Does The Water Cycle Create Rain

The water cycle in the deciduous forest occurs mostly in the stage of transpiration. Although there are bodies of water in the deciduous forest, water also evaporates from the leaves of the plants and into the atmosphere. The water vapor will condense into tiny droplets which form clouds; the clouds will then return the water back to the ground in the form of precipitation. The water falls to the floor of the deciduous forest and travels into the roots of the plants. The cycle will then start over again.

Clouds to form in the atmosphere have to have water vapor present. This water vapor makes up a cloud. The water vapor in the atmosphere comes from evaporation or deposition. Also the temperature of the air is below the dew point. When the water is fully saturated, it starts to rise and the expansional cooling process begins. During the process of condensation, the aerosol particles act like a nuclei in the atmosphere, which began to grow, creating ice crystals that are big enough to produce a cloud.

Evaporation happens every day, everywhere on Earth. It is the process of water turning into water vapor. It then travels to the clouds and condenses. This is condensation, where water vapor turns into clouds. When the clouds get too heavy, they then drop all the water in them. This stage is precipitation, or rain, snow, sleet, or hail. It then runs off into a stream, lake, creek, or ocean, the cycle then repeats. This cycle is called the water cycle.

Below freezing air is used to make snow and snowflakes. Moisture from lakes and oceans to form clouds.warm, rising air to form precipitation.

because the dew point is below freezing and the moisture goes from a gas to a

Growing up, we all went through the water cycle lesson and we will never forget it. The reason being, we encounter the water cycle throughout our entire life and it will always effect our systems and more importantly our water system. As illustrated in the picture, our water cycle includes the processes of evaporation, condensation, precipitation, which then goes to many places. During evaporation, the sun is used as a main power to make this happen. The sun’s rays beat down onto the ground creating all of the moisture and water to fizzle into a gas state into the atmosphere and get stored away into the clouds. When it is stored into the clouds it is condensing. Condensation means that the gas is again forming itself back into its liquid state to get ready to return to Earth. The condensation then forms into precipitation. Precipitation comes in many different forms. You can see it as rain, snow, sleet, or hail making its way back to us. What happens to it then depends on the area. The water might end up as runoff, or become

It is best described as water evaporating into the atmosphere and continues to condense into the clouds. It will than fall back to earth as precipitation. This precipitation soaks down into the soil as a process called infiltration, where it joins the groundwater, or it will run off over the landscape to join surface water. The surface water may evaporate out of the lake and back into the atmosphere or the water will move through the soil towards the groundwater and be taken up by plants that will put it back into the atmosphere. This process will just keep continuing and continuing over and

The water cycle represents how water is exchanged and cycled through Earth’s land, oceans, and atmosphere (2010 pg.1). Evaporation, condensation, and precipitation are all three main factors within the water cycle. Evaporation occurs when a liquids surface changes to gas. For example, when water from rivers, oceans or lakes evaporate, it becomes water vapor. Condensation occurs when gas changes to a liquid. For example, clouds form when water vapor condescends. Precipitation is described as any liquid or solid water that falls to earth from above. A great and simple example would be rain, snow or hail (2010 pg.1). Within the water cycle, there are three states of water: solid, liquid and gas. Most of Earth’s freshwater is

So the warm moist air creates clouds of rain and thunderstorm. Adding to that winds with different speed going in different directions assisting in expanding these great clouds of rain and thunderstorm. With

Cloud seeding is when a cloud gets seeded with chemicals to produce more rain. For a cloud to produce rain the temperature in the cloud needs to be below the freezing point of water. When reached below the freezing point the cooled water has meet specks of dust,

When the air parcel rises in the troposphere, the more energy transfer. The reason why the energy transfers is because the water vapor must have an equivalent temp to the surrounding air. More energy causes it to have more evaporation transferring more water vapor to the surrounding air. As the energy transfer occurs, the water vapor gets through condensation and turns to liquid water. The higher the parcel gets, the colder it is in the surrounding air which causes the water to condense and come out as rain. This is important because when the temperature of the air parcel is higher, it will rise higher in the troposphere and the higher the cloud is in the troposphere, the more rain that will fall. Also, the modeling tool tells us that storms 2 and 3 had all the same factors ( water vapor, troposphere temperature and surface water) but, the parcel temperature, was higher in storm 3 which caused it to have more rain. Lastly, the reason why the weather has been acting up is the new lake. The lake is causing more evaporation (the process by which a liquid changes into a gas). This is important because the more evaporation there is, the more condensation (the process by which a gas changes into a

It all begins with what meteorologists call a “tropical disturbance”, or a group of thunderstorms over warm tropical waters. As low-level winds flow into the disturbance, they evaporate water from the ocean surface. This process transfers energy from the ocean into the atmosphere. When the winds arrive at the disturbance, they rise up and release that energy into the air as they form clouds and precipitation. This warms the air and makes it

As the warmer air rises it gets further away from the earth and in to thinner atmosphere where it is colder. When the air reaches these high altitudes the molecules lose energy (heat) and slow down slowly coming back towards one another joining together as water molecules, becoming heavier and they begin to sink back towards the Earth most commonly known as rain. If you have been inside a two story house and gone upstairs you probably have noticed that the upstairs is much hotter than the downstairs, this is caused by convection. The cooled air, usually by an air conditioner, releases air molecules with less energy and it diffuses throughout the house and any warm air is pushed upwards but is usually trapped by the roof of the house.

HYDROLOGIC CYCLE The hydrologic cycle is a constant movement of water above, on, and below the earth's surface. It is a cycle that replenishes ground water supplies. It begins as water vaporizes into the atmosphere from vegetation, soil, lakes, rivers, snowfields and oceans-a process called evapotranspiration. As the water vapor rises it condenses to form clouds that return water to the land through precipitation: rain, snow, or hail. Precipitation falls on the earth and either percolates into the soil or flows across the ground. Usually it does both. When precipitation percolates into the soil it is called infiltration when it flows across the ground it is called surface run off. The amount of precipitation that infiltrates, versus the

A type of precipitation is rainfall and it develops when water vapor condenses into droplets in the atmosphere thus becoming too heavy to stay suspended in the air so gravity causes them to fall. The pattern or occurrence of rainfall in the United States or basically anywhere in the world depends on several factors such as ground elevation, wind directions, location within a continental mass, areas of low pressure, cool fronts, jet streams and even mountain ranges. For instance mountains have an influence on wind and wind is an important feature in rainfall, “The windward sides of mountainous islands in the trade wind regime are among the rainiest places on earth, where rains exceed