Exempel på the troposphere

• Above the troposphere is the stratosphere which is much more stably stratified.

• The lower atmosphere (the troposphere) thus experiences a positive lapse rate (negative temperature change with height).

• This assumption requires the aspect ratio to be small, troposphere and 10-3 in the stratosphere.

• For example, the passing of air over mountains and hills can cause the formation and breaking of internal waves in the troposphere and stratosphere.

• While tritium remains in the troposphere, many reemissions are possible, but in this work only the first reemission after the release is considered.

• Experience has shown that this method should be used with caution as it treats the troposphere in two smoothed layers, over its entire depth.

• First, the eruption must be explosive enough to inject eruption products into the stratosphere, the par t of the atmosphere above the troposphere.

• Higher levels of pollutants in the lower troposphere may stimulate seed germination when other external conditions are inappropriate for seedling growth.

• A change in the current density and in the initial values of electrical power delivered to the simulated troposphere resulted in differences in the type and amount of compounds formed.

• These rising air currents diverge in the upper troposphere and move away from the equator at high altitude in both northerly and southerly directions.

• The retreat and thinning is attributed to a decrease in precipitations and a warming of the upper troposphere over the last decades.

• The fragments were displaced in the lower atmosphere (troposphere) from their expected trajectories by strong wind.

• Surface anticyclones form due to downward motion through the troposphere, the atmospheric layer where weather occurs.

• Strengthening storm systems within the troposphere can act to intensify the polar vortex by significantly cooling the poles.

• These changes aloft force changes below in the troposphere.