• 30-11-2007


    Days go By



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  • Começei uma caixa nova de memória para o computador perdi alguns
    retratos sem importância aprendendo como trabalhar esta coisa nova.
    Mas eu penso que tenho alguma idéia como ei de fazer agora.
    Meu computador é velho agora, ele era um computador muito bom e caro há 8 anos.
    Eu realmente nunca usei a sua potencialidade máxima.
    Após alguma consideração eu decidi-me não pedir ao pai natal para trazer um novo.
    Este terá que arremediar por agora


    " Perdido na Tradução "

    " Lost in Translation "


    Got a new memory box for the computer.
    I lost a few unimportant pictures learning in how to work this new thing.
    But I think I got some idea how to work it now.
    My computer is old now he was a very good and expensive computer.
    8 years ago.
    I really never did use him to his maximum capability.
    After some consideration I decided not to ask Father Christmas to get a new one.
    This will have to do for the time being.

    MMaxi

    Photo: HgO on Tolar


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  • I only hope to find a way to work this new technology


    In the morning, when i get up. I desire waking up in a relaxed state.
    With the idea that I can write a good story from the tolar daily
    life.

    Eu espero somente encontrar uma maneira de trabalhar esta tecnologia
    nova

    De manhã, quando eu me levantar. Eu desejo acordar acima em um
    estado relaxado. Com a idéia que eu posso escrever uma história boa
    da vida diária tolar.

    J'attends seulement trouver une manière de travailler cette
    technologie nouvelle

    Dans le matin, quand je se soulever. Je désire me réveiller
    ci-dessus dans un état relâché. Avec l'idée que je peux écrire
    une histoire bonne de la vie quotidienne tolar.

    Nunca imaginei o quanto deve ser possivel escrever um livro ou um conto.
    E traduzir em varias linguas ao mesmo tempo.
    Vamos ver o que se vai passar.
    O novo tema no Tolar " Perdido na tradução "


    Je n'ai jamais imaginé combien il doit être possible d'écrire à un
    livre ou à une histoire. Et traduisez en beaucoup de différents
    langages en même temps. Nous verrons ce qui se produira. Le nouveau
    thème dans le Tolar " Perdu dans la traduction "

    I never imagined how much it must be possivel to write a book or a
    story. And at the same time translate in many different languages.
    We will see what happens.
    The new theme in Tolar " lost in translation "


    " Perdido na tradução "
    MMaxi


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  • DAYS GO BY


    Earth's Atmosphere



    The Earth is surrounded by a blanket of air, which we call the atmosphere. It reaches over 560 kilometers (348 miles) from the surface of the Earth, so we are only able to see what occurs fairly close to the ground. Early attempts at studying the nature of the atmosphere used clues from the weather, the beautiful multi-colored sunsets and sunrises, and the twinkling of stars. With the use of sensitive instruments from space, we are able to get a better view of the functioning of our atmosphere.



    Life on Earth is supported by the atmosphere, solar energy, and our planet's magnetic fields. The atmosphere absorbs the energy from the Sun, recycles water and other chemicals, and works with the electrical and magnetic forces to provide a moderate climate. The atmosphere also protects us from high-energy radiation and the frigid vacuum of space.



    The envelope of gas surrounding the Earth changes from the ground up. Four distinct layers have been identified using thermal characteristics (temperature changes), chemical composition, movement, and density.



    Troposphere



    The troposphere starts at the Earth's surface and extends 8 to 14.5 kilometers high (5 to 9 miles). This part of the atmosphere is the most dense. As you climb higher in this layer, the temperature drops from about 17 to -52 degrees Celsius. Almost all weather is in this region. The tropopause separates the troposphere from the next layer. The tropopause and the troposphere are known as the lower atmosphere.

    Stratosphere



    The stratosphere starts just above the troposphere and extends to 50 kilometers (31 miles) high. Compared to the troposphere, this part of the atmosphere is dry and less dense. The temperature in this region increases gradually to -3 degrees Celsius, due to the absorbtion of ultraviolet radiation. The ozone layer, which absorbs and scatters the solar ultraviolet radiation, is in this layer. Ninety-nine percent of "air" is located in the troposphere and stratosphere. The stratopause separates the stratosphere from the next layer.

    Mesosphere



    The mesosphere starts just above the stratosphere and extends to 85 kilometers (53 miles) high. In this region, the temperatures again fall as low as -93 degrees Celsius as you increase in altitude. The chemicals are in an excited state, as they absorb energy from the Sun. The mesopause separates the mesophere from the thermosphere.



    The regions of the stratosphere and the mesosphere, along with the stratopause and mesopause, are called the middle atmosphere by scientists. This area has been closely studied on the ATLAS Spacelab mission series.

    Thermosphere



    The thermosphere starts just above the mesosphere and extends to 600 kilometers (372 miles) high. The temperatures go up as you increase in altitude due to the Sun's energy. Temperatures in this region can go as high as 1,727 degrees Celsius. Chemical reactions occur much faster here than on the surface of the Earth. This layer is known as the upper atmosphere.



    The upper and lower layers of the thermosphere will be studied more closely during the Tethered Satellite Mission (TSS-1R).

    Composition of the Atmosphere



    The atmosphere is primarily composed of Nitrogen (N2, 78%), Oxygen (O2, 21%), and Argon (Ar, 1%). A myriad of other very influential components are also present which include the water (H2O, 0 - 7%), "greenhouse" gases or Ozone (O, 0 - 0.01%), Carbon Dioxide (CO2, 0.01-0.1%),

    Beyond the Atmosphere



    The exosphere starts at the top to the thermosphere and continues until it merges with interplanetary gases, or space. In this region of the atmosphere, Hydrogen and Helium are the prime components and are only present at extremely low densities.


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