Difference between revisions of "October 19, 2004"

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=Rays of Light=
 
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<td width="50%"><h2><nobr>Rays of Light</nobr></h2></td>
 
 
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<tr><td><div align="center" class="main_sm">Image Credit: [mailto:rspellman@mindspring.com Robert Spellman]</p>
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<tr><td><div align="center" class="main_sm"><p>Image Credit: [mailto:rspellman@mindspring.com Robert Spellman]</p>
 
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<p align="center"><b>Rays of Light</b></p>
 
<p align="center"><b>Rays of Light</b></p>
 
<p align="left">As the sun rises over a crater, its rim casts a long shadow across the floor. If the rim were of even height and the floor were perfectly flat, the shadow would be a smooth curve. This is what most small simple craters look like (the [[September_23,_2004|BIO]] types). But larger craters have more topographic variations in their rims and floors. Long sunrise (or sunset) shadows map out local high spots in the rim, and bright bands or rays between shadows mark where the peaks are lower. And the neat thing is that these bright and dark rays are fun to observe, partially because they are only visible for a few hours each month. Here Robert Spellman has captured shadows and bright cones streaking the floor of the crater la Condamine in the rubble behind Sinus Iridum. By use of a video camera, he documented variations in the bright and darks bands through time. The upper left image was taken at 2:14 UT and the bottom right one was 26 minutes later. You can see that the shadows shortened slightly. On the mouseover image I have drawn lines that bound the bright and dark bands and show how they connect back to locally high (H) and low (L) spots on the crater rim. On Robert's web site he also shows the Lunar Orbiter IV image that I have annotated to match his photos. The Orbiter image shows that the rim of la Condamine is mostly even except for where it has been cut by secondary craters. The image also shows that la Condamine is a floor-fractured crater with an uneven floor. So here, I would guess, shadows and bright bands are mostly due to rim height variations, with some complexity added by floor roughness.  </p>
 
<p align="left">As the sun rises over a crater, its rim casts a long shadow across the floor. If the rim were of even height and the floor were perfectly flat, the shadow would be a smooth curve. This is what most small simple craters look like (the [[September_23,_2004|BIO]] types). But larger craters have more topographic variations in their rims and floors. Long sunrise (or sunset) shadows map out local high spots in the rim, and bright bands or rays between shadows mark where the peaks are lower. And the neat thing is that these bright and dark rays are fun to observe, partially because they are only visible for a few hours each month. Here Robert Spellman has captured shadows and bright cones streaking the floor of the crater la Condamine in the rubble behind Sinus Iridum. By use of a video camera, he documented variations in the bright and darks bands through time. The upper left image was taken at 2:14 UT and the bottom right one was 26 minutes later. You can see that the shadows shortened slightly. On the mouseover image I have drawn lines that bound the bright and dark bands and show how they connect back to locally high (H) and low (L) spots on the crater rim. On Robert's web site he also shows the Lunar Orbiter IV image that I have annotated to match his photos. The Orbiter image shows that the rim of la Condamine is mostly even except for where it has been cut by secondary craters. The image also shows that la Condamine is a floor-fractured crater with an uneven floor. So here, I would guess, shadows and bright bands are mostly due to rim height variations, with some complexity added by floor roughness.  </p>
<blockquote><p align="right">&#8212; [mailto:tychocrater@yahoo.com Chuck Wood]</blockquote>
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<blockquote>
<p align="left"><p><b>Technical Details:</b><br>
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<p align="right">&#8212; [mailto:tychocrater@yahoo.com Chuck Wood]</p></blockquote>
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<p align="left"><b>Technical Details:</b><br>
 
5" refractor equiped with a Supercircuts PC-23 video camera and recorded on a Panasonic DVD recorder. </p>
 
5" refractor equiped with a Supercircuts PC-23 video camera and recorded on a Panasonic DVD recorder. </p>
 
<p><b>Related Links:</b><br>
 
<p><b>Related Links:</b><br>
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<br>Rukl <i>Atlas of the Moon,</i> Sheet 2
 
<br>Rukl <i>Atlas of the Moon,</i> Sheet 2
 
<br>[http://www.lunar-occultations.com/rlo/rays/rays.htm Robinson Observatory - Sunrise & Sunset Rays]
 
<br>[http://www.lunar-occultations.com/rlo/rays/rays.htm Robinson Observatory - Sunrise & Sunset Rays]
<p align="left"><b>Tomorrow's LPOD: </b> Rough Domes</p>
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</p>
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<p><b>Yesterday's LPOD:</b> [[October 18, 2004|1826 Moon]] </p>
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<p><b>Tomorrow's LPOD:</b> [[October 20, 2004|Rough Domes]] </p>
 
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<p align="center" class="main_titles"><b>Author &amp; Editor:</b><br>  
 
<p align="center" class="main_titles"><b>Author &amp; Editor:</b><br>  
 
[mailto:tychocrater@yahoo.com Charles A. Wood]</p>
 
[mailto:tychocrater@yahoo.com Charles A. Wood]</p>
<p align="center" class="main_titles"><b>Technical Consultant:</b><br>
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[mailto:anthony@perseus.gr Anthony Ayiomamitis]</p>
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<p align="center" class="main_titles"><b>Contact Translator:</b><br>
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[mailto:pablolonnie@yahoo.com.mx Pablo Lonnie Pacheco Railey]  (Es)<br>
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[mailto:chlegrand@free.fr Christian Legrand] (Fr)</p>
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<p align="center" class="main_titles"><b>[mailto:webuser@observingthesky.org Contact Webmaster]</b></p>
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<p align="center" class="main_titles"><b>A service of:</b><br>
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[http://www.observingthesky.org/ ObservingTheSky.Org]</p>
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<!-- Cleanup of credits -->
<p align="center" class="main_titles"><b>Visit these other PODs:</b> <br>
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[http://antwrp.gsfc.nasa.gov/apod/astropix.html Astronomy] | [http://www.msss.com/ Mars] | [http://epod.usra.edu/ Earth]</p>
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<p>&nbsp;</p>
 
<p>&nbsp;</p>
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===COMMENTS?===
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Latest revision as of 15:01, 15 March 2015

Rays of Light


LPOD-2004-10-19.jpeg

LPOD-2004-10-19b.jpeg

Image Credit: Robert Spellman


Rays of Light

As the sun rises over a crater, its rim casts a long shadow across the floor. If the rim were of even height and the floor were perfectly flat, the shadow would be a smooth curve. This is what most small simple craters look like (the BIO types). But larger craters have more topographic variations in their rims and floors. Long sunrise (or sunset) shadows map out local high spots in the rim, and bright bands or rays between shadows mark where the peaks are lower. And the neat thing is that these bright and dark rays are fun to observe, partially because they are only visible for a few hours each month. Here Robert Spellman has captured shadows and bright cones streaking the floor of the crater la Condamine in the rubble behind Sinus Iridum. By use of a video camera, he documented variations in the bright and darks bands through time. The upper left image was taken at 2:14 UT and the bottom right one was 26 minutes later. You can see that the shadows shortened slightly. On the mouseover image I have drawn lines that bound the bright and dark bands and show how they connect back to locally high (H) and low (L) spots on the crater rim. On Robert's web site he also shows the Lunar Orbiter IV image that I have annotated to match his photos. The Orbiter image shows that the rim of la Condamine is mostly even except for where it has been cut by secondary craters. The image also shows that la Condamine is a floor-fractured crater with an uneven floor. So here, I would guess, shadows and bright bands are mostly due to rim height variations, with some complexity added by floor roughness.

Chuck Wood

Technical Details:
5" refractor equiped with a Supercircuts PC-23 video camera and recorded on a Panasonic DVD recorder.

Related Links:
Robert's Web Site
Lunar Orbiter IV View
Rukl Atlas of the Moon, Sheet 2
Robinson Observatory - Sunrise & Sunset Rays

Yesterday's LPOD: 1826 Moon

Tomorrow's LPOD: Rough Domes



Author & Editor:
Charles A. Wood

 


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