Difference between revisions of "AY Honors/Weather/Answer Key"
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| − | '''Orographic lift''' occurs when | + | '''Orographic lift''' occurs when an [[air mass]] is forced from a low[[elevation]]to a higher elevation as it moves over rising terrain. As the air mass gains [[altitude]]the it expands and cools [[Adiabatic cooling|adiabatically]]. This cooler air cannot hold the moisture as well as warm air and this effectively raises the [[relative humidity]] to 100%, creating [[precipitation (meteorology)|precipitation]]. |
Orographic Lift is demonstrated in many places in the world, but few examples are as clear as those in the [[United States]]. In the [[United States|U.S.]] states of [[Washington]] and [[Oregon]], places on the sea-facing side of the mountains see over 100 inches (over 2.5 m) of [[precipitation (meteorology)|precipitation]] per year. These places are on the side of the [[mountain]]s which is in the way of [[storm]] systems, and therefore receives the moisture which is effectively squeezed from the clouds. However, on the other side of the [[mountain]]s, sometimes as little as 15 miles (25 km) away, annual [[precipitation (meteorology)|precipitation]] can be as low as 8 inches (200 mm) per year. | Orographic Lift is demonstrated in many places in the world, but few examples are as clear as those in the [[United States]]. In the [[United States|U.S.]] states of [[Washington]] and [[Oregon]], places on the sea-facing side of the mountains see over 100 inches (over 2.5 m) of [[precipitation (meteorology)|precipitation]] per year. These places are on the side of the [[mountain]]s which is in the way of [[storm]] systems, and therefore receives the moisture which is effectively squeezed from the clouds. However, on the other side of the [[mountain]]s, sometimes as little as 15 miles (25 km) away, annual [[precipitation (meteorology)|precipitation]] can be as low as 8 inches (200 mm) per year. | ||
Revision as of 18:32, 27 September 2005
Orographic lift occurs when an air mass is forced from a lowelevationto a higher elevation as it moves over rising terrain. As the air mass gains altitudethe it expands and cools adiabatically. This cooler air cannot hold the moisture as well as warm air and this effectively raises the relative humidity to 100%, creating precipitation.
Orographic Lift is demonstrated in many places in the world, but few examples are as clear as those in the United States. In the U.S. states of Washington and Oregon, places on the sea-facing side of the mountains see over 100 inches (over 2.5 m) of precipitation per year. These places are on the side of the mountains which is in the way of storm systems, and therefore receives the moisture which is effectively squeezed from the clouds. However, on the other side of the mountains, sometimes as little as 15 miles (25 km) away, annual precipitation can be as low as 8 inches (200 mm) per year.
