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	<title>KQED QUEST &#187; lander</title>
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	<description>Explore science, nature and environment stories from Northern California and beyond with KQED’s multimedia series</description>
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		<title>Martian Robot Roundup</title>
		<link>http://science.kqed.org/quest/2010/01/15/martian-robot-roundup/</link>
		<comments>http://science.kqed.org/quest/2010/01/15/martian-robot-roundup/#comments</comments>
		<pubDate>Fri, 15 Jan 2010 16:00:21 +0000</pubDate>
		<dc:creator>Ben Burress</dc:creator>
				<category><![CDATA[Uncategorized]]></category>
		<category><![CDATA[ESA]]></category>
		<category><![CDATA[express]]></category>
		<category><![CDATA[lander]]></category>
		<category><![CDATA[mars]]></category>
		<category><![CDATA[nasa]]></category>
		<category><![CDATA[odyssey]]></category>
		<category><![CDATA[opportunity]]></category>
		<category><![CDATA[orbiter]]></category>
		<category><![CDATA[reconnaissance]]></category>
		<category><![CDATA[rover]]></category>
		<category><![CDATA[spirit]]></category>

		<guid isPermaLink="false">http://www.kqed.org/quest/blog/?p=4804</guid>
		<description><![CDATA[Out of about 17 successul Mars missions, three orbiters, two rovers, and maybe—MAYbe—one lander are still active.]]></description>
			<content:encoded><![CDATA[<p><span class="left"><img src="http://science.kqed.org/quest/files/2010/01/MRO-gullies.jpg" /><em>Gullies in wall of Hale Crater.  Credit: NASA/MRO</em></span>Out of about <a href="http://marsprogram.jpl.nasa.gov/missions/log/">40 robotic missions </a>launched toward Mars since the early 1960's, about 17 of them have been successful (I say "about" to hedge my bets, because the "success" of some of those missions is a bit gray), and of all of those, three orbiters, two rovers, and maybe—MAYbe—one lander are still active. </p>
<p>Here's a quick status on the active ones: </p>
<p><a href="http://marsprogram.jpl.nasa.gov/mro/">Mars Reconnaissance Orbiter</a>: The most recent arrival at Mars (2006), MRO's 5-year mission (hmmm—sound vaguely familiar?) is to study the history of water and climate on Mars, as well as to serve as a telecommunications relay for other spacecraft.  Armed with a suite of powerful instruments to study the atmosphere, surface, and subsurface of Mars—including a camera, <a href="http://hirise.lpl.arizona.edu/katalogos.php">HiRISE</a>, that can almost read the license plates on Martian automobiles—MRO has to date sent back more data than all other Mars missions combined.  It's not been a glitchless flight, however:  in 2009, MRO's computer reset itself four times for unknown reasons; the last reset, in August, was followed by a 4-month operational hiatus as Earth-side controllers performed some careful programming updates to help guard against effects of any future resets.  MRO resumed operation in December. </p>
<p><a href="http://marsprogram.jpl.nasa.gov/odyssey/">Mars Odyssey 2001</a>: NASA's 2001 Odyssey is still going fine after nine years—although the computer glitchiness out around Mars seems to be catching:  Odyssey's computer put itself into a safe mode last November 2009 in response to a memory error.  This was corrected and Odyssey has resumed doing science.  Among Odyssey's major discoveries was the detection of huge expanses of water ice just under the surface of polar lowlands, and the surveying of <a href="http://uanews.org/node/22563">deposits of water-related minerals </a>in various locations around the planet.  </p>
<p><a href="http://sci.esa.int/science-e/www/area/index.cfm?fareaid=9">Mars Express</a>:  Arriving at Mars in 2004, Mars Express became the European Space Agency's first mission to another planet, which was recently extended to 2012.  Though the Beagle 2 lander component of the mission fell to Mars and was never heard from again, the Mars Express orbiter has sent back years of captivating images and important data, including the confirmation of methane in Mars' atmosphere (whose source is in all likelihood subsurface, and the origin of which—organic or inorganic processes—is being debated).  </p>
<p>Mars Exploration Rover Opportunity: After six years of crawling around Meridiani Planum discovering chemical and geological evidence for past water on Mars, Opportunity is now on a long march to a large impact crater, which it will reach (if it can keep on running) in about two years.  Currently, the rover has stopped to RAT out chemical and geological information from a rock called <a href="http://marsrover.nasa.gov/gallery/press/opportunity/20091125a.html">Marquette Island</a>—the RAT is its rock abrasion tool, or rock grinder.  Still going….</p>
<p><a href="http://marsrover.nasa.gov/newsroom/pressreleases/20091231a.html">Mars Exploration Rover Spirit</a>:  Also still alive after six years—almost 25 times longer than it was planned to run—Spirit has been stuck in a sand bog for the last six months.  With a couple of wheels on the fritz, Earth-side operators have been confounded in trying to free the robot—but Spirit has continued to make scientific measurements anyway…and in fact made a <a href="http://science.kqed.org/quest/2009/12/18/spirit-digs-a-little-deeper-into-martian-geology/">significant discovery </a>in the course of trying to get unstuck. </p>
<p><a href="http://www.nasa.gov/mission_pages/phoenix/main/index.html">Phoenix lander</a>: Although it's been in the deep dark freeze of a Martian winter since November 2008, the Phoenix lander has an outside chance of survival.  Now that light is returning to Phoenix's landing site, NASA is listening for the robot's radio signal, in case the return of solar power means that Phoenix will rise from the frost and live again! So far, no such signal….</p>
<p>Next up:  The <a href="http://marsprogram.jpl.nasa.gov/msl/">Mars Science Laboratory </a>rover, "Curiosity."  </p>
<p> 37.8148 -122.178</p>

	Tags: <a href="http://science.kqed.org/quest/tag/esa/" title="ESA" rel="tag">ESA</a>, <a href="http://science.kqed.org/quest/tag/express/" title="express" rel="tag">express</a>, <a href="http://science.kqed.org/quest/tag/lander/" title="lander" rel="tag">lander</a>, <a href="http://science.kqed.org/quest/tag/mars/" title="mars" rel="tag">mars</a>, <a href="http://science.kqed.org/quest/tag/nasa/" title="nasa" rel="tag">nasa</a>, <a href="http://science.kqed.org/quest/tag/odyssey/" title="odyssey" rel="tag">odyssey</a>, <a href="http://science.kqed.org/quest/tag/opportunity/" title="opportunity" rel="tag">opportunity</a>, <a href="http://science.kqed.org/quest/tag/orbiter/" title="orbiter" rel="tag">orbiter</a>, <a href="http://science.kqed.org/quest/tag/reconnaissance/" title="reconnaissance" rel="tag">reconnaissance</a>, <a href="http://science.kqed.org/quest/tag/rover/" title="rover" rel="tag">rover</a>, <a href="http://science.kqed.org/quest/tag/spirit/" title="spirit" rel="tag">spirit</a><br />
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		<title>Last Gasps from Phoenix?</title>
		<link>http://science.kqed.org/quest/2008/11/07/last-gasps-from-phoenix/</link>
		<comments>http://science.kqed.org/quest/2008/11/07/last-gasps-from-phoenix/#comments</comments>
		<pubDate>Sat, 08 Nov 2008 01:08:48 +0000</pubDate>
		<dc:creator>Ben Burress</dc:creator>
				<category><![CDATA[Astronomy]]></category>
		<category><![CDATA[Partners]]></category>
		<category><![CDATA[calcite]]></category>
		<category><![CDATA[ice]]></category>
		<category><![CDATA[lander]]></category>
		<category><![CDATA[mars]]></category>
		<category><![CDATA[Mars rovers]]></category>
		<category><![CDATA[nasa]]></category>
		<category><![CDATA[perchlorate]]></category>
		<category><![CDATA[Phoenix]]></category>
		<category><![CDATA[solar energy]]></category>
		<category><![CDATA[virga]]></category>
		<category><![CDATA[water]]></category>

		<guid isPermaLink="false">http://www.kqed.org/quest/blog/?p=927</guid>
		<description><![CDATA[It seems like only last month that we witnessed the drama of NASA's Phoenix landing on Mars.  We were on the edge of our seats in Chabot's planetarium during those "seven minutes of terror" as Phoenix burned a meteoric path through Mars' atmosphere.]]></description>
			<content:encoded><![CDATA[<p><span class="left"><img src="http://science.kqed.org/quest/files/2008/11/phoenix-mars-lander.jpg" alt="" /><em>Artist concept of the Phoenix lander,<br />
sleeping under the darkening polar skies of Martian autumn.</em></span>It seems like only last month that we witnessed the drama of NASA's Phoenix landing on Mars.  We were on the edge of our seats in Chabot's planetarium during those "seven minutes of terror" as Phoenix burned a meteoric path through Mars' atmosphere.</p>
<p>But that was last May, and Phoenix has operated near Mars' northern polar ice cap going on six months now! The mission has continued a couple months longer than originally planned, giving Phoenix more time to dig in the icy soil, bake scooped up samples to detect what chemicals sublimate, track the polar weather day and night, and look to the skies with its various instruments.</p>
<p>Phoenix sent back some very interesting news.  Indeed, it had landed on what turned out to be dust-coated water ice; ice that contains chemicals like calcite and <a href="http://www.space.com/scienceastronomy/080804-phoenix-perchlorate.html">perchlorate</a>&#8211; the former of which may indicate past liquid water on Mars, the latter of which, however, is generally toxic, and may complicate arguments for life, past or present, on Mars.</p>
<p>One of the more "fanciful" detections by Phoenix was <a href="http://www.nasa.gov/mission_pages/phoenix/news/phoenix-20080929.html">falling snow</a>:  two or three miles above, Phoenix detected ice crystals falling from clouds&#8211; albeit flakes that never made it to the ground, instead evaporating like Earthly virga back into the atmosphere.</p>
<p>But Phoenix’s mission has a built-in conclusion (unlike the seemingly perpetual Energizer Bunnies exploring the Martian tropics, aka the Mars Exploration Rovers).  Phoenix landed at 68 degrees north latitude&#8211; that’s equivalent on Earth to the north coast of Alaska, Norway, or south central Greenland&#8211; prior to Martian northern summer solstice (which was June 25).  As with Earthly summertime, the polar days were unending, the Sun above the horizon 24 hours a day (yes, Mars' day is about 24 hours long, just as on Earth).  This provided Phoenix with its electrical power, generated by photovoltaic panels. </p>
<p>But now the Sun is dipping below the horizon several hours a day as the Martian northern hemisphere slides in the direction of autumnal equinox (December 26, 2008), at which time the Sun will spend half the time below the horizon, the other half never rising very high.  Already, Phoenix's solar panels are generating considerably less power than in the heyday of its mission.  A <a href="http://phoenix.lpl.arizona.edu/video/Sol_139/phx_enhanced_137_1F7D0.gif">dust storm</a>, filling the air and blocking some of the already weak sunlight, has also cut available power to the lander for a time in October.</p>
<p>The diminishing conditions also caused Phoenix to put itself into an automatic "sleep" mode in late October, waking up for only a short time each day, when solar energy was at a peak.  To give a flavor of the temperatures Phoenix is enduring, on Sol 151 (the 151<sup>st</sup> Martian day since landing-October 27<sup>th</sup>, Earth time), the daily high reached a balmy 50.8 degrees F-<span style="text-decoration: underline">negative</span> 50.8 that is! The night time low hit -128 degrees F&#8230; .</p>
<p>With every day possibly being the last we hear from Phoenix, scientists are collecting as much data as possible, mostly focusing on meteorological conditions.  <em>Reporting from the Martian polar ice cap, as the icy darkness of winter begins to settle in, this is Phoenix Lander, signing off&#8230;.</em></p>
<p> 37.8148 -122.178</p>

	Tags: <a href="http://science.kqed.org/quest/tag/calcite/" title="calcite" rel="tag">calcite</a>, <a href="http://science.kqed.org/quest/tag/ice/" title="ice" rel="tag">ice</a>, <a href="http://science.kqed.org/quest/tag/lander/" title="lander" rel="tag">lander</a>, <a href="http://science.kqed.org/quest/tag/mars/" title="mars" rel="tag">mars</a>, <a href="http://science.kqed.org/quest/tag/mars-rovers/" title="Mars rovers" rel="tag">Mars rovers</a>, <a href="http://science.kqed.org/quest/tag/nasa/" title="nasa" rel="tag">nasa</a>, <a href="http://science.kqed.org/quest/tag/perchlorate/" title="perchlorate" rel="tag">perchlorate</a>, <a href="http://science.kqed.org/quest/tag/phoenix/" title="Phoenix" rel="tag">Phoenix</a>, <a href="http://science.kqed.org/quest/tag/solar-energy/" title="solar energy" rel="tag">solar energy</a>, <a href="http://science.kqed.org/quest/tag/virga/" title="virga" rel="tag">virga</a>, <a href="http://science.kqed.org/quest/tag/water/" title="water" rel="tag">water</a><br />
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