Heavenly Look-Alikes: Animal-Shaped Nebulas and Their Earthly Doppelgangers
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Space Science Stamps Launched by Royal Mail
This year marks the 50th anniversary of Britain’s first contribution to space exploration.
On 26 April 1962, its first satellite, Ariel 1, was launched by NASA, carrying experiments designed by British universities and making Britain the world’s third spacefaring nation, after Russia and America. Royal Mail is celebrating with a set of six commemorative stamps, which went on sale the 16th of October, featuring images from European Space Agency missions.
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It’s Official! Water Ice Discovered on Mercury
It’s time to add Mercury to the list of worlds where you can go ice-skating. Confirming decades of suspicion, a NASA spacecraft has spotted vast deposits of water ice on the planet closest to the sun.
Temperatures on Mercury can reach 800 degrees Fahrenheit (427 degrees Celsius), but around the north pole, in areas permanently shielded from the sun’s heat, NASA’s Messenger spacecraft found a mix of frozen water and possible organic materials.
Evidence of big pockets of ice is visible from a latitude of 85 degrees north up to the pole, with smaller deposits scattered as far away as 65 degrees north.
The find is so enticing that NASA will direct Messenger’s observation toward that area in the coming months — when the angle of the sun allows — to get a better look, said Gregory Neumann, a Messenger instrument scientist at NASA’s Goddard Space Flight Center in Maryland. [Latest Mercury Photos from Messenger]
“There is an ongoing campaign, when the spacecraft permits, to look further northward,” said Neumann, the lead author of one of three Mercury studies published online in the Nov. 29 edition of the journal Science.
Researchers also believe the south pole has ice, but Messenger’s orbit has not allowed them to obtain extensive measurements of that region yet.
Messenger will spiral closer to the planet in 2014 and 2015 as it runs out of fuel and is perturbed by the sun’s and Mercury’s gravity. This will let researchers peer closer at the water ice as they figure out how much is there.
$12.8 Billion Budget Approved for European Space Agency
I know for a fact that Tumblr science readers hold a special place in their hearts for anything astronomy-related (along with Brian Cox, Carl Sagan and Neil deGrasse Tyson…)
So, without further ado, rejoice!
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Series of images tracking the development of Saturn’s giant storm, as seen at visible wavelengths during much of 2011. While the clouds from this turbulent storm have long since faded, the glow of the giant vortex associated with the storm, visible only at infrared wavelengths, is likely to persist until 2013.
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NASA’s Suomi Satellite: The Suomi National Polar-orbiting Partnership (NPP)
The Suomi National Polar-orbiting Partnership (NPP) mission represents a critical first step in building the next-generation Earth-observing satellite system that will collect data on both long-term climate change and short-term weather conditions. NPP is the result of a partnership between NASA, the National Oceanic and Atmospheric Administration, and the Department of Defense.
NPP will extend and improve upon the Earth system data records established by NASA’s Earth Observing System (EOS) fleet of satellites that have provided critical insights into the dynamics of the entire Earth system: clouds, oceans, vegetation, ice, solid Earth and atmosphere.
The NPP spacecraft lifted off aboard a United Launch Alliance Delta II rocket from Space Launch Complex 2 at Vandenberg Air Force Base in California on Oct. 28, 2011 at 5:48 a.m. EDT.
Image 1: Overnight on October 4-5, 2012, a mass of energetic particles from the atmosphere of the Sun were flung out into space, a phenomenon known as a coronal mass ejection. Three days later, the storm from the Sun stirred up the magnetic field around Earth and produced gorgeous displays of northern lights. NASA satellites track such storms from their origin to their crossing of interplanetary space to their arrival in the atmosphere of Earth.
Using the “day-night band” (DNB) of the Visible Infrared Imaging Radiometer Suite (VIIRS), the Suomi National Polar-orbiting Partnership (Suomi NPP) satellite acquired this view of the aurora borealis early on the morning of October 8, 2012. The northern lights stretch across Canada’s Quebec and Ontario provinces in the image, and are part of the auroral oval that expanded to middle latitudes because of a geomagnetic storm.
The DNB sensor detects dim light signals such as auroras, airglow, gas flares, city lights, and reflected moonlight. In the case of the image above, the sensor detected the visible light emissions as energetic particles rained down from Earth’s magnetosphere and into the gases of the upper atmosphere. The images are similar to those collected by the Operational Linescan System flown on U.S. Defense Meteorological Satellite Program (DMSP) satellites for the past three decades. “When I first saw images like this as a graduate student, I was immediately struck by the fluid dynamic characteristics of the aurora,” said Tom Moore, a space physicist at NASA’s Goddard Space Flight Center. “Viewing the aurora in this way makes it immediately clear that space weather is an interaction of fluids from the Sun with those of the Earth’s upper atmosphere. The electrodynamics make for important differences between plasmas and ordinary fluids, but familiar behaviors (for example, waves and vortices) are still very apparent. It makes me wonder at the ability of apparently empty space to behave like a fluid.”
Auroras typically occur when solar flares and coronal mass ejections—or even an active solar wind stream—disturb and distort the magnetosphere, the cocoon of space protected by Earth’s magnetic field. The collision of solar particles and pressure into our planet’s magnetosphere accelerates particles trapped in the space around Earth (such as in the radiation belts). Those particles are sent crashing down into Earth’s upper atmosphere—at altitudes of 100 to 400 kilometers (60 to 250 miles)—where they excite oxygen and nitrogen molecules and release photons of light. The results are rays, sheets, and curtains of dancing light in the sky.
Auroras are a beautiful expression of the connection between Sun and Earth, but not all of the connections are benign. Auroras are connected to geomagnetic storms, which can distort radio communications (particularly high frequencies), disrupt electric power systems on the ground, and give slight but detectable doses of radiation to flight crews and passengers on high-latitude airplane flights and on spacecraft.
The advantage of images like those from VIIRS and DMSP is resolution, according to space physicist Patrick Newell of the Johns Hopkins University Applied Physics Laboratory. “You can see very fine detail in the aurora because of the low altitude and the high resolution of the camera,” he said. Most aurora scientists prefer to use images from missions dedicated to aurora studies (such as Polar, IMAGE, and ground-based imagers), which can offer many more images of a storm (rather than one per orbit) and can allow researchers to calculate the energy moving through the atmosphere. There are no science satellites flying right now that provide such a view, though astronauts regularly photograph and film auroras from the International Space Station.
NASA Earth Observatory image by Jesse Allen and Robert Simmon, using VIIRS Day-Night Band data from the Suomi National Polar-orbiting Partnership (Suomi NPP) and the University of Wisconsin’s Community Satellite Processing Package. Suomi NPP is the result of a partnership between NASA, the National Oceanic and Atmospheric Administration, and the Department of Defense. Caption by Mike Carlowicz.
Image and caption: NASA Earth Observatory
Image 2: Early on August 28, 2012, the Visible Infrared Imaging Radiometer Suite (VIIRS) on the Suomi-NPP satellite captured this nighttime view of Tropical Storm Isaac and the cities near the Gulf Coast of the United States. The image was acquired just after local midnight by the VIIRS “day-night band,” which detects light in a range of wavelengths from green to near-infrared and uses light intensification to enable the detection of dim signals. In this case, the clouds of Isaac were lit by moonlight.
Image: NASA Earth Observatory
Image 3: This image was taken from the VIIRS instrument aboard NASA’s Earth-observing satellite, Suomi NPP. This composite image uses a number of swaths of the Earth’s surface taken on January 4, 2012. The NPP satellite was renamed ‘Suomi NPP’ on January 24, 2012 to honor the late Verner E. Suomi of the University of Wisconsin.
Image and caption: NASA/NOAA/GSFC/Suomi NPP/VIIRS/Norman Kuring
Image 4: The new image is a composite of six separate orbits taken on January 23, 2012 by the Suomi National Polar-orbiting Partnership satellite. Both of these new ‘Blue Marble’ images are images taken by a new instrument flying aboard Suomi NPP, the Visible Infrared Imaging Radiometer Suite (VIIRS).
Compiled by NASA Goddard scientist Norman Kuring, this image has the perspective of a viewer looking down from 7,918 miles (about 12,742 kilometers) above the Earth’s surface from a viewpoint of 10 degrees South by 45 degrees East. The four vertical lines of ‘haze’ visible in this image shows the reflection of sunlight off the ocean, or ‘glint,’ that VIIRS captured as it orbited the globe. Suomi NPP is the result of a partnership between NASA, NOAA and the Department of Defense.
Image and Caption: NASA/NOAA
Image 5: Fifteen orbits of the recently launched Suomi NPP satellite provided the VIIRS instrument enough time (and longitude) to gather the pixels for this synthesized view of Earth showing the Arctic, Europe, and Asia.
Image: NASA/GSFC/Suomi NPP
Image 6: The world is currently in an active period for the production of atmospheric aerosols, according to Colin Seftor, an atmospheric physicist at NASA Goddard Space Flight Center in Greenbelt, Md., who compiled this image. Seftor works for Science Systems and Applications, Inc. This image is a combination of a VIIRS RGB image with OMPS aerosol index (AI) data for September 15, 2012.
The OMPS AI shows dust from the Sahara over northern Africa that is being blown over the Atlantic (with yellow, less opaque colors representing less dust and pink, more opaque colors representing more dust). Dust can also be seen over Saudi Arabia and parts of Iran, Afghanistan, and Pakistan. However, the aerosol index signal over the Western U.S. is due to dense smoke from wildfires, while smoke from agricultural biomass burning is visible over both South American and southern Africa. The sun glint in the middle of each swath shows the pattern of the satellite’s view in orbit.
Image: NASA Goddard Space Flight Center
Image 7: A ‘true-color’ image of the Southeastern United States taken on January 19, 2012, the first day the full complement of VIIRS’ 22 channels were active. This images was taken between 5:57 pm USA EST and 6:04 pm USA EST (17:57 - 18:04 UTC).
Suomi NPP is carrying five instruments on board. The biggest and most important instrument is The Visible/Infrared Imager Radiometer Suite or VIIRS.
Image and caption: NASA/Suomi NPP/Atmosphere PEATE/Univ. of Wisconsin-Madison/Liam Gumley
Image 8: From its vantage 824 kilometers (512 miles) above Earth, the Visible Infrared Imager Radiometer Suite (VIIRS) on the NPOESS Preparatory Project (NPP) satellite gets a complete view of our planet every day. This image from November 24, 2011, is the first complete global image from VIIRS.
The NPP satellite launched on October 28, 2011, and VIIRS acquired its first measurements on November 21. To date, the images are preliminary, used to gauge the health of the sensor as engineers continue to power it up for full operation.
Rising from the south and setting in the north on the daylight side of Earth, VIIRS images the surface in long wedges measuring 3,000 kilometers (1,900 miles) across. The swaths from each successive orbit overlap one another, so that at the end of the day, the sensor has a complete view of the globe. The Arctic is missing because it is too dark to view in visible light during the winter.
The NPP satellite was placed in a Sun-synchronous orbit, a unique path that takes the satellite over the equator at the same local (ground) time in every orbit. So, when NPP flies over Kenya, it is about 1:30 p.m. on the ground. When NPP reaches Gabon—about 3,000 kilometers to the west—on the next orbit, it is close to 1:30 p.m. on the ground. This orbit allows the satellite to maintain the same angle between the Earth and the Sun so that all images have similar lighting.
The consistent lighting is evident in the daily global image. Stripes of sunlight (sunglint) reflect off the ocean in the same place on the left side of every swath. The consistent angle is important because it allows scientists to compare images from year to year without worrying about extreme changes in shadows and lighting.
The image also shows a band of haze along the right side of every orbit swath. When light travels through the atmosphere, it bounces off particles or scatters, making the atmosphere look hazy. The scattering effect is most pronounced along the edge of the swath, where the sensor is looking at an angle through more of the atmosphere. Scientists can correct for this scattering effect, but need measurements from a range of wavelengths to do so. The degree to which light scatters depends partly on the wavelength of the light. Blue light scatters more than red light, for example, which is why the sky is blue. VIIRS measures 22 different wavelengths of light, but not all of the sensor’s detectors are operating at peak performance yet. Those measuring thermal infrared light are not yet cold enough to collect reliable measurements.
Once VIIRS begins full operations, it will produce a range of measurements from ocean temperature to clouds to the locations of fires. These measurements will help extend the record from earlier sensors like the Moderate Resolution Imaging Spectroradiometer (MODIS). VIIRS is very similar to MODIS, but flies at a higher altitude to measure the whole planet without gaps. (MODIS daily measurements have gaps at the equator. See the MODIS image from November 24.) VIIRS also sees the Earth in less detail, 375 meters per pixel, compared to 250 meters per pixel for MODIS.
Image: NASA Earth Observatory
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Like A Falling Apple
Formulated in 1687, Newton’s Law of Universal Gravitation was a turning point in physics. While the legend of the apple falling on his head is an exaggeration of the truth, Newton did have a brilliant insight: that every object in the universe attracts every other object. The force of attraction between two objects depends on only two things: the mass of the objects, and the distance between them. So, more massive objects exert a stronger force, while more distant objects exert a weaker force. Newton was able to formulate a simple equation to describe this, pictured above: force is equal to Newton’s gravitational constant, multiplied by masses of the objects, then divided by the square of the distance between the objects. What’s remarkable is that the law truly is universal—not only can it predict how things move here on Earth, but it can also predict the movements of the moon, planets, stars and even galaxies millions of lightyears away. Newton believed that the movement of every object in our universe could be predicted, but we know now that while his theory generally holds true, it is not precise. Einstein’s theory of general relativity had to step in to fill the holes.
(Image Credit: The Wonders Collection)
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Black Sun and Inverted Starfield
Does this strange dark ball look somehow familiar? If so, that might be because it is our Sun. In the above image, a detailed solar view was captured originally in a very specific color of red light, then rendered in black and white, and then color inverted.
Once complete, the resulting image was added to a starfield, then also color inverted. Visible in the above image of the Sun are long light filaments, dark active regions, prominences peaking around the edge, and a moving carpet of hot gas.
The surface of our Sun has become a particularly busy place over the past two years because it is now nearing Solar Maximum, the time when its surface magnetic field is wound up the most. Besides an active Sun being so picturesque, the plasma expelled can also become picturesque when it impacts the Earth’s magnetosphere and creates auroras.
(via itscandidlycara)
Henry: “It’s gettin’ darker and darker.”
Me: “The sun goes away every night and then comes back in the morning.”
Sarah: “The sun is always moving, and sometimes it lights up certain parts of the earth, and other times it lights up the other parts. So when it’s nighttime here, it’s daytime somewhere else.”
Me: “Well, I think the earth is actually doing the moving.”
Sarah: “Right, yeah. Well, they’re both moving but the Earth’s movement is the relevant one to this particular issue.”
Henry: “It’s gettin’ darker and darker!”
Me: “The Sun is orbiting? Around what?”
Sarah: “Around the center of the Milky Way. I remember from Astronomy.”
Me: “You’re suggesting that we’re orbiting a sun that is itself orbiting the Milky Way.”
Sarah: “Yes, and in fact there is also a moon orbiting us.”
Henry: “The sun is moving?”
Me: “Well, the earth is moving; that’s why the Sun is going down.”
Henry: “We are moving?”
Sarah: “That’s correct, but the sun is also moving.”
Henry: “It’s gettin’ darker and darker.”
Minimal Posters - Five Groundbreaking Moments In Astronomy.
Thanks to HydrogenePortfolio for sending us this great collection of Physics art!
This Is a Full Resolution Video of Curiosity Touching Down on Mars
One of the biggest bummers about Mars Rover Curiosity’s epic landing is that there was no news crew on the surface to catch footage of the descent. This full resolution video of Curiosity touching down from its own point of view is the next best thing.
This isn’t the first video of touchdown, but it’s the best. It’s the result of stringing together all the high resolution shots the rover took on its way to the surface, high resolution shots that took a lot longer to get back to Earth than the initial thumbnails. If it seems a bit choppy, that’s because Curiosity only took about four pictures per second. It might not be movie quality, but this is the best video out there of what it’s like to land on Mars. Incredible.
[via bookofjoe]
Spectacular Meteor Shower Should Be Visible to Most
One of the best meteor shower events of the year will be happening this weekend, peaking late tonight. Most of the country should have at least a decent view.
(via physicsphysics)
As we mentioned in this post earlier, there will be a meteor shower visible in the night sky of North America over the next few days.
If any of you happen to get any nice shots of the Perseid Meteor Shower this weekend, feel free to send them our way through either http://physicsphysics.tumblr.com/submit or as a photo reply to this post. From there we will see to it that your picture gets posted on physicsphysics for all to see.
Enjoy the shower!
Embrace Your Ignorance: An Interview With Neil deGrasse Tyson
So many people only want answers. To be a scientist you have to learn to love the questions. You’ll learn that some of the greatest mysteries of the universe remain unanswered, and that’s the fun part. That’s the part that gets you awake in the morning and running to the office, because there’s a problem awaiting your attention that you might just solve that day. You have to embrace the unknown and embrace your own ignorance.
— Neil deGrasse Tyson
(via physicsphysics)