dissabte, 5 de desembre de 2015

THE PETER PAN PAN EFFECT When hydrocarbons are present, nitric oxide reacts with them instead of the ozone. This reaction produces a variety of toxic products, such as a volatile compound known as PAN (peroxyacetyl nitrate). NO + hydrocarbons----------------->PAN and various other compounds. Also, NO2 +hydrocarbons------------------>PAN and various other compounds So, there are two results (at least) from the reaction of nitrogen oxides with hydrocarbons. One is that a lot of volatile, reactive organic compounds are generated directly. The other is that when the nitric oxide (NO) is busy reacting with hydrocarbons, it is not reacting with ozone to break it back down to molecular oxygen. So the amount of ozone in the air increases. With nitric oxide reacting with hydrocarbons, ozone may accumulate to damaging levels. (Ozone may also be released into the air naturally by forest fires. But in a natural situation, ozone would react with nitric oxide and be broken down to oxygen, as noted above). The result, then, is an accumulation of ozone and volatile organic compounds such as PAN. These are referred to as secondary pollutants, because they are formed by the reaction of primary pollutants, nitrogen oxides and hydrocarbons, emitted by burning fossil fuels. The energy from the sun moves the reactions along. This forms photochemical smog, the brown gunk we see in the sky, especially on hot sunny days. Photochemical smog can cause eye irritation and poor visibility. Strong oxidants such as ozone can damage the lungs. The oxidants irritate the linings of lungs. Damage to the lungs may stress the heart. Health damage is worse for people with existing lung and heart conditions. Other health implications may include loss of immune system function, increased susceptibility to infections, and fatigue. The damage can be caused by exposure to large amounts of the pollutant over a short time span, and also by chronic exposure to small amounts over long periods of time. Oxidants can kill plant cells, causing leaves to develop brown spots or drop off the plant, reduce plant growth, and make plants more susceptible to damage from other causes. Oxidants such as ozone can also corrode and destroy many materials such as rubber, nylon, fabric, and paint. The above is a simplified discussion of photochemical smog The bottom line is that conditions in California frequently favor the development of temperature inversions. The pollutants will continue to become more concentrated until a change in the weather leads to the breakup of the inversion layer Thermal Inversions In the normal situation, the temperature decreases as you go up in altitude in the troposphere. The rate of decrease varies, but an accepted average value is 6.5 degrees Celsius per 1000 meters (this is called the normal lapse rate). That is, if you start at sea level and go up (say, in a balloon) 1000 meters in the atmosphere, you can expect that the temperature of the surrounding air will drop an average of 6.5 degrees Celsius. Go up another 1000 meters (one kilometer), and the temperature will drop another 6.5 degrees (that is, it will be 13 degrees colder than it was when you started at sea level). If you are measuring in feet and Fahrenheit degrees, this translates to a drop of about 3.6 degrees F per 1000 feet Did An Optical Illusion Doom the Titanic? ... caused by a thermal inversion in the area south of Newfoundland were the ship was sailing. INVERSÃO TÉRMICA FENÓMENO FREQUENTE EM NOITES CLARAS E CALMAS DE INVERNIA AGORA TAMBÉM NO OUTONO FRIO E LÍMPIDO O SOLO ARREFECE MAIS DEPRESSA QUE A ATMOSFERA ACIMA DELE E COM ELE AS CAMADAS DE AR EM CONTACTO DIRECTO ...FENÓMENO COMUM EM FUNDOS DE VALES E EM VALES SEM FUNDOS PARA ONDE DESLIZA O AR MAIS FRIO DAS VERTENTES MAIS QUENTES Photochemical smog is brown smog, the gray-brown haze that fills the air in many cities. It is especially a problem in warm, sunny regions where there are lots of cars burning gasoline. Researchers in the 1940's and 1950's in Los Angeles noticed that the kinds of pollutants in the air varied over the course of the day. Some pollutants increased in the morning, as people started driving their cars. Other pollutants, including the visible, brown smoggy haze, were most common in the middle of the day. The mix of pollutants changed again in the late afternoon and evening. It became apparent that the chemical reactions among the various pollutants were related to sunlight. Smog is worse in Los Angeles--and everywhere--in the summer, because the light energy from the sun moves some of the reactions along. To form photochemical smog, three main ingredients are needed: nitrogen oxides (NOx), hydrocarbons, and energy from the sun in the form of ultraviolet light (UV). The first thing that starts the chain of events is that people start driving in the morning. As gasoline is burned, nitrogen (N2) in the atmosphere is also burned, or oxidized, forming nitric oxide (NO) N2 + O2 =2NO Hydrocarbons and carbon monoxide (CO) will also be emitted by cars. Hydrocarbons are volatile organic compounds that may include acetaldehyde, formaldehyde, ethylene, and many other compounds. In the air, nitric oxide combines with molecular oxygen to form nitrogen dioxide within a few hours. 2NO + O2--------->2NO2

É FREQUENTE VER-SE O FUMO DAS CHAMINÉS INFLECTIR-SE AO CHEGAR À SUPERFÍCIE DE INVERSÃO E MARCHAR-NOS PELOS PULMÕES ABAIXO CHAMA-SE A ISSO THE PETER PAN PAN MESMO EFFECT This normal decrease in temperature with altitude has lots of implications for weather. In the context of air pollution, it means that the decrease in temperature helps to mix the air, and disperse pollutants. If a parcel of air is warmer than the surrounding air, it is less dense, more bouyant, and it has a tendency to rise up until it finds air that is about the same temperature and density as it is. This helps disperse pollutants at the surface. On the other hand, air which is cold and dense is likely to be stable, and stay put. A very stable situation would occur when cold air is near the ground, and there is a layer of warmer air above it. This is a departure from the normal situation, and is called a temperature inversion, or thermal inversion. This cold air is denser than the warm air above it. It resists rising, and is described as stable air. Above the inversion layer, the air will again cool off with increasing altitude. There are several reasons why an inversion might develop. One situation in which a low level, or surface inversion, might take place is on a clear night, when the earth's surface radiates heat away rapidly. If the air is clear, the ground, and the air directly above it, can be cooler than the air at higher altitudes. This type of situation may occur on winter nights in California, and can be a problem for citrus growers, because if enough heat radiates away, the temperature at the ground surface can drop below the freezing level. Another type of inversion, called an advectional inversion, involves a horizontal inflow of cold air. This might be air blowing in from cold water to a coastal area. Along the California coast, winds frequently blow onshore, passing over the cold ocean waters before reaching land. When this occurs, the air at ground level may be colder than the air above it, and the air is stable. A third type of surface inversion takes place at night in valleys, when cold, dense air flows downslope under the influence of gravity, draining off the slopes and uplands, and into the valleys. The air in the valley bottoms is colder than the air above. Other types of inversions may also develop under various conditions. In California, upper air inversions develop because much of California is on the eastern edge of the subtropical high pressure cell in the Pacific Ocean. This high pressure cell develops in response to global patterns of atmospheric pressure and circulation, rather than local conditions. The presence of high pressure means that the air in the region is subsiding from high altitudes in the atmosphere. Subsiding air is compressed by the increasing pressure of the surrounding air as it descends, so the air warms up as it subsides. So not only is there cool air at ground level (from onshore flow of cool air), there is also a general subsidence of warm air aloft. The inversion layer acts as a lid to prevent air at ground level from rising and dispersing. If there are mountains inland, the mountains can also help trap the air. This means that any pollutants emitted accumulate in the trapped air.

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  1. Previous studies revealed that frontal cyclones are distinct from their synopticscale counterparts not only in spatial and temporal scales but sometimes in intensifying mechanisms. For example, most synoptic-scale cyclones are baroclinically driven and modulated by latent-heat release (Davis et al. 1993; Huo et al. 1996). In contrast, frontal cyclogenesis may result from latent-heat release and subsequent growth in the frontal zone (Joly and Thorpe 1990), the growth of a low-level warm band with uniform potential vorticity (PV) (Sch¨ar and Davies 1990), the interaction with an upper-level PV cut-off (Thorncroft and Hoskins 1990), the growth of low-level PV anomalies under the in uence of frontogenetic deformation (Bishop and Thorpe 1994), the propagation of upper-level PV anomalies across the low-level frontal zone (Hoskins et al. 1985) or a combination of the above processes (Zhang et al. 1999a,b). As compared with the synoptic-scale counterpart, there appears to be no general agreement on the dominant role of any particular parameter in triggering frontal cyclogenesis and in determining the structures and the Ž nal intensity of frontal cyclones (Parker 1998). In fact, a large variety of secondary cyclones with different structures and intensifying mechanisms have been sampled during FASTEX (see Baehr et al. 1999; Joly et al. 1999). In addition, some secondary cyclogenesis appears to be sensitive to slight changes in the model initial conditions and the model physics representations5 de desembre de 2015 a les 18:00

    Although there have been considerable advances in understanding the structures
    and behaviour of synoptic-scale extratropical cyclones (see the comprehensive reviews
    given in Newton and Holopainen (1990) and Shapiro and Gronas (1999)), our knowledge
    of frontal or secondary cyclogenesis† and its behaviour in relation to larger-scale
     ows is rather limited. So far, only a few frontal-cyclogenesis studies have been conducted
    owing to the lack of high-resolution meteorological observations. However,
    growing attention has recently been paid to the frontal cyclogenesis phenomenon since
    the conduct of the Fronts and Atlantic Storm-Track EXperiment (FASTEX, Snyder
    1996; Joly et al. 1997

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    Titus Andronicus Raymond
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    Pedro Morais
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    Titus Andronicus Raymond
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    1. ESTE gaijo é multi-tasco dá piadas brejeiras receitas de cu li n'área etc etc só faltou a bejeca no final do show por sinel do tal si nelo ...isse é nome de cigano da pedreira dos húngaros ou da linha de sintra? Curtir · Responder · 37 min Titus Andronicus Raymond Titus Andronicus Raymond dantes um gajo com a barba mal amanhada era cigano ou capitão-general d'abril ou afinfador em manifes agora sabe-se lá ...virou moda deve ser o efeito andropausa que abril vos deixou em testamento né Curtir · Responder · 35 min Titus Andronicus Raymond Titus Andronicus Raymond the peter PAN PAN deffect ou diz-se cigano chique por sinel ou por chinelo xi nelo metro sexualis aciganado em dia de casório cigano pode cuadotar?7 de desembre de 2015 a les 14:37

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