Pilliod David S, Welty Justin L, Arkle Robert S
Snake River Field Station U.S. Geological Survey, Forest and Rangeland Ecosystem Science Center Boise ID USA.
Ecol Evol. 2017 Sep 25;7(19):8126-8151. doi: 10.1002/ece3.3414. eCollection 2017 Oct.
Larger, more frequent wildfires in arid and semi-arid ecosystems have been associated with invasion by non-native annual grasses, yet a complete understanding of fine fuel development and subsequent wildfire trends is lacking. We investigated the complex relationships among weather, fine fuels, and fire in the Great Basin, USA. We first modeled the annual and time-lagged effects of precipitation and temperature on herbaceous vegetation cover and litter accumulation over a 26-year period in the northern Great Basin. We then modeled how these fine fuels and weather patterns influence subsequent wildfires. We found that cheatgrass cover increased in years with higher precipitation and especially when one of the previous 3 years also was particularly wet. Cover of non-native forbs and native herbs also increased in wet years, but only after several dry years. The area burned by wildfire in a given year was mostly associated with native herb and non-native forb cover, whereas cheatgrass mainly influenced area burned in the form of litter derived from previous years' growth. Consequently, multiyear weather patterns, including precipitation in the previous 1-3 years, was a strong predictor of wildfire in a given year because of the time needed to develop these fine fuel loads. The strong relationship between precipitation and wildfire allowed us to expand our inference to 10,162 wildfires across the entire Great Basin over a 35-year period from 1980 to 2014. Our results suggest that the region's precipitation pattern of consecutive wet years followed by consecutive dry years results in a cycle of fuel accumulation followed by weather conditions that increase the probability of wildfire events in the year when the cycle transitions from wet to dry. These patterns varied regionally but were strong enough to allow us to model annual wildfire risk across the Great Basin based on precipitation alone.
在干旱和半干旱生态系统中,更大规模、更频繁的野火与非本地一年生草本植物的入侵有关,但目前仍缺乏对细燃料发育及后续野火趋势的全面了解。我们研究了美国大盆地地区天气、细燃料和火灾之间的复杂关系。我们首先模拟了降水和温度对大盆地北部26年期间草本植被覆盖和凋落物积累的年度及滞后影响。然后我们模拟了这些细燃料和天气模式如何影响后续野火。我们发现,在降水较多的年份,尤其是前三年中有一年也特别湿润时,黑麦草的覆盖面积会增加。在湿润年份,非本地杂草和本地草本植物的覆盖面积也会增加,但前提是此前经历了数年干旱。特定年份野火燃烧的面积主要与本地草本植物和非本地杂草的覆盖面积有关,而黑麦草主要通过前几年生长形成的凋落物形式影响燃烧面积。因此,包括前1至3年降水情况在内的多年天气模式,是特定年份野火的有力预测指标,因为形成这些细燃料负荷需要时间。降水与野火之间的紧密关系使我们能够将推断范围扩大到1980年至2014年35年间整个大盆地的10162起野火。我们的研究结果表明,该地区连续湿润年份后接连续干旱年份的降水模式,导致了一个燃料积累周期,随后是在周期从湿润转为干旱的年份里增加野火事件发生概率的天气状况。这些模式在区域上有所不同,但足以让我们仅根据降水情况对大盆地的年度野火风险进行建模。