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The mean location of the center of lapetus' leading side (the hemisphere facing the direction of lapetus' motion) is not at 90.0°W longitude, but rather at 93.5°W because the surface coordinate system is defined so as to place the crater Almeric at 276.0°W 04).
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Reference (18) mentions an increase of the dust flux by ∼20%, whereas (35) finds as much as a factor of 3 for some cases.
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Reference (18) mentions an increase of the dust flux by ∼20%, whereas (35) finds as much as a factor of 3 for some cases.
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23
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75749106897
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The leading sides of the moons beyond Mimas and inside Titan should be substantially coated by E-ring particles (24, 36, 37), making them less useful for this argument.
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The leading sides of the moons beyond Mimas and inside Titan should be substantially coated by E-ring particles (24, 36, 37), making them less useful for this argument.
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This idea was developed in several papers (18, 38, 39), but under the assumption that dust from the outer saturnian moons formed lapetus' albedo dichotomy.
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This idea was developed in several papers (18, 38, 39), but under the assumption that dust from the outer saturnian moons formed lapetus' albedo dichotomy.
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32
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75749126033
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note
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We acknowledge the individuals at CICLOPS (at the Space Science Institute in Boulder, CO) and JPL (Pasadena, CA), as well as the members and associates of the Imaging Team for the successful conduct of the ISS experiment onboard the Cassini spacecraft. This paper is dedicated to Steve Ostro, whose work helped considerably to explain the nature of lapetus' dark terrain. This work has been funded by the German Aerospace Center (DLR) and NASA/JPL.
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