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Fire history of a pinyon-juniper/ponderosa pine ecosystem in the Intermountain West.

机译:西山际松树,杜松/黄松的生态历史。

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摘要

Dendrochronology techniques were applied to reconstruct the fire history of a pinyon-juniper/ponderosa pine woodland in the Great Basin. The goals of our study were to describe the frequency and spatial extent of fire on Mount Irish, in southeastern Nevada, and to identify any temporal changes in fire regime over the past few centuries. The topographically complex Mount Irish study area encompasses approximately 1.6 km² and ranges from 2400 to 2560 meters in elevation. The climate of the study area is typical of the southern Great Basin with an average annual rainfall of about 300 millimeters, most of which falls in the winter months with relatively dry summers. Mount Irish is a relatively pristine site with a short history of past EuroAmerican silver mining in the late 1800s. To reconstruct fire history on Mount Irish, we sampled all fire-scarred trees within the study area. We collected a total of 255 fire-scar wedge sample, of which 197 were successfully crossdated. Most of the crossdated samples were from ponderosa pine (87%), and the rest consisted of white fir (11%) and pinyon pine (2%). The fire history reconstruction covers 860 years, from 1146 to 2006 AD, and includes 492 fire scars. Fire severity was low enough at the site to leave evidence of fire scars behind throughout the last 850 years. Pre-settlement fire frequency was also relatively high during the 1780-1840 period when fire was reduced or absent in many other fire history studies of the western United States. A dramatic decrease in fire occurrence was coincident with EuroAmerican settlement of the region. In terms of spatial patterns, fire events were usually patchy but could occur throughout the study area in a single year, which suggests multiple ignitions during a single year. Since older trees were scattered over the landscape evidence for stand replacing fires was scarce.
机译:运用树轮年代学技术重建了大盆地的一个松-杜松/黄松林地的火灾历史。我们研究的目的是描述内华达州东南部爱尔兰山上火的频率和空间范围,并确定过去几个世纪以来火势的任何时间变化。地形复杂的爱尔兰山研究区占地约1.6km²,海拔2400至2560米。该研究区的气候是大盆地南部的典型特征,年平均降雨量约为300毫米,其中大部分降雨是在冬季,而夏季相对干燥。爱尔兰山是一个相对原始的地方,在1800年代后期,过去的欧美银矿开采历史很短。为了重建爱尔兰山的火灾历史,我们对研究区域内所有烧焦的树木进行了采样。我们总共收集了255个火疤楔形样本,其中197个被成功划破。大部分杂交样品来自美国黄松(87%),其余包括白杉(11%)和松子(2%)。从1146年到2006年的火灾历史重建历时860年,其中包括492处火伤痕迹。在过去的850年中,该地点的火灾严重程度低至足以留下火灾痕迹的证据。在1780-1840年期间,在美国西部许多其他火灾历史研究中减少或不发生火灾时,结算前的火灾频率也相对较高。发生火灾的急剧减少与该地区的欧洲美国人定居点相吻合。就空间格局而言,火灾通常是零星的,但一年内可能会在整个研究区域内发生,这表明一年内会多次起火。由于较老的树木散落在景观上,因此缺乏能替代林火的证据。

著录项

  • 作者

    Jamieson, Leia P.;

  • 作者单位

    University of Nevada, Reno.;

  • 授予单位 University of Nevada, Reno.;
  • 学科 Geography.
  • 学位 M.S.
  • 年度 2008
  • 页码 94 p.
  • 总页数 94
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 自然地理学 ;
  • 关键词

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