Hello steemians friend. How are you today? Hopefully always in good health and fun. On this occasion, I will write about how the hydrological cycle process? I hope this article can benefit every blog reader.
Understanding the hydrological cycle
Hydrologi cycle, is the never-ending cycle of water from the earth's atmosphere, and from the earth back to the atmosphere through condensation, precipitation, evaporation, and transparency.
The key to the beginning of this hydrological cycle process is the start of the sun warming up on seawater. It continues to evaporate and then falls as precipitation in various forms, such as rain, ice, snow and rain drizzling.
On its way to the earth, some can evaporate back up or fall straight down and then be intercepted by the plant before it reaches the ground.
How is the hydrological cycle movement?
In the process of hydrological cycle movement has three different ways that continue to move continuously. First, evaporation / tranpiration or movement through evaporation processes that exist in the sea, rivers, land, plants and so forth. Second, called infiltration or percolation into the soil.
In this process, water moves from behind the gaps and pores of the soil and rocks to the face of the water in the soil. And the third is called surface water which is the movement of water above the surface of the soil through the cracks and pores of the ground close to the mainstream like a lake. The deeper the soil and the fewer the pores of the soil the flow on the surface becomes larger.
Type of hydrological cycle
Based on the movement and the length of the hydrological cycle, the hydrologic cycle can be divided into three types. Namely long hydrology, short hydrology and moderate hydrology.
All three have different water processes and motions such as long hydrology, this cycle is a cycle that generally occurs in subtropical or mountainous areas. In hydrological cycle this long, the cloud is not directly converted into water, but first comes down in the form of snow and glacier-shaped.
And short hydrologic cycle is the movement of sea water exposed to the heat of the sun will experience evaporation and become water vapor. The water vapor will form condensation and form clouds. And then the crew will become rain and descend around the sea level.
And the latter is a moderate hydrologic cycle, which is a surface water event that evaporates and becomes a cloud. Medium hydrologic cycle this will happen one evaporation process because the steam is moved by the wind breeze of the land. The water drops on the surface of the land and then the water moves back toward the sea.
How does the hydrology cycle take place?
As mentioned above. This hydrological cycle does not just happen. There are several stages what you need to know about the process of the occurrence of this hydrological cycle, such as evaporation, transpiration, evapotranspiration, sublimation, condensation, advection, precipitation, larvae and infiltration.
The hydrological process occurs through the evaporation of the ocean water due to the evaporation caused by solar thermal energy. The steam moves upwards and how much at a height and forms a cloud. Some clouds settle in various forms like ice, snow, rain and others are driven to the ground by wind and become rainfall and then some evaporate back into the atmosphere.
Part of the water that reaches into the ground will enter the earth's surface and enter the various layers that exist in the soil and increase the water content. Vegetation sends some water from the earth's surface back to the atmosphere through the transport process.
After the water seeps into the soil. The layers are formed above the ground, flowing through the contours of the soil leading to the rivers and lakes and eventually flowing and joining the ocean after many years. Some amount of water is maintained as a store of depression.
And then this water cycle process continues, by blowing cold sea air. Smashed water that thickens and precipitates and becomes rainfall. Depression storage is part of the precipitation required to fill the depression zone in the soil.