| dryadiabaticrate | | temperature where a parcel of air is saturated |
| hygrometer | | directly converting a gas to a solid |
| fog | | a curl of hair, or high, white, thin clouds |
| localizedconvectivelifting | | directly converting a solid to a gas |
| convergence | | rratio of actual water content to how much air can hold |
| condensation | | process of changing a liquid to a gas |
| stratus | | heat needed for a change of state |
| frontalwedging | | a layer, or clouds that cover most of the sky |
| relativehumidity | | lifting of air by the coming together of two winds |
| cumulus | | process of changing a gas to a liquid |
| sublimation | | rate of cooling or heating of unsaturated air |
| evaporation | | all forms of water in the air |
| deposition | | lifting of air bysmall areas of warm surface area |
| precipitation | | lifting of air by air masses |
| humidity | | tools used to measure humidity |
| latent heat | | lifting of air by landforms, usually mountains |
| wetadiabaticrate | | when the air is full of water |
| orographiclifting | | amount of water vapor in the air |
| dewpoint | | ground clouds |
| cirrus | | a pile, or puffy individual clouds |
| saturated | | rate of cooling of saturated air |