Water Vapour
Water vapour is one of the essential components of the atmosphere, contributing between 1% to 4% by volume depending on the geographic and climatic conditions. In warm and humid regions, such as the tropics, water vapour can make up to 4% of the atmosphere, while in cold and arid regions, it may decline to less than 1%.
The amount of water vapour in the atmosphere also diminishes from the equator towards the poles due to varying temperatures. Being a gaseous form of water, it plays a crucial role in absorbing solar insolation and retaining the Earth's thermal radiation, functioning as a thermal blanket that helps regulate the planet's temperature.
Moreover, water vapour affects both air stability and instability within the atmosphere, influencing weather patterns and precipitation. Understanding the properties and behavior of water vapour is vital for comprehending broader climate dynamics, including the greenhouse effect and global warming.