The height of the troposphere depends on the temperature of the troposphere. The temperature varies due to latitude and from day to night and due to seasonal variations.
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The highest sea-level pressure on Earth occurs in Siberia, where the Siberian High often attains a sea-level pressure above 1050 hPa (105 kPa; 31 inHg), with record highs close to 1085 hPa (108.5 kPa; 32.0 inHg).
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How does atmospheric pressure change within the troposphere? It decreases with increasing altitude.
The uneven heating of the regions of the troposphere by the sun ( the sun warms the air at the equator more than the air at the poles )causes convection currents, large-scale patterns of winds that move heat and moisture around the globe.
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At sea level, the weight of the air above this unit area would (on average) weigh 14.7 pounds! That means pressure applied by this air on the unit area would be 14.7 pounds per square inch. Meteorologists use a metric unit for pressure called a millibar and the average pressure at sea level is 1013.25 millibars. I.
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As altitude rises, air pressure drops. In other words, if the indicated altitude is high, the air pressure is low.
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The 3 main factors that affect barometric (air) pressure are: Temperature of air. Altitude or Elevation. Moisture.
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The thickness of the troposphere is primarily determined by its average temperature. This is why its thickness can vary from about 23,000 feet during…
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Atmospheric pressure is an indicator of weather. When a low-pressure system moves into an area, it usually leads to cloudiness, wind, and precipitation. High-pressure systems usually lead to fair, calm weather.
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High air pressure produces clear sky, dry and stable weather. In a low pressure zone, wind is circulated inwards and upwards rapidly. As a result, air rises and cools; clouds and precipitate are formed. Low air pressure produces unstable weather conditions like rain or storms.
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Air Pressure Basics It increases as air density increases and lowers as air density lowers. It increases as temperatures increase and lowers as temperatures cool. It increases at lower altitudes and decreases at higher altitudes. Air moves from high pressure to low pressure.
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1 Answer. The lowest layer will always have the highest pressure.
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For this reason, density of gases decreases as distance from Earth’s surface increases. Put another way, air pressure (i.e., density) decreases as altitude increases. Temperature varies with altitude, as follows: In the troposphere, temperature decreases as altitude increases.
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Atmospheric pressure is the force exerted on objects by the weight of the air molecules above them. While air molecules are invisible, they have mass and occupy space. However, as altitude increases, atmospheric pressure decreases.
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The exosphere’s pressure is about 0.0007 atmospheres at its base to virtually nothing in the outer reaches.
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When pressure increases, density increases. When the pressure decreases, density decreases.
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For any given liquid with constant density throughout, pressure increases with increasing depth.
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Water vapor is relatively light compared to diatomic Oxygen and diatomic Nitrogen ” the dominant components in air. When vapor content increases in moist air the amount of Oxygen and Nitrogen are decreased per unit volume and the density of the mix decreases since the mass is decreasing.
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Temperature in the stratosphere rises with increasing altitude, because the ozone layer absorbs the greater part of the solar ultraviolet radiation. The ozone layer is an absorbing agent that protects life on Earth.
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Air pressure decreases with increase in altitudes. The rate of change varies because pressure decreases rapidly near Earth’s surface and more gradually at greater heights.
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The temperature gets colder as you go upward in the troposphere. Original artwork by Windows to the Universe staff (Randy Russell). The temperature gets colder as you go upward in the troposphere. Light from the Sun heats the ground.
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The global average temperature at the surface is 59 degrees F (15 degrees C) but decreases to around minus 82 degrees F (minus 63 degrees C) at the top of the troposphere. On the basis of mean tropospheric depth, the average rate of temperature decrease is 3.6 degrees F per 1,000 ft.
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As you move higher into the troposphere (say, to the top of a mountain), both air temperature and air pressure decrease. Weather happens in the troposphere. A weather map shows what the troposphere is like in different places. As you go up from the ground, the temperature decreases.
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As the density of the gases in this layer decrease with height, the air becomes thinner. Therefore, the temperature in the troposphere also decreases with height in response. As one climbs higher, the temperature drops from an average around 62°F (17°C) to -60°F (-51°C) at the tropopause.