The Cause of Warm, Dry Conditions On The Lee Side
The condition exists because warm moist air rises through "orographic lifting" up and over the top of a mountain range or large mountain. Because of decreasing atmospheric pressure with increasing altitude, the air expanded and adiabatically cooled at the dry adiabatic lapse rate to the point that the air reaches its adiabatic dew point (which is not the same as its constant pressure dew point commonly reported in weather forecasts). Upon reaching the adiabatic dew point, water vapor in the air begins to condense, with the release of latent heat from condensation slowing the overall rate of adiabatic cooling of the air to the saturated adiabatic lapse rate as the air continues to rise. Condensation is also commonly followed by precipitation on the top and windward sides of the mountain. As the air descends on the leeward side, it is warmed by adiabatic compression at the dry adiabatic lapse rate. Because the air has lost much of its original water vapor content, the descending air creates an arid region on the leeward side of the mountain.
Read more about this topic: Foehn Wind
Famous quotes containing the words dry, conditions, lee and/or side:
“The Plains are not forgiving. Anything that is shallowthe easy optimism of a homesteader; the false hope that denies geography, climate, history; the tree whose roots dont reach ground waterwill dry up and blow away.”
—Kathleen Norris (b. 1947)
“One cannot divine nor forecast the conditions that will make happiness; one only stumbles upon them by chance, in a lucky hour, at the worlds end somewhere, and hold fast to the days, as to fortune or fame.”
—Willa Cather (18761947)
“Soldier: Hey colonel, I got me a prisoner. What should I do with him?
Col. John Marlowe: Spank him.”
—John Lee Mahin (19021984)
“Rock of ages, cleft for me,
Let me hide myself in thee!
Let the water and the blood,
From thy riven side which flowed,
Be of sin the double cure;
Cleanse me from its guilt and powr.”
—Augustus Montague Toplady (17401778)