Answer:
100m is 24.5°C,
1500m is 17.5°C,
2000m is 15°C.
Step-by-step explanation:
To calculate the temperature at different altitudes using the given humid adiabatic gradient, we'll use the formula:
T2 = T1 - (gradient * (altitude2 - altitude1))
Given:
Surface temperature (altitude1) = 25°C
Humid adiabatic gradient = 0.5°C/100m
Let's calculate the temperatures at the specified altitudes:
At 100m:
altitude2 - altitude1 = 100m - 0m = 100m
T2 = T1 - (gradient * (altitude2 - altitude1))
T2 = 25°C - (0.5°C/100m * 100m)
T2 = 25°C - 0.5°C
T2 = 24.5°C
At 1500m:
altitude2 - altitude1 = 1500m - 0m = 1500m
T2 = T1 - (gradient * (altitude2 - altitude1))
T2 = 25°C - (0.5°C/100m * 1500m)
T2 = 25°C - 7.5°C
T2 = 17.5°C
At 2000m:
altitude2 - altitude1 = 2000m - 0m = 2000m
T2 = T1 - (gradient * (altitude2 - altitude1))
T2 = 25°C - (0.5°C/100m * 2000m)
T2 = 25°C - 10°C
T2 = 15°C
Therefore, the temperature at 100m is 24.5°C, at 1500m is 17.5°C, and at 2000m is 15°C. These values are obtained by subtracting the appropriate temperature change (determined by the humid adiabatic gradient) from the initial temperature at the surface.