AEA Astronomy Club
Newsletter August 2015
Contents
AEA Astronomy Club News & Calendar p.1
Video(s) & Picture(s) of the Month p. 2
Astronomy News p. 8
General Calendar p.114
Colloquia, lectures, mtgs. p. 14
Observing p. 16
Useful Links p. 17
About the Club p. 18
Club News & Calendar.
Club Calendar
AEA Astronomy Club News & Calendar p.1
Video(s) & Picture(s) of the Month p. 2
Astronomy News p. 8
General Calendar p.114
Colloquia, lectures, mtgs. p. 14
Observing p. 16
Useful Links p. 17
About the Club p. 18
Club News & Calendar.
Club Calendar
Club Meeting Schedule:
6 August
|
AEA Astronomy
Club Meeting
|
A DVD from our Library. In June we learned why the night sky is
dark (not trivial)
|
A1/1026
|
AEA
Astronomy Club meetings are now on 1st Thursdays at 11:45am. For all of (except Aug. 6) 2015, the meeting
room is A1/1735.
Club
News:
Sept. 18 – 18 club members will have a half night of observing on
the historic Mt. Wilson 100-inch telescope.
They also will tour the new Aerospace
facilities on Mt. Wilson before the guided Mt. Wilson tour
From
Kristine P. Maine:
To all: Many of you attended my talk on the Star Trails workshop that I attended last year. Paul’s Photo
is sponsoring another one Dec. 10 out in Death Valley. It cost around
$280.00. If you are interested, visit the web page below. There is a pre- and post-event workshop
locally.
Kristine P. Maine
From Jim
Edwards:
“Last night's observing
session was among my best and most successful ever... the skies were beautiful and calm, all of the complex
equipment played nicely together, and I collected a lot of good submittable
(ie, "publishable") data against several asteroids and double stars.
Plus I was able to record some excellent (for me, at this location) long exposures of M27, the Dumbbell Nebula. I combined and processed the best six of these these, each 5 minutes long (with the aid for some very cool auto-guiding h/w & s/w) to get a "pretty picture" equivalent to a 30 minute exposure... nebula are not bright!
Of course there are countless amateurs who can (and regularly do!) generate much, much better images than that which I attached herein but I'm satisfied this as a first long exposure success for me. Are there problems with the pic? You bet'cha. But not too bad, just the same. :-).”
Plus I was able to record some excellent (for me, at this location) long exposures of M27, the Dumbbell Nebula. I combined and processed the best six of these these, each 5 minutes long (with the aid for some very cool auto-guiding h/w & s/w) to get a "pretty picture" equivalent to a 30 minute exposure... nebula are not bright!
Of course there are countless amateurs who can (and regularly do!) generate much, much better images than that which I attached herein but I'm satisfied this as a first long exposure success for me. Are there problems with the pic? You bet'cha. But not too bad, just the same. :-).”
Astronomy Video(s)
& Picture(s) of the Month
(from
Astronomy Picture of the Day, APOD: http://apod.nasa.gov/apod/archivepix.html)
VIDEO: Fly Over Pluto
https://youtu.be/ydU-YrG_INk
Video Credit: NASA, Johns Hopkins Univ./APL, Southwest Research Inst.
Explanation: It took 9.5 years to get this close, but you can now take a virtual
flight over Pluto in this animation of image data from the New
Horizons spacecraft. The Plutonian terrain unfolding 48,000 miles (77,000 kilometers)
below is identified as Norgay Montes, followed by Sputnik Planum. The icy
mountains, informally named for one of the first two Mount Everest climbers
Tenzing Norgay, reach up to 11,000 feet (3,500 meters) above the surface. The
frozen, young, craterless plains are informally named for the Earth's first
artificial satellite. Sputnik Planum is north of Norgay Montes, within Pluto's expansive,
bright, heart-shaped feature provisionally known as Tombaugh Regio for Clyde Tombaugh, who
discovered Pluto in 1930.Video Credit: NASA, Johns Hopkins Univ./APL, Southwest Research Inst.
Gamma-ray Rain from 3C 279 https://youtu.be/9Rl4l6tuHGg
Video Credit: NASA, DOE, International Fermi LAT Collaboration
Explanation: If
gamma-rays were raindrops a flare from a supermassive black hole might look
like this. Not so gently falling on the Fermi Gamma-ray Space
Telescope from June
14 to June 16 the gamma-ray photons, with
energies up to 50 billion electron volts, originated in active galaxy 3C 279
some 5 billion light-years away. Each gamma-ray "drop" is an
expanding circle in the timelapse visualization, the color and maximum size
determined by the gamma-ray's measured energy. Starting with a background
drizzle, the sudden downpour that then trails off is the intense, high energy
flare. The creative and
calming presentation
of the historically bright flare covers a 5 degree wide region of the gamma-ray sky centered on 3C 279.Video Credit: NASA, DOE, International Fermi LAT Collaboration
Colorful
Clouds Near Rho Ophiuchi
Image Credit & Copyright: Markus Noller (Deep-Sky-Images)
Explanation: Why is the
sky near Antares and Rho
Ophiuchi so
colorful? The colors result from a mixture of objects and processes. Fine dust
illuminated from the front by starlight produces blue reflection nebulae. Gaseous
clouds whose atoms are excited by ultraviolet starlight produce reddish emission nebulae. Backlit dust clouds block starlight and so appear dark. Antares, a red supergiant and one of the brighter stars in the
night sky, lights up the yellow-red clouds on the lower center of the featured image. Rho Ophiuchi lies at the center of the blue nebula on the
left. The distant globular cluster M4 is visible to the upper right of center. These
star clouds are even more colorful than humans can see, emitting light across the electromagnetic
spectrum.Image Credit & Copyright: Markus Noller (Deep-Sky-Images)
Messier 43
Image Credit & Copyright: Yuri Beletsky (Carnegie Las Campanas Obs.), Igor Chilingarian (Harvard-Smithsonian CfA)
Explanation: Often imaged but rarely mentioned, Messier 43 is a large star forming region in its own
right. It's just part of the star forming complex of gas and dust that includes
the larger, more famous neighboring Messier 42, the Great Orion Nebula. In fact, the Great Orion Nebula
itself lies off the lower edge of this scene. The close-up of Messier 43 was made
while testing the capabilities of a near-infrared instrument with one of the
twin 6.5 meter Magellantelescopes
at Las Campanas Observatory in the Chilean Andes. The composite image shifts
the otherwise invisible infrared wavelengths to blue, green, and red colors. Peering into caverns of interstellar dust hidden from visible light,
the near-infrared view can also be used to study cool, brown dwarf stars in the complex region. Along with its celebrity neighbor, Messier
43 lies about 1,500 light-years away, at the edge of Orion's giant molecular
cloud. At that distance, this field of view spans about 5 light-years.Image Credit & Copyright: Yuri Beletsky (Carnegie Las Campanas Obs.), Igor Chilingarian (Harvard-Smithsonian CfA)
Pluto
Resolved
Image Credit & Copyright: NASA, Johns Hopkins Univ./APL, Southwest Research Inst.
Explanation: New
Horizons has survived its close
encounter with Pluto and has
resumed sending back images and data. The robotic spacecraft reported
back on time,
with all systems working, and with
the expected volume of datastored. Featured here is the highest resolution image of Pluto taken before closest approach, an image that
really brings Pluto into a satisfying focus. At first glance, Pluto
is reddish and has several craters. Toward the image
bottom is a surprisingly featureless light-covered region that resembles an iconic heart, and
mountainous terrain appears on the lower right. This image, however,
is only the beginning. As more images and data pour in today, during the coming week,
and over the next year, humanity's understanding of Pluto and its moons will likely become revolutionized.Image Credit & Copyright: NASA, Johns Hopkins Univ./APL, Southwest Research Inst.
Comet
PanSTARRS and a Crescent Moon
Image Credit & Copyright: Yuri Beletsky (Las Campanas Observatory, Carnegie Institution)
Explanation: A comet has
brightened quickly and unexpectedly. Discovered last year, Comet C/2014 Q1
(PanSTARRS) is expected
to be visible now for a few days to the unaided eye, just after
sunset, from some locations. The comet rounded the Sun on July 6 and apparently has
shed quite a bit of gas and dust. Today it is now as close as it will ever get
to the Earth, which is another factor in its recent great apparent
brightness and the
large angular extent of its tails. In the featured image taken two days ago, Comet PanSTARRS is seen sporting a short white dust tail fading to the right, and a long blue ion tail pointing away from the recently set Sun. A
crescent moon dominates the image center. Tomorrow, Comet PannSTARRS will pass only 7 degrees away from a bright Jupiter, with even brighter Venus nearby. Due to its proximity to the Sun, the comet and its tails may best be seen in the sunset
din with binoculars or cameras using long-duration exposures.Image Credit & Copyright: Yuri Beletsky (Las Campanas Observatory, Carnegie Institution)
Ultraviolet
Rings of M31
Image Credit: GALEX, JPL-Caltech, NASA
Explanation: A mere 2.5
million light-years away the Andromeda Galaxy, also known as M31, really is
just next door as large galaxies go. So close and spanning some 260,000 light-years, it took 11 different
image fields from theGalaxy Evolution
Explorer (GALEX)
satellite's telescope to produce this gorgeous portrait of the spiral galaxy in ultraviolet light. While its
spiral arms stand out in visible light images of Andromeda, the arms look more like rings inthe GALEX ultraviolet
view, a view dominated by the energetic light from hot, young, massive
stars. As sites of intense star formation, the rings have been interpreted as
evidence Andromeda collided with its smaller neighboring elliptical galaxy M32
more than 200 million years ago. The large Andromeda galaxy and our own Milky Way are the most massive members of the local galaxy group.Image Credit: GALEX, JPL-Caltech, NASA
Rainbows
and Rays over Bryce Canyon
Image Credit & Copyright: John Rummel
Explanation: What's
happening over Bryce Canyon? Two different optical effects that were captured
in one image taken earlier this month. Both effects needed to have
the Sun situated directly behind the photographer. The nearest apparition was
the common rainbow, created by sunlight
streaming from the setting sun over the head of the photographer, and
scattering from raindrops in front of the canyon. If you look closely, even a second rainbow appears above the first. More rare, and perhaps
more striking, are the rays of light that emanate out from the horizon above
the canyon. These are known as anticrepuscular rays and result from sunlight streaming though
breaks in the clouds, around the sky, and converging at the point 180 degrees around from the Sun.
Geometrically, this antisolar point must coincide with the exact center of the
rainbows. Located in Utah, USA, Bryce Canyon itself contains a picturesque array of ancient sedimentary rock spires known as hoodoos.Image Credit & Copyright: John Rummel
Astronomy
News:
LATEST
NEWS
NASA/JHU
APL/SWRI
Pluto is alive—but where is the heat coming
from?
By
15 July 2015 7:00 pm
Towering mountains of water ice rise up to 3500 meters tall on
Pluto, above smooth plains covered in veneers of nitrogen and methane ice, NASA’s
New Horizons team announced today. The discovery, along with the finding that
parts of the dwarf planet’s surface are crater-free and therefore relatively
young, points to a place that has been geologically reworked in the recent
past. “It could even be active today,” said John Spencer, a New Horizons team
member at Southwest Research Institute (SWRI) in Boulder, Colorado, at a press
conference today at the Johns Hopkins University Applied Physics Laboratory
(APL) in Laurel, Maryland.
The team also showed off new images of unexpectedly smooth
surfaces on Pluto’s moon Charon—which, without an atmosphere, was expected to
have an even more battered surface than Pluto. Radioactive elements in both
bodies’ interiors could provide some of the heat needed for geological mountain
building or ice flows that repave the surface. But Pluto, and especially
Charon, are far too small for this heat to persist. The giant impact thought to
have formed the two worlds could also provide a source of energy, but that
probably happened billions of years ago.
“It’s going to send a lot of scientists back to the drawing
boards,” said Alan Stern, the mission’s principal investigator at SWRI, at the
press conference. Scientists outside the team suggest that the puzzlingly
youthful surfaces could be explained if the dwarf planet and its moon were
formed in a far more recent impact event, or if their reservoirs of water ice
were mixed with other compounds that can melt and flow and lower temperatures.
Although the number of TV crews parked outside APL has
diminished considerably since the
historic flyby on 14 July, the power of Pluto to dazzle continues
to grow. The New Horizons team still has not retrieved data from the moment of
close approach, which came on Tuesday as the probe swooped within 12,500
kilometers of the surface, 33 times closer than the moon is to Earth. Those
images will come much later, over the course of 16 months, after the spacecraft
completes its observations and can devote itself to beaming back data. At
distances of about 4.7 billion kilometers, it takes 4.5 hours for New Horizons
to communicate with Earth, and the data returns in trickles of a few kilobits
per seconds.
But the early images are still providing scientists with plenty
to chew on. One surprise was the discovery of the rugged water ice mountains in
a dark, equatorial region next to a bright, heart-shaped region. (The team said
it would informally name the “heart” Tombaugh Regio, after Pluto’s discoverer.)
The frigid temperatures on Pluto mean that water ice is hard and doesn’t move
or melt easily: It is Pluto’s bedrock. Seeing it protrude in mountains at the
surface suggests that layers of other, more volatile ices—methane, nitrogen,
and carbon monoxide—might only be a thin veneer of materials. Yet if these
layers are too thin, they would be lost completely relatively quickly as they
sublimate into the atmosphere and erode into space, Stern says. That means that
there must be a way of replenishing these more volatile ices from within
Pluto’s interior—perhaps through volcanoes of ice, called cryovolcanoes. “We
haven’t found geysers and we haven’t found cryovolcanoes, but this is very
strong evidence that will send us looking,” he says.
NASA-JHUAPL-SwRI
Smooth surfaces on Pluto's moon Charon imply geological
reworking in the recent past.
Geoffrey Collins, a planetary scientist at Wheaton College in
Norton, Massachusetts, unaffiliated with the team, is amazed by the images.
“Clearly we’re seeing internal activity on the surface of Pluto and Charon,” he
says. “Something is pulling apart their ice crusts.” Collins is excited because
there is no way to explain the activity with conventional models of heat loss.
“If the Charon-Pluto impact happened more recently, all the problems would be
solved,” he says.
Jonathan Lunine, a planetary scientist at Cornell University who
is not affiliated with the mission, agrees that the most curious discovery is
the youthful surfaces of both bodies. “How do you keep these things warm for so
long?” he asks. But he would rather find a mechanism besides a more recent
impact event, which he calls “special pleading.” A giant impact is more likely
to have occurred near the start of the solar system 4.5 billion years ago, when
the Kuiper belt—the distant shell of icy bodies in which Pluto resides—harbored
more potential impactors than it does today. But Lunine says it could be that
the dynamics of the Kuiper belt are different from those in the rest of the
solar system. Another mechanism to get water ice to move and flow more readily,
he suggests, is to mix it with other compounds, such as ammonia. Ammonia-water
mixes have been proposed for other icy bodies in the outer solar system, but
they have never been identified directly, he says. “Maybe that’s happening
here.”
Nancy Chabot, another planetary scientist at APL who is not
affiliated with the mission, says the most important discovery today will end
up being the ice mountains. “It’s going to be something people talk about for a
while,” she says. The mountains—and their implication of mountain-building
activity—runs counter to the expectation that Kuiper belt objects are cold,
pristine relics. “We talk about these things as time capsules from the early
solar system,” she says. That notion must evolve, she says. “Even though they
are primitive bodies, they are also active bodies.”
NASA is planning to reveal more images at press conferences on
Friday, 17 July, and a week later, on 24 July. After that, downloads of image
data from the spacecraft will pause until September, while the mission
concentrates on retrieving near real-time data from particle and plasma
measuring instruments. Even once the full dataset is retrieved, sometime toward
the end by 2016, the mission will not be over. In August, the team will choose
between two small Kuiper belt objects for an extended mission. If granted
funding, New Horizons will steer toward an encounter with one of those small
bodies in 2019.
With additional reporting by Richard Kerr
*See Science’s full
coverage of Pluto, including regular updates on the New Horizons flyby.
LATEST
NEWS
NASA/JHUAPL/SWRI
Potential geysers spotted on Pluto
By
17 July 2015 5:00 pm
Today, NASA’s New Horizons team unveiled the latest trove of
geological goodies in close-up pictures of the surface of Pluto: hummocky hills
that rise up above smooth plains of ice, patches of ice pocked by eroded pits,
and troughs that form the boundaries of mysterious polygonal structures. Most
tantalizing of all, the team has spotted streaks of material that may have
blown downwind from dark spots. Although the team is not yet ready to declare
that these spots are geysers shooting plumes above Pluto, scientists say the
spots and streaks resemble actively spewing geysers on Neptune’s moon Triton
that were discovered in 1989.
The evidence is accumulating that Pluto is an active world, and
not only as a place shaped by top-down atmospheric processes of frost and wind
and sublimating ice. There also appear to be processes working from the bottom
up: forces that lift up water ice mountains the size of the Rocky Mountains and
allow them to sit next to smooth plains of ice that, the team suspects, have
been resurfaced as recently as within the past 100 million years—or even last
week.
“Have a look at the icy frozen plains of Pluto,” said Alan
Stern, the mission’s principal investigator at Southwest Research Institute
(SwRI) in Boulder, Colorado, as he revealed a glimpse of a region named Sputnik
Planum in a press conference today at NASA headquarters. “Who would have
expected this kind of complexity?”
The team released the first results from measurements made as
the spacecraft passed behind Pluto into its shadow. By measuring the way
sunlight was eclipsed around the rim of Pluto, the team was able to analyze its
atmosphere—and rule out models showing a turbulent atmosphere in favor of one
that is more sluggish. Even with a more stagnant atmosphere, the part of it
closest to the surface could still harbor winds blowing at a meter per second
or two—enough to move tiny particles of ice around, says Randy Gladstone, a
mission co-investigator at SwRI in San Antonio, Texas.
But the pictures, as usual, stole the show. Sputnik Planum is a
region along the southern fringe of the left ventricle of the “heart,” now
informally called Tombaugh Regio after Pluto’s discoverer. “I’m still having to
remind myself to take deep breaths,” says Jeff Moore, a mission co-investigator
at NASA’s Ames Research Center in Moffett Field, California. “The landscape is
just astoundingly amazing.” To underscore the point, scientists used New
Horizons’ terrain measurements to simulate a dramatic flyover video of the area
and a nearby ice mountain range called Norgay Montes (see below).
Moore says that one of the few terrains that invites a confident
diagnosis are the pitted regions, which form as ice sublimates into the
atmosphere. He cannot say whether the hills are features that were pushed up
above the surrounding plains, or whether they are composed of tougher materials
that resisted erosion as the rest of the region wore down. “They can either be
popping up or emerging from an erosion-lowering process,” he says. The
polygonal troughs are also mysterious, he says. He doesn’t know whether they result
from convection in the interior—the large-scale patterns of heat upwelling in
Pluto’s mantle—or from contracting ice, analogously to the way mud cracks form
on Earth.
Flyover video: https://youtu.be/ydU-YrG_INk
Moore says it’s likely that the Sputnik Planum terrain—which
also contains the geyserlike spots—extends all the way up into the left
ventricle of the heart. Stern presented chemical evidence that this entire
region is enriched in carbon monoxide ice. It could be either a pool of very
thick layers of ice that welled up from below, or just a centimeter-thick
veneer of carbon monoxide snow from above. Moore says the jury is still out on
whether Tombaugh Regio was emplaced from below or shaped from above. Quite
possibly, he says, both processes are in play: The terrain may have been
deposited in a bout of activity a long time ago, and since been eroded. “It
could be there’s a source region there,” Stern says. “It’s a very special place
on the planet.”
New Horizons, a spacecraft the size of a baby grand piano, on
Tuesday made its closest
approach past Pluto, flying within 12,500 kilometers of its surface and making a
first-ever reconnaissance of an object in the Kuiper belt, the region of icy
worlds beyond Neptune. But images from Pluto are being returned to Earth in a
trickle over
the course of 16 months, because of the vast distances and the modest power of
New Horizon’s radio antenna. NASA Planetary Science Division Director Jim Green
says the spacecraft has returned only 1% to 2% of the data so far.
In pictures NASA released on Wednesday, the big surprise was mountains
of water ice rising 3500 meters up from
strikingly smooth, crater-free surfaces. The lack of craters—also seen on
Charon, Pluto’s largest moon—is evidence for youthfulness, and geological
activity that could pave over the surfaces in fresh icy materials. This was
unexpected, because many thought that the internal heat sources within Pluto
and Charon, leftover from their formation in a giant impact billions of years
ago, would have dissipated long ago.
Larry Soderblom, a retired scientist from the U.S. Geological
Survey in Flagstaff, Arizona, who helped explore Neptune’s moon Triton on
NASA’s Voyager mission, is impressed by both the similarities and differences
between that world and Pluto. Pluto is the
largest Kuiper belt object; Triton is thought to be a captured one.
Both harbor smooth surfaces that suggest repaving driven by internal heating.
But where that activity on Triton can be driven by the tidal pull of Neptune,
scientists are scratching their heads over what could be driving it on Pluto.
There are other differences between the worlds, Soderblom says: Triton lacks
Pluto’s tall mountains and its rugged, ropy pits. “Everywhere we go, we’re
surprised,” he says. “We should know better by now.”
NASA is planning its next press conference on 24 July. After
that, image retrievals from New Horizons’ cameras will pause for nearly 2
months while the team focuses on gathering data from its particle and plasma
instruments. In August, the team plans to choose between two candidate Kuiper
belt objects—far smaller than Pluto—and then steer the spacecraft to an
encounter with it in 2019. The $720 million mission is being operated by Johns
Hopkins University’s Applied Physics Laboratory in Laurel, Maryland.
With additional reporting by Richard Kerr.
*See Science’s full
coverage of Pluto, including regular updates on the New Horizons flyby.
(Video credit: NASA/JHUAPL/SWRI)
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. This year's
Astronomy Lecture Series will take place at A Noise Within on March 30, April 13, April 27, and May 11. Click here for more information.
6 August
|
AEA Astronomy
Club Meeting
|
A DVD from our Library.
In June we learned why the night sky is dark (not trivial)
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A1/1026
|
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7 Aug
|
Friday Night 7:30PM SBAS Monthly General Meeting
in the Planetarium at El Camino College (16007 Crenshaw
Bl. In Torrance)
Friday
Night 7:30PM Monthly General Meeting
Topic: “The
Google Lunar X Prize”
Speaker:
Nathan Wong
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10 Aug
|
LAAS
LAAS General Meeting.
|
Griffith
Observatory
Event Horizon Theater 8:00 PM to 10:00 PM |
August 13
& 14 The
von Kármán Lecture Series: 2015
Drought: Are We In or Out?
California's history is written in great droughts. With
California now in its fourth year of below-normal rainfall and snowpack, the
state faces its most severe drought emergency in decades. Governor Jerry Brown
has called for Californians to voluntarily reduce water, and mandatory
rationing could be ordered soon so that homes, businesses and farms don't run
dry. And, of course, the wildfire danger is also unusually high. How did we get
into this drought? In part, blame it on the Pacific Decadal Oscillation, or
"PDO," a slowly oscillating pattern of sea surface temperatures in
the Pacific Ocean. At the moment, the PDO might being 'flipping' out of its dry
phase--a condition historically linked to extreme high-pressure ridges that
block West Coast storms and give the Midwest and East Coast punishing winters.
Will a much advertised El Nino give us drought relief? How does drought impact
the Southern California coastal marine environment? To find out how this story
may develop this winter, the current prognosis for continued drought and how we
deal with future droughts, attend this talk!
Speaker:
Dr. William Patzert, Climatologist, JPL
Dr. William Patzert, Climatologist, JPL
Locations:
|
Thursday, Aug. 13, 2015, 7pm
The von Kármán Auditorium at JPL 4800 Oak Grove Drive Pasadena, CA › Directions Friday, Aug 14, 2015, 7pm The Vosloh Forum at Pasadena City College 1570 East Colorado Blvd. Pasadena, CA › Directions |
|
Webcast:
|
We offer two
options to view the live streaming of our webcast on Thursday: › 1) Ustream with real-time web chat to take public questions. › 2) Flash Player with open captioning If you don't have Flash Player, you can download for free here. |
|
Observing:
The
following data are from the 2015 Observer’s Handbook, and Sky & Telescope’s
2015 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 August:
Moon: Aug 7 last quarter, Aug
14 new, Aug 22 1st quarter, Aug 29 full
Planets:
Jupiter sets in the W an hour after sunset. Saturn
is in the S & SW until just
before midnight. Venus & Mars rise and are visible
in the East briefly before sunrise. Mercury is hidden in the Sun’s glare
all month.
Other
Events:
1 August Alpha
Capricornids Meteor Shower Peak The duration of this shower extends from
July 15 to September 11. Maximum seems to occur during August 1. The maximum
ZHR ranges from 6-14, while the meteors are generally described as slow. The
shower has the reputation of producing some of the brightest meteors of the
major 6
6 August Southern
Iota Aquarids Meteor Shower Peak The August 6 maximum produces an hourly
rate of 7-8. 7 August Friday Night 7:30PM Monthly General Meeting Topic: The
Google Lunar X Prize Speaker: Nathan Wong 7 August Mercury Passes 0.6 Degrees
from Jupiter
8 Aug
|
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 August Perseids
Meteor Shower Peak The maximum hourly rate for this major meteor shower is
usually 50 or more per hour.
13/14 August Northern
Delta Aquarids Meteor Shower Peak The maximum hourly rate typically reaches
10.
15 Aug
|
SBAS
out-of-town Dark Sky observing – contact Greg Benecke to coordinate a
location. http://www.sbastro.net/.
|
5,12,19,26 Aug
|
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
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18 July
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LAAS
private dark sky night
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22 Aug
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LAAS
Public Star Party: Griffith Observatory Grounds 2-10pm
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25 August Northern
Iota Aquarids Meteor Shower Peak The maximum hourly rate typically reaches
5 – 10.
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
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