They evaporate.
The process of water droplets condensing on a soda can on a hot summer day is exothermic. As water vapor in the air comes into contact with the cold surface of the soda can, it releases heat energy, causing the water vapor to condense into liquid water droplets.
Evaporation occurs when the liquid (dewy) appearance of the water droplets turn into a vapor and disappear.
Condensation occurs when a gas turns into a liquid as it loses heat. This process results in the formation of water droplets on a surface, such as the inside of a window on a cold day.
That is the water vapor from our breath, that condenses to water droplets. Water vapor by itself is invisible - it becomes visible when it forms droplets.
The warm water vapour in your breath condenses into water droplets when it hits the cold air.
As the day warms up, the temperature rises, causing the water droplets on the spider web to evaporate. The heat increases the water's energy, allowing it to transition from liquid to vapor more rapidly. Additionally, increased sunlight can accelerate evaporation by providing more energy to the water molecules. Consequently, the droplets disappear as they turn into water vapor and dissipate into the air.
As the moist air rises, water vapor condenses and clouds form. Clouds are made of tiny droplets of liquid water or ice.
exothermic
The process responsible for water droplets forming on the outside of a glass of lemonade on a hot summer day is condensation. When the warm, humid air comes into contact with the cold surface of the glass, the temperature of the air near the glass decreases. This cooling causes the water vapor in the air to lose energy and transition into liquid form, resulting in the formation of tiny water droplets on the glass's surface.
Condensation occurs when warm air contacts a cold surface, causing the air to cool and release moisture in the form of water droplets. An example of condensation is water droplets forming on the outside of a cold glass of water on a hot day.
The process of water droplets forming on a cold glass is similar to cloud formation in the atmosphere. In both cases, warm air containing water vapor comes into contact with a cooler surface or air mass, causing the vapor to condense and form droplets. This illustrates how clouds form when warm, moist air rises and cools at higher altitudes, leading to the condensation of water vapor into visible droplets.
Condensation is formed when water vapor in the air cools and changes into liquid water droplets, usually when it comes into contact with a cold surface. This process is responsible for the droplets you see on the external surface of a cold glass or on the inside of a window on a cold day.