The highest mountains have a permanent snow line because the temperature at those elevations is consistently colder, allowing snow and ice to accumulate year-round. The higher altitude decreases the temperature, which prevents the snow from melting completely.
To convert a time in a 100m dash to miles per hour (mph), you can use the formula: mph = 3600 / (time in seconds). If the time in the 100m dash is 13.00 seconds, then the calculation would be: 3600 / 13.00 = 276.92 mph.
If you mean HECTARE- that is a unit of land measurement of 10,000 sq. meters (100m by 100m). So 3 hectares would be 30,000 square meters.
The sprinter's displacement is 100m west. Displacement measures the shortest distance and direction from the initial to the final position. In this case, the sprinter ended up 100m west from her starting point after accounting for both the distances covered in each direction.
There are 100m in a hectometre
100m above sea llevel
yes, it decreases about 1 deg Celsius for every 100m you ascend in altitude.
On average, it ws about 100m above current levels. See the related link.
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.
Potential temperature increases with height in a stable atmosphere because as air parcels rise, they expand and cool due to decreasing pressure. However, since no heat is exchanged with the surroundings, the parcel maintains its potential temperature, which increases with height. This process is known as adiabatic heating.
Yes, on average, temperature decreases by 6.5°C per kilometer as altitude increases in the troposphere. This is known as the normal lapse rate. However, in some regions, temperature inversions can cause temperatures to increase with altitude.
165M above sea level, and that is the Centenary Tower, perched on the ridge around the Valley Lake. Main residential area from 100m (on the side of the crater) down to about 10m (flat areas)
tavera
100m
50m
1 hectare
The dimensions of a duck egg are ranging from 1cm*1cm*1cm to 100m*100m*100m