Both the sun is above the horizon for less than 12 hours in January in the north and at low sun angles, the received sunlight is spread over a larger surface area.
IT is winter. The sun is facing away from the northern hemisphere and towards the southern hemisphere. This means north america, in the northern hemisphere, is getting a minimum amount of energy and therefore temperatures are lowest.
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Actually, the earth passes its perihelion, the point in its orbit at which it is closest to the sun, in early January. Although the total amount of the sun's energy that is reaching the earth decreases as the earth's distance from the sun increases, that difference is insignificant compared to the effect of the angle at which the sun's rays are contacting the various parts of the earth.
During the winter solstice in the northern hemisphere the 23 parallel in the southern hemisphere is receiving the most direct sunlight.
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Both the sun is above the horizon for less than 12 hours in January in the north and at low sun angles, the received sunlight is spread over a larger surface area.
Summer
Typically, the winter season has the least amount of rain in northern latitudes due to colder temperatures leading to less moisture in the air. This results in lower precipitation levels compared to other seasons.
The tilt of the earth's axis makes the amount of sunlight at different latitudes vary during the year
latitude
People in northern latitudes have fair skin because they have a smaller amount of the pigment melanin in their skin. The purpose of melanin is to block excessive amounts of sunlight and UV radiation from being absorbed. Modern humans, homo sapiens originated in Africa, a region which reaches high temperatures and is exposed to large amounts of sunlight, therefor, requiring a large amount of melanin.Northern latitudes have less sunlight than other regions, therefore, the humans in those places must compensate(adapt) for the lack of sunlight by being able to absorb a greater amount of it when exposed.
The low-angle sunlight has to travel through more atmosphere, which results in loss. The same amount of light is spread over a larger area because of the angle at which it hits
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Amount (temperature) or A(t)
While the amount of sunlight in the northern hemisphere does start to increase, it is still below what it is in the other seasons, and most of the area north of the Arctic Circle is still in darkness. As a result, the high northern latitudes are still losing more heat to space than they receive from the sun.
SUCH AN INSIGNIFICANT AMOUNT THAT IT JUST SOFTENS THE WINTER AND SUMMER TEMPERATURES IN THE NORTHERN HEMISPHERE. THE REASON IS BECAUSE THE EARTH IS CLOSEST TO THE SUN IN JANUARY.
Because the liquid evaporates.