Aurinkokulma

Aurinkokulma refers to the angle of the sun in the sky relative to the horizon. It is a crucial factor in determining the amount of solar radiation that reaches the Earth's surface. The aurinkokulma varies throughout the day and year due to the Earth's rotation and its orbit around the sun. At noon, the sun is generally at its highest point, resulting in the largest aurinkokulma and maximum solar intensity. Conversely, at sunrise and sunset, the sun is low on the horizon, and the aurinkokulma is small, leading to weaker solar radiation. The latitude of a location also significantly influences the aurinkokulma. Higher latitudes experience lower aurinkokulmat, especially during winter months, leading to less solar energy. This concept is fundamental in fields such as solar energy engineering, agriculture, and climate science, as it directly impacts temperature, plant growth, and the efficiency of solar power generation. Understanding and calculating the aurinkokulma is essential for optimizing the design of solar panels, predicting crop yields, and modeling climate patterns.