scholarly journals Sustaining Heritage Patterns in Mining Towns of the North American West: A Historico-Geographical Approach

Heritage ◽  
2021 ◽  
Vol 4 (2) ◽  
pp. 961-978
Author(s):  
Wendy R. McClure

Urban morphology provides essential methodologies to inform processes for heritage preservation and design intervention in historic places. Among principal research methods used by urban morphologists, the historico-geographical approach is particularly helpful for interpreting formative and transformative processes and for identifying key elements that define the physical structure of historic contexts at a town or neighbourhood scale. This article will discuss applications of an adapted historico-geographical approach to analyse heritage patterns in 19th-century mining towns located in mountainous regions of the western United States. Profiled case studies are part of an ongoing study intended to inform design and revitalization processes by architects, planners and community stakeholders in the region.

2002 ◽  
Vol 88 (4) ◽  
pp. 1514
Author(s):  
J. M. Bumsted ◽  
Ferenc Morton Szasz

2015 ◽  
Vol 16 (1) ◽  
pp. 118-128 ◽  
Author(s):  
Michael D. Warner ◽  
Clifford F. Mass ◽  
Eric P. Salathé

Abstract Most extreme precipitation events that occur along the North American west coast are associated with winter atmospheric river (AR) events. Global climate models have sufficient resolution to simulate synoptic features associated with AR events, such as high values of vertically integrated water vapor transport (IVT) approaching the coast. From phase 5 of the Coupled Model Intercomparison Project (CMIP5), 10 simulations are used to identify changes in ARs impacting the west coast of North America between historical (1970–99) and end-of-century (2070–99) runs, using representative concentration pathway (RCP) 8.5. The most extreme ARs are identified in both time periods by the 99th percentile of IVT days along a north–south transect offshore of the coast. Integrated water vapor (IWV) and IVT are predicted to increase, while lower-tropospheric winds change little. Winter mean precipitation along the west coast increases by 11%–18% [from 4% to 6% (°C)−1], while precipitation on extreme IVT days increases by 15%–39% [from 5% to 19% (°C)−1]. The frequency of IVT days above the historical 99th percentile threshold increases as much as 290% by the end of this century.


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