| Revision as of 12:28, 31 December 2003 editSlawojarek (talk | contribs)3,017 editsm +pl← Previous edit | Revision as of 15:29, 10 January 2004 edit undoDino (talk | contribs)Administrators14,022 editsm link to recent articleNext edit → | ||
| Line 7: | Line 7: | ||
| In ], '''precipitation''' is any kind of ] that falls from the sky as part of the ]. This includes ], ], ], ] and ]. Precipitation is a major part of the ], and is responsible for depositing most of the ] on the planet. Precipitation is generated in ]s, which reach a point of saturation; at this point larger and larger droplets (or pieces of ]) form, which then fall to the earth under ]. It is possible to 'seed' clouds to induce precipitation by releasing a fine dust or appropriate chemical (commonly ]) into a cloud, encouraging droplets to form, and increasing the probability of precipitation. | In ], '''precipitation''' is any kind of ] that falls from the sky as part of the ]. This includes ], ], ], ] and ]. Precipitation is a major part of the ], and is responsible for depositing most of the ] on the planet. Precipitation is generated in ]s, which reach a point of saturation; at this point larger and larger droplets (or pieces of ]) form, which then fall to the earth under ]. It is possible to 'seed' clouds to induce precipitation by releasing a fine dust or appropriate chemical (commonly ]) into a cloud, encouraging droplets to form, and increasing the probability of precipitation. | ||
| '''Orographic precipitation''' is precipitation generated by upward movement of air upon encountering a physiographic upland. This upwards movement cools the air, resulting in cloud formation and rainfall. In parts of the world subjected to consistent winds (for example the ]), a wetter ] prevails on the windward side of a mountain than on the leeward (downwind) side as moisture is removed by orographic precipitation, leaving drier air on the descending (generally warming), leeward side. | '''Orographic precipitation''' (see also ]) is precipitation generated by upward movement of air upon encountering a physiographic upland. This upwards movement cools the air, resulting in cloud formation and rainfall. In parts of the world subjected to consistent winds (for example the ]), a wetter ] prevails on the windward side of a mountain than on the leeward (downwind) side as moisture is removed by orographic precipitation, leaving drier air on the descending (generally warming), leeward side. | ||
| See also ]. | See also ]. | ||
Revision as of 15:29, 10 January 2004
]
In meteorology, precipitation is any kind of water that falls from the sky as part of the weather. This includes snow, rain, sleet, freezing rain and hail. Precipitation is a major part of the hydrologic cycle, and is responsible for depositing most of the fresh water on the planet. Precipitation is generated in clouds, which reach a point of saturation; at this point larger and larger droplets (or pieces of ice) form, which then fall to the earth under gravity. It is possible to 'seed' clouds to induce precipitation by releasing a fine dust or appropriate chemical (commonly silver nitrate) into a cloud, encouraging droplets to form, and increasing the probability of precipitation.
Orographic precipitation (see also rain shadow) is precipitation generated by upward movement of air upon encountering a physiographic upland. This upwards movement cools the air, resulting in cloud formation and rainfall. In parts of the world subjected to consistent winds (for example the Tradewinds), a wetter climate prevails on the windward side of a mountain than on the leeward (downwind) side as moisture is removed by orographic precipitation, leaving drier air on the descending (generally warming), leeward side.
See also umbrella.