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  2. Troposphere - Wikipedia

    en.wikipedia.org/wiki/Troposphere

    The temperature of the troposphere decreases with increased altitude, and the rate of decrease in air temperature is measured with the Environmental Lapse Rate (/) which is the numeric difference between the temperature of the planetary surface and the temperature of the tropopause divided by the altitude.

  3. Tropopause - Wikipedia

    en.wikipedia.org/wiki/Tropopause

    The tropopause is defined as the lowest level at which the lapse rate decreases to 2°C/km or less, provided that the average lapse-rate, between that level and all other higher levels within 2.0 km does not exceed 2°C/km. [1] The tropopause is a first-order discontinuity surface, in which temperature as a function of height varies ...

  4. Lapse rate - Wikipedia

    en.wikipedia.org/wiki/Lapse_rate

    The saturated adiabatic lapse rate (SALR), or moist adiabatic lapse rate (MALR), is the decrease in temperature of a parcel of water-saturated air that rises in the atmosphere. It varies with the temperature and pressure of the parcel and is often in the range 3.6 to 9.2 °C/km (2 to 5 °F/1000 ft ), as obtained from the International Civil ...

  5. Electromagnetic absorption by water - Wikipedia

    en.wikipedia.org/wiki/Electromagnetic_absorption...

    Water at the top of the troposphere, particularly in liquid and solid states, cools as it emits net photons to space. Neighboring gas molecules other than water (e.g. nitrogen) are cooled by passing their heat kinetically to the water. This is why temperatures at the top of the troposphere (known as the tropopause) are about -50 degrees Celsius.

  6. Weak temperature gradient approximation - Wikipedia

    en.wikipedia.org/wiki/Weak_temperature_gradient...

    Free tropospheric temperature refers to the temperature in the upper layers of the troposphere where the influence from the surface and the boundary layer is negligible. Although the framework is formulated with the gradients of free tropospheric temperature, this phenomena occurs as a result of gradients and fluctuations in buoyancy .

  7. Why does it feel colder than the actual temperature? Here's ...

    www.aol.com/why-does-feel-colder-actual...

    With high wind speeds forecasted in the state, it'll feel much colder than the actual temperature. Here's what to know about wind chill and what the term means.

  8. Inversion (meteorology) - Wikipedia

    en.wikipedia.org/wiki/Inversion_(meteorology)

    In meteorology, an inversion (or temperature inversion) is a phenomenon in which a layer of warmer air overlies cooler air. Normally, air temperature gradually decreases as altitude increases, but this relationship is reversed in an inversion. [2] An inversion traps air pollution, such as smog, near the ground.

  9. The Effects Of Extreme Heat On Diabetes - AOL

    www.aol.com/news/effects-extreme-heat-diabetes...

    Changes in temperature can affect blood sugar levels, especially during the warmer months. Dehydration can cause blood sugar to rise as the glucose in your blood becomes more concentrated.