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March 2008

March 31, 2008

Building Blocks of Planets

The following article is from the Jet Propulsion Laboratory.  Check out NASA.gov for more information.   

     Researchers using NASA's Spitzer Space Telescope have discovered large amounts of simple organic gases and water vapor in a possible planet-forming region around an infant star, along with evidence that these molecules were created there.  They've also found water in the same zone around two other young stars.

     By pushing the telescope's capabilities to a new level, astronomers now have a better view of the earliest stages of planetary formation, which may help shed light on the origins of our own solar system and the potential for life to develop in others.

     John Carr of the Naval Research Laboratory, Washington, and Joan Najita of the National Optical Astronomy Observatory, Tucson, Ariz., developed a new technique using Spitzer's infrared spectrograph to measure and analyze the chemical composition of the gases within protoplanetary disks. These are flattened disks of gas and dust that encircle young stars. Scientists believe they provide the building materials for planets and moons and eventually, over millions of years, evolve into orbiting planetary systems like our own.

     "Most of the material within the disks is gas," said Carr, "but until now it has been difficult to study the gas composition in the regions where planets should form.  Much more attention has been given to the solid dust particles, which are easier to observe."

     In their project, Carr and Najita took an in-depth look at the gases in the planet-forming region in the disk around the star AA Tauri. Less than a million years old, AA Tauri is a typical example of a young star with a protoplanetary disk.

     With their new procedures, they were able to detect the minute spectral signatures for three simple organic molecules--hydrogen cyanide, acetylene and carbon dioxide--plus water vapor. In addition, they found more of these substances in the disk than are found in the dense interstellar gas called molecular clouds from which the disk originated. "Molecular clouds provide the raw material from which the protoplanetary disks are created," said Carr. "So this is evidence for an active organic chemistry going on within the disk, forming and enhancing these molecules."

     Spitzer's infrared spectrograph detected these same organic gases in a protoplanetary disk once before. But the observation was dependent on the star's disk being oriented in just the right way. Now researchers have a new method for studying the primordial mix of gases in the disks of hundreds of young star systems.

     Astronomers will be able to fill an important gap--they know that water and organics are abundant in the interstellar medium but not what happens to them after they are incorporated into a disk. "Are these molecules destroyed, preserved or enhanced in the disk?" said Carr. "Now that we can identify these molecules and inventory them, we will have a better understanding of the origins and evolution of the basic building blocks of life--where they come from and how they evolve."  Carr and Najita's research results appear in the March 14 issue of Science.

     Taking advantage of Spitzer's spectroscopic capabilities, another group of scientists looked for water molecules in the disks around young stars and found them--twice. "This is one of the very few times that water vapor has been directly shown to exist in the inner part of a protoplanetary disk--the most likely place for terrestrial planets to form," said Colette Salyk, a graduate student in geological and planetary sciences at the California Institute of Technology in Pasadena. She is the lead author on a paper about the results in the March 20 issue of Astrophysical Journal Letters.

     Salyk and her colleagues used Spitzer to look at dozens of young stars with protoplanetary disks and found water in many. They honed in on two stars and followed up the initial detection of water with complementary high-resolution measurements from the Keck II Telescope in Hawaii. "While we don't detect nearly as much water as exists in the oceans on Earth, we see essentially only the disk's

surface, so the implication is that the water is quite abundant," said Geoffrey Blake, professor of cosmochemistry and planetary sciences at Caltech and one of the paper's co-authors.

     "This is a much larger story than just one or two disks," said Blake. "Spitzer can efficiently measure these water signatures in many objects, so this is just the beginning of what we will learn."

     "With upcoming Spitzer observations and data in hand," Carr added, "we will develop a good understanding of the distribution and abundance of water and organics in planet-forming disks."

March 28, 2008

EARTH HOUR

Earth Hour takes place from 8 to 9 PM on Saturday.  It's an hour when cities, buildings, homeowners, etc, turn off all unnecessary lights.  The idea is to raise awareness that even one person can make a difference.  By turning off unnecessary lights we can see how much energy we are wasting.  Also in southern Arizona it brings the issue of light pollution to the forefront.  Reducing light pollution is a good thing since a good portion of our economy has to do with astronomy.  Phoenix is participating.  Check out the details about Earth Hour by clicking here

March 26, 2008

NASA NEWS!

THIS STORY WAS WRITTEN BY NASA.

Heat radiating from the entire length of 150 kilometer (95 mile)-long fractures

is seen in this best-yet heat map of the active south polar region of Saturn's

ice moon Enceladus.

Image credit: NASA/JPL/Space Science Institute
Nasa's Cassini found organic brew erupting in geyser-like fashion from Saturn's moon Enceladus during a close flyby on March 12. Scientists are amazed that this tiny moon is so active, "hot" and brimming with water vapor and organic chemicals.

New heat maps of the surface show higher temperatures than previously known in the south polar region, with hot tracks running the length of giant fissures. Additionally, scientists say the organics "taste and smell" like some of those found in a comet. The jets themselves harmlessly peppered Cassini, exerting measurable torque on the spacecraft, and providing an indirect measure of the plume density.

"A completely unexpected surprise is that the chemistry of Enceladus, what's coming out from inside, resembles that of a comet," said Hunter Waite, principal investigator for the Cassini Ion and Neutral Mass Spectrometer at the Southwest Research Institute in San Antonio. "To have primordial material coming out from inside a Saturn moon raises many questions on the formation of the Saturn system."

"Enceladus is by no means a comet. Comets have tails and orbit the sun, and Enceladus' activity is powered by internal heat while comet activity is powered by sunlight. Enceladus' brew is like carbonated water with an essence of natural gas," said Waite.

The Ion and Neutral Mass Spectrometer saw a much higher density of volatile gases, water vapor, carbon dioxide and carbon monoxide, as well as organic materials, some 20 times denser than expected. This dramatic increase in density was evident as the spacecraft flew over the area of the plumes.

New structure, density and composition measurements of Enceladus' water plume were obtained when the Cassini spacecraft's Ultraviolet Imaging Spectrograph observed the star zeta Orionis pass behind the plume Oct. 24, 2007, as seen in this animation. Image credit: NASA/JPL
›  Full image, caption and animation

Related images:
›  Gas and Dust Jets Match Up
›  Stripes and Heat Map Side-by-Side
›  Enceladus Plume Neutral Mass Spectrum
›  Comets and Enceladus -- Similar Chemistry
›  Peak Water Density
New high-resolution heat maps of the south pole by Cassini's Composite Infrared Spectrometer show that the so-called tiger stripes, giant fissures that are the source of the geysers, are warm along almost their entire lengths, and reveal other warm fissures nearby. These more precise new measurements reveal temperatures of at least minus 93 degrees Celsius (minus 135 Fahrenheit.) That is 17 degrees Celsius (63 degrees Fahrenheit) warmer than previously seen and 93 degrees Celsius (200 degrees Fahrenheit) warmer than other regions of the moon. The warmest regions along the tiger stripes correspond to two of the jet locations seen in Cassini images.

"These spectacular new data will really help us understand what powers the geysers. The surprisingly high temperatures make it more likely that there's liquid water not far below the surface," said John Spencer, Cassini scientist on the Composite Infrared Spectrometer team at the Southwest Research Institute in Boulder, Colo.

Previous ultraviolet observations showed four jet sources, matching the locations of the plumes seen in previous images. This indicates that gas in the plume blasts off the surface into space, blending to form the larger plume.

Images from previous observations show individual jets and mark places from which they emanate. New images show how hot spot fractures are related to other surface features. In future imaging observations, scientists hope to see individual plume sources and investigate differences among fractures.

"Enceladus has got warmth, water and organic chemicals, some of the essential building blocks needed for life," said Dennis Matson, Cassini project scientist at NASA's Jet Propulsion Laboratory in Pasadena, Calif. "We have quite a recipe for life on our hands, but we have yet to find the final ingredient, liquid water, but Enceladus is only whetting our appetites for more."

At closest approach, Cassini was only 30 miles from Enceladus. When it flew through the plumes it was 120 miles from the moon's surface. Cassini's next flyby of Enceladus is in August.

The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. The mission is managed by JPL for NASA's Science Mission Directorate, Washington.

For images and more information, visit http://www.nasa.gov/cassini and http://saturn.jpl.nasa.gov
.

March 25, 2008

Shuttle Endeavor Landing

Shuttle Endeavor is set to land at 4:05 PM Tucson time on Wednesday.  It looks like the weather will cooperate.  The NASA Shuttle Landing Blog will be up and running around 2 PM.  You can get the latest landing updates there. 

March 24, 2008

HERE'S THE INFO ON THE ISS

Hi!  So sorry about the link that doesn't work in the posting below. 

Here is the direct link to find out when a satellite, like the I.S.S., is flying over your zipcode.

http://spaceweather.com/flybys/

And, here are all of the Tucson times for the next few days:

Date Mag Starts Max. altitude Ends
Time Alt. Az. Time Alt. Az. Time Alt. Az.
24 Mar 0.1 05:01:57 14 S 05:01:57 14 S 05:02:29 10 SSE
24 Mar -1.9 19:44:04 10 SSW 19:46:46 39 SE 19:46:47 39 SE
25 Mar -1.1 20:06:22 10 WSW 20:09:06 40 NW 20:09:45 34 N
26 Mar -1.7 18:53:47 10 SSW 18:56:27 37 SE 18:59:08 10 ENE
26 Mar 0.8 20:30:08 10 WNW 20:31:38 13 NW 20:32:25 12 NNW
27 Mar -1.2 19:15:58 10 WSW 19:18:43 43 NW 19:21:28 10 NNE
28 Mar 0.8 19:39:34 10 WNW 19:41:11 14 NW 19:42:48 10 N

MOON BUGGY COMPETITION

Check out this cool competition coming up in Alabama.  The article is from NASA. - First Alert Meteorologist Erin Jordan

Each year around this time, John Tripp walks across a lunar surface, pondering the challenges ahead for explorers brave enough to take on its cratered terrain.

For now, his "moon" is a winding ribbon of cement footpaths looped around Huntsville's famed U.S. Space and Rocket Center, where Tripp is a construction foreman.

By month's end, a half-mile of the paths will be transformed into a harsh lunar landscape that will test the engineering savvy and physical endurance of about 400 high school and college students on 68 teams. They're converging here April 4-5 for NASA's 15th annual Great Moonbuggy Race, organized by NASA's Marshall Space Flight Center in Huntsville.

The students, hailing from 20 states, Puerto Rico, Canada, India and Germany, will race lightweight moonbuggies they designed, based on the original lunar rover first used during the Apollo 15 moon mission in 1971. Tripp's construction team will greet them with 17 unique course obstacles, built of plywood and old tires, and covered with 20 tons of gravel and 5 tons of sand. All of it will be reshaped into moon-like ridges, craters, basins and lava-etched "rilles."

The course was designed in 1993 by Dr. Larry Taylor, a lunar geologist at the University of Tennessee at Knoxville, Dr. J.M. Wersinger, a physics professor at Auburn University in Auburn, Ala., and the Marshall Center's Dr. Frank Six, now the university affairs officer supporting the race.

The course proved so challenging, race planners have added more and more hay bales to the route each year for added safety. Some 175 bales will line the course this year.

Even so, "seatbelts are not optional," Tripp chuckled. "They're a requirement."

 The students appear ready for the challenge. For two days, their vehicles will brave the course against the backdrop of some of America's most famous rockets and space vehicles. Cheered on by hundreds of friends and spectators, they'll vie for cash prizes and trophies awarded by NASA and corporate sponsors.
Each moonbuggy starts the competition disassembled and folded for transport -- like the actual rovers flown to the moon in the early 1970s. Each buggy must fit into a space no larger than 4 feet in width, height and length. It must be carried in "collapsed" mode to the starting line, assembled, then checked for all required parts -- fenders, a flag and simulated hardware, including batteries, a communications antenna, radio and TV camera.

Then, they're off. Each rover is piloted by two students: one male, one female. The buggies race against the clock instead of each other. Drivers push hard to conquer each obstacle without exceeding the race's 15-minute time limit -- a new rule in 2008.

Tripp keeps the moonbuggy course safe, but tough. As the person in charge of the course for the past 13 years, he's made a science of getting the right blend of sand and rock, and building the right combinations of steep and shallow features. He has to stay sharp, he said, because student builders grow ever more sophisticated, refining their designs from year to year to field sturdier buggies. The schools also consult with each another. Veterans compare concepts and give new teams free insight.

"That camaraderie is exciting to see," said Tammy Rowan, manager of Marshall's Academic Affairs Office, which organizes the race each year. It's just one of dozens of educational programs and initiatives led by the center, to help attract and inspire America's next generation of scientists, engineers and explorers -- those who will carry on the nation's mission of exploration, to the moon and onward into the solar system.

"NASA's Great Moonbuggy Race doesn't just pit schools against one another," Rowan said. "It's a shared experience for students who love math, science and engineering. We hope it shows them the community and partnership that awaits them in these career fields, and provides practical, hands-on experience to reinforce their class work."

Tripp admits he enjoys making the experience as "practical and hands-on" as possible. His course never fails to keep the pit crews in NASA's repairs tent busy on race day -- welding snapped struts, and replacing bent wheels and sprockets.

But most teams push through, and Tripp likes that too. "Some of them reach the end and just fall over exhausted," Tripp said. "But they get there. That's what it's all about."

For more information on the Moon Buggy Race check out NASA.gov.

March 21, 2008

Why is Easter So Early?

Easter is always the first Sunday after the first full moon after the Spring Equinox which occurred at 10:48 PM on Wednesday night.  The full moon occurs at 11:39 AM this Friday morning. 

This dating of Easter is based on the lunar calendar that Hebrew people used to identify Passover, which is why it moves around on our Roman calendar. This year, Easter falls on March 23.

Based on the above, Easter can actually be one day earlier (March 22) but that is pretty rare. This year is the earliest Easter any of us will ever see the rest of our lives, and only the most elderly of our population (95 years old or above) have ever seen it this early before. None of us have ever, or will ever, see it a day earlier.

The next time Easter will be this early (March 23) will be the year 2228 (220 years from now). The last time it was this early was 1913 (so if you're 95 or older, you are the only ones that were around for that).

The next time it will be a day earlier, March 22, will be in the year 2285 (277 years from now). The last time it was on March 22 was 1818.  So, no one alive today has or will ever see it any earlier than this year.

March 20, 2008

Invite to the American Meteorological Society Meeting Tonight

Snow has been on our minds this week!  So join the American Meteorological Society tonight to talk about the evolution and classification of snow crystals.  The public is invited.  The meeting begins at 6:30 PM at the National Weather Service.  Their offices are on the University of Arizona campus in the Environment and Natural Resources Building at 520 N. Park Ave.  Basically it's on the corner of Park and 6th. There is a parking garage just to the east of this building and there are always spots in there.  I can't go to the meeting because I have to go to bed early to get you the weather in the morning.  But if you do go, leave a comment on this blog.  Let me know what you thought of the presentation. - First Alert Meteorologist Erin Jordan

March 19, 2008

International Space Station Sightings

Date Mag Starts Max. altitude Ends
Time Alt. Az. Time Alt. Az. Time Alt. Az.
20 Mar 0.5 05:03:05 10 N 05:05:03 17 NE 05:07:00 10 E
21 Mar -1.8 05:24:59 11 NW 05:27:40 58 NE 05:30:28 10 SE
22 Mar 1.1 04:16:05 13 ENE 04:16:05 13 ENE 04:16:48 10 ENE
22 Mar -1.3 05:47:31 10 WNW 05:50:01 27 SW 05:52:30 10 SSE
23 Mar -0.3 04:38:51 26 ESE 04:38:51 26 ESE 04:40:19 10 ESE
24 Mar 0.1 05:01:52 14 S 05:01:52 14 S 05:02:24 10 SSE
24 Mar -1.9 19:44:01 10 SSW 19:46:42 39 SE 19:46:44 39 SE
25 Mar -1.1 20:06:22 10 WSW 20:09:05 40 NW 20:09:45 33 N
26 Mar -1.7 18:53:51 10 SSW 18:56:30 37 SE 18:59:11 10 ENE
26 Mar 0.8 20:30:12 10 WNW 20:31:42 13 NW 20:32:29 12 NNW
27 Mar -1.1 19:16:08 10 WSW 19:18:52 43 NW 19:21:36 10 NNE
28 Mar 0.8 19:39:51 10 WNW 19:41:27 14 NW 19:43:03 10 N

Clear skies make for great stargazing the next couple of days! And you can check out the the passing of the International Space Station in the early morning hours until Monday and then we have some evening passings after that.  Check out the chart above for the schedule.  Not in Tucson? No worries, just go to the Heavens Above website and select your location. 

March 18, 2008

Spring Begins Wednesday Night For Arizona

You may notice your calender saying that spring begins on the Thursday, March 20th.  Technically it does, but not here in Arizona.  We measure all time across the world from the Prime Meridian, which is 0 degrees longitutude. This line runs through Greenwhich, England, which we use as the offical base for our world time.  We refer to time zones as plus or minus hours and half-hours from the time in Greenwhich.  The vernal equinox, the official beginning of spring in the northern Hemisphere (versus fall in the southern hemisphere), occurs at 5:48 AM Greenwhich Mean Time or GMT.  GMT is also referred to as Universal Coordinated Time (UTC) or Zulu (a military term).  Arizona is 7 hours behind GMT.  That means spring begins at 10:48 PM on Wednesday for our area. - First Alert Meteorologist Erin Jordan