{"id":88,"date":"2018-01-05T18:26:28","date_gmt":"2018-01-05T23:26:28","guid":{"rendered":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/chapter\/2-5-are-there-other-earths-2\/"},"modified":"2021-07-02T20:35:06","modified_gmt":"2021-07-03T00:35:06","slug":"2-5-are-there-other-earths-2","status":"publish","type":"chapter","link":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/chapter\/2-5-are-there-other-earths-2\/","title":{"raw":"2.5 Are There Other Earths?","rendered":"2.5 Are There Other Earths?"},"content":{"raw":"As of July 2021, 4,777 <strong>exoplanets<\/strong>\u2014extrasolar planets, or planets outside of our solar system\u2014have been confirmed. An additional 4,640 potential exoplanets have been detected and await confirmation. The majority of exoplanets have been detected using the transit technique, which involves looking for periodic fluctuations in light from a star from planets transiting in front of the star, causing it to appear dimmer (Figure 2.15).\r\n\r\n&nbsp;\r\n\r\n[caption id=\"attachment_1433\" align=\"aligncenter\" width=\"650\"]<a href=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Transit-method.png\" rel=\"attachment wp-att-1433\"><img class=\"wp-image-1433\" src=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Transit-method.png\" alt=\"\" width=\"650\" height=\"424\" \/><\/a> <strong>Figure 2.15<\/strong> The transit method identifies stars with possible planets in orbit by looking for brief decreases in the brightness of the star. If this happens regularly, it could mean that a planet is periodically blocking some of the star's light. Source: Karla Panchuk (2021) CC BY-NC-SA. Modified after NASA\/HESARC\/TESS (2021), Public Domain. <a href=\"https:\/\/heasarc.gsfc.nasa.gov\/docs\/tess\/primary-science.html\">View source<\/a>. <a href=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/chapter\/2-5-are-there-other-earths-2\/transit-method\/\">Click for more attributions.<\/a>[\/caption]\r\n\r\nIf \"other Earths\" are defined as planets where we could walk out of a spaceship with no equipment other than a picnic basket, and enjoy a pleasant afternoon on a grassy slope near a stream, then it remains to be seen whether any of these planets fit the description (although NASA's <a href=\"https:\/\/exoplanets.nasa.gov\/alien-worlds\/exoplanet-travel-bureau\/\">Exoplanet Travel Bureau<\/a> would like to make some suggestions for you to explore and find out for yourself; Figure 2.16.)\r\n\r\n&nbsp;\r\n\r\n[caption id=\"attachment_1438\" align=\"aligncenter\" width=\"1623\"]<a href=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/chapter\/2-5-are-there-other-earths-2\/exoplanet-travel-bureau\/\" rel=\"attachment wp-att-1438\"><img class=\"wp-image-1438 size-full\" src=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Exoplanet-travel-bureau.png\" alt=\"\" width=\"1623\" height=\"1193\" \/><\/a> <strong>Figure 2.16<\/strong> NASA Exoplanet Travel Bureau travel posters for two Earth-like planets, Trappist-1e, and Kepler-186f. <a href=\"https:\/\/exoplanets.nasa.gov\/resources\/2159\/planet-hop-from-trappist-1e\/?layout=magic_shell&amp;travel_bureau=true\">I want to visit Trappist-1e<\/a>. <a href=\"https:\/\/exoplanets.nasa.gov\/resources\/2081\/where-the-grass-is-always-redder\/?layout=magic_shell&amp;travel_bureau=true\">I want to visit Kepler-186f<\/a>. Source: NASA-JPL\/Caltech (2021), Public Domain. <a href=\"https:\/\/exoplanets.nasa.gov\/alien-worlds\/exoplanet-travel-bureau\/\">Go to the Travel Bureau<\/a>.[\/caption]\r\n\r\nOn the other hand, if \"other Earths\" refers to rocky worlds approximately Earth\u2019s size, and orbiting within their star\u2019s <strong>habitable zone<\/strong> (the zone in which liquid water, and potentially life, can exist), then as of the October 2020 update of the <a href=\"http:\/\/phl.upr.edu\/projects\/habitable-exoplanets-catalog\">Habitable Exoplanets Catalog<\/a>, it's possible that we have found 60 such worlds.\r\n\r\nPart of the uncertainty about the 60 possible Earth-like worlds is related to their composition. Only five have been confirmed to be rocky, but it's tempting to conclude that the others are because they're similar in size to Earth. Remember the rules of the accretion game: you can only begin to collect gas once you're a certain size, and how much matter you collect depends on how far away from the sun you are. Given how large our gas giant and ice giant planets are compared to Earth, and how far away they are from the sun, we would expect that a planet similar in size to Earth, and a similar distance from its star, should be rocky.\r\n\r\nBut it isn\u2019t quite as simple as that. We're finding that the rules to the accretion game can result in planetary systems very different from our own. In the planetary systems we've observed, it's common to have planets larger than Earth orbiting closer to their star than Mercury does to the sun. Planets as large as Jupiter are rare, and where large planets do exist, they're much closer to their star than Jupiter is to the sun. To summarize, we need to be cautious about drawing conclusions from our own solar system, just in case we're basing those conclusions on something truly unusual.\r\n\r\nOn the other hand, the seemingly unique features of our solar system would make planetary systems like ours difficult to spot. Using the transit method, small planets are harder to detect because they block less of a star\u2019s light than larger planets. Larger planets farther from a star\u2014like our gas giant planets\u2014are difficult to spot because they don\u2019t go past the star as frequently. If someone were observing our solar system, they might have to watch for up to 12 years to see Jupiter pass in front of the sun. For Saturn, they might have to watch for 30 years.\r\n\r\n&nbsp;\r\n<div class=\"textbox shaded\">\r\n\r\n<strong>Key Ideas About the Hunt for Other Planets<\/strong>\r\n\r\n[h5p id=\"133\"]\r\n\r\n<\/div>\r\n<div>\r\n<h1>If Habitable Zone Planets Are Terrestrial, Could We Live There?<\/h1>\r\nThe operational definition of \u201cother Earths\u201d involving a terrestrial composition, a size constraint of one to two times that of Earth, and location within a star\u2019s habitable zone, does not preclude worlds incapable of supporting life as we know it. By those criteria, Venus is an \u201cother Earth,\u201d albeit right on the edge of the habitable zone for our sun. Venus is much too hot for us, with a constant surface temperature of 465\u00b0C (lead melts at 327\u00b0C). Its atmosphere is almost entirely carbon dioxide, and the atmospheric pressure at its surface is 92 times higher than on Earth. Any liquid water on its surface boiled off long ago. Yet the characteristics that make Venus a terrible picnic destination aren\u2019t entirely things we could predict from its distance from the sun. They depend in part on the geochemical evolution of Venus, and at one time Venus might have been a lot more like a youthful Earth. These are the kinds of things we won\u2019t know about until we can look carefully at the atmospheres and compositions of habitable-zone exoplanets.\r\n\r\n&nbsp;\r\n<div class=\"textbox shaded\">\r\n\r\n<strong>Using Our Solar System to Understand the Kepler-102 Exoplanet System<\/strong>\r\n\r\n[h5p id=\"132\"]\r\n\r\n<\/div>\r\n<\/div>\r\n&nbsp;","rendered":"<p>As of July 2021, 4,777 <strong>exoplanets<\/strong>\u2014extrasolar planets, or planets outside of our solar system\u2014have been confirmed. An additional 4,640 potential exoplanets have been detected and await confirmation. The majority of exoplanets have been detected using the transit technique, which involves looking for periodic fluctuations in light from a star from planets transiting in front of the star, causing it to appear dimmer (Figure 2.15).<\/p>\n<p>&nbsp;<\/p>\n<figure id=\"attachment_1433\" aria-describedby=\"caption-attachment-1433\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Transit-method.png\" rel=\"attachment wp-att-1433\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1433\" src=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Transit-method.png\" alt=\"\" width=\"650\" height=\"424\" srcset=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Transit-method.png 1080w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Transit-method-300x196.png 300w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Transit-method-1024x667.png 1024w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Transit-method-768x501.png 768w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Transit-method-65x42.png 65w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Transit-method-225x147.png 225w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Transit-method-350x228.png 350w\" sizes=\"auto, (max-width: 650px) 100vw, 650px\" \/><\/a><figcaption id=\"caption-attachment-1433\" class=\"wp-caption-text\"><strong>Figure 2.15<\/strong> The transit method identifies stars with possible planets in orbit by looking for brief decreases in the brightness of the star. If this happens regularly, it could mean that a planet is periodically blocking some of the star&#8217;s light. Source: Karla Panchuk (2021) CC BY-NC-SA. Modified after NASA\/HESARC\/TESS (2021), Public Domain. <a href=\"https:\/\/heasarc.gsfc.nasa.gov\/docs\/tess\/primary-science.html\">View source<\/a>. <a href=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/chapter\/2-5-are-there-other-earths-2\/transit-method\/\">Click for more attributions.<\/a><\/figcaption><\/figure>\n<p>If &#8220;other Earths&#8221; are defined as planets where we could walk out of a spaceship with no equipment other than a picnic basket, and enjoy a pleasant afternoon on a grassy slope near a stream, then it remains to be seen whether any of these planets fit the description (although NASA&#8217;s <a href=\"https:\/\/exoplanets.nasa.gov\/alien-worlds\/exoplanet-travel-bureau\/\">Exoplanet Travel Bureau<\/a> would like to make some suggestions for you to explore and find out for yourself; Figure 2.16.)<\/p>\n<p>&nbsp;<\/p>\n<figure id=\"attachment_1438\" aria-describedby=\"caption-attachment-1438\" style=\"width: 1623px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/chapter\/2-5-are-there-other-earths-2\/exoplanet-travel-bureau\/\" rel=\"attachment wp-att-1438\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1438 size-full\" src=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Exoplanet-travel-bureau.png\" alt=\"\" width=\"1623\" height=\"1193\" srcset=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Exoplanet-travel-bureau.png 1623w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Exoplanet-travel-bureau-300x221.png 300w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Exoplanet-travel-bureau-1024x753.png 1024w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Exoplanet-travel-bureau-768x565.png 768w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Exoplanet-travel-bureau-1536x1129.png 1536w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Exoplanet-travel-bureau-65x48.png 65w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Exoplanet-travel-bureau-225x165.png 225w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2018\/01\/Exoplanet-travel-bureau-350x257.png 350w\" sizes=\"auto, (max-width: 1623px) 100vw, 1623px\" \/><\/a><figcaption id=\"caption-attachment-1438\" class=\"wp-caption-text\"><strong>Figure 2.16<\/strong> NASA Exoplanet Travel Bureau travel posters for two Earth-like planets, Trappist-1e, and Kepler-186f. <a href=\"https:\/\/exoplanets.nasa.gov\/resources\/2159\/planet-hop-from-trappist-1e\/?layout=magic_shell&amp;travel_bureau=true\">I want to visit Trappist-1e<\/a>. <a href=\"https:\/\/exoplanets.nasa.gov\/resources\/2081\/where-the-grass-is-always-redder\/?layout=magic_shell&amp;travel_bureau=true\">I want to visit Kepler-186f<\/a>. Source: NASA-JPL\/Caltech (2021), Public Domain. <a href=\"https:\/\/exoplanets.nasa.gov\/alien-worlds\/exoplanet-travel-bureau\/\">Go to the Travel Bureau<\/a>.<\/figcaption><\/figure>\n<p>On the other hand, if &#8220;other Earths&#8221; refers to rocky worlds approximately Earth\u2019s size, and orbiting within their star\u2019s <strong>habitable zone<\/strong> (the zone in which liquid water, and potentially life, can exist), then as of the October 2020 update of the <a href=\"http:\/\/phl.upr.edu\/projects\/habitable-exoplanets-catalog\">Habitable Exoplanets Catalog<\/a>, it&#8217;s possible that we have found 60 such worlds.<\/p>\n<p>Part of the uncertainty about the 60 possible Earth-like worlds is related to their composition. Only five have been confirmed to be rocky, but it&#8217;s tempting to conclude that the others are because they&#8217;re similar in size to Earth. Remember the rules of the accretion game: you can only begin to collect gas once you&#8217;re a certain size, and how much matter you collect depends on how far away from the sun you are. Given how large our gas giant and ice giant planets are compared to Earth, and how far away they are from the sun, we would expect that a planet similar in size to Earth, and a similar distance from its star, should be rocky.<\/p>\n<p>But it isn\u2019t quite as simple as that. We&#8217;re finding that the rules to the accretion game can result in planetary systems very different from our own. In the planetary systems we&#8217;ve observed, it&#8217;s common to have planets larger than Earth orbiting closer to their star than Mercury does to the sun. Planets as large as Jupiter are rare, and where large planets do exist, they&#8217;re much closer to their star than Jupiter is to the sun. To summarize, we need to be cautious about drawing conclusions from our own solar system, just in case we&#8217;re basing those conclusions on something truly unusual.<\/p>\n<p>On the other hand, the seemingly unique features of our solar system would make planetary systems like ours difficult to spot. Using the transit method, small planets are harder to detect because they block less of a star\u2019s light than larger planets. Larger planets farther from a star\u2014like our gas giant planets\u2014are difficult to spot because they don\u2019t go past the star as frequently. If someone were observing our solar system, they might have to watch for up to 12 years to see Jupiter pass in front of the sun. For Saturn, they might have to watch for 30 years.<\/p>\n<p>&nbsp;<\/p>\n<div class=\"textbox shaded\">\n<p><strong>Key Ideas About the Hunt for Other Planets<\/strong><\/p>\n<div id=\"h5p-133\">\n<div class=\"h5p-iframe-wrapper\"><iframe id=\"h5p-iframe-133\" class=\"h5p-iframe\" data-content-id=\"133\" style=\"height:1px\" src=\"about:blank\" frameBorder=\"0\" scrolling=\"no\" title=\"Key ideas about the hunt for other planets\"><\/iframe><\/div>\n<\/div>\n<\/div>\n<div>\n<h1>If Habitable Zone Planets Are Terrestrial, Could We Live There?<\/h1>\n<p>The operational definition of \u201cother Earths\u201d involving a terrestrial composition, a size constraint of one to two times that of Earth, and location within a star\u2019s habitable zone, does not preclude worlds incapable of supporting life as we know it. By those criteria, Venus is an \u201cother Earth,\u201d albeit right on the edge of the habitable zone for our sun. Venus is much too hot for us, with a constant surface temperature of 465\u00b0C (lead melts at 327\u00b0C). Its atmosphere is almost entirely carbon dioxide, and the atmospheric pressure at its surface is 92 times higher than on Earth. Any liquid water on its surface boiled off long ago. Yet the characteristics that make Venus a terrible picnic destination aren\u2019t entirely things we could predict from its distance from the sun. They depend in part on the geochemical evolution of Venus, and at one time Venus might have been a lot more like a youthful Earth. These are the kinds of things we won\u2019t know about until we can look carefully at the atmospheres and compositions of habitable-zone exoplanets.<\/p>\n<p>&nbsp;<\/p>\n<div class=\"textbox shaded\">\n<p><strong>Using Our Solar System to Understand the Kepler-102 Exoplanet System<\/strong><\/p>\n<div id=\"h5p-132\">\n<div class=\"h5p-iframe-wrapper\"><iframe id=\"h5p-iframe-132\" class=\"h5p-iframe\" data-content-id=\"132\" style=\"height:1px\" src=\"about:blank\" frameBorder=\"0\" scrolling=\"no\" title=\"Analysis of Kepler-102 exoplanet system\"><\/iframe><\/div>\n<\/div>\n<\/div>\n<\/div>\n<p>&nbsp;<\/p>\n","protected":false},"author":103,"menu_order":1,"template":"","meta":{"pb_show_title":"on","pb_short_title":"","pb_subtitle":"","pb_authors":[],"pb_section_license":""},"chapter-type":[47],"contributor":[],"license":[],"class_list":["post-88","chapter","type-chapter","status-publish","hentry","chapter-type-standard"],"part":69,"_links":{"self":[{"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapters\/88","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapters"}],"about":[{"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/types\/chapter"}],"author":[{"embeddable":true,"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/users\/103"}],"version-history":[{"count":16,"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapters\/88\/revisions"}],"predecessor-version":[{"id":1446,"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapters\/88\/revisions\/1446"}],"part":[{"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/parts\/69"}],"metadata":[{"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapters\/88\/metadata\/"}],"wp:attachment":[{"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/media?parent=88"}],"wp:term":[{"taxonomy":"chapter-type","embeddable":true,"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapter-type?post=88"},{"taxonomy":"contributor","embeddable":true,"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/contributor?post=88"},{"taxonomy":"license","embeddable":true,"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/license?post=88"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}