November 12, 2014
Michigan in Pictures regular Shawn Malone of Lake Superior Photo is one of the best photographers of the Michigan night sky around, and on the evening of November 22nd , you have a chance to learn from her at a Night Sky Workshop. She writes:
The Upper Peninsula of Michigan is a wonderful place to discover the magic of night sky photography, due to the abundance of easily accessible dark sky locations. These night sky workshops are designed for those looking for a basic understanding of the equipment and technique necessary for capturing the night sky.
Photography workshops will take place at LakeSuperiorPhoto- gallery/studio on 211 S. Front, Marquette Mi. 49855. There will be an hour class at the studio where I will cover techniques for capturing night sky photos, from basic camera set up and settings, to a brief discussion of post processing to helpful websites and software to help you come away with great night sky photos.
During this workshop we will concentrate on the techniques necessary to capture low light and night sky photos. Hopefully the weather cooperates and we have a chance to photograph the stars or maybe even possibly the northern lights. No matter what weather conditon – we will conduct the workshop and you will come away with everything you need to know about capturing great night sky images.
She has 4 spaces left – click here to register!
The Philae (fee-LAY) lander is scheduled to touch down on Comet 67P/Churyumov-Gerasimenko on November 12, 2014 at 10:35 a.m. EST (15:35 UTC). We on Earth – 300 million miles (500 million km) away – won’t know the lander has set down successfully until a signal is received back at about 11:02 a.m. EST (16:02 UTC). Both NASA and ESA will provide live online coverage of this first-ever attempted landing on a comet.
Rosetta spacecraft will do the equivalent of transferring an object from one speeding bullet to another, when it tries to place its Philae lander on its comet. Read more about the mission’s dramatic attempt to land on a comet here.
After landing, Philae will obtain the first images ever taken from a comet’s surface. It also will drill into the surface to study the composition and witness close up how a comet changes as its exposure to the sun varies.
Philae can remain active on the surface for approximately two-and-a-half days. Its “mothership” – the Rosetta spacecraft – will remain in orbit around the comet through 2015. The orbiter will continue detailed studies of the comet as it approaches the sun for its July 2015 perihelion (closest point), and then moves away.
October 22, 2014
If it seems to you that fall colors are more erratic this year than usual, it’s not all in your head! The Great Lakes Echo feature by Juliana Moxley titled Last winter’s cold legacy: Fall colors slower to peak explains (in part) that last winter’s extreme cold is the culprit:
The harsh 2014 winter is partly to blame, said Bert Cregg, a professor in the department of horticulture at Michigan State University.
We are still having a good fall color season in Michigan, but we are likely to see some trees in full color while others are just beginning to turn, he said.
“As you’ll recall, last winter was extremely cold — one of the coldest winters on record,” Cregg said. “The winter stress delayed leaf-out for many trees, and then the tree’s timing was further delayed by a cold rather than normal spring.”
A warming climate can also affect fall color, said Howard Neufeld, a professor in the department of biology at Appalachian State University in North Carolina. Higher temperatures, altered timing and/or amounts of precipitation, changes in humidity, changes in cloud cover, increases in the length of the growing season and higher levels of nitrogen inputs in the ecosystem can all affect fall color variance.
“Increased precipitation means that light levels are most likely lower, and trees will do less photosynthesis,” Neufeld said. “With less photosynthesis, there are fewer sugars in the leaves. Warmer temperatures mean higher respiration rates, and more sugars will be metabolized.”
You can read on for lots more including an explanation of the scientific processes that impact color change.
October 21, 2014
Wikipedia says that Portage Lake is part of the Keweenaw Waterway, a partly natural, partly artificial waterway that cuts across the Keweenaw Peninsula to provide access for shipping from Lake Superior. If you click the link you can get an aerial view.
Saw the fog on Lake Portage from my apartment window after I woke up today. I knew the potential this fog can bring so I darted down to the lake shore. But the fog was so heavy that the foliage on the other bank were completely blocked. Just when I was about to give up and head back for school, the fog started to break as the sun rises. And then the magic started to unfold before my eyes. Soon the fog lifted and fill the campus uphill, the entire campus was bathed in soft morning light and there were Tyndall effect everywhere! I can not think of a better way to start a day of work.
What’s the Tyndall effect you ask? The UC Davis ChemWiki explains that the Tyndall effect was identified by 19th Century Irish scientist John Tyndall.
Because a colloidal solution or substance (like fog) is made up of scattered particles (like dust and water in air), light cannot travel straight through. Rather, it collides with these micro-particles and scatters causing the effect of a visible light beam. This effect was observed and described by John Tyndall as the Tyndall Effect.
The Tyndall effect is an easy way of determining whether a mixture is colloidal or not. When light is shined through a true solution, the light passes cleanly through the solution, however when light is passed through a colloidal solution, the substance in the dispersed phases scatters the light in all directions, making it readily seen.
For example, light is not reflected when passing through water because it is not a colloid. It is however reflected in all directions when it passes through milk, which is colloidal. A second example is shining a flashlight into fog or smog; the beam of light can be easily seen because the fog is a colloid.
September 25, 2014
Three years ago I posted this. It’s such good and useful information that I thought I’d share it again! #TBT?
The Science of Color in Autumn Leaves from the United States National Arboretum explains that process that starts the cascade of events that result in fall color is a growth process that starts in late summer or early autumn. When the nights get long enough, a layer of cells called the abscission layer forms that begins to block transport of materials from the leaf to the branch.
During the growing season, chlorophyll is replaced constantly in the leaves. Chlorophyll breaks down with exposure to light in the same way that colored paper fades in sunlight. The leaves must manufacture new chlorophyll to replace chlorophyll that is lost in this way. In autumn, when the connection between the leaf and the rest of the plant begins to be blocked off, the production of chlorophyll slows and then stops. In a relatively short time period, the chlorophyll disappears completely.
This is when autumn colors are revealed. Chlorophyll normally masks the yellow pigments known as xanthophylls and the orange pigments called carotenoids — both then become visible when the green chlorophyll is gone. These colors are present in the leaf throughout the growing season. Red and purple pigments come from anthocyanins. In the fall anthocyanins are manufactured from the sugars that are trapped in the leaf. In most plants anthocyanins are typically not present during the growing season.
As autumn progresses, the cells in the abscission layer become more dry and corky. The connections between cells become weakened, and the leaves break off with time. Many trees and shrubs lose their leaves when they are still very colorful. Some plants retain a great deal of their foliage through much of the winter, but the leaves do not retain their color for long. Like chlorophyll, the other pigments eventually break down in light or when they are frozen. The only pigments that remain are tannins, which are brown.
The explain that because the starting time of the whole process is dependent on night length, fall colors appear at more or less the same time every year and are not overly dependent on temperature, rainfall or other factors, other than the fact that weather can shorten or prolong the show by stripping leaves from trees.
Lots more fall color on Michigan in Pictures!
April 11, 2014
In “A sad day” for Michigan bats: White-nose syndrome found in 3 counties, Michigan Radio reports:
The Michigan Department of Natural Resources today confirmed the presence of white-nose syndrome in three counties: Alpena, Dickinson and Mackinac.
White-nose syndrome is blamed for the deaths of six million bats in 27 states and five Canadian provinces since 2006. In some places where the fungus outbreak has taken hold, 90% of the bats have died.
“We anticipated that this day would come. It’s not unexpected. But it’s still a sad day,” says Dan O’Brien, a state wildlife veterinarian. “Once this fungus gets into a bat hibernacula it’s going to be there, current evidence suggests, for a long time.”
The fungal disease could have a big impact on Michigan’s economy. Wildlife biologists estimate bats have a roughly $1 billion impact on the state’s agriculture industry by eating harmful insects.
“At this point, there is no effective treatment for WNS and no practical way to deliver the treatment to millions of affected bats even if treatment existed. Rehabilitation of bats is prohibited in Michigan because of the potential for the exposure of humans to rabies,” said O’Brien. “The best thing the public can do when they find a dying or dead bat is to leave it alone and keep children, livestock and pets away from it.”
Bat die-offs can be reported through an observation report on the DNR website at www.michigan.gov/wildlife or by calling the DNR at 517-336-3050.
More animals on Michigan in Pictures.
April 5, 2014
For as long as we know, celestial signs have been read to signify calamity and change, and apparently the total lunar eclipse in the early morning hours of April 15, 2014 that kicks off a two-year tetrad of lunar eclipses is no exception.
We’ve been receiving a number of inquiries about Blood Moons in 2014 and 2015. The Blood Moons most people are asking about are not part of astronomy. Their origin is religious, at least according to Christian pastor John Hagee, who wrote a 2013 book about Blood Moons. However, both astronomers and some proponents of Christian prophesy are talking about the upcoming lunar tetrad – a series of total lunar eclipses – which begins on the night of April 14-15, 2014. We at EarthSky don’t have any special knowledge about the purported Blood Moons of Biblical prophesy. But, since they’re moons, and since people are asking us, we wanted to reply.
The full moon nearly always appears coppery red during a total lunar eclipse. That’s because the dispersed light from all the Earth’s sunrises and sunsets falls on the face of the moon at mid-eclipse. Thus the term blood moon can be and probably is applied to any and all total lunar eclipses…
Both astronomers and followers of certain Christian pastors are talking about the lunar tetrad of 2014-2015. What is a tetrad? It’s four successive total lunar eclipses, with no partial lunar eclipses in between, each of which is separated from the other by six lunar months (six full moons)
We’re not experts on prophecy of any kind. But we’ll tell you what we know about the new definition for Blood Moon that has raised so many questions recently.
From what we’ve been able to gather, two Christian pastors, Mark Blitz and John Hagee, use the term Blood Moon to apply to the full moons of the upcoming tetrad – four successive total lunar eclipses, with no partial lunar eclipses in between, each of which is separated from the other by six lunar months (six full moons) – in 2014 and 2015. John Hagee appears to have popularized the term in his 2013 book Four Blood Moons: Something is About to Change.
As if we didn’t have enough to look forward to on April 15th! Read on for lots more. The four eclipses are this one, October 8 2014 and April 4 & September 28, 2015. Here’s the eclipse viewing times for Michigan – times for other time zones can be found on EarthSky.
The April 15th eclipse begins at 2 AM Eastern time when the edge of the moon first enters the amber core of Earth’s shadow. Totality occurs during a 78 minute interval beginning around 3 o’clock in the morning on the east coast, midnight on the west coast. Weather permitting, the red moon will be easy to see across the entirety of North America.
Eastern Daylight Time (April 15, 2014)
Partial umbral eclipse begins: 1:58 a.m. EDT on April 15
Total eclipse begins: 3:07 a.m. EDT
Greatest eclipse: 3:46 a.m. EDT
Total eclipse ends: 4:25 a.m. EDT
Partial eclipse ends: 5:33 a.m. EDT
Michael took this photo of the lunar eclipse on February 20, 2008. View it bigger and see more in his The Moon slideshow.
More of the moon on Michigan in Pictures!
March 12, 2014
The Earth Science class for educators at Michigan Tech has an online textbook on Michigan Geography & Geology that’s pretty cool. The chapter on the Ledges at Grand Ledge includes At the Edge of an Ancient Ocean that talks about the rocks that make up The Ledges and begins:
The rocks at Grand Ledge are significant for several reasons. Grand Ledge is an “oasis” of bedrock in an “ocean” of glacial drift that blankets the Lower Peninsula, providing geologists a window into the distant past. The diverse set of sedimentary rocks contains a wealth of information on the plants and animals that dominated the Pennsylvanian Period, about 320 to 290 million years ago. The characteristics of the rocks allowed geologists to reconstruct the changing environment that marked the demise of a great inland ocean. The rocks have been quarried and hold economic value. Lastly, Grand Ledge is scenic and enjoyed by hikers, paddlers, and climbers.
Nearly all students of Michigan geology make a pilgrimage to Grand Ledge at some point in their careers. Good exposures of sedimentary rocks are rare in the Lower Peninsula. Not only are the rocks well exposed but they offer an opportunity to test your skills in identifying a variety of sandstones, some shale and limestone, and even 2 coal. The rocks are exposed in a few abandon quarries and in exposures along the Grand River. To get a good look at the rocks you will need drive between exposure north and south of the river. But don’t be discouraged; the distances are short.
As always in geology, the best place to start is at the base of the stratigraphic section, the oldest rocks. The lower part of the section contains shale, siltstone, and type of sandstone called greywacke. The shale is gray and so fine-grained that you cannot see the mud-sized particles that compose it. If you are brave, you might put a tiny piece in your mouth and push it around a bit. Shale feels smooth, almost creamy, a result of the mud. The shale is also soft and erodes to relatively gentle slopes. Shale is exposed at the base of the layers at the Face Brick Quarry. Think of the light-colored siltstone as a silty shale. You might rub the rock against your thumb and see if any small, visible grains come loose. Again, a taste test might be in order. Siltstone will leave a 3 gritty feel in your mouth. Siltstone is exposed at the base of the rock layers at the American Vitrified Quarry. The greywacke is a greenish-gray colored sandstone and the sand grains are visible to your unaided eye, no tasting required. With a hand lens you can see the rock is made of a mixture of sand sizes, what geologists call poor sorting, and a variety of sand compositions, including quartz, feldspar, mica, and fragments of pre-existing rocks. Greywacke is exposed just above the beach at the Face Brick Quarry.
More winter wallpaper on Michigan in Pictures.