It doesn't. In fact, due to it's elliptical orbit, Earth is closer to the sun in the northern hemisphere's winter than the northern hemisphere's summer.
The sun is higher in the sky in summer because of the tilt of the Earth's axis. During the summer solstice, the hemisphere tilted towards the sun receives more direct sunlight, causing the sun to appear higher in the sky and create longer days.
Our shadow starts to fad when the sun lowers in the sky because there is no light for our shadow to appear. (Also, as the sun gets lower, shadows get longer.)
The sun reaches its farthest north point in the sky during the summer solstice, which occurs around June 21st in the northern hemisphere. This is when the North Pole is tilted closest to the sun, causing the sun to appear at its highest point in the sky.
The sun is higher in the sky at noon in the summer due to the tilt of the Earth's axis. During summer in the Northern Hemisphere, the North Pole is tilted toward the sun, resulting in longer days and a higher sun angle. This angle causes the sun to reach its peak point in the sky at noon during the summer months.
The sun is highest in the sky during summer due to the tilt of the Earth's axis. This causes the sun's rays to be more direct, leading to longer daylight hours and warmer temperatures. In winter, the sun is lower in the sky, resulting in shorter days and cooler temperatures.
The Earth's axis tilt is responsible.
In the Southern Hemisphere, the sun appears lower in the sky in December due to the summer solstice occurring during that month, resulting in longer days and higher temperatures. In June, during the winter solstice, the sun is higher in the sky and the days are shorter and cooler.
The sun reaches its highest elevation at the moment that summer begins.
The sun's apparent height in the sky varies throughout the year due to the tilt of the Earth's axis. In June, the Northern Hemisphere is tilted towards the sun, causing it to appear higher in the sky. In December, the Northern Hemisphere is tilted away from the sun, making it appear lower in the sky.
The sun is higher in the sky in summer because of the tilt of the Earth's axis. During the summer solstice, the hemisphere tilted towards the sun receives more direct sunlight, causing the sun to appear higher in the sky and create longer days.
The sun is lower in the sky
Because of the tilt of Earth's axis.
In the summer, the sun is higher in the sky, casting shadows that are shorter. In the winter, the sun is lower in the sky, creating longer shadows. This difference in the angle of the sun's rays causes the length of shadows to vary between the seasons.
In the summer - or more specifically, on the summer solstice (June 21 in the northern hemisphere, December 21 in the southern hemisphere) the noon Sun is as high in the sky as it will get. If the Sun were directly overhead, you would cast no shadow at all. As summer progresses into fall, the noon Sun will be lower and lower in the sky until the winter solstice, when the noon Sun is low in the sky, and the noon shadows will be longer.
Our shadow starts to fad when the sun lowers in the sky because there is no light for our shadow to appear. (Also, as the sun gets lower, shadows get longer.)
You can see the sun to the south when it is highest in the sky in Britain.
why the sun is higher in summer is because the earths top of the axis is pointed to the sun which makes this hotter and in winter the axis is pointed away from the sun which makes it colder