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PD-17-00001 Marian Meadows Full Record with Index (2)
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2018-03-06 10:00 AM - Commissioners' Agenda
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PD-17-00001 Marian Meadows Full Record with Index (2)
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Last modified
4/10/2018 2:21:02 PM
Creation date
4/10/2018 12:02:05 PM
Metadata
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Meeting
Date
3/6/2018
Meeting title
Commissioners' Agenda
Location
Commissioners' Auditorium
Address
205 West 5th Room 109 - Ellensburg
Meeting type
Regular
Meeting document type
Supporting documentation
Supplemental fields
Alpha Order
a
Item
Closed Record Meeting to Consider the Hearing Examiner's Recommendation for Marian Meadows Planned Unit Development (PD-17-00001) Conditional Use Permit (CU-17-00001) and Plat (LP-17-0001)
Order
1
Placement
Board Discussion and Decision
Row ID
42915
Type
Conduct closed record meeting
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<br />Marian Meadows Rezone and Subdivision Final Environmental Impact Statement 3-147 <br />Fuel <br /> Lighter fuels such as grasses, leaves, and needles quickly expel moisture and burn rapidly, while <br />heavier fuels such as tree branches, logs, and trunks take longer to warm and ignite. <br /> Snags and hazard trees, those that are diseased, dying, or dead, are larger west of the Cascades, but <br />more prolific east of the Cascades. In 2005, about 2.5 million acres of the state’s 21 million acres of <br />forest land contained trees killed or defoliated by forest insects and diseases. <br />Weather <br /> East of the Cascades, summer drying typically starts in mid-June and runs through early September, <br />with drought conditions extending this season. <br /> Passage of a dry, cold front through this region can result in sudden increase in wind speeds and a <br />change in wind direction affecting fire spread. <br /> Thunderstorm activity, which typically begins in June with wet storms, turns dry with little or no <br />precipitation reaching the ground as the season progresses into July and August. Thunderstorms <br />with dry lightning are more prevalent in Eastern Washington. <br />Terrain <br /> Topography of a region or a local area influences the amount and moisture of fuel. <br /> Elevation and slope of landforms affect the spread and intensity of fire, which spreads more easily <br />as it moves uphill than downhill and dries and heats fuels in its path, making it easier to ignite and <br />burn. The fire can create its own winds through convection that further intensifies the fire and <br />increase spread. <br /> Barriers such as highways and lakes can affect the spread of fire depending on their width and <br />location. In an intense fire, wind tends to carry burning debris considerable distance and can jump <br />such fire barriers. <br />All of the factors for creating extreme hazard conditions are present in the Easton area, especially on the <br />slopes surrounding the valley. Adding to the risk is the near constant wind from the west that quickly <br />dries forests after snowmelt (Munroe 2010). <br />4 How will the proposal and alternatives affect fire protection facilities and services? <br />The addition of residences generally adds to the incidence of fire as well as the demands placed on the <br />fire district to control these fires. If all factors were equal, the risk and need for additional fire protection <br />services would be proportional to the increase. This is not the case, however, because the factors <br />affecting risk differ by location and character of development. <br />In the case of the proposed Marian Meadows development, the addition of 443 residents adds about <br />30 percent to the number of potential sources of residential fires. The provision of water supply and fire
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