Geathen rocks
The Earth's atmosphere is stable because is mostly oxygen and nitrogen. These two parts of the atmosphere are equal to about 99% of all dry air gas. Water vapor accounts for negligible amounts. While the composition of water vapor, carbon dioxide and ozone can vary in concentration, all other elements remain stable.
What vapor will condense onto any object that is at a lower temperature, or when the amount of water vapor able to be held in the air is exceeded. It's known as the DEW POINT and it changes with the temperature and climate.
Oxygen, Nitrogen and Argon comprise 99% of the air.
The variable gases are are those atmospheric gases whose concentrations vary through time. The variable gases are sometimes called the "minor gases" because they make up such a small percentage of the atmosphere by volume.. Carbon dioxide, methane, and water vapor are examples of variable gases.
weather. The state of the atmosphere at a given time and place, with respect to variables such as temperature, moisture, wind velocity, and barometric pressure. a. Adverse or destructive atmospheric conditions, such as high winds or heavy rain: encountered weather five miles out to sea.
the shape and height causes it to vary with temperature,pressure,and the amount of water vapor in the atmosphere
No. Not across the whole planet. The concentrations of some of the gases, particularly water vapor, vary from one area to the next.
Water vapor, Argon and Carbon Dioxide are gases that vary between zero and 5 % of the atmosphere. The atmosphere also contains about 78% Nitrogen and 21% Oxygen.
The Earth's atmosphere is stable because is mostly oxygen and nitrogen. These two parts of the atmosphere are equal to about 99% of all dry air gas. Water vapor accounts for negligible amounts. While the composition of water vapor, carbon dioxide and ozone can vary in concentration, all other elements remain stable.
The amount of radiation absorbed per 100 units by water vapor and clouds can vary depending on factors like the amount of water vapor present, cloud density, and the type of radiation (e.g. solar or terrestrial). On average, water vapor absorbs a significant portion of solar radiation and emits it back into the atmosphere. Clouds can further enhance this absorption and scattering of radiation, leading to a net increase in energy absorption compared to clear skies.
The specific heat of water when it comes to a boiling point is 100 degrees Celcius, or 212 degrees Fahrenheit. The boiling temperature can vary based on the vapor pressure of the atmosphere.
The main products that they release into the atmosphere are water vapor and oxygen gas. There are also other molecules that are released in some plants and other producers but, these vary with the plant and are in much lower quantity.
The air receives water wapor by evaporation, and by circulation, and loses it to condensation and precipitation. The actual amount that the air can hold is determined by the temperature and pressure. The warmer the air, the more water vapor it can hold. (Conversely, the denser the air, the more water vapor it can hold, but denser air is usually also cooler air.)
Yes.
What vapor will condense onto any object that is at a lower temperature, or when the amount of water vapor able to be held in the air is exceeded. It's known as the DEW POINT and it changes with the temperature and climate.
The density of water vapor can vary depending on temperature and pressure. At standard temperature and pressure (STP), the density of water vapor is approximately 0.804 grams per liter (g/L). However, as temperature increases or pressure decreases, the density of water vapor decreases.
Regulations that are introduced to restrict the amount of pollution discharged into the atmosphere. They will vary according to the country you are referring to