Because mountain is a higher and the air is top and right and left of a mountain.🙂
-60 c
.....A person can experience the coolest air temperature in a mountain, when he/she is on the left slope.......
Wind is blowing air up over the mountain. Going from about 1,000 feet at the base to 7,000 feet at the top, the temperature changes as the air goes over the mountain.
The approximate speed of sound in air at 25°C is 346.45 m/s².
The approximate velocity of sound in air at room temperature is about 343 meters per second (1235 kilometers per hour). The actual velocity may vary based on factors like temperature, humidity, and air pressure.
Mountain breezes typically form during the night. As the sun sets, the air in the valley cools more quickly than the air on the mountain, creating a temperature difference. This temperature difference causes the air to flow from the mountain down into the valley, creating a mountain breeze.
the temperature gets lower as you get higher. That'swhy there is ice caps on top of the mountain.
The approximate temperature of descending air at an elevation of 1600 meters can be estimated using the adiabatic lapse rate, which is about 6.5°C per kilometer. At this elevation, the temperature could decrease by roughly 10.4°C from sea level, assuming a starting temperature of around 20°C. Therefore, the temperature of the descending air at 1600 meters would be approximately 9.6°C. However, actual temperatures can vary based on local conditions and weather systems.
At the top of the mountain you feel more colder than the normal temperature.
Wind is blowing air up over the mountain. Going from about 1,000 feet at the base to 7,000 feet at the top, the temperature changes as the air goes over the mountain.
At the base of the mountain.
To calculate the dew point when the air temperature is 26°C and the relative humidity is 77%, you can use the formula or an online calculator. The approximate dew point in this case is around 21.5°C. This indicates the temperature at which the air would become saturated with moisture, leading to condensation.