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  2. Rain shadow - Wikipedia

    en.wikipedia.org/wiki/Rain_shadow

    Effect of a rain shadow The Tibetan Plateau (center), perhaps the best example of a rain shadow. Rainfalls from the southern South Asian monsoon do not make it far past the Himalayas (seen by the snow line at the bottom), leading to an arid climate on the leeward (north) side of the mountain range and the desertification of the Tarim Basin (top).

  3. Puget Sound Convergence Zone - Wikipedia

    en.wikipedia.org/wiki/Puget_Sound_Convergence_Zone

    The proximity of the Convergence Zone to the King-Snohomish County line is the reason that cities located just north or south of the line, which are located within the rain shadow of the Olympic Mountains, approach Seattle in annual precipitation. The effect of the Puget Sound Convergence Zone nearly offsets that of the rain shadow. [4]

  4. United States rainfall climatology - Wikipedia

    en.wikipedia.org/wiki/United_States_rainfall...

    The western part of the contiguous United States west of the 98th meridian, the mountains of the Pacific Northwest, the Willamette Valley, and the Sierra Nevada range are the wetter portions of the nation, with average rainfall exceeding 30 inches (760 mm) per year. The drier areas are the Desert Southwest, Great Basin, valleys of northeast ...

  5. Foehn wind - Wikipedia

    en.wikipedia.org/wiki/Foehn_wind

    Dry Foehn conditions are responsible for the occurrence of rain shadows in the lee of mountains, where clear, sunny conditions prevail. This often leads to greater daytime radiative (solar) warming under Foehn conditions. This type of warming is particularly important in cold regions where snow or ice melt is a concern or where avalanches are a ...

  6. Orographic lift - Wikipedia

    en.wikipedia.org/wiki/Orographic_lift

    As the air descends the lee side of the mountain, it warms and dries, creating a rain shadow. On the lee side of the mountains, sometimes as little as 15 miles (25 km) away from high precipitation zones, annual precipitation can be as low as 8 inches (200 mm) per year. [3] Areas where this effect is observed include:

  7. Eastern Cascades Slopes and Foothills - Wikipedia

    en.wikipedia.org/wiki/Eastern_Cascades_slopes...

    In the rain shadow of the Cascade Range, the eastern side of the mountains experiences greater temperature extremes and receives less precipitation than the west side. Open forests of ponderosa pine and some lodgepole pine distinguish this region from the Cascades ecoregion , where hemlock and fir forests are more common, and from the lower ...

  8. Answering TikTok: What does a '30% chance of rain' actually mean?

    www.aol.com/weather/answering-tiktok-does-30...

    What does a 30% chance of rain actually mean? Don't overthink it, meteorologists say. The question was sparked by a viral video that has received millions of views, originating on TikTok by user ...

  9. Chihuahuan Desert - Wikipedia

    en.wikipedia.org/wiki/Chihuahuan_Desert

    The desert is mainly a rain shadow desert because the two main mountain ranges which bound the desert, the Sierra Madre Occidental to the west and the Sierra Madre Oriental to the east, block most moisture from the Pacific Ocean and the Gulf of Mexico, respectively. [3]