sztratoszférájában

The term "sztratoszférájában" is the Hungarian genitive case of "stratoszféra," which translates to "stratosphere" in English. Therefore, "sztratoszférájában" literally means "in the stratosphere." This refers to a specific layer of Earth's atmosphere.

The stratosphere is the second major layer of Earth's atmosphere, above the troposphere and below the mesosphere. It extends from the top of the troposphere at an average altitude of about 10 to 15 kilometers (6 to 9 miles) up to about 50 kilometers (31 miles) above the Earth's surface. A significant feature of the stratosphere is its temperature profile. Unlike the troposphere, where temperature decreases with altitude, the temperature in the stratosphere increases with altitude. This phenomenon is primarily due to the absorption of ultraviolet (UV) radiation from the Sun by ozone molecules, which are concentrated in a region known as the ozone layer within the stratosphere.

The stratosphere is characterized by stable, dry air with very little vertical mixing. This stability is a consequence of the temperature inversion, where warmer air is above cooler air. Because of this lack of turbulence, commercial airplanes often fly in the lower stratosphere to avoid the weather disturbances that occur in the troposphere. The ozone layer within the stratosphere plays a crucial role in protecting life on Earth by absorbing most of the Sun's harmful UV radiation. The conditions "sztratoszférájában" are thus relatively calm and characterized by ozone activity.