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This cover is available for your custom order! Consider making it a clock, picture frame, or wall-hanging. Check out our etsy shop for more information.
6.5" x 10" This cover is best suited to be a clock or a wall hanging.
Molarchae's BOOK collection melds together our love of science, creativity, and reuse. Science is an ever-evolving body of knowledge, and as a result, many older books are almost laughably outdated. We rescue books that are past their informative and/or physical prime and give them a new life with the help of a laser cutter and a lot of love.
Governor Moore and Lt. Governor Miller Meet with the Behavioral Health System of Baltimore. by Patrick Siebert at 100 S Charles St 8th floor, Baltimore, MD 21201
The Pinkberry treat that I purchased because I received a coupon for checking in on FourSquare. Proof that incentives drive behavior?
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I thought maybe this male mallard was injured or asleep when I spotted him not moving and lying nearly flat in the grass. He is not foraging here; he just laid there with his beak nudged down into the grass. It seemed like an odd place to rest as he is at least 30 feet from the nearest water but only about 15 feet off a heavily traveled walking trail for humans. He was not asleep (his eyes were wide open), and he did not move or change his position as I approached a little closer. I did not notice any obvious injury, so maybe he was just resting. I got close enough to snap a couple shots, then just let him be.
Hummel Park
Plainfield, Indiana
Twilight is light produced by sunlight scattering in the upper atmosphere, when the Sun is below the horizon, which illuminates the lower atmosphere and the Earth's surface. The word twilight can also refer to the periods of time when this illumination occurs.
The lower the Sun is beneath the horizon, the dimmer the twilight (other factors such as atmospheric conditions being equal). When the Sun reaches 18° below the horizon, the twilight's brightness is nearly zero, and evening twilight becomes nighttime. When the Sun again reaches 18° below the horizon, nighttime becomes morning twilight. Owing to its distinctive quality, primarily the absence of shadows and the appearance of objects silhouetted against the lit sky, twilight has long been popular with photographers and painters, who often refer to it as the blue hour, after the French expression l'heure bleue.
By analogy with evening twilight, the word twilight is also sometimes used metaphorically, to imply that something is losing strength and approaching its end. For example, very old people may be said to be "in the twilight of their lives". The collateral adjective for twilight is crepuscular, which may be used to describe the behavior of animals that are most active during this period.
Twilight is defined according to the solar elevation angle θs, which is the position of the geometric center of the Sun relative to the horizon. There are three established and widely accepted subcategories of twilight: civil twilight (nearest the horizon), nautical twilight, and astronomical twilight (farthest from the horizon).
Civil twilight is the time when the geometric center of the Sun is between the horizon and 6° below the horizon.
Civil twilight is the period when enough natural light remains that artificial light in towns and cities is not needed. In the United States' military, the initialisms BMCT (begin morning civil twilight, i.e., civil dawn) and EECT (end evening civil twilight, i.e., civil dusk) are used to refer to the start of morning civil twilight and the end of evening civil twilight, respectively. Civil dawn is preceded by morning nautical twilight and civil dusk is followed by evening nautical twilight.
Under clear weather conditions, civil twilight approximates the limit at which solar illumination suffices for the human eye to clearly distinguish terrestrial objects. Enough illumination renders artificial sources unnecessary for most outdoor activities. At civil dawn and at civil dusk sunlight clearly defines the horizon while the brightest stars and planets can appear. As observed from the Earth (see apparent magnitude), sky-gazers know Venus, the brightest planet, as the "morning star" or "evening star" because they can see it during civil twilight.
Lawmakers have enshrined the concept of civil twilight. Such statutes typically use a fixed period after sunset or before sunrise (most commonly 20–30 minutes), rather than how many degrees the Sun is below the horizon. Examples include when drivers of automobiles must turn on their headlights (called lighting-up time in the UK), when hunting is restricted, or when the crime of burglary is to be treated as nighttime burglary, which carries stiffer penalties in some jurisdictions.
The period may affect when extra equipment, such as anti-collision lights, is required for aircraft to operate. In the US, civil twilight for aviation is defined in Part 1.1 of the Federal Aviation Regulations (FARs) as the time listed in the American Air Almanac.
Nautical twilight is defined as when the geometric center of the Sun is between 12° and 6° below the horizon.
Before nautical dawn and after nautical dusk, sailors cannot navigate via the horizon at sea as they cannot clearly see the horizon. At nautical dawn and nautical dusk, the human eye finds it difficult, if not impossible, to discern traces of illumination near the sunset or sunrise point of the horizon (first light after nautical dawn but before civil dawn and nightfall after civil dusk but before nautical dusk).
Sailors can take reliable star sightings of well-known stars, during the stage of nautical twilight when they can distinguish a visible horizon for reference (i.e. after astronomic dawn or before astronomic dusk).
Under good atmospheric conditions with the absence of other illumination, during nautical twilight, the human eye may distinguish general outlines of ground objects but cannot participate in detailed outdoor operations.
Nautical twilight has military considerations as well. The initialisms BMNT (begin morning nautical twilight, i.e. nautical dawn) and EENT (end evening nautical twilight, i.e. nautical dusk) are used and considered when planning military operations. A military unit may treat BMNT and EENT with heightened security, e.g. by "standing to", in which everyone assumes a defensive position.
Astronomical twilight is defined as when the geometric center of the Sun is between 18° and 12° below the horizon.[3][4][2] During astronomical twilight, the sky is dark enough to permit astronomical observation of point sources of light such as stars, except in regions with more intense skyglow due to light pollution, moonlight, auroras, and other sources of light. Some critical observations, such as of faint diffuse items such as nebulae and galaxies, may require observation beyond the limit of astronomical twilight. Theoretically, the faintest stars detectable by the naked eye (those of approximately the sixth magnitude) will become visible in the evening at astronomical dusk, and become invisible at astronomical dawn.
Observers within about 48°34' of the Equator can view twilight twice each day on every date of the year between astronomical dawn, nautical dawn, or civil dawn, and sunrise as well as between sunset and civil dusk, nautical dusk, or astronomical dusk. This also occurs for most observers at higher latitudes on many dates throughout the year, except those around the summer solstice. However, at latitudes closer than 8°35' (between 81°25’ and 90°) to either Pole, the Sun cannot rise above the horizon nor sink more than 18° below it on the same day on any date, so this example of twilight cannot occur because the angular difference between solar noon and solar midnight is less than 17°10’.
Observers within 63°47'50" of the Equator can view twilight twice each day on every date between the month of the autumnal equinox and the month of vernal equinox between astronomical dawn, nautical dawn, or civil dawn, and sunrise as well as between sunset and civil dusk, nautical dusk, or astronomical dusk, i.e., from September 1 to March 31 of the following year in the Northern Hemisphere and from March 1 to September 30 in the Southern Hemisphere.
The nighttime/twilight boundary solar midnight's latitude varies depending on the certain month:
In the months of January or July, astronomical dawn to sunrise or sunset to astronomical dusk occurs at latitudes less than 48°54' North or South, because in the months of January or July the Sun's declination is less than 23°06' from the Equator;
In the months of February or August, astronomical dawn to sunrise or sunset to astronomical dusk occurs at latitudes less than 54°02' North or South, because in the months of February or August the Sun's declination is less than 17°58' from the Equator;
In the months of March or September before the equinoxes, astronomical dawn to sunrise or sunset to astronomical dusk occurs at latitudes less than 63°47' North or South, because in the months of March or September before the equinoxes the Sun's declination is less than 8°13' from the Equator;
During the equinoxes, astronomical dawn to sunrise or sunset to astronomical dusk occurs at latitudes less than 72°00' North or South, because during the equinoxes the Sun is crossing the Equator line;
In the months of March or September after the equinoxes, astronomical dawn to sunrise or sunset to astronomical dusk occurs at latitudes less than 67°45' North or South, because in the months of March or September after the equinoxes the Sun's declination is less than 4°15' from the Equator;
In the months of April or October, astronomical dawn to sunrise or sunset to astronomical dusk occurs at latitudes less than 57°09' North or South, because in the months of April or October the Sun's declination is less than 14°51' from the Equator;
In the months of May or November, astronomical dawn to sunrise or sunset to astronomical dusk occurs at latitudes less than 50°03' North or South, because in the months of May or November the Sun's declination is less than 21°57' from the Equator;
In the months of June or December, astronomical dawn to sunrise or sunset to astronomical dusk occurs at latitudes less than 48°34' North or South, because in the month of June the Sun crosses the Tropic of Cancer (about 23°26' North) and in the month of December the Sun crosses the Tropic of Capricorn (about 23°26' South).
At latitudes greater than about 48°34' North or South, on dates near the summer solstice (June 21 in the Northern Hemisphere or December 21 in the Southern Hemisphere), twilight can last from sunset to sunrise, since the Sun does not sink more than 18 degrees below the horizon, so complete darkness does not occur even at solar midnight. These latitudes include many densely populated regions of the Earth, including the entire United Kingdom and other countries in northern Europe and even parts of central Europe. This also occurs in the Southern Hemisphere, but occurs on December 21. This type of twilight also occurs between one day and the next at latitudes within the polar circles shortly before and shortly after the period of midnight sun. The summer solstice in the Northern Hemisphere is on June 21st, while the summer solstice in the Southern Hemisphere is on December 21st.
Civil twilight: between about 60°34' and 65°44' north or south. In the northern hemisphere, this includes the center of Alaska,Iceland, Finland, Sweden, Norway, Faroe Islands and Shetland. In the southern hemisphere this includes parts of the Southern Ocean and the northern tip of the Antarctic Peninsula. When civil twilight lasts all night, this is also referred as a white night.
Nautical twilight: between about 54°34' and 60°34' north or south. In the northern hemisphere this includes the center of Alaska, Russia, Canada, Estonia, Latvia, Scotland, Norway, Sweden,Finland, Lithuania, and Denmark. In the southern hemisphere this includes the southernmost point of South America, and Ushuaia in Argentina. When nautical twilight lasts all night, this is also referred as a white night.
Astronomical twilight: between about 48°34' and 54°34' north or south. In the northern hemisphere, this includes the center of Isle of Man, Aleutian Islands, United Kingdom, Belarus, Ireland, Netherlands, Poland, Germany, Belgium, Czech Republic, Bellingham, Washington, Orcas Island, Washington, Vancouver, British Columbia, Paris, France, Luxembourg, Guernsey, Ukraine, Slovakia and Hungary. In the southern hemisphere this includes the center of South Georgia and the South Sandwich Islands, Bouvet Island, Heard Island, Falkland Islands. It also includes El Calafate and RÃo Gallegos in Argentina, and Puerto Natales in Chile. When astronomical twilight lasts all night, this does not constitute a white night. This phenomenon is known as the grey nights, nights when it does not get dark enough for astronomers to do their observations of the deep sky.
In Arctic and Antarctic latitudes in wintertime, the polar night only rarely produces complete darkness for 24 hours each day. This can occur only at locations within about 5.5 degrees of latitude of the Pole, and there only on dates close to the winter solstice. At all other latitudes and dates, the polar night includes a daily period of twilight, when the Sun is not far below the horizon. Around winter solstice, when the solar declination changes slowly, complete darkness lasts several weeks at the Pole itself, e.g., from May 11 to July 31 at Amundsen–Scott South Pole Station. North Pole has the experience of this from November 13 to January 29.
Solar noon at civil twilight during a polar night: between about 67°24' and 72°34' north or south.
Solar noon at nautical twilight during a polar night: between about 72°34' and 78°34' north or south.
Solar noon at astronomical twilight during a polar night: between about 78°34' and 84°34' north or south.
Solar noon at night during a polar night: between approximately 84°34' and exactly 90° north or south.
At latitudes greater than 81°25' North or South, as the Sun's angular elevation difference is less than 18 degrees, twilight can last for the entire 24 hours. This occurs for one day at latitudes near 8°35’ from the Pole and extends up to several weeks the further toward the Pole one goes. This happens both near the North Pole and near the South Pole. The only permanent settlement to experience this condition is Alert, Nunavut, Canada, where it occurs from February 22–26, and again from October 15–19.
The duration of twilight depends on the latitude and the time of the year. The apparent travel of the Sun occurs at the rate of 15 degrees per hour (360° per day), but sunrise and sunset happen typically at oblique angles to the horizon and the actual duration of any twilight period will be a function of that angle, being longer for more oblique angles. This angle of the Sun's motion with respect to the horizon changes with latitude as well as the time of year (affecting the angle of the Earth's axis with respect to the Sun).
At Greenwich, England (51.5°N), the duration of civil twilight will vary from 33 minutes to 48 minutes, depending on the time of year. At the equator, civil twilight can last as little as 24 minutes. This is true because at low latitudes the Sun's apparent movement is perpendicular to the observer's horizon. But at the poles, civil twilight can be as long as 2–3 weeks. In the Arctic and Antarctic regions, twilight (if there is any) can last for several hours. There is no astronomical twilight at the poles near the winter solstice (for about 74 days at the North Pole and about 80 days at the South Pole). As one gets closer to the Arctic and Antarctic circles, the Sun's disk moves toward the observer's horizon at a lower angle. The observer's earthly location will pass through the various twilight zones less directly, taking more time.
Within the polar circles, twenty-four-hour daylight is encountered in summer, and in regions very close to the poles, twilight can last for weeks on the winter side of the equinoxes. Outside the polar circles, where the angular distance from the polar circle is less than the angle which defines twilight (see above), twilight can continue through local midnight near the summer solstice. The precise position of the polar circles, and the regions where twilight can continue through local midnight, varies slightly from year to year with Earth's axial tilt. The lowest latitudes at which the various twilights can continue through local midnight are approximately 60.561° (60°33′43″) for civil twilight, 54.561° (54°33′43″) for nautical twilight and 48.561° (48°33′43″) for astronomical twilight.
Lake Maggiore or Verbano ( Lagh Magior in Lombard and Piedmontese ) is a pre-Alpine lake of fluvioglacial origin in the Italian geographical region . Its shores are shared between Switzerland ( Canton Ticino ) and Italy (provinces of Verbano-Cusio-Ossola and Novara , in Piedmont , and Varese , in Lombardy ).
The name Maggiore derives from the fact that it is the largest of the lakes in the area, but among the Italian lakes it is the second in surface area after Lake Garda (as well as the second in depth after Lake Como ). In the past it was joined to Lake Mergozzo , from which it was separated due to the formation of the Fondotoce Plain .
Lake Maggiore is located at a height of approximately 193 meters above sea level . Its surface area is 212 km² , most of which, approximately 80%, is in Italian territory. It has a perimeter of 170 km and a length of 64.37 km (the largest among Italian lakes); the maximum width is 10 km and the average width is 3.9 km. The volume of water contained is equal to 37.5 billion m³ with a theoretical replacement time of approximately 4 years. The hydrographic basin is approximately 6,598 km² of which 3,229 are in Italian territory and 3,369 in Swiss territory (the ratio between the surface area of ​​the basin and that of the lake is 31.1). The maximum altitude of the catchment basin is Punta Dufour in the Monte Rosa massif (4,633 m above sea level), while the average altitude is 1,270 m above sea level. The basin is characterized by the existence of around thirty artificial reservoirs with a collection of approximately 600 million of m³ of water which, if released simultaneously, would raise the lake level by approximately 2.5 m. The maximum depth is approximately 370 m (in the cryptodepression between Ghiffa and Porto Valtravaglia ) which is therefore 177 m below sea level.
The major tributaries are the Ticino , the Maggia , the Toce (which receives the waters of the Strona torrent and therefore of Lake Orta ) and the Tresa (in turn an emissary of Lake Lugano and fed by the Margorabbia ). The major tributaries have a different flow pattern, while Ticino and Toce, which have a catchment basin at high altitudes, reach a maximum flow in the period between May and October coinciding with the melting of snow and glaciers ; the other tributaries have a trend strongly influenced by rainfall . Minor tributaries are the Verzasca , Cannobino , San Bernardino , San Giovanni , Giona and Boesio streams . The only emissary is the Ticino which flows from the lake to Sesto Calende .
Envoys
Bardello
Boesio
Mergozzo Canal
Cannobino
Erno
Fraud of Caldè
Fraud of Porto Valtravaglia
Jonah
Maggia
Molinera
Monvallina
Riale Corto
Riale del Molino
Riale del Roddo
Riale di Casere
Rio Ballona
Rio Colmegnino (or Rio di Colmegna)
Rio Colorio
Rio dell'Asino
Rio Molinetto
Rio Valmara
Rone
San Bernardino
Saint John
San Giovanni di Bedero
Thick Forest
Stronetta
Tiasca
Ticino
Toce
Aquanegra stream
Tresa
Trigo
Versella or Varesella
Verzasca
Vevera
Geology
The origin of Lake Maggiore is partly glacial, as evidenced by the layout of the hills formed by moraine deposits of a glacial nature, but it is ascertained that the glacial excavation took place on a pre-existing river valley, the profile of the lake in fact has the typical V shape of river valleys.
Baveno pink granite was widely used as a building material in the past . Furthermore, the ancient construction uses of Angera stone are known (used for example in classical antiquity and in the medieval period), while the Caldè limestone quarries provided for many centuries the raw material for the lime with which high-rise buildings were built. Lombardy and Piedmont: thanks to the ease of transport by boat, first on the lake, then on the Milanese canals
Lake Maggiore is characterized by cold winters, but milder than inland, and moderately snowy (with average accumulations of 10 cm for each snowfall and sometimes even higher than 30 cm up to a maximum of 50 cm), summers are moderately hot, humid and stormy, the average temperature in January is around 2 degrees centigrade, with peaks of 3 degrees on the northern side of the Borromean Gulf (due to the extensive exposure to the sun), night temperatures can drop below 0, up to -10, but very rarely go below this value. In summer the average temperatures are around 22 degrees centigrade, with daytime peaks rarely exceeding 32 degrees. Proceeding towards the internal valleys the temperatures gradually become more rigid. The area is very rainy and sometimes, especially in intermediate seasons, floods can occur. The temperature of the surface waters (up to 2 meters deep) of the lake reach winter peaks of 5-6 degrees, while in summer they reach an average of 22-24 degrees.
Some statistics on Lake Maggiore . It should be noted that during lean periods the water level between Locarno and Sesto Calende can vary by 1 cm, while during floods up to 30 cm
Like all pre-Alpine lakes, Lake Maggiore is crossed, especially in the summer, by two types of prevailing winds, one which blows in the morning from the mountains towards the plain (called moscendrino as it comes from the Monte Ceneri Pass , sometimes tramontana ) and a small breeze that blows from the plain to the mountains especially during the afternoon (called inverna ). These constant winds make the pre-Alpine lakes an excellent field for practicing sports that use the wind, such as sailing and windsurfing . Lake Maggiore has some particular points, especially in the upper part, where the mountains squeeze together to form a narrow valley in which these winds blow very strongly.
Then there are other winds typical of this lake such as the winter wind , which blows from the south-west and generally brings storms, the major one , which comes from the north-east and is very dangerous as it agitates the lake a lot, the valmaggine which blows slightly from the valleys behind Locarno , the mergozzo , which blows especially at night, from the north-west
In Lake Maggiore there are many large, small or tiny islands , divided between 8 in Piedmont, 2 in Switzerland and 2 in Lombardy, for a total of 12.
Borromean Islands
Beautiful island
Isola Madre
Isola dei Pescatori (or Isola Superiore or Isola Superiore dei Pescatori)
Islet of San Giovanni
Malghera islet (or rock).
Brissago Islands
San Pancrazio Island (or Big Island)
Island of Sant'Apollinare (or Isolino)
Castles of Cannero
Isolino Partegora
Sasso Galletto
Between Stresa and Verbania there is the Borromean archipelago: Isola Madre (the largest in the lake basin), Isola Bella and Isola Superiore dei Pescatori (also known more simply as Isola dei Pescatori or Isola Superiore)
Opposite the Swiss town of Ronco sopra Ascona are the two islands of Brissago, the larger of which hosts a botanical garden.
In front of the coast of Cannero Riviera there are the three emerged rocks called Castelli di Cannero: the major rock, totally occupied today by the Vitaliana war artefact, a fortress commissioned by Count Ludovico Borromeo starting from 1518, the minor rock, on which the ruins of the so-called "prisons" stand, but in fact a small advanced tower with a falconette gunboat garrisoning the southern canal port, and finally the little rock (towards Maccagno ) of the "Melgonaro", on which only a stunted but tenacious plant grows fascinated poets and engravers such as Piero Chiara , Marco Costantini , Carlo Rapp .
Finally, we must mention the small island of San Giovanni in front of Verbania (famous because it was the residence of the orchestra director Arturo Toscanini in the seventeenth-century Palazzo Borromeo for many years ), the small island of La Malghera also known as Isola delle Bambole , among 'Isola Bella and that of the Fishermen and therefore the Isolino Partegora in the small gulf of Angera .
History:
The finds and evidence found tell us that following the actual creation of the lake, with the complete retreat of the ice, the surrounding area was inhabited by nomadic groups , who used the territory mainly as a place for hunting and supplies.
In the Chalcolithic historical period, the first residential areas were built in the immediate vicinity of the lake and from that moment there was a slow consolidation of sedentary groups .
On the shores of the lake, the Golasecca culture developed between the 9th and 4th centuries BC , a Celtic -speaking Iron Age civilization . The Golasecchians advanced as far as some areas of present-day Lombardy , only to be pushed back again to their western borders by the descent of the Celts into the Italian peninsula , probably the population of the Taurine Gauls .
The Gauls therefore had supremacy over the lake territory until the advance of the Romans who turned the Piedmont and Lombard areas back into provinces of the empire . The " Verbanus Lacus " (name given to it by the Romans, from which the nomenclature Lake Verbano will probably derive ) or " Lacus Maximus " (another name even attributed to it by Virgil ) will remain firmly in the hands of the Roman Empire . In Roman times, navigation along the lake experienced particular development, so much so that ships could descend the Ticino and thus reach Pavia , from where they could reach, thanks to the Po , as far as the Adriatic Sea . It is no coincidence that the excavations of the Angera settlement have brought to light finds that show strong connections between the lake and the upper Adriatic. This shipping line experienced particular development during the early Middle Ages , when Pavia was the capital of the Lombard kingdom first and then of the kingdom of Italy.
To arrive at a period of rebirth of the cities on the lake we had to wait until the Middle Ages , which led to the creation of villages, castles and in general a very different example of the physiognomy of inhabited places.
In this period the area around the lake, as well as numerous territories in the surroundings of Milan , passed into the hands of various families such as the Della Torre , the Visconti , the ruling house of the Habsburgs from 1713 and in particular the Borromeo family , which had enormous influence for many years on Lake Maggiore, starting from the acquisition of the fiefdom of Arona in 1445. Another very illustrious lineage that had a great influence in the medieval era is that of the Marquises Morigi or Moriggia, who received numerous territories from the Viscontis such as the degagne of San Maurizio and San Martino, the Valtravaglia which were nicknamed "Morigie lands". Over the centuries the families of Borromeo and Morigi fought bitterly for hegemony over these lands. The Borromeo themselves also had, between 1523 and 1524, actual armed clashes against Francesco II Sforza who on several occasions sent troops and armed ships against the Borromeo fortresses located on the islands of Cannero . Other noble families linked to the territory since the Middle Ages were the Besozzi , the Sessa , the Luini and the Capitanei of Locarno.
Starting from the 14th century, navigation along the lake was also exploited to transport the heavy blocks of marble coming from Candoglia and other quarries located in the surroundings of the lake towards the two main Lombard construction sites of the Middle Ages and the Renaissance: the cathedral of Milan and the Charterhouse of Pavia
The Behavioral Operations Management Summer Institute for PhD students at the Ross School of Business of the University of Michigan, Ann Arbor (BOMSI2019). The lead faculty were Ryan Buell (Harvard Business School), Stephen Leider (Ross School of Business, University of Michigan), and Jordan Tong (Wisconsin School of Business, University of Wisconsin-Madison). From the website, "The inaugural Behavioral Operations Management Summer Institute for PhD students will be held June 10-14, 2019, at the University of Michigan, Ross School of Business in partnership with the Center for Value Chain Innovation. The conference is co-sponsored by the business schools at the University of Michigan, and the University of Wisconsin-Madison. Support for this event is also being provided by Harvard Business School's Technology and Operations Management Unit. The 1-week intensive summer institute is designed to provide PhD students who are interested in behavioral research a solid foundation to conduct behavioral operations management research. Additionally, we hope that the summer institute will encourage collaboration and the creation of a research community among the next generation of researchers. Each day of the institute will include morning and afternoon sessions. Morning sessions will provide a general overview of BOM, review core behavioral economics/psychology topics, and discuss OM applications. Afternoon sessions will be focused more on small groups, practicums (e.g., applying ideas to actual research activity), and roundtables (more informal discussions). There will also be free time to prepare for the next day, have office hours, pair up to work on ideas, and hang out!" Pictures from the sessions taken over the week.
Congratulations to an inaugural class of 22 officers from the Royal Grenada Police Force who completed an 8-week Social & Behavioral Policing program with SGU's School of Arts & Sciences.
Held Thursday 09/14/2017, the Center on Finance, Law, and Policy hosted a symposium discussing behavioral finance. This event included keynote speakers, interdisciplinary panel discussions, and an interactive audience experiment, exploring topics of technological progress in our overall economy.
Details: fordschool.umich.edu/events/2017/behavioral-finance-sympo...
Available for free download under a Creative Commons Attribution-NoDerivatives 4.0 International license. Mandatory attribution can be listed as: Peter Smith / Gerald R. Ford School of Public Policy
Photo from an exhibition at The Cooper Union (Oct. 4 – Nov. 18, 2022), curated by Anyone Corporation.
Olana Orchard Studio Architectural Model (2019) by SAA/Stan Allen Architect
A feisty relationship in the nest. This was one of ten pecking attacks that went back and forth in about 20 minutes of shooting. Makes for a good shot thought.
Held Thursday 09/14/2017, the Center on Finance, Law, and Policy hosted a symposium discussing behavioral finance. This event included keynote speakers, interdisciplinary panel discussions, and an interactive audience experiment, exploring topics of technological progress in our overall economy.
Details: fordschool.umich.edu/events/2017/behavioral-finance-sympo...
Available for free download under a Creative Commons Attribution-NoDerivatives 4.0 International license. Mandatory attribution can be listed as: Peter Smith / Gerald R. Ford School of Public Policy
Held Thursday 09/14/2017, the Center on Finance, Law, and Policy hosted a symposium discussing behavioral finance. This event included keynote speakers, interdisciplinary panel discussions, and an interactive audience experiment, exploring topics of technological progress in our overall economy.
Details: fordschool.umich.edu/events/2017/behavioral-finance-sympo...
Available for free download under a Creative Commons Attribution-NoDerivatives 4.0 International license. Mandatory attribution can be listed as: Peter Smith / Gerald R. Ford School of Public Policy
Currently considered a subspecies of White Wagtail, Motacilla alba. A vagrant at Pismo Creek Mouth, Pismo Beach, CA.
This is how I first saw him. Because something or other kept making a racket, I was finally drawn to my sunroom where the Brown Thrasher you see here was frantically pounding on the window. He's still nearby returning every so often to pound some more.
Thank you for your visit. Your friendship and kind suggestions mean a lot to me.
A few weeks ago, I posted some information about the dangers linked to the mistaken interpretation of ocular data.
While data capture is greatly facilitated thanks to companies like Tobii (I would like to take this opportunity to thank the whole Tobii team for its in-depth work on hardware eyetracking), the analysis of data requires thorough knowledge of the perceptive-cognitive system.
Unfortunately, nowadays to make eyetracking popular, the software on offer is too simplistic to draw reliable conclusions.
More info on www.simplifyinginterfaces.com
Baby's big enough to sit in restaurant's high chairs now. But his patience is still limited and after a while he wants out.
Canada Geese, Butler WI. I spent an hour and a half this evening just watching the amazing behavior of these Geese, I know there must be a reason for the lowered heads but for the life of me can't figure it out, any ideas?
Held Thursday 09/14/2017, the Center on Finance, Law, and Policy hosted a symposium discussing behavioral finance. This event included keynote speakers, interdisciplinary panel discussions, and an interactive audience experiment, exploring topics of technological progress in our overall economy.
Details: fordschool.umich.edu/events/2017/behavioral-finance-sympo...
Available for free download under a Creative Commons Attribution-NoDerivatives 4.0 International license. Mandatory attribution can be listed as: Peter Smith / Gerald R. Ford School of Public Policy
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