Our farm store features fresh produce, eggs, grains, frozen meats, and an array of preserved goods like pickles, sauerkraut, tomato sauce, jams, and more! We will be making wood-fired pizzas for lunch, weather permitting, every Saturday this winter.
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Come out to the farm for lunch, and stock up on stored veggies, grains, meat, and preserved goods. Read more about the history of Rainshadow and the values guiding our work in sustainable agriculture. Downtown farmers market on Wednesdays from pm This market is our CSA pick-up location for the season Northwest Crossings farmers market on Saturdays from 10am-2pm.
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Your commitment helps us get started in the beginning of the season and offers you more flexibility than a traditional CSA share. Concentrate on getting what you want, while still trying some new items. Please note that Market Bucks must be spent within the market season they are purchased for. They do not roll over into the next season.
Rain shadow - Simple English Wikipedia, the free encyclopedia
Check out News, and Musings from the farm. I love that Rainshadow had so many squash growing in so many places on the farm that they had to conduct The Great Squash Tasting. This may be helpful next year, but for now,. When the days are long and warm, it is nice to have something cool and refreshing. The mountains block the passage of rain-producing weather systems and cast a "shadow" of dryness behind them. Wind and moist air is drawn by the prevailing winds towards the top of the mountains, where it condenses and precipitates before it crosses the top.
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The air, without much moisture left, advances across the mountains creating a drier side called the "rain shadow". The condition exists because warm moist air rises by orographic lifting to the top of a mountain range. As atmospheric pressure decreases with increasing altitude, the air has expanded and adiabatically cooled 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.
At the adiabatic dew point, moisture condenses onto the mountain and it precipitates on the top and windward sides of the mountain.
Rain shadow
The air descends on the leeward side, but due to the precipitation it has lost much of its moisture. Typically, descending air also gets warmer because of adiabatic compression see Foehn winds down the leeward side of the mountain, which increases the amount of moisture that it can absorb and creates an arid region.
There are regular patterns of prevailing winds found in bands round the Earth's equatorial region. The westerlies are the prevailing winds in the middle latitudes between 30 and 60 degrees latitude , blowing predominantly from the southwest in the Northern Hemisphere and from the northwest in the Southern Hemisphere. The strongest westerly winds in the middle latitudes can come in the Roaring Forties between 30 and 50 degrees latitude.
On the largest scale, the entirety of the North American Interior Plains are shielded from the prevailing Westerlies carrying moist Pacific weather by the North American Cordillera.
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