Gravity occurs everywhere, its just in space it seems like there's no gravity because its very slight gravitational pull from the sun. And the reason you can float away forever is because there is extremely little friction because there's almost no gases
the troposphere
The climate of the earth and the earths atmosphere
Studies in real laboratories, as well as many public opinion surveys, have confirmed the popular intuitive supposition that they occur in the ratio of 1 : 1 .
Earth's breathable atmosphere extends to about 10 kilometers (6.2 miles) in thickness, primarily composed of nitrogen and oxygen gases. The majority of Earth's atmosphere lies within the troposphere, the lowest layer of the atmosphere where weather systems occur. Beyond this layer, the atmosphere gradually thins out into the stratosphere, mesosphere, thermosphere, and exosphere.
The vast majority of the moisture in the earths's atmosphere. The amounts in the other layers are generally inconesquential.
The troposphere is the most abundant layer in Earth's atmosphere. It is where most weather phenomena occur and contains about 75% of the atmosphere's mass.
the trees gow the more heat there is
The layer closest to the Earth's surface is the troposphere. It contains most of the atmosphere's mass and is where weather events occur.
The lowest level of the Earth's atmosphere is called the troposphere. It is where most weather phenomena occur and contains approximately 75% of the atmosphere's mass.
For an object such as a planet or moon to have weather, it must have an atmosphere. Asteroids do not have strong enough gravity to maintain an atmosphere.
The most of Earth's weather occurs in the troposphere, which is the lowest layer of the atmosphere. This is where clouds, precipitation, winds, and storms occur due to the mixing of warm and cold air masses.
The troposphere is the layer of Earth's atmosphere where most weather events occur. It is the lowest layer of the atmosphere and is where most clouds, precipitation, and storms are formed due to the mixing of air masses and the presence of moisture and temperature gradients.