Hydrological cycle
Hydrological cycle
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Name: I Gusti Agung Ursja Anna DewiNo: 34Class: XI PB
Explanation:Hydrological cycle is the circulation of water that never cease from the earth's atmosphere and back into the atmosphere through condensation, precipitation, evaporation, and transpiration. Warm ocean water by sunlight is the key process of the hydrological cycle can be run continuously (continuous). Berevaporasi water, and then falls as precipitation in the form of rain, snow, hail, sleet and snow (sleet), drizzle or fog. On the way to the earth some precipitation may berevaporasi back up or straight down and then intercepted by the plant before it reaches the ground. After reaching land, the hydrologic cycle continues to move continuously (continuous), in three different ways:1.Evaporasi / TranspirationWater in the sea, on land, in rivers, in plants, and so forth. Then it will evaporate into the air (atmosphere) and then going into the clouds. In the state of saturated water vapor (clouds) it will be water spots and it will be down (precipitation) in the form of rain, snow, ice.2. Infiltration / Percolation into the groundWater moves into the soil through cracks and pores of the soil and rocks into the groundwater. Water can move due to capillary action or water can move vertically or horizontally below the soil surface until the water is re-entering the surface water system.3. Surface waterAir moving over the surface of the ground close to the main stream or lake, the gently sloping land and fewer peri-porous soil, the surface currents of the greater. Surface flow can be seen usually in urban areas. The rivers join each other and form a major river that carries the entire surface of the water around the watershed to the sea. And some subsurface water will accumulate and form a river flowing into the sea and ends. The process of water traveling in the mainland took place in the hydrological cycle components that make up the watershed system (DAS). The amount of water on earth as a whole is a relatively permanent change form and place. Greatest place in the sea.
Various kinds of Hydrological Cycle Process and Phasesa. Short cycles / minor cycleA. Sea water evaporates into vapor gas in the sun2. Condensation and cloud formation occur3. Rain on ocean surfaceb. Cycle isA. Sea water evaporates into vapor gas in the sun2. Condensation occurs3. Moved by the wind blowing steam into the ground4. Cloud formation5. Rain fell on the ground surface6. River water flowing into the sea againc. Cycle Length / Great CycleA. Sea water evaporates into vapor gas in the sun2. Sublimation of water vapor has3. Formation of clouds containing ice crystals4. Clouds moving by the wind to land5. Cloud formation6. Snow7. Formation of glaciers8. Melting glaciers formed the river9. Water flows in the river to the ground and then into the sea.
Explanation:Hydrological cycle is the circulation of water that never cease from the earth's atmosphere and back into the atmosphere through condensation, precipitation, evaporation, and transpiration. Warm ocean water by sunlight is the key process of the hydrological cycle can be run continuously (continuous). Berevaporasi water, and then falls as precipitation in the form of rain, snow, hail, sleet and snow (sleet), drizzle or fog. On the way to the earth some precipitation may berevaporasi back up or straight down and then intercepted by the plant before it reaches the ground. After reaching land, the hydrologic cycle continues to move continuously (continuous), in three different ways:1.Evaporasi / TranspirationWater in the sea, on land, in rivers, in plants, and so forth. Then it will evaporate into the air (atmosphere) and then going into the clouds. In the state of saturated water vapor (clouds) it will be water spots and it will be down (precipitation) in the form of rain, snow, ice.2. Infiltration / Percolation into the groundWater moves into the soil through cracks and pores of the soil and rocks into the groundwater. Water can move due to capillary action or water can move vertically or horizontally below the soil surface until the water is re-entering the surface water system.3. Surface waterAir moving over the surface of the ground close to the main stream or lake, the gently sloping land and fewer peri-porous soil, the surface currents of the greater. Surface flow can be seen usually in urban areas. The rivers join each other and form a major river that carries the entire surface of the water around the watershed to the sea. And some subsurface water will accumulate and form a river flowing into the sea and ends. The process of water traveling in the mainland took place in the hydrological cycle components that make up the watershed system (DAS). The amount of water on earth as a whole is a relatively permanent change form and place. Greatest place in the sea.
Various kinds of Hydrological Cycle Process and Phasesa. Short cycles / minor cycleA. Sea water evaporates into vapor gas in the sun2. Condensation and cloud formation occur3. Rain on ocean surfaceb. Cycle isA. Sea water evaporates into vapor gas in the sun2. Condensation occurs3. Moved by the wind blowing steam into the ground4. Cloud formation5. Rain fell on the ground surface6. River water flowing into the sea againc. Cycle Length / Great CycleA. Sea water evaporates into vapor gas in the sun2. Sublimation of water vapor has3. Formation of clouds containing ice crystals4. Clouds moving by the wind to land5. Cloud formation6. Snow7. Formation of glaciers8. Melting glaciers formed the river9. Water flows in the river to the ground and then into the sea.
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