barometric pressure
There are several conditions that influence temperature and precipitation. Landforms, ocean currents, winds, latitude areas, and many other things can affect temperature and precipitation.
Temperature and precipitation
Geogrophy
The average annual precipitation in Germany varies in different regions. The range of annual precipitation is anywhere from 23 inches in most areas to up to 48 inches in the Alpine mountain region.
wet
Temperature and precipitation are related to climate in how they affect it. Areas with very high temperatures and low precipitation, like deserts, are considered arid.
There are several conditions that influence temperature and precipitation. Landforms, ocean currents, winds, latitude areas, and many other things can affect temperature and precipitation.
Temperature and precipitation
It is because there is different amounts of cloud in different areas, thus the amount of precipitation is different. From, Anomynous
Geogrophy
The average yearly precipitation will depend on location. This includes the amount of rainfall in inches throughout the United States. Drier states and regions will have less precipitation than coastal areas.
because of distance from the sea
Temperate deciduous forests are located in the mid-latitude areas. This means that they are found between the polar regions and the tropics. The deciduous forest regions are exposed to warm and cold air masses. IT cause this area to have four seasons. The temperature varies widely from season to season with cold winters and hot, wet summers. The average yearly temperature is about 10°C. The areas in which deciduous forests are located get about 750 to 1,500 mm of precipitation spread fairly evenly throughout the year.
Both are considered to have less than 25 centimeters of rain each year
The average annual precipitation in Germany varies in different regions. The range of annual precipitation is anywhere from 23 inches in most areas to up to 48 inches in the Alpine mountain region.
The direction that heat flows in is From a warmer object to a cooler object.
To show areas that have similar measurements of precipitation, temperature, gravity, magnetism, density, elevation, or chemical composition.