No, it is much colder near the tropopause.
For the most part, yes. (There are exceptions, of course.)
The atmosphere tries to balance the unequal heating of Earth's surface through convection, where warmer air rises and cooler air sinks to distribute heat more evenly. Additionally, winds help transport heat from warmer regions to cooler regions, and cloud cover can reflect sunlight back into space to regulate temperature.
The atmosphere balances the unequal heating of Earth's surface by moving air through convection currents. These currents transfer heat from warmer regions to cooler regions, helping to regulate temperature gradients and create more stable climate conditions.
The tropopause prevents cool air in the troposphere from mixing with the warmer air in the stratosphere above it. This layer acts as a barrier separating the two regions and helps maintain the stability of the atmosphere.
The atmosphere helps to balance the unequal heating of Earth's surface by redistributing heat through convection and wind patterns. This process involves transferring heat from warmer areas to cooler areas, helping to regulate temperature across the globe. The atmosphere also absorbs and reemits solar radiation, which further contributes to stabilizing Earth's temperature.
the earth temperature become cool in warm temperature
it is way warmer there than on earth! earths average temperature is 14C mercurys average temperature is 66C
For the most part, yes. (There are exceptions, of course.)
water changes from a liquid to a solid when you drop it below 32 F or 0 C. It also evaporates, changing into a gas in warmer weather.
water changes from a liquid to a solid when you drop it below 32 F or 0 C. It also evaporates, changing into a gas in warmer weather.
Earth's surface is free to radiate heat into space. The interior is not. The interior does transfer heat the the surface, but rather slowly. It is hot due to residual heat from Earth's formation and from the heat generated by the decay of radioactive elements.
The atmosphere tries to balance the unequal heating of Earth's surface through convection, where warmer air rises and cooler air sinks to distribute heat more evenly. Additionally, winds help transport heat from warmer regions to cooler regions, and cloud cover can reflect sunlight back into space to regulate temperature.
The temperature usually becomes a lot warmer during a tropical storm as water vapor is transported into the troposphere. In tropical oceans, the sea surface temperature (SST) becomes warmer as the water changes rapidly in a layer of the ocean called the thermocline.
This depends on what you are measuring the temperature of. Clouds tend to reduce the amount of radiation from the sun that reaches the Earths surface, thus feeling cooler to us when we are outside.
The atmosphere balances the unequal heating of Earth's surface by moving air through convection currents. These currents transfer heat from warmer regions to cooler regions, helping to regulate temperature gradients and create more stable climate conditions.
The tropopause prevents cool air in the troposphere from mixing with the warmer air in the stratosphere above it. This layer acts as a barrier separating the two regions and helps maintain the stability of the atmosphere.
No, the tropopause is actually highest near the equator and lowest near the poles. This is because the tropopause is defined as the boundary between the troposphere and the stratosphere, and the troposphere is thicker at the equator due to the Earth's rotation and warmer temperatures.