The base of the cloud occurs at the dewpoint temperature of the airmass. See: http://www.csgnetwork.com/estcloudbasecalc.html
This cloud is located in the middle altitude category, known as an altostratus cloud. Altostratus clouds typically form between 2 to 6 kilometers above the ground.
The low-altitude billowy cloud is called cumulus cloud.
An approximate value can be calculated by the following expression: Condensation Level (in feet) = [Surface Temperature(F) - Surface Dew Point Temperature(F)]*(1000/2.2) or Condensation Level (in meters) = [Surface Temperature(C) - Surface Dew Point Temperature(C)]*(200) Solution: Dry Adiabatic Lapse Rate (DALR) => -5.5 F/1000 ft of altitude (-1C/100m) Saturated Adiabatic Lapse Rate (SALR) => -3.3F/1000ft of altitude (-0.5C/100m) The SALR is not linear and varies with the initial surface temperature The Level of Condensation will occur at the altitude where the Air Temperature is equal to the Dew Point temperature at that altitude. Setting the two equations equal to each other will give an approximate value. TA: temperature at altitude; TS: temperature at surface; DA: dew point temperature at altitude; DS: dew point temperature at surface TA = TS-(5.5F/1000ft)*altitude or TS-(1C/100m)*altitude DA = DS-(3.3F/1000ft)*altitude or DS-(0.5C/100m)*altitude Setting TA = DA and rearranging quantities gives the equations given above The level of condensation derived by the above method will only yield an approximate value.
Cloud base refers to the altitude above the ground at which the lowest portion of a cloud is observed. Cloud ceiling, on the other hand, is the height above the ground of the lowest cloud layer covering more than half of the sky. Cloud base is the specific altitude at which a cloud starts, while cloud ceiling is the overall height of the lowest cloud layer in the sky.
Thick cloud cover can act as a blanket, trapping heat and causing the surface temperature to increase. Conversely, it can also reflect sunlight back into space, leading to a cooling effect on the surface temperature. The net effect depends on factors such as cloud altitude, composition, and thickness.
This cloud is located in the middle altitude category, known as an altostratus cloud. Altostratus clouds typically form between 2 to 6 kilometers above the ground.
The low-altitude billowy cloud is called cumulus cloud.
Yes, "cloud" can function as a preposition when used in phrases like "in the cloud" or "above the cloud." In these cases, it shows the relationship between an object and its location in relation to the cloud.
An approximate value can be calculated by the following expression: Condensation Level (in feet) = [Surface Temperature(F) - Surface Dew Point Temperature(F)]*(1000/2.2) or Condensation Level (in meters) = [Surface Temperature(C) - Surface Dew Point Temperature(C)]*(200) Solution: Dry Adiabatic Lapse Rate (DALR) => -5.5 F/1000 ft of altitude (-1C/100m) Saturated Adiabatic Lapse Rate (SALR) => -3.3F/1000ft of altitude (-0.5C/100m) The SALR is not linear and varies with the initial surface temperature The Level of Condensation will occur at the altitude where the Air Temperature is equal to the Dew Point temperature at that altitude. Setting the two equations equal to each other will give an approximate value. TA: temperature at altitude; TS: temperature at surface; DA: dew point temperature at altitude; DS: dew point temperature at surface TA = TS-(5.5F/1000ft)*altitude or TS-(1C/100m)*altitude DA = DS-(3.3F/1000ft)*altitude or DS-(0.5C/100m)*altitude Setting TA = DA and rearranging quantities gives the equations given above The level of condensation derived by the above method will only yield an approximate value.
Troposphere only
As cloud cover increases, Earth's temperature can be influenced in two main ways. High-altitude clouds tend to trap heat, leading to a warming effect, while low-altitude clouds can reflect sunlight, resulting in cooling. The overall impact on temperature depends on the type, thickness, and altitude of the clouds, as well as the specific climatic conditions. Thus, increased cloud cover can lead to complex interactions that either warm or cool the Earth's surface.
Cloud base refers to the altitude above the ground at which the lowest portion of a cloud is observed. Cloud ceiling, on the other hand, is the height above the ground of the lowest cloud layer covering more than half of the sky. Cloud base is the specific altitude at which a cloud starts, while cloud ceiling is the overall height of the lowest cloud layer in the sky.
Thick cloud cover can act as a blanket, trapping heat and causing the surface temperature to increase. Conversely, it can also reflect sunlight back into space, leading to a cooling effect on the surface temperature. The net effect depends on factors such as cloud altitude, composition, and thickness.
The altitude of St. Cloud, MN is approximately 1,132 feet (345 meters) above sea level.
The temperature inside a cloud can vary depending on its altitude and the surrounding air temperature. In general, clouds are composed of tiny water droplets or ice crystals that are typically colder than the air at the surface but not at freezing temperatures.
The temperature of a body of air will typically decrease when a cloud forms. This is because the cloud forms a buffer between the air and the suns warming rays.
a cold, high altitude cloud