The stratosphere which contains most of the atmosphere's ozone.
The jet stream is near the top of the troposphere. It is where all weather happens. Most of the air in the atmosphere is in the troposphere.
it is cold and bumpy and frozen and beautiful it is the coldest of all
Status clouds.
It keeps getting colder. (to about -70 degrees F).
is Carl f. Von Weizsaccker
they're all cloud levels... i mean orbitals the first two rows are S cloud, the middle (transition metals) is the D cloud, the six rows on the left are the P cloud and the lanthanide series is F cloud
fog or mist
-40 °c (-40 °f)
William F. Cloud was born on 1825-03-23.
William F. Cloud died on 1905-03-04.
It is a circle with a line coming up from the top of it . Kind of like F 0
The Troposphere is 3.5 degrees f per thousand feet and 6.5 degrees s per kilometer.
It keeps getting colder. (to about -70 degrees F).
The troposphere, the lowest layer of Earth's atmosphere, is heated from below. The troposphere is warmest at the bottom near Earth's surface. The troposphere is coldest at its top, where it meets up with the layer above (the stratosphere) at a boundary region called the tropopause. Temperatures drop as you move upward through the troposphere.Sunlight streams down from space through the atmosphere, striking the ground or ocean beneath. The sunlight heats the surface, and that surface radiates the heat into the adjacent atmosphere. Atmospheric scientists use a concept called a "standard atmosphere" to represent an average atmosphere with variations caused by weather, latitude, season, and so forth, removed. In the standard atmosphere model, the temperature at sea level at the bottom of the troposphere is 15° C (59° F). Higher up in the troposphere, where less heat from the surface warms the air, the temperature drops. Typically, the temperature drops about 6.5° C with each increase in altitude of 1 kilometer (about 3.6° F per 1,000 feet). The rate at which the temperature changes with altitude is called the "lapse rate". In the standard atmosphere, by the time you reach the top of the troposphere the temperature has fallen to a chilly -57° C (-70° F).Of course, the atmosphere is always changing and is never "standard". Temperatures in the troposphere, both at the surface and at various altitudes, do vary based on latitude, season, time of day or night, regional weather conditions, and so on. In some circumstances, the temperature at the top of the troposphere can be as low as -80° C (-110° F). When a weather phenomenon called at "temperature inversion" occurs, temperature in some part of the troposphere gets warmer with increasing altitude, contrary to the normal situation.In the layer above the troposphere, the stratosphere, temperature rises with increasing altitude. In the stratosphere, the air is heated from above by ultraviolet "light" which is absorbed by ozone molecules in the air. The tropopause is the boundary between the troposphere (below) and the stratosphere (above). The tropopause occurs where the temperature stops dropping with increasing altitude (in the troposphere) and begins climbing with increasing altitude (the stratosphere).
Possession of a controlled substance. The F indicates that it is a felony charge.
Bass clef, because it indicates the position of F.
F clef, because it indicates the position of the note F.
funnel cloud
It indicates that the cell is in column F and row 7. This sort of notation is often used on spreadsheets.
H. F. Leeke has written: 'A cloud of singing things'