its because of the ozone layer turning the suns rays into longwaves and sending them back into space
Much of the sun's radiation is reflected back into space by Earth's atmosphere and surface through a process known as albedo. The albedo effect varies depending on the surface type; for example, ice and snow have high albedo, reflecting most sunlight, while forests and oceans absorb more radiation. This reflection helps regulate Earth's temperature and climate. However, changes in land use and climate can alter albedo, impacting global warming and weather patterns.
No, the Earth does not intercept most of the Sun's radiation. In fact, only about 1/2,000,000th of the Sun's total energy output reaches the Earth, as much of it disperses in space. Approximately 70% of the incoming solar radiation is absorbed by the Earth's atmosphere, oceans, and land, while the rest is reflected back into space. This balance is crucial for maintaining the planet's climate and supporting life.
Yes. Indeed one proposed solution for the global warming suffered by our planet is to increase the amount of energy reflected back into space by increasing our own oceans ability to reflect it.
Some of the sun's energy reflects back into space because of the Earth's atmosphere and surface. When sunlight hits the Earth, some of it is absorbed by clouds, atmospheric gases, ice, snow, and the Earth's surface, and then reflected back into space. This phenomenon is known as albedo.
When Earth has an albedo of about 30 percent, it means that approximately 30 percent of the incoming solar radiation is reflected back into space rather than being absorbed. This reflective property helps regulate the planet's temperature and climate. A higher albedo can contribute to cooler global temperatures, while a lower albedo could lead to warming, as more energy is absorbed. Factors influencing albedo include cloud cover, ice and snow cover, and land use changes.
About 30% of the sun's radiation is reflected back into space by the Earth's surface, clouds, and atmosphere. This reflection is known as albedo and helps regulate the Earth's temperature.
It goes back into space.
Yes, about 30% of it goes back.
5%
About 50% of the sun's radiation that reaches Earth's atmosphere is absorbed by the Earth's surface. The remaining energy is either reflected back to space or absorbed by the atmosphere.
Approximately 30% of the Sun's energy that reaches Earth is reflected back into space by clouds, atmospheric particles, and Earth's surface. This reflected energy is known as the albedo effect. The remaining energy is absorbed by the Earth, warming the planet and driving various processes, such as weather and climate. Ultimately, a portion of the absorbed energy is reradiated back into space as infrared radiation.
Such reflection is called the albedo. For the earth it is 30 - 35%
Roughly 70% of the sun's radiation is absorbed by the Earth's surface, while the remaining 30% is reflected back into space. This absorbed energy plays a crucial role in driving Earth's climate and weather patterns.
why
Much of the sun's radiation is reflected back into space by Earth's atmosphere and surface through a process known as albedo. The albedo effect varies depending on the surface type; for example, ice and snow have high albedo, reflecting most sunlight, while forests and oceans absorb more radiation. This reflection helps regulate Earth's temperature and climate. However, changes in land use and climate can alter albedo, impacting global warming and weather patterns.
Radiation.
No, the Earth does not intercept most of the Sun's radiation. In fact, only about 1/2,000,000th of the Sun's total energy output reaches the Earth, as much of it disperses in space. Approximately 70% of the incoming solar radiation is absorbed by the Earth's atmosphere, oceans, and land, while the rest is reflected back into space. This balance is crucial for maintaining the planet's climate and supporting life.