how does temperature vary with altitude in earth's atmosphere
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Atmospheric temperature In the Earth's atmosphere, temperature varies greatly at different heights relative to the Earth 's surface. The coldest temperatures lie near the mesopause, an area approximately 85 km (53 mi) to 100 km (62 mi) above the surface.n the Earth's atmosphere, temperature varies greatly at different heights relative to the Earth 's surface. The coldest temperatures lie near the mesopause, an area approximately 85 km (53 mi) to 100 km (62 mi) above the surface.
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Layers of Earth's Atmosphere The atmosphere is divided into regions defined primarily by temperature. The height and temperature of these layers can vary from season to season. From the Earths surface through the bottom layer of atmosphere, called the troposphere, temperature decreases with altitude. Weather occurs in this layer.
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Atmosphere of Earth In general, air pressure and density decrease with altitude in the atmosphere. 1  However, temperature has a more complicated profile with altitude, and may remain relatively constant or even increase with altitude in some regions (see the temperature section, below).
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- The change of temperature with height is known as the lapse rate. The standard lapse rate for the troposphere is a decrease of about 6.5 degrees Celsius (C) per kilometer (km) (or about 12 degrees F). Near the surface, the lapse rate changes dramatically from hour to hour on clear days and nights. Sometimes the temperature does not decrease with height, but increases.
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- Making the world better, one answer at a time. Temperature and altitude are inversely proportional in the troposphere. This means that as one increases, the other decreases. Approximately 165 meters up in the troposphere is equivalent to a 1 degree Celsius drop.he relationship between atmospheric pressure and altitude is the higher you go, the lesser the atmospheric pressure becomes. if the air above you is less, then there is less … weight being pressed upon the air you are on. anonymous boy from small heath school y8 2011.
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Layers of Earth's Atmosphere The atmosphere is divided into regions defined primarily by temperature. The height and temperature of these layers can vary from season to season. From the Earth s surface through the bottom layer of atmosphere, called the troposphere, temperature decreases with altitude. Weather occurs in this layer. It s also the layer we live in. The next layer up is called the stratosphere. In the stratosphere, temperature increases with altitude. This is because of ozone. When the ozone in this layer absorbs UV light from the sun, it increases in temperature. In the mesosphere, ozone concentration decreases.
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- V. Temperature Structure of the Atmosphere: The atmosphere is largely warmed from below. The farther away the air is from the Earth’s surface, the cooler the air will be. The decrease in measured air temperature with increasing altitude is called the lapse rate. This rate measures the drop in temperature in degrees celcius per 1000m.
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Why does the temperature of the atmosphere vary? Most people know that it is colder on top of a mountain compared to the ground, but few actually know why. And even less know that the atmosphere actually warms up again! The true temperature profile of the atmosphere is shown in the image. The air at the surface up to around 10 kilometers is called the troposphere.ost people know that it is colder on top of a mountain compared to the ground, but few actually know why. And even less know that the atmosphere actually warms up again! The true temperature profile of the atmosphere is shown in the image. The air at the surface up to around 10 kilometers is called the troposphere.
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Atmospheric temperature Comparison of the 1962 US Standard Atmosphere graph of geometric altitude against air density, pressure, the speed of sound and temperature with approximate altitudes of various objects. Atmospheric temperature is a measure of temperature at different levels of the Earth's atmosphere.It is governed by many factors, including incoming solar radiation, humidity and altitude.omparison of the 1962 US Standard Atmosphere graph of geometric altitude against air density, pressure, the speed of sound and temperature with approximate altitudes of various objects. Atmospheric temperature is a measure of temperature at different levels of the Earth's atmosphere.
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Geography- Factors affecting temperature • Altitude is the height of a point above the sea level. • Temperature decreases by 6.5 deg C for every increase in 1,000m increase in altitude • The air at high altitudes is thin. At higher altitudes, the air is made up of a smaller concentration of gas, dust and water vapour than the dense air at sea level.
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How does the temperature change within the stratosphere? Making the world better, one answer at a time. The temperature changes within the stratosphere with increasing distance from the earth. The temperature increases with altitude, reaching a maximum of about 2 degrees Celsius This is unlike the troposphere, where the temperature decreases with increasing altitude.n the stratosphere, the temperature increas … es with height due to absorption of radiation by ozone. Temperature changes when altitude is in the stratosphere because of  one things. It already rises when you climb up in the stratosphere.
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Vertical Structure of the Atmosphere The rate of change of air temperature with height is called the lapse rate. In the troposphere, the lapse rate is generally about 6.5 deg C per kilometer increase in altitude. The temperature can increase with height in the lower troposphere. When this happens, it is called an inversion. If the temperature remains the same with height, it is called isothermal. The actual lapse rate varies with location, time of day, weather conditions, season, etc.
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TEMPERATURE â There are definite variations in temperature with altitude and with latitude. Naturally, the mountains and the elevated valleys have the cooler climates, with the lower areas of the State having the higher temperatures. There is about a 3 Â° F decrease in mean annual temperature for each 1,000-foot increase in altitude, and approximately 1.5 to 2 Â° F decrease in average yearly temperature for each one degree increase in latitude. Thus, weather stations in the southern counties generally have average annual temperatures 6 to 8 degrees higher than those at similar altitudes over the northern counties. Also, the mountain ranges over the western United States, particularly the Sierra Nevada and Cascade Ranges and the Rocky Mountains, have a marked influence on the climate of the State. Pacific storms, before reaching Utah, must first cross the Sierras or Cascades.
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Layers of Earth's Atmosphere The temperature decreases with altitude. Stratosphere: The stratosphere is found from about 7 to 30 miles (11-48 kilometers) above the Earth’s surface. In this region of the atmosphere is the ozone layer, which absorbs most of the harmful ultraviolet radiation from the Sun. The temperature increases slightly with altitude in the stratosphere. The highest temperature in this region is about 32 degrees Fahrenheit or 0 degrees Celsius.
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- In the stratosphere, the temperature increases with increasing altitude as the amount of ozone-absorbing ultraviolet rays increases. In the mesosphere, temperatures decrease as altitude increases and can reach -194 degrees Fahrenheit. By contrast, temperatures in the thermosphere can reach over 2,700 degrees Fahrenheit. Learn more about Atmosphere
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- The temperature decreases with altitude. Stratosphere: The stratosphere is found from about 7 to 30 miles (11-48 kilometers) above the Earths surface. In this region of the atmosphere is the ozone layer, which absorbs most of the harmful ultraviolet radiation from the Sun.The temperature increases slightly with altitude in the stratosphere. The highest temperature in this region is about 32 degrees Fahrenheit or 0 degrees Celsius.n this region of the atmosphere is the ozone layer, which absorbs most of the harmful ultraviolet radiation from the Sun. The temperature increases slightly with altitude in the stratosphere. The highest temperature in this region is about 32 degrees Fahrenheit or 0 degrees Celsius.
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- Air pressure change in each layer of the earth as altitude  increases due to variation in the density of air. At high altitude,  air pressure is low due to less density of a…ir up there..while at  sea level..air pressure is at utmost of it due to increase in the  density of air.
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Week 1: Intro to Atmosphere troposphere(temperature decreases with an increase in altitude), stratosphere(temperatures remain constant to a height of about 12 miles, temperatures increase in the stratosphere because it is in this layer that the atmosphere's ozone is concentrate), mesosphere (temperatures decrease with height.
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- The decrease of an atmospheric variable with height, the variable being temperature unless otherwise specified. In the lower regions of the atmosphere (up to altitudes of approximately 12,000 metres (39,000 ft), temperature decreases with altitude at a fairly uniform rate.lthough the actual atmospheric lapse rate varies, under normal atmospheric conditions the average atmospheric lapse rate results in a temperature decrease of 6.4 °C/km (3.5 °F or 1.95 °C/1,000 ft) of altitude above ground level. The measurable lapse rate is affected by the moisture content of the air (humidity).
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- • The environmental lapse rate (ELR) is the rate of change of temperature with height between. two altitudes in a layer of atmosphere. • ELR is assumed to be constant between those two points. • To calculate the ELR, one needs two temperatures at two different altitudes (heights).
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How Pressure Changes with Altitude in Earth's Atmosphere Air gets 'thinner' with increasing altitude. That's why mountain climbers sometimes need bottled oxygen to breathe, and why it is so easy to get 'winded' while hiking in high mountains or even visiting someplace at elevation. Atmospheric pressure is around 1,014 millibars (14.7 pounds/inch 2) at sea level. At an elevation of 10 km (6 miles or about 30,000 feet), roughly the height of Mt. Everest, pressure drops to 265 millibars. That's less than 30% of the pressure at sea level! Both atmospheric pressure and the density of air decrease with altitude.
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High School Earth Science/Atmospheric Layers A change in temperature with distance is called a temperature gradient. The atmosphere is divided into layers based on how the temperature in that layer changes with altitude, the layer's temperature gradient (Figure 15.4). The temperature gradient of each layer is different.n some layers, temperature increases with altitude and in others it decreases. The temperature gradient in each layer is determined by the heat source of the layer. The different temperature gradients in each of the four main layers create the thermal structure of the atmosphere.
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Why does the temperature of different layers of the atmosphere vary? It is a somewhat misleading question because the composition of the gases in each layer of the atmosphere doesn't change as per say. Our atmosphere is made of about 80 percent nitrogen, 20 percent oxygen and various so-called rare gases in minute quantities.But as pressure and solar radiation changes with altitude, it reacts differently and e.g. radiation is responsible for the ozone found in the stratosphere. need help its between these shoices: A) because air temperature increases as altitude increases. B) because the amount of energy radiated from the sun varies. C) because of interference by humans. D) because of the composition of gases in each layer. please help! thanks. Add your answer. Source.
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Why do the different layers of the atmosphere have different temperature? (3) In the mesosphere, the air is relatively mixed together, so the temperature decreases with altitude. The atmosphere reaches its coldest temperature of around -90°C in the mesosphere. This is also the layer in which a lot of meteors burn up while entering the Earth's atmosphere.(4) The thermosphere is the fourth layer of the Earth's atmosphere.The air is really thin in the thermosphere.A small change in energy can cause a large change in temperature. That's why the temperature is very sensitive to solar activity.4) The thermosphere is the fourth layer of the Earth's atmosphere. The air is really thin in the thermosphere. A small change in energy can cause a large change in temperature. That's why the temperature is very sensitive to solar activity.
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Why do the different layers of the atmosphere have different temperature? (1) The troposphere is the lowest layer of the Earth's atmosphere. The air is very well mixed and the temperature decreases with altitude. Air in the troposphere is heated from the ground up. The surface of the Earth absorbs energy and heats up faster than the air does.4) The thermosphere is the fourth layer of the Earth's atmosphere. The air is really thin in the thermosphere. A small change in energy can cause a large change in temperature. That's why the temperature is very sensitive to solar activity.
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Atmospheric temperature The instruments record microwave energy emitted from oxygen molecules in the atmosphere. In the Earth's atmosphere, temperature varies greatly at different heights relative to the Earth's surface. The coldest temperatures lie near the mesopause, an area approximately 85 km (53 mi) to 100 km (62 mi) above the surface.