apollo 11, 1969

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Lunar Laser Ranging

Apollo 15 reflector

Wettzell Lunar Laser Station

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Lunar Laser Ranging

Apollo 15 reflector

Wettzell Lunar Laser Station

The Moon recedes from Earth by 4m/cy

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• The Earth rotates faster than the Moon revolves

• The tidal bulge is advancing the direct LOS by 3°

• Earth rotates below the tidal bulge

• A location on the surface experiences periodically high and low tides

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Ocean tides are the directly visiblemanifestation of tidal forces

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• The Earth rotates faster than the Moon revolves

• The tidal bulge is advancing the direct LOS

• Torques try to pull the tidal bulge back into LOS

• Consequence is a slow down of Earth rotation (tidal friction)

• another consequence from conservation of angular momentum: the Moon recedes from the Earth

Is there a case in the solar system wherea moon revolves faster than the planet rotates?

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• The Earth rotates faster than the Moon revolves

• The tidal bulge is advancing the direct LOS

• Torques try to pull the tidal bulge back into LOS

• Consequence is a slow down of Earth rotation (tidal friction)

• another consequence from conservation of angular momentum: the Moon recedes from the Earth

Is there a case in the solar system wherea moon revolves faster than the planet rotates?

YES, there is!

Page 28: Tides on Earth, in the Solar System and Beyond….....Rosetta_CD\PR\what_is_RS.ppt, 10.06.2011 12:36AM, 1 483rd WE-Heraeus Seminar Extrasolar Planets: Towards Comparative Planetology

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The Mars/Phobos case

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The Mars/Phobos case

Phobossize : 26 x 22 x 18 kmperiod : 7 h 39 mdistance : 9,378 km

Deimossize : 15 x 12 x 10 kmperiod : 30 h 17 mdistance : 23,459 km

Marsradius : 3,990 km period : 24 h 37 m

Page 30: Tides on Earth, in the Solar System and Beyond….....Rosetta_CD\PR\what_is_RS.ppt, 10.06.2011 12:36AM, 1 483rd WE-Heraeus Seminar Extrasolar Planets: Towards Comparative Planetology

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The Mars/Phobos case

Phobossize : 26 x 22 x 18 kmperiod : 7 h 39 mdistance : 9,378 km

Deimossize : 15 x 12 x 10 kmperiod : 30 h 17 mdistance : 23,459 km

synchronous orbit:planetary rotation = moon revolution

Mars24 h 37 m

21,000 km distancePhobos: inside

Deimos: outside

Marsradius : 3,990 km period : 24 h 37 m

Page 31: Tides on Earth, in the Solar System and Beyond….....Rosetta_CD\PR\what_is_RS.ppt, 10.06.2011 12:36AM, 1 483rd WE-Heraeus Seminar Extrasolar Planets: Towards Comparative Planetology

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The Mars/Phobos case

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The Mars/Phobos case

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The Mars/Phobos case

The orbit of Phobos decays until the Roche limit is reached.

1/ 3 1/ 3

P PR S P

S S

Ma cR cRM

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The Mars/Phobos case

The orbit of Phobos decays until the Roche limit is reached.

Roche limit:

Proportionality factor c depends on the nature of thesecondary: fluid c = 2.44 => aR = 10,500 km

solid c = 1.26 => aR = 5,500 km rubble pile c = 1.54 => aR = 6,700 km

1/ 3 1/ 3

P PR S P

S S

Ma cR cRM

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The Mars/Phobos case

The orbit of Phobos decays until the Roche limit is reached.

Roche limit:

Proportionality factor c depends on the nature of thesecondary: fluid c = 2.44 => aR = 10,500 km

solid c = 1.26 => aR = 5,500 km rubble pile c = 1.54 => aR = 6,700 km

Phobos is highly porous => „rubble pile“ (Andert et al., 2010)

1/ 3 1/ 3

P PR S P

S S

Ma cR cRM

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When will Phobos reach the Roche limit?

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R

RocheMars Ph

Mars MarsMars Mars

a a

k M R GMQ M

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When will Phobos reach the Roche limit?

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Mars MarsMars Mars

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When will Phobos reach the Roche limit?

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Other tidal phenomena in the solar system

• forcing Mercury in a 3/2 resonance• forcing all moons in the solar system into synchronous

rotation• deforming the Jupiter moon Io periodically => tidal

heating => volcanic activity• and the non-plus-ultra:

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Other tidal phenomena in the solar system

• forcing Mercury in a 3/2 resonance• forcing all moons in the solar system into synchronous

rotation• deforming the Jupiter moon Io periodically => tidal

heating => volcanic activity• and the non-plus-ultra: synchronizing the Pluto system

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Tides in extrasolar systems

• studying tides in extrasolar planetary systems requires the knowledge of mass and size of the planet and the star

• feasible with transiting planets combined with radial velocity observations and spectroscopy

• orbital decay => survivability• stellar spin-up• spin-orbit coupling => synchronization of rotation and revolution• circularization => e -> 0

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The tidal potential or the Doodson constant

two tidal potentials:a)The primary acting on the secondaryb) The secondary acting on the primary

23

pps s

GMD R

a 2

3s

sp pGMD Ra

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The tidal potential or the Doodson constant

two tidal potentials:a) The primary acting on the secondaryb) The secondary acting on the primary

Earth/Moon system:Earth on Moon Moon on EarthDps = 20.9 m2/s2 Dsp = 3.5 m2/s2

Sun on EarthDsp = 1.6 m2/s2

23

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GMD R

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sp pGMD Ra

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When will the planet reach the stellar Roche limit?

13 / 2 13 / 2

52,

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3

R

Rochestar P

star starstar star

a a

k M R GMQ M

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When will the planet reach the stellar Roche limit?

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R

Rochestar P

star starstar star

a a

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stellar property factor

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When will the planet reach the stellar Roche limit?

13 / 2 13 / 2

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R

Rochestar P

star starstar star

a a

k M R GMQ M

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• tidal forces affect the evolution of extrasolar planetary systems

• if a < 0.1 AU• if Mp is large• may force orbits towards e -> 0• may lead to the loss of companions• may force massive companions into double-

synchronous rotation• but the companion is not safe….

• may spin-up stellar rotation (look for old fast rotating stars)

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…book your next boat tour when the tide is in!