A piece of Mars: Some time ago, something hit the ground on Mars and made this impact crater, right into a field of ripples. Stuff thrown up during the impact fell back down, burying the ripples with the gray ejecta rays that radiate from the crater. But the wind kept blowing, and in some places you can see where new ripples have formed on top of the ejecta. That’s Mars for you: wind, wind, wind, impact(!), more wind… (HiRISE ESP_038918_1650, NASA/JPL/Univ. of Arizona)
Can you believe it is December already!? As usual, it is a busy month with the AGU Fall Conference. I co-organized a session on small solar system bodies with Padma Yanamandra-Fisher (PSI) and Julie Castillo (JPL). We will talk about recent discoveries in this emerging field including the discovery of rings around Chariklo, the understanding of regolith motion on asteroids, the new lander for Hayabusa 2 (MASCOT) and off course adaptive optics observations of asteroids. Below more info. See you there!
Where: Thursday, December 18, 2014 01:40 PM – 03:40 PM
When: Moscone West 3002
Why: The composition and physical properties of Small Solar System Bodies (SSSBs), remnants of the formation of planets, are key to better understand the origins of our solar system and their potential as resources is necessary for robotic and human exploration. Missions such as ESA/Gaia, NASA/OSIRIS-REx, JAXA/Hyabusa-2, NASA/Dawn and NASA/New Horizons, to study asteroids, comets, dwarf planets and TNOs are poised to provide new in situ information. on SSSBs. Recent remote observations of bright and main belt comets; asteroid Chariklo, with its ring system; asteroid and KBO binaries illustrate that the distinction between comets and asteroids is blurred, providing a new paradigm for such classification. This session welcomes abstracts on the remarkable results bringing information on the internal structure and composition of SSSBs based on space and ground-based data, numerical models, as well as instrument/mission concepts in theprospect of future exploration.
A piece of Mars: On the left is a steep slope leading to a hill. On the right are waves – but not waves of water or any other kind of liquid. These are dunes or very large ripples, blown by the wind into intricate patterns. Sharp eyes might spy boulders that have rolled downslope into this “sea” – there’s even a dotted track that one boulder made as it went. Can you find the boulder? (HiRISE ESP_038799_1590, NASA/JPL/Univ. of Arizona)
A piece of Mars: This circular hill is 200 m (~656 ft) across and ~48 m (~160 ft) high. It stands alone on a relatively flat plain. Why is it there? The surface here used to be ~48 m higher than it is now – on that old surface, a crater formed. The crater was filled in by sediment. And then the surrounding terrain was eroded away by the wind (that’s a whole lot of stuff to be removed over time!). What’s left is the old crater fill, but one day it too will be blown away. (HiRISE ESP_038309_1870, NASA/JPL/Univ. of Arizona)
I just… felt like putting up a pretty picture from MAHLI, the microscopic imager on Curiosity. This is image 0817MH0003250050301497E01_DXXX, taken Nov. 23, 2014 (sol 817). The camera mainly takes closeup images of rocks, but it’s also good for a quick landscape shot. You can see where the camera was pointing here.
A piece of Mars: This 600×450 m (1969×1476 ft) scene of a hillside shows new, dark dustslides that slid downhill (to the lower left). Faint stripes of older dustslides are visible, covered by bright dust and small ripples. Thousands of these form every year on Mars, stretching several kilometers downslope – there is nothing quite like this here on Earth! (HiRISE ESP_038387_1855, NASA/JPL/Univ. of Arizona)
A piece of Mars. These are gullies on a martian hillside (upslope is to the upper right). Water may be what forms the channels, carrying soil and rocks downslope. The textured pattern of the lower slope is caused by the wind forming ripples on loose sediment that has been transported partway down the hill. (HiRISE ESP_038389_1105, NASA/JPL/Univ. of Arizona)
The intensive exploration of Mars is yielding a large amount of data about its properties and its past. However, two great enigmas are yet to be explained: what caused this planet to be different from planet Earth? Is there or has there been any biological activity on the Red Planet? Particularly revealing is the comparative study of both planets.
To follow up to Jason’s post, here’s a photo of our summit team today – much reduced in numbers here in person from a year ago, but this is just the tip of the GPI team iceberg, and we were joined online and via teleconference by at least a dozen other members of the team from California to Canada to Maryland to Australia. Not to mention all the tremendous contributions from so many team members to the hardware, software, target selection, and data analysis needed to bring this complex creature into reality.
And, without further ado, now that GPI is built, delivered, and commissioned… it’s time to let those mirrors dance!
One year ago, GPI saw its first starlight on the night of November 11-12, 2013. In the year since that, the GPI team has been very busy. We’ve detected our first exoplanet, had a series of commissioning runs, took the SPIE conference at Montreal by storm, and found a new friend. Tonight, the night of November 11-12, 2014, we are in the midst of starting what GPI was designed to do: discovering new exoplanets! To celebrate this exciting year for GPI, we tried to recreate this moment from first starlight:
Here’s our attempt:
The party this time around isn’t quite as packed. The observing crew is only half the size of our first light run. I think this shows we’ve made some significant strides in this last year. We’ve fixed a lot of problems and streamlined a lot of tasks so it doesn’t take as many people to observe with such a complicated instrument. However, arguably we have much more to be excited about. With GPI fully operational, we can now start discovering new worlds! Here’s to many more great years of GPI science!