Less light means the temperature falls. With fewer hours of daylight, there is less time for temps to increase at all. The combination produces longer periods of lower temperatures and a breeze or winds increase the cold's effects.
if the axis is over 90 degrees to the norh as it is in the summer
Daylight is greatly dependent on the sun. The number of daylight hours a city or country receives is dependent on its latitude.
If the Earth's axis was vertical - every point on its surface would have the same length of day and night, no matter what time of year it was. The tilt of the axis (to about 11 degrees) means that, as the Earth rotates, and travels around the sun, the length of day shortens and lengthens throughout the year.
12 hours
3 months of complete darkness.
In general there is a delay between the highest daylight hours and highest temperatures and between lowest daylight hours and lowest temperatures. The reason is energy absorbed. When the sun is pounding down during the summer the highest temperatures come approx 1 month after the longest day of the year because the enrgy absobed on the earth in the oceans and on land has a commulative effect. The same thing happens in winter.
Daylight typically has a color temperature ranging from 5000 to 6500 Kelvin, with midday sunlight around 5500K.
It depends on your location, in some places they are
Earth's axial tilt, approximately 23.5 degrees, significantly influences the number of daylight hours and temperature experienced at various locations. During summer in one hemisphere, that region is tilted toward the sun, resulting in longer daylight hours and higher temperatures. Conversely, during winter, the same hemisphere is tilted away from the sun, leading to shorter days and cooler temperatures. This axial tilt is responsible for the seasonal changes that impact climate and daylight duration across the planet.
if the axis is over 90 degrees to the norh as it is in the summer
Shade from surrounding trees has the least effect on lake water temperature.
The average number of hours of daylight per day in a specific location is determined by the Earth's rotation and the time of year. This can vary depending on the latitude of the location and the season.
The high temperature for a given city.
In general there is a delay between the highest daylight hours and highest temperatures and between lowest daylight hours and lowest temperatures. The reason is energy absorbed. When the sun is pounding down during the summer the highest temperatures come approx 1 month after the longest day of the year because the enrgy absobed on the earth in the oceans and on land has a commulative effect. The same thing happens in winter.
kd[2
The average number of hours of daylight per year in a specific location is determined by calculating the total number of daylight hours throughout the year and dividing it by the number of days in the year. This average can vary depending on the location's latitude and time of year.
To find the mean temperature of a given location, you would need to collect temperature data over a period of time, such as a month or a year. Add up all the temperatures recorded during that time period and then divide by the number of temperature readings taken. This will give you the mean temperature for that location.