The temperature in the atmosphere doesn't steadily increase or decrease as you move away from Earth's surface towards space because at the point where the atmospheric layers intersect, the temperature remains constant, just like when water changes state.
The upper layers of the atmosphere are heated from above, while the lower layers are heated from below, because infrared radiation is given off by the Earth's surface in response to solar heating. The lower troposphere (with its denser molecules and water vapor) receives heat from both re-radiation and convection. The result is that while the atmosphere always gets thinner with altitude, the temperature decreases with altitude in the troposphere, then increases with altitude in the stratosphere. The very high temperatures in the thermosphere are moot because of the low specific heat (energy capacity) of the tenuous gases there.
Global warming is an ongoing phenomenon, with temperatures steadily rising over the past few decades due to increased levels of greenhouse gases in the atmosphere. The most recent scientific data shows that global temperatures continue to increase, leading to more frequent extreme weather events and disruptions in ecosystems.
From the graph, we can infer the concentration of carbon dioxide in the atmosphere has increased steadily over the past decades. This increase is likely due to human activities such as burning fossil fuels. Additionally, we can see that the levels of methane and nitrous oxide have also increased, which are potent greenhouse gases contributing to global warming. Overall, the graph provides valuable insights into the changing composition of Earth's atmosphere and its implications for climate change.
The upper layer of the atmosphere is called the thermosphere because temperatures in this region can reach very high values, up to thousands of degrees Celsius. This is due to the absorption of solar radiation by gases in the thermosphere. Despite the high temperatures, the thermosphere would not feel hot to our skin because the air density is so low.
Carbon dioxide is abundant in Earth's atmosphere, making up about 0.04% of the gases present. Despite its relatively low concentration, it plays a crucial role in regulating Earth's temperature through the greenhouse effect. Its levels have been steadily increasing due to human activities such as burning fossil fuels.
The temperature in the atmosphere doesn't steadily increase or decrease as you move away from Earth's surface towards space because at the point where the atmospheric layers intersect, the temperature remains constant, just like when water changes state.
The temperature in the Earth's atmosphere does not increase or decrease steadily as you move from the surface towards space because it is influenced by various factors such as solar radiation, atmospheric composition, and the Earth's surface features. These factors create complex interactions that lead to temperature variations at different altitudes, resulting in the atmosphere having distinct layers with different temperature profiles.
Yes, the temperature of the atmosphere generally decreases with increasing altitude at a rate of about 6.4°C per kilometer. This is known as the lapse rate and is influenced by factors like the sun's radiation, convection, and the composition of the atmosphere.
The upper layers of the atmosphere are heated from above, while the lower layers are heated from below, because infrared radiation is given off by the Earth's surface in response to solar heating. The lower troposphere (with its denser molecules and water vapor) receives heat from both re-radiation and convection. The result is that while the atmosphere always gets thinner with altitude, the temperature decreases with altitude in the troposphere, then increases with altitude in the stratosphere. The very high temperatures in the thermosphere are moot because of the low specific heat (energy capacity) of the tenuous gases there.
The burning of fossil fuels (coal & oil) is the primary cause of the increase in carbon dioxide levels in the atmosphere.
To steadily increase the velocity of something, a consistent force must be applied in the direction of motion.
The temperature in the thermosphere rises because of the absorption of high-energy solar radiation by gases like oxygen and nitrogen in this layer of the atmosphere. The density of these gases is extremely low, so there are few particles to absorb the heat from the radiation, causing the temperature to increase significantly.
The upper layers of the atmosphere are heated from above, while the lower layers are heated from below, because infrared radiation is given off by the Earth's surface in response to solar heating. The lower troposphere (with its denser molecules and water vapor) receives heat from both re-radiation and convection. The result is that while the atmosphere always gets thinner with altitude, the temperature decreases with altitude in the troposphere, then increases with altitude in the stratosphere. The very high temperatures in the thermosphere are moot because of the low specific heat (energy capacity) of the tenuous gases there.
From the surface of the sun to its center, temperatures can be assumed to increase. The surface temperature of the sun is around 5500 degrees Celsius, while the core temperature is estimated to be around 15 million degrees Celsius.
The steady decrease in temperature with altitude in the troposphere is called the environmental lapse rate. This is due to the decreasing pressure and density of the air as altitude increases.
When the liquid is boiling steadily and the temperature has stabilised.
The average temperature of Jupiter's atmosphere is about -121°C (152.15 K), with its lowest temperature at -165°C (110.15 K). The temperature and pressure inside Jupiter increase steadily toward the core. At the phase transition region where hydrogen-heated beyond its critical point-becomes metallic, it is believed the temperature is 10,000 K and the pressure is 200 GPa. The temperature at the core boundary is estimated to be 36,000 K and the interior pressure is roughly 3,000-4,500 GPa. (for comparison the surface of the Sun is about 6600 K).