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Reso 2016-063
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Reso 2016-063
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Last modified
3/24/2017 4:55:06 PM
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5/25/2016 3:24:35 PM
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CM City Clerk-City Council
CM City Clerk-City Council - Document Type
Resolution
Document Date (6)
5/23/2016
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2A Business 2016 0523
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\City Clerk\City Council\Agenda Packets\2016\Packet 2016 0523
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<br /> <br />5.7.3.3 Urban Conflagration <br />While the primary fire threat in the Bay Area is from wildfire, urban conflagration, or a <br />large disastrous fire in an urban area, as a major hazard that can occur due to many causes <br />such as wildfires, earthquakes, gas leaks, chemical explosions, or arson. The urban fire <br />conflagration that followed the 1906 San Francisco Earthquake did more damage than the <br />earthquake itself. A source of danger to cities throughout human history, urban <br />conflagration has been reduced as a general source of risk to life and property through <br />improvements in community design, construction materials, and fire protection systems. <br />Although the frequency of urban conflagration fires has been reduced, they remain a risk to <br />human safety. One reason is the current trend toward increased urban density and infill in <br />areas adjacent to the wildland‐urban interface. In an effort to keep housing close to urban <br />jobs, areas previously left as open space due to steep slopes and high wildland fire risk may <br />be potentially considered as infill areas for high‐density housing. A memorable example <br />of urban conflagration linked to wildland is the 1991 Oakland Hills firestorm. The <br />firestorm occurred within a larger high fire hazard zone that is part of an approximately 60 <br />mile stretch of hills running from the Carquinez Strait to San Jose in the eastern San <br />Francisco Bay Area. The fire happened in an economically well‐off, largely built‐out <br />residential area that has a long standing fire history linked to hot, dry fall winds and the <br />presence of dense, flammable vegetation. 38 <br /> <br />5.8 Drought <br />A drought is a gradual phenomenon that occurs over several dry years, depleting reservoirs <br />and groundwater basins without the expected annual recharge from winter precipitation. <br />While drought does not have any primary impacts in the Bay Area, prolonged periods of <br />drought can cause secondary impacts that can affect the region, including: <br /> Reduced water supply for crops and livestock feed, impacting the economy centered <br />around the agriculture industry <br /> Increased wildfire hazard, including more fire starts and more prolonged <br />conflagrations fueled by excessively dry vegetation and reduced water supply for <br />firefighting purposes <br /> Subsidence due to a lowering water table <br /> May be correlated to high heat conditions. <br />Drought is not localized, but occurs simultaneously across the region, and may extend <br />statewide or across a larger expanse of western states. This has been the case in California <br />since 2013. While the drought exists in every county, the impacts of the drought are locally <br /> <br />38 State of California Multi-Hazard Mitigation Plan, California Governor’s Office of Emergency Services
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