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THE JOURNEY THROUGH TIME

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MY'STORY

The MOVE Fire

This is a personal recollection on the Move fire on May 13, 1985 Philadelphia police fired thousands of rounds at the MOVE house, city officials approved dropping an explosive device on the roof, the resulting fire was allowed to burn, 11 people—including five children—died, and 61 homes were destroyed. Philadelphia City Council later called it a “brutal attack carried out by the City of Philadelphia on its own citizens” and acknowledged that no individual faced criminal consequences for the bombing. One timeline correction worth preserving for the BHP record: the major previous MOVE-police confrontation was August 8, 1978, about seven years before the bombing, not a year or two earlier. Officer James Ramp was killed, other police and firefighters were wounded, nine MOVE members were later convicted, and television cameras recorded police beating Delbert Africa during his arrest. The 1985 MOVE Commission later specifically criticized city planners for failing to adequately use lessons from that 1978 confrontation. And that actually strengthens the point you’re making: 1985 did not happen without precedent or institutional memory. There had already been a deadly confrontation with MOVE, years of conflict, negotiations and police involvement before Osage Avenue.

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BLACK FACTS
The Truths They Never Taught You...

The Violence That Helped Spark the NAACP

In August 1908, a white mob attacked Springfield, Illinois’s Black community, destroying homes and businesses and lynching two Black men. National outrage over the violence helped spur the movement that created the NAACP the following year.

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Wikipedia

Aerial perspective

In this picture, the aerial perspective effect is emphasized by a range of mountains at different distances, photographed in a nearly contre-jour condition.

Aerial perspective, or atmospheric perspective, is the effect the atmosphere has on the appearance of an object as viewed from a distance. As the distance between an object and a viewer increases, the contrast between the object and its background decreases, and the contrast of any markings or details within the object also decreases. The colours of the object also become less saturated and shift toward the background colour, which is usually bluish, but may be some other colour under certain conditions (for instance, reddish around sunrise or sunset).

Aerial perspective as viewed towards a sunset, with the colour shifting toward red as a result of rayleigh scattering
Dai Jin, "Landscape in the Style of Yan Wengui", early Ming Dynasty (1368–1644); a Chinese landscape painting using atmospheric perspective to show recession in space
Frans Koppelaar, Landscape near Bologna, 2001; a painting featuring atmospheric perspective: distant objects appear paler, of lower contrast, and bluer than nearer objects.

History

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Atmospheric perspective was used in Pompeian Second Style frescos, one of the Pompeian Styles, dating as early as 30 BCE. Notable examples include the Garden Room Fresco from the Villa of Livia in Prima Porta, Italy, and the first-century Pompeian fresco Paris on Mount Ida.[1]

With varying degrees of accuracy, explanations of the effects of atmospheric perspective were written by polymaths such as Leon Battista Alberti and Leonardo da Vinci. The latter used aerial perspective in many of his paintings such as The Annunciation, the Mona Lisa, and The Last Supper, introducing a technique to paint the effect accurately that was adopted by his followers, the Leonardeschi. Art historians note that it is lacking in works by some artists of the same period, such as Raphael,[2] although he adopted the use of sfumato that was introduced by Leonardo at the same time.

Aerial perspective was used in paintings from the Netherlands in the fifteenth century by Leonardo da Vinci.

Optics

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The major component affecting the appearance of objects during daylight is scattering of light, called sky light, into the line of sight of the viewer. Scattering occurs from molecules of the air and also from larger particles in the atmosphere such as water vapour and smoke. Scattering adds the sky light as a veiling luminance onto the light from the object, reducing its contrast with the background sky light. Sky light usually contains more light of short wavelength than other wavelengths (this is why the sky usually appears blue), which is why distant objects appear bluish.

Why reducing contrast reduces clarity

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The ability of a person with normal visual acuity to see fine details is determined by contrast sensitivity.[3] Contrast sensitivity is the reciprocal of the smallest contrast for which a person can see a sine-wave grating. A person's contrast sensitivity function is contrast sensitivity as a function of spatial frequency. Normally, peak contrast sensitivity is at about four cycles per degree of visual angle. At higher spatial frequencies, comprising finer and finer lines, contrast sensitivity decreases, until at about forty cycles per degree even the brightest of bright lines and the darkest of dark lines cannot be seen.

The high spatial frequencies in an image give it fine details.[4] Reducing the contrast of an image reduces the visibility of these high spatial frequencies because contrast sensitivity for them already is poor. This is how a reduction of contrast can reduce the clarity of an image—by removing its fine details.

Reducing the contrast is not the same as blurring an image. Blurring is accomplished by reducing the contrast only of the high spatial frequencies. Aerial perspective reduces the contrast of all spatial frequencies.

In art

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In art, especially painting, aerial perspective or atmospheric perspective[5] refers to the technique of creating an illusion of depth by depicting distant objects as paler, less detailed, and usually bluer than near objects. This technique has a long history in visual art, appearing in ancient Roman frescoes such as those in the Villa of Livia and early Chinese landscape painting such as Eight Views of Xiaoxiang by Dong Yuan.

The technique allows a painter to capture the effect that atmosphere has on the appearance of an object as viewed from a distance. As the distance between an object and a viewer increases, the contrast between the object and its background decreases, and the contrast of any markings or details within the object also decreases. The colours of the object also become less saturated and shift towards the colour of the atmosphere, which is bluish when sunlit, but will shift to other colours under certain conditions (for instance, reddish around sunrise and sunset or saturated during fog).

(One caution: in common speech, the words perspective and viewpoint tend to be used interchangeably; however, in art, aerial perspective does not imply an aerial viewpoint, such as that forming the basis of the aerial landscape genre. The example by Frans Koppelaar pictured here shows the difference. This landscape is a good example of aerial perspective; however, it is not an aerial landscape, since apparently, the observer is standing on the ground.) As such, the term atmospheric perspective can be understood to better describe how properties of the scene's atmosphere affect the appearance of an object as it moves further from the viewer.

See also

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References

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  1. ^ Brooks, K. R. (2017). "Depth Perception and the History of Three-Dimensional Art: Who Produced the First Stereoscopic Images?". i-Perception. 8 (1). Sage: 204166951668011. doi:10.1177/2041669516680114. PMC 5298491. PMID 28203349.
  2. ^ Salmi, Mario; Becherucci, Luisa; Marabottini, Alessandro; Tempesti, Anna Forlani; Marchini, Giuseppe; Becatti, Giovanni; Castagnoli, Ferdinando; Golzio, Vincenzo (1969). The Complete Work of Raphael. New York: Reynal and Co., William Morrow and Company. pp. 616–17.
  3. ^ Kelly, D. H. (1977). Visual contrast sensitivity. Optica Acta, 24, 107-129.
  4. ^ Blake, R., & Sekuler, R. (2006). Perception (5th ed.). New York: McGraw-Hill.
  5. ^ Raybould, Barry John (18 December 2020). "How to use atmospheric perspective to create mood and feeling in art". www.virtualartacademy.com.

Source: Wikipedia. Article content is retrieved live through the MediaWiki API.

Wikipedia

Aerial perspective

Aerial perspective, or atmospheric perspective, is the effect the atmosphere has on the appearance of an object as viewed from a distance. As the distance between an object and a viewer increases, the contrast between the object and its background decreases, and the contrast of any markings or details within the object also decreases. The colours of the object also become less saturated and shift toward the background colour, which is usually bluish, but may be some other colour under certain conditions (for instance, reddish around sunrise or sunset).

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Wikipedia

Aerial perspective (disambiguation)

Aerial perspective or atmospheric perspective is the effect on the appearance of an object by the atmosphere between it and a viewer. Aerial perspective may also refer to: aerial photography aerial landscape art bird's-eye view, elevated view of an object from above top-down perspective

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Wikipedia

Farrukh Beg

Farrukh Beg (Persian: فرخ بیگ; c. 1547 – after 1615), also known as Farrukh Husayn, was a Persian painter, who spent a bulk of his career in Safavid Iran and Mughal India, praised by Mughal Emperor Jahangir as "unrivaled in the age." Farrukh Beg was credited with painting a plethora of Persian and Mughal paintings, a handful of which survive today. His work showed his distinct training in Persian manuscript painting, which later on evolved to include more experimental techniques such as atmospheric perspective and modeling. Farrukh had produced miniature paintings under the patronage of five known rulers in West Asia and South Asia: Ibrahim Mirza of Safavid Mashhad, Mirza Muhammad Hakim of Kabul, Akbar in Mughal India and later his son Jahangir, and Ibrahim Adil Shah II of the Sultanate of Bijapur. His distinct style came to be revered by his contemporaries and patrons, due to a distinct homogeneity, evolving as a result of his Persian training and experiences in cosmopolitan Mughal courts. His life was later mired in mystery due to his sudden hiatus from the Mughal court sometime after 1595, rejoining the Mughal atelier around 1609. Evidence has shown he spent a bulk of this time in Bijapur under the patronage of Ibrahim Adil Shah II of the Sultanate of Bijapur.

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Wikipedia

Geography of the Marquesas Islands

The Marquesas Islands are the island group farthest from any continent in the world, lying between 400 and 600 miles (600 and 1,000 km) south of the equator and approximately 740 miles (1,200 km) northeast of Tahiti. A pair of volcanic archipelagoes, they fall naturally into two geographical divisions, The northwestern group consists of Eïao, Hatutu (Hatutaa), Motu One, and the islands centered on the large island of Nuku Hiva: Motu Iti (Hatu Iti), Ua Pou, Motu Oa and Ua Huka. The southeastern group consists of Fatu Uku, Tahuata, Moho Tani (Motane), Terihi, Fatu Hiva and Motu Nao (Thomasset Rock), clustered around the main island of Hiva Oa which is the largest and most populous island of the southeastern group. With a combined land area of 405 square miles (1,050 km2), the Marquesas are among the largest island groups of French Polynesia, Nuku Hiva being the second largest island in the entire territory, after Tahiti. With the exception of Motu One, all the islands of the Marquesas are of volcanic origin. The Marquesas are one of the few island groups in Polynesia where precipitation is not abundant. Most of the islands are subject to frequent drought conditions due to their geographic location and periodic fluctuations in the normally prevailing easterly winds. Although the islands lie within the tropics, they are the first major break in the prevailing easterly winds spawned from the extraordinarily dry (from an atmospheric perspective) Humboldt Current. The annual rainfall is generally around 1,270 millimetres (50 inches), but this average is misleading because of very high variability. In La Niña years, rainfall can decline to less than 500 millimetres (20 inches), whilst in El Niño years when the ocean warms it can reach 2,800 millimetres (110 inches). Unlike the rest of French Polynesia, most rain falls during the cooler months, with May to July usually the wettest and November the driest. Because of their exceptionally variable climate, the islands are subject to extreme drought and flood conditions. Although they are mostly high and craggy with jagged peaks rising to 4,000 feet (1,200 metres) in places, only two of the ten islands have elevations above about 750 metres (2,500 feet) and these are the only ones that have sufficiently reliable precipitation for the development of rainforests. This has led to historical fluctuations in water supply, which has been a crucial factor in the sustainability of human populations in certain sections of the various islands throughout the archipelago. This is especially evident in the low historical population of Ua Huka which has a maximum elevation of 2,812 feet (860 metres), and the intermittent inhabitability of Eiao which has a maximum elevation of 1,890 feet (580 metres). The islands lack both coastal plains and coral reefs. As a result, habitation is generally found only where streams run down from the mountains in narrow valleys. Agricultural products include copra, taro, breadfruit, coffee beans and vanilla. The islands have also developed a tourist industry. The Marquesas Islands are thought to have formed from a center of upwelling magma called the Marquesas hotspot.

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TOPIC OF THE DAY

Greenwood / Black Wall Street

Before the 1921 destruction of Tulsa’s Greenwood District, Black residents had created a remarkable center of business and community life. The district included stores, professional offices, entertainment venues and homes owned by Black citizens. Understanding Greenwood means learning what was built—not only what was burned.

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TRIVIA QUESTION OF THE DAY

Which heavyweight champion was known as the “Brown Bomber”?

Joe Louis.