It's highest at local mid-day, which may or may not be noon by the clock.
the atmosphere makes it look yellow
That direction is called East.
half
The same direction that the Earth rotates around its axis.
Ice generally melts faster in the afternoon than in the morning. This is because the sun is typically higher in the sky and its rays are more direct during the afternoon, resulting in increased temperatures and greater heat absorption. Additionally, ambient temperatures are often warmer in the afternoon, further accelerating the melting process.
The Sun is in the West of the sky in the afternoon, so it's facing East.
In the late afternoon, an object's shadow typically falls toward the east. This is because the sun is positioned in the western part of the sky, causing shadows to extend in the opposite direction. The angle of the shadow can vary depending on the height of the sun, but it will generally point eastward as the sun sets.
South for early morning light and no direct sun in late afternoon.
The shadow is in front of you when the sun is behind you, typically in the late morning or early afternoon. The length and direction of the shadow will vary depending on the position of the sun in the sky.
In the morning, shadows are long and point west as the sun rises in the east. At midday, shadows are shortest as the sun is directly overhead, casting shadows directly below objects. In the afternoon, shadows lengthen and point east as the sun moves towards the west.
The difference between a morning shadow and a afternoon shadow is the face different ways and the opposite ways to the suns position.A morning shadow is very light but afternoon shadow is deep.
Morning is cooler then hotter in the afternoon because the sun has not made its way from our horizon into the sky, and by the time it takes the sun to reach the highest point in the sky ( where it will generate the most heat ) it is already the afternoon.
Rainbows are typically seen in the western part of the sky in the afternoon. This is because the sun is in the western part of the sky during that time, and rainbows form when sunlight is refracted and reflected off water droplets in the air.
A flagpole's shadow changes in length and direction throughout the day due to the movement of the sun across the sky. In the morning and late afternoon, shadows are longer as the sun is lower on the horizon, while at noon, shadows are shorter since the sun is at its highest point. Additionally, the angle of the shadow varies with the seasons as the sun's path changes, affecting the overall length and direction of the shadow cast by the flagpole.
When the Sun is high in the afternoon, your shadow will be shorter and appear directly beneath you. This is because the angle of the Sun is more overhead, resulting in a shorter shadow length.
because of the heat and the sun in the afternoon
Joe sun