1) latitude - affects the degree st which the suns rays strike the earth
2) altitude - the higher the colder: environmental lapse rate: every 150m a 1 degree (celcius) drop occurs
3) distance from large bodies of water land temperatures are modified due to the ocean (cooler in summer and warmer in winter) also the air masses that blow over the bodies of water absorb moisture from it and blow it over land
4) ocean currents affect the temperature of the air masses that blow over it. the temperature of the current depends on where the current originates. (i.e if it forms in the tropics the current will be warm etc.)
5)Mountain barriers (when moist warm wind blows up the windward side of a mountain it is forced to cool, and cool air cannot hold in the moisture. this causes precipitation which leads to a rain shadow on the leeward side of the mountain.
6) air masses volumes of air blowing due to unequal heating from the sun. where an air mass is formed affects the temperature of the air mass, and wherever the air mass blows is affected by the temperature of the air mass
7) prevailing wind systems - wind absorbs the heat and moisture from oceans and blows onto land.
Geothermal gradient refers to the increase in temperature with depth below the Earth's surface. On average, the geothermal gradient is about 25-30°C per kilometer. This gradient varies depending on factors like location and geologic conditions.
Nope, never, absolute zero cannot be reached by artificial or natural means.
Thermal heat does not directly affect Earth's tides. Tides are primarily influenced by the gravitational forces of the Moon and the Sun. However, thermal heat can impact the density and circulation of ocean waters, which may indirectly influence tides in localized areas.
The delay in Earth's absorption of solar energy is due to the time it takes for the land and water to heat up. This delay causes the warmest part of the day to occur in the late afternoon, after peak solar radiation has been received. The lag in temperature increase is a result of the Earth's thermal inertia and the redistribution of heat across the planet.
The Earth's magnetic field has changed polarity hundreds of times in the geological past. This phenomenon is known as geomagnetic reversal. The frequency at which these reversals occur is not regular, but on average, it is estimated to happen every few hundred thousand years.
its is about +20C and Night and _20f ina morning
it is way warmer there than on earth! earths average temperature is 14C mercurys average temperature is 66C
Mercury has an average surface temperature (67°) closest to the Earths average surface temperature (14°C). The temperature on Mercury varies a lot though - you could argue that Mars is closer in temperature.
Global. Warming
There is no average temperature on Earth in Celsius because so many places have different temperatures. The average temperature of some locations can be calculated.
The average temperature at sea level on Earth is around 15 degrees Celsius or 59 degrees Fahrenheit.
the average temperature for the Earth's lower mantle is 5400 degrees
Temperature, area times volume squared, earths orbit, and the tides.
The gradual increase of the average air temperature in Earth's lower atmosphere is known as global warming.
it depends on the deepth
The Earth's average surface temperature during the twentieth century was around 13.9 to 15.1 degrees Celsius, depending on data sources.
The earths temperature varies for example living on the equator it would be hotter but up in the north lets say iceland it would be a lot colder so there is no real earths temperature(unless you get to the core of the earth)