Yes it does. I'm sorry I don't know more details :)
Water vapour is a constituents in air because water vapour rises in the atmosphere & is always present in the atmospere in some or the other quantity.Also 0.0001% of air consist water vapour
The amount of water vapor in the atmosphere can vary based on temperature, air pressure, and geography. Today, the percentage of water vapor may be small due to factors like low humidity, dry air masses, or lack of recent rainfall reducing the amount of water entering the atmosphere.
Clouds are made up of tiny water droplets or ice crystals. These droplets form when water vapor in the air condenses onto particles such as dust or salt. The different types of clouds can vary in altitude, thickness, and composition.
Yes, water vapor is present in the atmosphere at all times, including nighttime. The amount of water vapor in the air can vary depending on factors such as temperature, humidity, and weather conditions.
Yes, it is possible to have water vapor at -10 degrees Celsius, as water vapor can exist in the air at various temperatures. The presence of water vapor depends on the air's humidity and saturation point, which can vary with temperature. However, at -10 degrees Celsius, water vapor may condense into ice or frost if the air reaches saturation. This means that while water vapor can exist at this temperature, it is more likely to be found in solid form under certain conditions.
The amount of water per unit air is called, I believe the Absolute Humidity, and this is closely related to dew point. If the amount of water in a parcel of air remains constant, the temperature and relative humidity can vary all over the place, but the absolute humidity is constant and so, I believe, is the dew point.
Water vapour is a constituents in air because water vapour rises in the atmosphere & is always present in the atmospere in some or the other quantity.Also 0.0001% of air consist water vapour
The amount of water vapor in inhaled air can vary based on factors such as temperature, humidity, and environmental conditions. In colder and drier environments, the air will typically contain less water vapor compared to warmer and more humid conditions. Additionally, the physiological processes of the individual, like breathing rate and hydration level, can also influence the amount of water vapor in inhaled air.
Ordinary room air will have only about 4% of water vapour in it, but this can increase quite a lot before the air feels uncomfortable.Relative Humidity is the usual measure of the amount of water vapour in the air, and can vary from a few% (normal) to over 90% (humid). At 90%, the air is NOT 90% water vapour; that figure indicates that the air contains 90% of the amount of water vapour it could contain when fully saturated.For very low percentages of water vapour in the air, (say below 1%) a useful measure and one more easily made, is to measure the dew point of the air. For this, the instrument contains a small shiny mirror that may be cooled to the point where dew just forms on the mirror surface, thus spoiling the reflection.
The percentage of water vapour present in the earth's atmosphere is variable, it keeps changing from place to place as well as time to time. In rainy season it is very high but in the dry season it is very low.
On average, a person exhales about 10-15 milliliters of water vapor per breath. This amount can vary based on factors such as breathing rate, humidity levels, and individual differences.
Ozone levels do vary place to place. Equator has the maximum amount of ozone.
Often it is water vapour, which can vary from 0 to 4 %. Otherwise it is argon, at nearly 1%
True. The amount of nitrogen, oxygen, and water vapor in the atmosphere can vary depending on location, altitude, weather conditions, and human activities. These variations can impact local air quality and climate.
natural vegitation vary from place to place because it all depends on the rainfall which helps the plants to grow there,temperature and the amount of sunlight over there
The air above the sea typically contains a lot of water vapor due to evaporation from the water surface. The amount of water vapor in the air can vary depending on factors such as temperature, humidity, and wind speed.
The speed of sound in water vapor is approximately 330 meters per second at room temperature. This speed can vary depending on the temperature and pressure of the vapor.