AEA Astronomy Club
Newsletter May
2018
Contents
AEA Astronomy Club News & Calendar p.1
Video(s) & Picture(s) of the Month p. 3
Astronomy News p. 10
General Calendar p. 13
Colloquia, lectures, mtgs. p. 13
Observing p. 17
Observing p. 17
Useful
Links p. 19
About the Club p. 19
Club News & Calendar.
Club Calendar
About the Club p. 19
Club News & Calendar.
Club Calendar
Club Meeting Schedule:
3 May
|
AEA Astronomy Club Meeting
|
Additive
Manufacturing on Mars
|
(A1/1026)
|
7 June
|
AEA Astronomy Club Meeting
|
Exoplanets: Finding Life in the Galaxy
|
(A1/1735)
|
|
|
|
|
AEA
Astronomy Club meetings are now on 1st Thursdays at 11:45 am. For 2018:
Jan. 4 in A1/1029 A/B, Feb. 1 & March 1 in A1/2906 and for the rest
of 2018 (April-Dec), the meeting room is A1/1735.
May 3 Presentation: “From pasta machines to robotic
arms -- 3D printing a Mars Habitat using indigenous materials”
As humanity moves closer to our
vision to settle the moon, and then Mars, the ability to generate critical
infrastructure “on site” in space becomes increasingly important for cost control,
timelines and safety. 3D printing with indigenous Mars materials in an
autonomous robotic way, before humans set foot on Mars may be the key. My team
has been participating in the NASA Centennial Challenge to 3D print a Mars
Habitat for the past 3 years to develop this concept and technology.
In this presentation I will
first illustrate how our adventures started from the garage, while being
unfunded and understaffed. We borrowed key hardware components, including a
pasta machine that substituted for a clay printer extruder and a 10 foot
robotic arm, from industry and academic partners. We even generated our own
Mars regolith simulant based on volcanic basalt rocks we handpicked in Northern
Israel.
Despite many challenges, ranging
from limited access to materials, short deadlines, and zero dollars in funding,
we were able to print the first physical deliverable, which significantly
outperformed the NASA required minimum in initial mechanical testing. In
delivering the second physical deliverable, we overcame operational challenges,
recruited new team members from around the world, and increased the printing
accuracy. We struggled with optimizing the curing time and heat exposure to the
printing nozzle.
The BubbleBase team was recently
“adopted” by Caltech, in a strategic move to enhance our US presence and
increase manpower working on the project, especially in the field of robotics
and autonomy. The talk will elaborate on additional challenges currently facing
the team, including: merging teams from different disciplines and cultures,
technology challenges in material science, robotics and civil engineering,
funding requirements, and operational challenges. It will conclude with the
team’s plans for the future (on Earth, and on Mars) and how you can follow our
work and get involved in the project.
Speaker: Helen Wexler
Helen Wexler is an award winning
“ArchiTech,” positioned at the intersection of architecture and technology. She
is the founder of BubbleBase, an aerospace project developing technology to 3D
print and robotically assemble housing on Mars for the NASA Centennial
Challenge. She has served as architect in leading New York and Austria based
firms before becoming a technology analyst in the VC industry.
She was previously Director of the The Jnext Hi-Tech & Entrepreneurship Program at the Jerusalem Development Authority, where she oversaw the emerging tech ecosystem of Israel’s capital city, while innovating economic development policy.
Ms. Wexler holds a degree in Architecture from the Bezalel Academy of Art and Design where she is Lecturer on “Technology Paradigms in Architecture.” She is a graduate of the MEET MIT Computer Science Program and Israel Academy of Arts and Sciences (outstanding honors). Helen was named to Forbes Israel 30 under 30 list and has recently completed the International Space Studies Program as an Ilan Ramon Scholarship Fellow.
She was previously Director of the The Jnext Hi-Tech & Entrepreneurship Program at the Jerusalem Development Authority, where she oversaw the emerging tech ecosystem of Israel’s capital city, while innovating economic development policy.
Ms. Wexler holds a degree in Architecture from the Bezalel Academy of Art and Design where she is Lecturer on “Technology Paradigms in Architecture.” She is a graduate of the MEET MIT Computer Science Program and Israel Academy of Arts and Sciences (outstanding honors). Helen was named to Forbes Israel 30 under 30 list and has recently completed the International Space Studies Program as an Ilan Ramon Scholarship Fellow.
We have reserved the night of
Sat. Sept. 8 on the Mt. Wilson 100-inch telescope. We do have a full manifest already –
carry-overs from the 2017 night cancelled due to bad weather. But if interested, we can still put you on
the waiting list in case of cancellations, which typically do occur.
June 7 speaker from JPL – Rob Zellem, doing research on exoplanetary atmospheres.
“Exoplanets: Finding
Life in the Galaxy”
Rob was born just outside the Philadelphia city limits but
grew up in Hendersonville, TN. He went to Villanova University where he
graduated with his Bachelor of Science in Astronomy and Astrophysics, minoring
in Physics, Mathematics, and Classics, and getting an Honors Concentration. His
love of travel and learning about other cultures brought him to University
College London in England where he got his MSc in Space Science. He then moved
out west to Tucson, AZ, where he received his PhD in Planetary Sciences from
the Lunar and Planetary Laboratory at the University of Arizona. He is
currently a scientist at NASA’s Jet Propulsion Laboratory supporting ground-
and space-based instruments that will measure the atmospheres of extrasolar
planets.
Club
News:
We need volunteers to help with:
·
Populating
our club Sharepoint site with material & links to the club’s Aerowiki
& Aerolink materials
·
Arranging
future club programs
·
Managing
club equipment
Astronomy Video(s)
& Picture(s) of the Month
(from Astronomy
Picture of the Day, APOD: http://apod.nasa.gov/apod/archivepix.html VIDEO: Wanderers https://apod.nasa.gov/apod/ap180429.html
Video Credit: Visuals: Erik Wernquist; Music: Christian Sandquist Words & Voice: Carl Sagan
Explanation: How far out will humanity explore? If this video's fusion of real space imagery and fictional space visualizations is on the right track, then at least the Solar System. Some of the video's wondrous sequences depict future humans drifting through the rings of Saturn, exploring Jupiterfrom a nearby spacecraft, and jumping off a high cliff in the low gravity of a moon of Uranus. Although no one can know the future, wandering and exploring beyond boundaries -- both physical and intellectual -- is part of the human spirit and has frequently served humanity well in the past.
VIDEO: Flyover of
Jupiter's North Pole in Infrared https://apod.nasa.gov/apod/ap180416.html
Animation Credit: NASA, JPL-Caltech, SwRI, ASI, INAF, JIRAM
Explanation: What would it look like to fly over the North Pole of
Jupiter? A fictional
animation made from real images and
data captured by NASA's Juno
spacecraft shows an answer. Since the
pole is presently in shadow, the video uses infrared light emitted by Jupiter -- specifically aninfrared
color where the hottest features
glows the brightest. As the animation starts, Juno zooms in on the enormous world. Soon,
one of the eight
cyclones orbiting the North Pole is
featured. One by one, all eight cyclones circling the pole are inspected, each
the size of an entire continent onEarth, and each containing bumpy and fragmented spiral walls.
The virtual trip ends with a zoom out. Studying Jovian cyclones helps humanity
to better
understand dangerous storm systems that occur here on Earth. Juno has recently concluded
another close
pass by Jupiter -- Perijove 12 -- and seems healthy enough to complete several
more of the two-month orbits.Animation Credit: NASA, JPL-Caltech, SwRI, ASI, INAF, JIRAM
VIDEO: The Sun Unleashed: Monster Filament in Ultraviolet https://apod.nasa.gov/apod/ap180409.html
Video Credit: NASA GSFC's Scientific Visualization Studio, Solar Dynamics Obs.
Explanation: One of the most spectacular solar sights is an explosive
flare. In 2011 June, the Sun unleashed somewhat impressive, medium-sized solar
flare as rotation carried active regions of sunpots toward the solar limb. That flare, though, was followed by an astounding gush of magnetizedplasma -- a monster filament seen erupting at the Sun's edge
in this extreme ultraviolet image from NASA's Solar Dynamics
Observatory. Featured here is a time-lapse video of that hours-long event showing darker, cooler plasma raining down across a broad area of the Sun's
surface, arcing along otherwise invisible magnetic field lines. An associated coronal mass ejection, a massive cloud of high energy particles, was blasted in
the general direction of the Earth,and made a glancing blow to Earth's magnetosphere.Video Credit: NASA GSFC's Scientific Visualization Studio, Solar Dynamics Obs.
Interactive: Play Saturn's Rings Like a Harp https://apod.nasa.gov/apod/ap180424.html
Image Credit: NASA, JPL-Caltech, SSI, Cassini; Sonification: Matt Russo (SYSTEM Sounds)
Explanation: Sure, you've seen Saturn's rings -- but have you ever heard them?
Well then please take this opportunity to play Saturn's rings like a harp. In the featured sonification, increasing brighter regions of Saturn's central B-ring play as increasingly higher pitched notes. With a computer browser, click anywhere on the
image to begin, and pluck consecutive strings by sliding the spacecraft
icon's magnetometer
boom across the strings. Both manual
and automatic modes are possible. The featured
natural-color image was taken by
the late Cassini
spacecraft in 2017 July as itgrazed Saturn's rings and took the highest-resolution ring
images ever. The reason why the mostly water-ice rings have a tan hue -- instead of white -- is currently a topic of research. Played in minor harmony, a different
false-color version of the same image
appears where regions with a greater abundance of water ice appears more red.Image Credit: NASA, JPL-Caltech, SSI, Cassini; Sonification: Matt Russo (SYSTEM Sounds)
The Snows of Churyumov-Gerasimenko
Image Credit: ESA, Rosetta, MPS, OSIRIS; UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA -
GIF Animation: Jacint Roger Perez
Explanation: You
couldn't really be caught in this
blizzard while standing by a cliff on Churyumov-Gerasimenko, also known as comet 67P. Orbiting the comet in June of
2016 the Rosetta spacecraft's narrow angle camera did record streaks of dust
and ice particles though, as they drifted across the field of view near the
camera and above the comet's surface. Some of the bright
specks in the scene are likely due to
a rain of energetic charged particles or cosmic
rays hitting the camera, and the
dense background of stars
in the direction of the constellation
Canis Major. Click on this single frame to play and the background stars are
easy to spot trailing from top to bottom in an animated
gif (7.7MB). The 33 frames of the time
compressed animation span about 25 minutes of real time. The stunning gif was
constructed from consecutive
images taken while Rosetta cruised
some 13 kilometers from the comet's nucleus.Image Credit: ESA, Rosetta, MPS, OSIRIS; UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA -
GIF Animation: Jacint Roger Perez
Martian Chiaroscuro
Image Credit: HiRISE, MRO, LPL (U. Arizona), NASA
Explanation: Deep shadows create dramatic contrasts between light and dark in this high-resolution
close-up of the martian surface.
Recorded on January 24, 2014 by the HiRISE camera onboard the Mars
Reconnaissance Orbiter, the scene spans about 1.5 kilometers. From 250
kilometers above the Red Planet the camera is looking down at a sand dune field
in a southern highlands crater. Captured when the Sun was about 5 degrees above
the local horizon, only the dune crests were caught in full sunlight. A long,
cold winter is coming to the southern hemisphere and bright ridges of seasonal frost line the martian dunes.Image Credit: HiRISE, MRO, LPL (U. Arizona), NASA
The Blue Horsehead Nebula in Infrared
Image Credit: WISE, IRSA, NASA; Processing & Copyright : Francesco Antonucci
Explanation: The Blue Horsehead Nebula looks quite different in infrared
light. In visible
light, the reflecting dust of the nebula appears blue and shaped
like a horse's head. In infrared light, however, a complex labyrinth of filaments, caverns, and
cocoons of glowing dust and gas emerges, making it hard to even identify the equine
icon. The featured image of the nebula was
created in three infrared colors (R=22, G=12, B=4.6 microns) from data taken by NASA's orbiting Wide Field Infrared
Survey Explorer (WISE)
spacecraft. The
nebula is cataloged as IC 4592 and spans about 40 light years, lying about 400 light
years away toward the constellation Scorpius along the plane of our Milky Way Galaxy. IC 4592 is fainter but covers an angularly greater region
than the better known Horsehead Nebula of Orion. The star that predominantly illuminates and heats the
dust isNu
Scorpii, visible as the reddened star left
of center.Image Credit: WISE, IRSA, NASA; Processing & Copyright : Francesco Antonucci
Meteor Over Crater Lake
Image Credit & Copyright: Brad Goldpaint (Goldpaint Photography)
Explanation: Did you see it? One of the more common questions during
a meteor
shower occurs because the time it
takes for a meteor to flash is typically less than the time it takes for a head
to turn. Possibly, though, the glory of seeing bright meteors shoot across and knowing
that they were once small granules on
another world might make it all worthwhile, even if your observing
partner(s) could not share in every
particular experience. Peaking late tonight, a dark sky should enable the Lyrids meteor shower to exhibit as many as 20 visible meteors per hour from some locations. In the featured
composite of nine exposures taken
during the 2012 shower, a bright Lyrid meteor streaks above picturesque Crater Lake in Oregon, USA. Snow covers the foreground, while the majestic central band of our home galaxy arches well behind the serene lake. Other
meteor showersthis year -- and every year
-- include the Perseids in mid-August and the Leonids in mid-November.Image Credit & Copyright: Brad Goldpaint (Goldpaint Photography)
TESS Launch Close Up
Image Credit & Copyright: John Kraus
Explanation: NASA's Transiting
Exoplanet Survey Satellite (TESS)
began its search for planets orbiting other stars by leaving planet Earth on
April 18. The
exoplanet hunter rode to orbit on top of a Falcon 9 rocket. The Falcon 9 is so designated for its 9 Merlin first stage engines
seen in this sound-activated camera close-up from Space Launch Complex 40 at
Cape Canaveral Air Force Station. In the coming weeks, TESS will use a series
of thruster burns to boost it into a high-Earth, highly elliptical orbit. A
lunar gravity assist maneuver will allow it to reach a previously untried
stable orbit with half the orbital period of the Moon and a maximum distance
from Earth of about 373,000 kilometers (232,000 miles). From
there, TESS will carry out a two year
survey to search for planets around the brightest and closest stars in the sky.Image Credit & Copyright: John Kraus
Fortuitous Flash Candidate for the Farthest Star Yet
Seen
Image Credit: NASA, ESA, & P. Kelly (U. Minnesota) et al.
Explanation: Was this flash the farthest star yet seen? An unexpected
flash of light noticed fortuitously on Hubble
Space Telescope images may prove to
be not only an unusual gravitational
lensing event but also an image of a
normal star 100 times farther away than any star previously imaged
individually. The featured image shows the galaxy cluster on the left complete with many yellowish galaxies,
while on the right is an expanded square where a source appeared in 2016 that
was not evident in 2011. The spectrum and variability of this
source are strangely unlike a supernova, but rather appear more consistent with a normal blue
supergiant star magnified by about a
factor of 2000 by a confluence of aligned gravitational
lenses. Dubbed Icarus, the source is in a galaxy well behind the galaxy cluster and far across the
universe -- at redshift 1.5. If the lens
interpretation is correct and Icarus
is not an exploding
star, further observations of it and other
similarly magnified stars could give information about the stellar and dark
matter content in the galaxy cluster
and the
universe.Image Credit: NASA, ESA, & P. Kelly (U. Minnesota) et al.
Total Solar Eclipse Corona in HDR
Image Credit & Copyright: Nicolas Lefaudeux
Explanation: How great was the Great
American Eclipse? The featured
HDR image shows it to be perhaps
greater than we knew. On August 21 of last year, the Moon blocked the Sun for a few minutes along a narrow path across the USA. Although one of the most photographed events in human history, this image -- only recently
completed after an extraordinary
amount of digital processing -- shows
one of the most detailed
depictions of a solar corona ever taken.
Composed of extremely
hot gas, the solar corona is only visible to the unaided eye during a total
solar eclipse. The featured image combined over 70 images of different time
exposures. The series of complementary HDR images recovered enough detail to see motion
of the solar corona. The images were taken
in Unity, Oregon in the morning to get steady atmospheric seeing
conditions. The next total solar
eclipse visible on Earth will be in
2019 July, while the next one visible across North America and the USA will
occur in 2024
April.Image Credit & Copyright: Nicolas Lefaudeux
Astronomy
News:
(from
https://www.sciencedaily.com
)
Mercury's thin, dense crust
Mercury's crust
is thinner than anyone thought, new mathematical calculations reveal
Date:
April 27,
2018
Source:
University
of Arizona
Summary:
A planetary scientist has used careful
mathematical calculations to determine the density of Mercury's crust, which is
thinner than anyone thought.
Share:
FULL STORY
Though
Mercury may look drab to the human eye, different minerals appear in a rainbow
of colors in this image from NASA's MESSENGER spacecraft.
Credit:
NASA/Johns Hopkins University APL/Carnegie Institution of Washington
Mercury is small, fast and close to the sun,
making the rocky world challenging to visit. Only one probe has ever orbited
the planet and collected enough data to tell scientists about the chemistry and
landscape of Mercury's surface. Learning about what is beneath the surface,
however, requires careful estimation.
After the
probe's mission ended in 2015, planetary scientists estimated Mercury's crust
was roughly 22 miles thick. One University of Arizona scientist disagrees.
Using the
most recent mathematical formulas, Lunar and Planetary Laboratory associate
staff scientist Michael Sori estimates that the Mercurial crust is just 16
miles thick and is denser than aluminum. His study, "A Thin, Dense Crust
for Mercury," will be published May 1 in Earth and Planetary Science
Letters and is currently available online.
Sori
determined the density of Mercury's crust using data collected by the Mercury
Surface, Space Environment and Geochemistry Ranging (MESSENGER) spacecraft. He
created his estimate using a formula developed by Isamu Matsuyama, a professor
in the Lunar and Planetary Laboratory, and University of California Berkeley scientist
Douglas Hemingway.
Sori's
estimate supports the theory that Mercury's crust formed largely through
volcanic activity. Understanding how the crust was formed may allow scientists
to understand the formation of the entire oddly structured planet.
"Of
the terrestrial planets, Mercury has the biggest core relative to its
size," Sori said.
Mercury's
core is believed to occupy 60 percent of the planet's entire volume. For
comparison, Earth's core takes up roughly 15 percent of its volume. Why is
Mercury's core so large?
"Maybe
it formed closer to a normal planet and maybe a lot of the crust and mantle got
stripped away by giant impacts," Sori said. "Another idea is that
maybe, when you're forming so close to the sun, the solar winds blow away a lot
of the rock and you get a large core size very early on. There's not an answer
that everyone agrees to yet."
Sori's
work may help point scientists in the right direction. Already, it has solved a
problem regarding the rocks in Mercury's crust.
Mercury's
Mysterious Rocks
When the
planets and Earth's moon formed, their crusts were born from their mantles, the
layer between a planet's core and crust that oozes and flows over the course of
millions of years. The volume of a planet's crust represents the percentage of
mantle that was turned into rocks.
Before
Sori's study, estimates of the thickness of Mercury's crust led scientists to
believe 11 percent of the planet's original mantle had been turned into rocks
in the crust. For the Earth's moon -- the celestial body closest in size to
Mercury -- the number is lower, near 7 percent.
"The
two bodies formed their crusts in very different ways, so it wasn't necessarily
alarming that they didn't have the exact same percentage of rocks in their
crust," Sori said.
The moon's
crust formed when less dense minerals floated to the surface of an ocean of
liquid rock that became the body's mantle. At the top of the magma ocean, the
moon's buoyant minerals cooled and hardened into a "flotation crust."
Eons of volcanic eruptions coated Mercury's surface and created its
"magmatic crust."
Explaining
why Mercury created more rocks than the moon did was a scientific mystery no
one had solved. Now, the case can be closed, as Sori's study places the
percentage of rocks in Mercury's crust at 7 percent. Mercury is no better than
the moon at making rocks.
Sori
solved the mystery by estimating the crust's depth and density, which meant he
had to find out what kind of isostasy supported Mercury's crust.
Determining
Density and Depth
The most
natural shape for a planetary body to take is a smooth sphere, where all points
on the surface are an equal distance from the planet's core. Isostasy describes
how mountains, valleys and hills are supported and kept from flattening into
smooth plains.
There are
two main types isostasy: Pratt and Airy. Both focus on balancing the masses of
equally sized slices of the planet. If the mass in one slice is much greater
than the mass in a slice next to it, the planet's mantle will ooze, shifting
the crust on top of it until the masses of every slice are equal.
Pratt
isostasy states that a planet's crust varies in density. A slice of the planet
that contains a mountain has the same mass as a slice that contains flat land,
because the crust that makes the mountain is less dense than the crust that
makes flat land. In all points of the planet, the bottom of the crust floats
evenly on the mantle.
Until Sori
completed his study, no scientist had explained why Pratt isostasy would or
wouldn't support Mercury's landscape. To test it, Sori needed to relate the
planet's density to its topography. Scientists had already constructed a
topographic map of Mercury using data from MESSENGER, but a map of density
didn't exist. So Sori made his own using MESSENGER's data about the elements
found on Mercury's surface.
"We
know what minerals usually form rocks, and we know what elements each of these
minerals contain. We can intelligently divide all the chemical abundances into
a list of minerals," Sori said of the process he used to determine the
location and abundance of minerals on the surface. "We know the densities
of each of these minerals. We add them all up, and we get a map of
density."
Sori then
compared his density map with the topographic map. If Pratt isostasy could explain
Mercury's landscape, Sori expected to find high-density minerals in craters and
low-density minerals in mountains; however, he found no such relationship. On
Mercury, minerals of high and low density are found in mountains and craters
alike.
With Pratt
isostasy disproven, Sori considered Airy isostasy, which has been used to make
estimates of Mercury's crustal thickness. Airy isostasy states that the depth
of a planet's crust varies depending on the topography.
"If
you see a mountain on the surface, it can be supported by a root beneath
it," Sori said, likening it to an iceberg floating on water.
The tip of
an iceberg is supported by a mass of ice that protrudes deep underwater. The
iceberg contains the same mass as the water it displaces. Similarly, a mountain
and its root will contain the same mass as the mantle material being displaced.
In craters, the crust is thin, and the mantle is closer to the surface. A wedge
of the planet containing a mountain would have the same mass as a wedge
containing a crater.
"These
arguments work in two dimensions, but when you account for spherical geometry,
the formula doesn't exactly work out," Sori said.
The
formula recently developed by Matsuyama and Hemingway, though, does work for
spherical bodies like planets. Instead of balancing the masses of the crust and
mantle, the formula balances the pressure the crust exerts on the mantle,
providing a more accurate estimate of crustal thickness.
Sori used
his estimates of the crust's density and Hemingway and Matsuyama's formula to
find the crust's thickness. Sori is confident his estimate of Mercury's crustal
thickness in its northern hemisphere will not be disproven, even if new data
about Mercury is collected. He does not share this confidence about Mercury's
crustal density.
MESSENGER
collected much more data on the northern hemisphere than the southern, and Sori
predicts the average density of the planet's surface will change when density
data is collected over the entire planet. He already sees the need for a
follow-up study in the future.
The next
mission to Mercury will arrive at the planet in 2025. In the meantime,
scientists will continue to use MESSENGER data and mathematical formulas to
learn everything they can about the first rock from the sun.
Story
Source:
Materials provided by University of Arizona. Original
written by Emily Walla. Note:
Content may be edited for style and length.
Journal
Reference:
1. Michael M.
Sori. A thin, dense crust for Mercury. Earth and Planetary Science Letters,
2018; 489: 92 DOI: 10.1016/j.epsl.2018.02.033
General Calendar:
Colloquia, Lectures, Seminars, Meetings, Open Houses & Tours:
Colloquia, Lectures, Seminars, Meetings, Open Houses & Tours:
Colloquia: Carnegie (Tues.
4pm), UCLA, Caltech (Wed. 4pm), IPAC (Wed. 12:15pm) & other Pasadena (daily
12-4pm): http://obs.carnegiescience.edu/seminars/
Carnegie
astronomy lectures
– only 4 per year in the Spring www.obs.carnegiescience.edu. Visit www.huntington.org for directions. For more
information about the Carnegie Observatories or this lecture series, please
contact Reed Haynie. . Click here for more information.
Monday evenings: April
9th, April 23rd, May 7th and May 21st.
AT THE HUNTINGTON LIBRARY AND BOTANICAL GARDENS
1151 Oxford Road, San Marino
All Lectures are in Rothenberg Auditorium. Directions can be found here.
1151 Oxford Road, San Marino
All Lectures are in Rothenberg Auditorium. Directions can be found here.
The lectures are free. Because seating is limited, however,
reservations are required for each lecture through Eventbrite. Additionally,
the lectures will be streamed live through Livestream and simultanously on our
Facebook CarnegieAstro page.
Doors open at 6:45 p.m. Each Lecture will be preceded by a brief
musical performance by students from The Colburn School starting at 7:00
p.m. Lectures start at 7:30 p.m. Light refreshments will be
available.
Image: SDSS / David Kirby
Monday,
May 7th 2018
Dark
Energy and Cosmic Sound
Dr. Daniel Eisenstein
Professor of Astronomy, Harvard University
Director, Sloan Digital Sky Survey III
Dr. Daniel Eisenstein
Professor of Astronomy, Harvard University
Director, Sloan Digital Sky Survey III
Sound waves propagating through the Universe only 400,000 years
after the Big Bang now offer some of our most-precise measures of the
composiiton and history of the Universe. In the last decade, we have detected
the fossil imprint of these sound waves using maps of the distribution of
galaxies from the Sloan Digital Sky Survey. Dr. Eisenstein will describe these
waves and the ambitious experiments that use them to extend our cosmological
reach.
Image: Carnegie Institution for Science/ Robin Dienel
Monday,
May 12st 2018
Astronomical Alchemy: The Origin of the Elements
Dr. Maria
Drout
Hubble and Carnegie-Dunlap Fellow,
Carnegie Institution for Science
Hubble and Carnegie-Dunlap Fellow,
Carnegie Institution for Science
As Carl Sagan once said, "We are all made of star
stuff." However, each element has its own astronomical origins story.
Elements are created everywhere from the centers of stars, to supernovae
explosions, to the Big Bang itself. Dr. Drout will take us on a journey through
the perioidic table, highlighting how our recent discovery of a 'kilonova'
associated with the cataclysmic merger of two neutron stars has filled in one
of the final pieces of the elemental puzzle—the origin of many of the
heaviest elements in the universe.
14 May
|
LAAS General Mtg. 7:30pm Griffith Observatory
|
The
von Kármán Lecture Series: 2018
May
17 & 18
Juno
is a solar-powered spacecraft which has been orbiting Jupiter since July 4,
2016. For a few hours every 53 days, Juno passes within a few thousand
kilometers of the giant planet, and collects a wealth of new information about
Jupiter. The data collected so far have revolutionized our understanding of
Jupiter, and of giant planets in general. Dr. Steve Levin, Project Scientist
for the Juno spacecraft, will present some of Juno’s current science results on
the planet's origins, interior structure, deep atmosphere, and magnetosphere,
and discuss the science expected from Juno in the coming years.
Speaker:
Dr. Steve Levin – Juno Project Scientist and lead co-investigator for Juno’s MicroWave Radiometer instrument
Dr. Steve Levin – Juno Project Scientist and lead co-investigator for Juno’s MicroWave Radiometer instrument
Location:
Thursday, May 17, 2018, 7pm
The von Kármán Auditorium at JPL
4800 Oak Grove Drive
Pasadena, CA
› Directions
Friday, May 18, 2018, 7pm
The Vosloh Forum at Pasadena City College
1570 East Colorado Blvd.
Pasadena, CA
› Directions
Thursday, May 17, 2018, 7pm
The von Kármán Auditorium at JPL
4800 Oak Grove Drive
Pasadena, CA
› Directions
Friday, May 18, 2018, 7pm
The Vosloh Forum at Pasadena City College
1570 East Colorado Blvd.
Pasadena, CA
› Directions
7 June
|
AEA Astronomy Club Meeting
|
Exoplanets: Finding Life in the Galaxy
|
(A1/1735)
|
Observing:
The
following data are from the 2018 Observer’s Handbook, and Sky & Telescope’s
2018 Skygazer’s Almanac & monthly Sky at a Glance.
Current
sun & moon rise/set/phase data for L.A.:
http://www.timeanddate.com/astronomy/usa/los-angeles
Sun, Moon
& Planets for May:
Moon: May 8 last quarter, May
15 new, May 22 1st quarter, May 29 Full,
Other
Events:
2,9,16,23,30 May
|
LAAS
The Garvey Ranch Observatory is open to the public every
Wednesday evening from 7:30 PM to 10 PM. Go into the dome to use the 8 Inch
Refractor or observe through one of our telescopes on the lawn. Visit our
workshop to learn how you can build your own telescope, grind your own
mirror, or sign up for our free seasonal astronomy classes.
Call 213-673-7355 for further information.
Time: 7:30
PM - 10:00 PM
Location: Garvey
Ranch Obs. , 781 Orange Ave., Monterey Park, CA 91755
|
9 May Jupiter at
opposition
?
|
SBAS
Saturday Night In Town Dark Sky Observing Session at Ridgecrest Middle School– 28915 North Bay Rd. RPV, Weather
Permitting: Please contact Greg Benecke to confirm that the gate will be
opened! http://www.sbastro.net/
|
12 May
|
LAAS Private dark sky Star Party
|
?
|
SBAS
out-of-town Dark Sky observing – contact Greg Benecke to coordinate a
location. http://www.sbastro.net/.
|
19 May
|
LAAS Public Star Party: Griffith Observatory Grounds
2-10pm
|
Internet
Links:
Telescope, Binocular & Accessory Buying
Guides
General
About the
Club
Club Websites: Internal (Aerospace): https://aeropedia.aero.org/aeropedia/index.php/Astronomy_Club It is updated to reflect this newsletter, in addition to a listing of past club mtg. presentations, astronomy news, photos & events from prior newsletters, club equipment, membership & constitution. We have linked some presentation materials from past mtgs. Our club newsletters are also being posted to an external blog, “An Astronomical View” http://astronomicalview.blogspot.com/.
Club Websites: Internal (Aerospace): https://aeropedia.aero.org/aeropedia/index.php/Astronomy_Club It is updated to reflect this newsletter, in addition to a listing of past club mtg. presentations, astronomy news, photos & events from prior newsletters, club equipment, membership & constitution. We have linked some presentation materials from past mtgs. Our club newsletters are also being posted to an external blog, “An Astronomical View” http://astronomicalview.blogspot.com/.
Membership. For information, current dues & application, contact Alan Olson, or see the club website (or Aerolink folder) where a form is also available (go to the membership link/folder & look at the bottom). Benefits will include use of club telescope(s) & library/software, membership in The Astronomical League, discounts on Sky & Telescope magazine and Observer’s Handbook, field trips, great programs, having a say in club activities, acquisitions & elections, etc.
Committee Suggestions & Volunteers. Feel free to contact: Mark Clayson, President & Program Committee Chairman (& acting club VP), TBD Activities Committee Chairman (& club Secretary), or Alan Olson, Resource Committee Chairman (over equipment & library, and club Treasurer).
Mark Clayson,
AEA Astronomy Club President
No comments:
Post a Comment