Steepness of Slopes at the Luna-Glob Landing Sites: Estimating by the Shaded Area Percentage in the LROC NAC Images
The paper presents estimates of the occurrence probability of slopes, whose steep surfaces could be dangerous for the landing of the Luna-Glob descent probe ( Luna -25) given the baseline of the span between the landing pads (~3.5 m), for five potential landing ellipses. As a rule, digital terrain m...
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description | The paper presents estimates of the occurrence probability of slopes, whose steep surfaces could be dangerous for the landing of the
Luna-Glob
descent probe (
Luna
-25) given the baseline of the span between the landing pads (~3.5 m), for five potential landing ellipses. As a rule, digital terrain models built from stereo pairs of high-resolution images (here, the images taken by the Narrow Angle Camera onboard the Lunar Reconnaissance Orbiter (LROC NAC)) are used in such cases. However, the planned landing sites are at high latitudes (67°–74° S), which makes it impossible to build digital terrain models, since the difference in the observation angle of the overlapping images is insufficient at these latitudes. Because of this, to estimate the steepness of slopes, we considered the interrelation between the shaded area percentage in the image and the Sun angle over horizon at the moment of imaging. For five proposed landing ellipses, the LROC NAC images (175 images in total) with a resolution from 0.4 to 1.2 m/pixel were analyzed. From the results of the measurements in each of the ellipses, the dependence of the shaded area percentage on the solar angle were built, which was converted to the occurrence probability of slopes. For this, the data on the
Apollo 16
landing region ware used, which is covered by both the LROC NAC images and the digital terrain model with high resolution. As a result, the occurrence probability of slopes with different steepness has been estimated on the baseline of 3.5 m for five landing ellipses according to the steepness categories of 20°. |
doi_str_mv | 10.1134/S0038094618010045 |
format | Article |
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Luna-Glob
descent probe (
Luna
-25) given the baseline of the span between the landing pads (~3.5 m), for five potential landing ellipses. As a rule, digital terrain models built from stereo pairs of high-resolution images (here, the images taken by the Narrow Angle Camera onboard the Lunar Reconnaissance Orbiter (LROC NAC)) are used in such cases. However, the planned landing sites are at high latitudes (67°–74° S), which makes it impossible to build digital terrain models, since the difference in the observation angle of the overlapping images is insufficient at these latitudes. Because of this, to estimate the steepness of slopes, we considered the interrelation between the shaded area percentage in the image and the Sun angle over horizon at the moment of imaging. For five proposed landing ellipses, the LROC NAC images (175 images in total) with a resolution from 0.4 to 1.2 m/pixel were analyzed. From the results of the measurements in each of the ellipses, the dependence of the shaded area percentage on the solar angle were built, which was converted to the occurrence probability of slopes. For this, the data on the
Apollo 16
landing region ware used, which is covered by both the LROC NAC images and the digital terrain model with high resolution. As a result, the occurrence probability of slopes with different steepness has been estimated on the baseline of 3.5 m for five landing ellipses according to the steepness categories of <7°, 7°–10°, 10°–15°, 15°–20°, and >20°.</description><identifier>ISSN: 0038-0946</identifier><identifier>EISSN: 1608-3423</identifier><identifier>DOI: 10.1134/S0038094618010045</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Astronomy ; Astrophysics and Astroparticles ; Astrophysics and Cosmology ; Digital imaging ; Ellipses ; High resolution ; Image resolution ; Landing sites ; Lunar spacecraft ; Observations and Techniques ; Physics ; Physics and Astronomy ; Planetology ; Slopes ; Terrain ; Terrain models</subject><ispartof>Solar system research, 2018-03, Vol.52 (2), p.87-97</ispartof><rights>Pleiades Publishing, Inc. 2018</rights><rights>Solar System Research is a copyright of Springer, (2018). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c316t-7005521395ded1d820cbbe8eb99124b4d3c817f6e5b725c9b84f4877090a9e483</citedby><cites>FETCH-LOGICAL-c316t-7005521395ded1d820cbbe8eb99124b4d3c817f6e5b725c9b84f4877090a9e483</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S0038094618010045$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S0038094618010045$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Krasilnikov, S. S.</creatorcontrib><creatorcontrib>Basilevsky, A. T.</creatorcontrib><creatorcontrib>Ivanov, M. A.</creatorcontrib><creatorcontrib>Abdrakhimov, A. M.</creatorcontrib><creatorcontrib>Kokhanov, A. A.</creatorcontrib><title>Steepness of Slopes at the Luna-Glob Landing Sites: Estimating by the Shaded Area Percentage in the LROC NAC Images</title><title>Solar system research</title><addtitle>Sol Syst Res</addtitle><description>The paper presents estimates of the occurrence probability of slopes, whose steep surfaces could be dangerous for the landing of the
Luna-Glob
descent probe (
Luna
-25) given the baseline of the span between the landing pads (~3.5 m), for five potential landing ellipses. As a rule, digital terrain models built from stereo pairs of high-resolution images (here, the images taken by the Narrow Angle Camera onboard the Lunar Reconnaissance Orbiter (LROC NAC)) are used in such cases. However, the planned landing sites are at high latitudes (67°–74° S), which makes it impossible to build digital terrain models, since the difference in the observation angle of the overlapping images is insufficient at these latitudes. Because of this, to estimate the steepness of slopes, we considered the interrelation between the shaded area percentage in the image and the Sun angle over horizon at the moment of imaging. For five proposed landing ellipses, the LROC NAC images (175 images in total) with a resolution from 0.4 to 1.2 m/pixel were analyzed. From the results of the measurements in each of the ellipses, the dependence of the shaded area percentage on the solar angle were built, which was converted to the occurrence probability of slopes. For this, the data on the
Apollo 16
landing region ware used, which is covered by both the LROC NAC images and the digital terrain model with high resolution. As a result, the occurrence probability of slopes with different steepness has been estimated on the baseline of 3.5 m for five landing ellipses according to the steepness categories of <7°, 7°–10°, 10°–15°, 15°–20°, and >20°.</description><subject>Astronomy</subject><subject>Astrophysics and Astroparticles</subject><subject>Astrophysics and Cosmology</subject><subject>Digital imaging</subject><subject>Ellipses</subject><subject>High resolution</subject><subject>Image resolution</subject><subject>Landing sites</subject><subject>Lunar spacecraft</subject><subject>Observations and Techniques</subject><subject>Physics</subject><subject>Physics and Astronomy</subject><subject>Planetology</subject><subject>Slopes</subject><subject>Terrain</subject><subject>Terrain models</subject><issn>0038-0946</issn><issn>1608-3423</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kE9Lw0AQxRdRsFY_gLcFz9H9l-zGWym1FoIVo-ewm0zalHYTd7eHfnsTI3gQTwPv_d4bZhC6peSeUi4eckK4IqlIqCKUEBGfoQlNiIq4YPwcTQY7GvxLdOX9jgyQTCbI5wGgs-A9bmuc79sOPNYBhy3g7Gh1tNy3BmfaVo3d4LwJ4B_xwofmoMOgmNM3mm91BRWeOdD4FVwJNugN4MaORW_rOX6ZzfHq0Kv-Gl3Ueu_h5mdO0cfT4n3-HGXr5Wo-y6KS0yREkpA4ZpSncV9NK8VIaQwoMGlKmTCi4qWisk4gNpLFZWqUqIWSkqREpyAUn6K7sbdz7ecRfCh27dHZfmXBCKMyFpKJnqIjVbrWewd10bn-OncqKCmG3xZ_fttn2JjxPWs34H6b_w99ATHMeIc</recordid><startdate>20180301</startdate><enddate>20180301</enddate><creator>Krasilnikov, S. S.</creator><creator>Basilevsky, A. T.</creator><creator>Ivanov, M. A.</creator><creator>Abdrakhimov, A. M.</creator><creator>Kokhanov, A. A.</creator><general>Pleiades Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>H8D</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L7M</scope><scope>M2P</scope><scope>P5Z</scope><scope>P62</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope></search><sort><creationdate>20180301</creationdate><title>Steepness of Slopes at the Luna-Glob Landing Sites: Estimating by the Shaded Area Percentage in the LROC NAC Images</title><author>Krasilnikov, S. S. ; Basilevsky, A. T. ; Ivanov, M. A. ; Abdrakhimov, A. M. ; Kokhanov, A. A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c316t-7005521395ded1d820cbbe8eb99124b4d3c817f6e5b725c9b84f4877090a9e483</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Astronomy</topic><topic>Astrophysics and Astroparticles</topic><topic>Astrophysics and Cosmology</topic><topic>Digital imaging</topic><topic>Ellipses</topic><topic>High resolution</topic><topic>Image resolution</topic><topic>Landing sites</topic><topic>Lunar spacecraft</topic><topic>Observations and Techniques</topic><topic>Physics</topic><topic>Physics and Astronomy</topic><topic>Planetology</topic><topic>Slopes</topic><topic>Terrain</topic><topic>Terrain models</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Krasilnikov, S. S.</creatorcontrib><creatorcontrib>Basilevsky, A. T.</creatorcontrib><creatorcontrib>Ivanov, M. A.</creatorcontrib><creatorcontrib>Abdrakhimov, A. M.</creatorcontrib><creatorcontrib>Kokhanov, A. A.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ProQuest Central Student</collection><collection>Aerospace Database</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Science Database</collection><collection>Advanced Technologies & Aerospace Database</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><jtitle>Solar system research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Krasilnikov, S. S.</au><au>Basilevsky, A. T.</au><au>Ivanov, M. A.</au><au>Abdrakhimov, A. M.</au><au>Kokhanov, A. A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Steepness of Slopes at the Luna-Glob Landing Sites: Estimating by the Shaded Area Percentage in the LROC NAC Images</atitle><jtitle>Solar system research</jtitle><stitle>Sol Syst Res</stitle><date>2018-03-01</date><risdate>2018</risdate><volume>52</volume><issue>2</issue><spage>87</spage><epage>97</epage><pages>87-97</pages><issn>0038-0946</issn><eissn>1608-3423</eissn><abstract>The paper presents estimates of the occurrence probability of slopes, whose steep surfaces could be dangerous for the landing of the
Luna-Glob
descent probe (
Luna
-25) given the baseline of the span between the landing pads (~3.5 m), for five potential landing ellipses. As a rule, digital terrain models built from stereo pairs of high-resolution images (here, the images taken by the Narrow Angle Camera onboard the Lunar Reconnaissance Orbiter (LROC NAC)) are used in such cases. However, the planned landing sites are at high latitudes (67°–74° S), which makes it impossible to build digital terrain models, since the difference in the observation angle of the overlapping images is insufficient at these latitudes. Because of this, to estimate the steepness of slopes, we considered the interrelation between the shaded area percentage in the image and the Sun angle over horizon at the moment of imaging. For five proposed landing ellipses, the LROC NAC images (175 images in total) with a resolution from 0.4 to 1.2 m/pixel were analyzed. From the results of the measurements in each of the ellipses, the dependence of the shaded area percentage on the solar angle were built, which was converted to the occurrence probability of slopes. For this, the data on the
Apollo 16
landing region ware used, which is covered by both the LROC NAC images and the digital terrain model with high resolution. As a result, the occurrence probability of slopes with different steepness has been estimated on the baseline of 3.5 m for five landing ellipses according to the steepness categories of <7°, 7°–10°, 10°–15°, 15°–20°, and >20°.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S0038094618010045</doi><tpages>11</tpages></addata></record> |
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subjects | Astronomy Astrophysics and Astroparticles Astrophysics and Cosmology Digital imaging Ellipses High resolution Image resolution Landing sites Lunar spacecraft Observations and Techniques Physics Physics and Astronomy Planetology Slopes Terrain Terrain models |
title | Steepness of Slopes at the Luna-Glob Landing Sites: Estimating by the Shaded Area Percentage in the LROC NAC Images |
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