How to Define Value in Relation to Art

How to Define Value in Relation to Art As an element of art, value refers to the visible lightness or darkness of a color. Value is synonymous with luminosity in this context and can be measured in various units designating electromagnetic radiation. Indeed, the science of optics  is a fascinating branch of physics, albeit one to which visual artists typically devote little to no thought. Value is relevant to the lightness or darkness of any color, but its importance is easy to visualize in a work with no colors other than black, white, and a grayscale. For a great example of value in action, think of a black and white photograph. You can easily visualize how the infinite variations of gray suggest planes and textures. The Subjective Value of Art While value can be a technical term related to color, it can be a more subjective term related to either the importance of a work or its monetary worth. Value can also refer to the sentimental, cultural, ritualistic, or aesthetic importance of work. Unlike luminosity, this type of value cannot be measured. It is entirely subjective and open to, literally, billions of interpretations.   For instance, anyone can admire a sand mandala, but its creation and destruction hold specific ceremonial values in Tibetan Buddhism. Leonardos ​Last Supper ​mural was a technical disaster, but its depiction of a defining moment in Christianity has made it a religious treasure worthy of conservation. Egypt, Greece, Peru, and other countries have sought the return of significant cultural works of art that were sold abroad in earlier centuries. Many a mother has carefully preserved many pieces of refrigerator art, for their emotional value is incalculable.   The Monetary Value of Art Value may additionally refer to the monetary worth attached to any given work of art. In this context, value is pertinent to resale prices  or  insurance premiums. Fiscal value is primarily objective, assigned by acknowledged art-historic specialists who eat, breathe and sleep fine art market values.  To a smaller extent, this definition of value is subjective in that certain collectors are willing to pay any amount of money to own a particular work of art. To illustrate this seeming dichotomy, refer to the  May 16, 2007, Post-War and Contemporary Art Evening Sale at Christies New York City showroom. One of original Marilyn silkscreen paintings by Andy Warhol had an estimated (objective) pre-sale value of more than  $18,000,000. $18,000,001 would have been accurate, but the actual gavel price plus buyers premium was a whopping (subjective)  $28,040,000. Someone, somewhere obviously felt that hanging in his or her underground lair was worth an additional $10,000,000. Quotations About Value In preparing a study or a picture, it seems to me very important to begin by an indication of the darkest values... and to continue in order to the lightest value. From the darkest to the lightest I would establish twenty shades.(Jean-Baptiste-Camille Corot) Strive not to be a success, but rather to be of value.(Albert Einstein) Its impossible to make a picture without values. Values are the basis. If they are not, tell me what is the basis.(William Morris Hunt) Nowadays people know the price of everything and the value of nothing.(Oscar Wilde) Color is an inborn gift, but appreciation of value is merely training of the eye, which everyone ought to be able to acquire.(John Singer Sargent) There is no value in life except what you choose to place upon it and no happiness in any place except what you bring to it yourself.(Henry David Thoreau)

Learn About Thermal Inversion

Learn About Thermal Inversion Temperature inversion layers also called thermal inversions or just inversion layers, are areas where the normal decrease in air temperature with increasing altitude is reversed and air above the ground is warmer than the air below it. Inversion layers can occur anywhere from close to ground level up to thousands of feet into the atmosphere. Inversion layers are significant to meteorology because they block atmospheric flow which causes the air over an area experiencing an inversion to become stable. This can then result in various types of weather patterns. More importantly, though, areas with heavy pollution are prone to unhealthy air and an increase in smog when an inversion is present because they trap pollutants at ground level instead of circulating them away. Causes of Temperature Inversions Normally, air temperature decreases at a rate of 3.5Â °F for every 1000 feet (or roughly 6.4Â °C for every kilometer) you climb into the atmosphere. When this normal cycle is present, it is considered an unstable air mass and air constantly flow between the warm and cool areas. As such the air is better able to mix and spread around pollutants. During an inversion episode, temperatures increase with increasing altitude. The warm inversion layer then acts as a cap and stops atmospheric mixing. This is why inversion layers are called stable air masses. Temperature inversions are a result of other weather conditions in an area. They occur most often when a warm, less dense air mass moves over a dense, cold air mass. This can happen for example when the air near the ground rapidly loses its heat on a clear night. In this situation, the ground becomes cooled quickly while the air above it retains the heat the ground was holding during the day. Additionally, temperature inversions occur in some coastal areas because upwelling of cold water can decrease surface air temperature and the cold air mass stays under warmer ones. Topography can also play a role in creating a temperature inversion since it can sometimes cause cold air to flow from mountain peaks down into valleys. This cold air then pushes under the warmer air rising from the valley, creating the inversion. In addition, inversions can also form in areas with significant snow cover because the snow at ground level is cold and its white color reflects almost all heat coming in. Thus, the air above the snow is often warmer because it holds the reflected energy. Consequences of Temperature Inversions Some of the most significant consequences of temperature inversions are the extreme weather conditions they can sometimes create. One example of these is freezing rain. This phenomenon develops with a temperature inversion in a cold area because snow melts as it moves through the warm inversion layer. The precipitation then continues to fall and passes through the cold layer of air near the ground. When it moves through this final cold air mass it becomes super-cooled (cooled below freezing without becoming solid). The supercooled drops then become ice when they land on items like cars and trees and the result is freezing rain or an ice storm. Intense thunderstorms and tornadoes are also associated with inversions because of the intense energy that is released after an inversion blocks an area’s normal convection patterns. Smog Although freezing rain, thunderstorms, and tornadoes are significant weather events, one of the most important things impacted by an inversion layer is smog. This is the brownish-gray haze that covers many of the world’s largest cities and is a result of dust, auto exhaust, and industrial manufacturing. Smog is impacted by the inversion layer because it is in essence, capped when the warm air mass moves over an area. This happens because the warmer air layer sits over a city and prevents the normal mixing of cooler, denser air. The air instead becomes still and over time the lack of mixing causes pollutants to become trapped under the inversion, developing significant amounts of smog. During severe inversions that last over long periods, smog can cover entire metropolitan areas and cause respiratory problems for the inhabitants of those areas. In December 1952, for example, such an inversion occurred in London. Because of the cold December weather at the time, Londoners began to burn more coal, which increased air pollution in the city. Since the inversion was present over the city at the same time, these pollutants became trapped and increased London’s air pollution. The result was the Great Smog of 1952 that was blamed for thousands of deaths. Like London, Mexico City has also experienced problems with smog that have been exacerbated by the presence of an inversion layer. This city is infamous for its poor air quality but these conditions are worsened when warm sub-tropical high-pressure systems move over the city and trap air in the Valley of Mexico. When these pressure systems trap the valley’s air, pollutants are also trapped and intense smog develops. Since 2000, Mexicos government has developed a ten-year plan aimed at reducing ozone and particulates released into the air over the city. London’s Great Smog and Mexico’s similar problems are extreme examples of smog being impacted by the presence of an inversion layer. This is a problem all over the world though and cities like Los Angeles, California; Mumbai, India; Santiago, Chile; and Tehran, Iran, frequently experience intense smog when an inversion layer develops over them. Because of this, many of these cities and others are working to reduce their air pollution. To make the most of these changes and to reduce smog in the presence of a temperature inversion, it’s important to first understand all aspects of this phenomenon, making it an important component of the study of meteorology, a significant sub-field within geography.