STRATOSPHERE

The stratosphere is the gaseous layer in the earth that is present above the stratosphere. In this space, air flight can be suitable for flying, and especially, it is reliable for jet planes without reducing sounds while flying. This place has no clouds and water vapor. The study is going to focus on the role of the stratosphere as well as the effects of the absence of water vapour in the stratosphere. In the layer of the stratosphere, the element of temperature enhances with height and this surface consists of the layer of ozone, the chemical symbol of Ozone is O3. Vultures, cranes, and swans can fly effectively in the layer of the stratosphere.  

Role of stratosphere

The stratosphere is the second layer in the earth’s atmosphere. This layer has been situated above the troposphere layer and below the mesosphere layer. The height of the stratosphere is almost 10 KM from the surface of the earth. Besides, the stratosphere extends 6.2 miles above the troposphere layer and almost 40 km has been extended this layer from the troposphere. It can be stated against what accounts for the absence of water vapor in the stratosphere that it develops surface temperatures. In this layer, huge amounts of ozone molecules have been presented that are the main cause to heat the comparative layer in the earth. The main advantage of this layer is to absorb all the energy of the ultraviolet rays which are coming from the sun.

It can be defined against the stratosphere, specifically, the lower stratosphere passage seems to dry out. Water vapor can be defined as a greenhouse gas. In the layer of the stratosphere, warm air provides effective stability. The major layers of the atmosphere of the earth are the exosphere, thermosphere, mesosphere, stratosphere, as well as troposphere.  The stratosphere, specifically the lower stratosphere passage seems to be drying out effectively in terms of being lower stratosphere. The layer of the stratosphere plays a critical role in protecting the people of earth from ultraviolet radiation as the ozone layer effectively absorbs the UV radiation from the sun. 

The stratosphere effectively absorbs biologically harmful UV radiation.  There are multiple elements of the stratosphere in this surface of the atmosphere for instance bromine atom, wavelength, troposphere, mesosphere, chlorine, chlorofluorocarbon, ozone, as well as nitric oxide. There are multiple characteristics of this layer as there is no availability of clouds, and weather changes in this layer due to which there is an effective significance of safe travel. In the layer of the stratosphere, temperature effectively begins to enhance. Ozone can be defined as a form of oxygen. 

Effects of the absence of water vapor in the stratosphere

The layer saves the effect of ultraviolet rays from the living things on the planet. In the stratosphere layer, the temperature rate is increasing rapidly while transferring upward in the stratosphere layer. At the bottom of the stratosphere, the temperature is comparatively low. The maximum cold temperature is -60 degrees. It can be stated against what accounts for the absence of water vapor in the stratosphere that it leads to effective additional working. 

Water vapor plays a critical role and it is one of the most significant gases of greenhouse gasses in the atmosphere. Since the layer of the stratosphere is an effective dry layer that holds little water vapor. The rise of global warming can happen because of the absence of water vapor in the stratosphere. Water vapor can be described as a common atmospheric constituent and there is an effective presence of water vapor in the solar atmosphere as well as astronomical objects. The additional warming increases as stratospheric water vapor are an effective greenhouse gas due to which people can face different challenges.  

The increasing rate of water vapor in the surfaces of the atmosphere develops warming as well as effectively enhances the effect of the greenhouse. Water vapor is also well known as a crucial part of the process of global warming. Being a dry layer and holding little water vapor, few clouds occur in this layer. The clouds of polar stratospheric are the exception. The element of water vapor in the surface of the stratosphere comes from the layer of the troposphere through water vapor transport as well as from methane and hydrogen that demote to make water. Hydrogen and water methane are transported to the layer of the stratosphere by upwelling in the regions of tropical. Lack of water cycles can affect the climates as well as the functions of living things on the earth. 

Conclusion 

Based on the above discussion it can be concluded that the layer of the stratosphere is a composition of the layers of stratified temperature with cold layers as well as warm layers. The study has discussed the role of the stratosphere and the effects of the absence of water vapor in the stratosphere. Moreover, it can be stated that there is an effective sign of this layer in terms of protecting people on the earth from the radiation of ultraviolet rays. The absence of water vapor can assist in the rising global warming. Therefore, the concept of the stratosphere and all its aspects are demonstrated in this study.