Abstract

AbstractUnraveling the effects of climate and land use on historical fire regimes provides important insights into broader human–fire–climate dynamics, which are necessary for ecologically based forest management. We developed a spatial human land‐use model for Navajo Nation forests across which we sampled a network of tree‐ring fire history sites to reflect contrasting historical land‐use intensity: high human use, primarily in the Chuska Mountains, and low human use, primarily on the central Defiance Plateau. We tested for and compared human‐ and climate‐driven changes in the fire regimes by applying change point detection, regression, and superposed epoch analyses. The historical fire regimes and fire–climate relationships reflect those of similar forests regionally and are similar between the two Navajo landscapes until the early 1800s. We then determined that a previously identified, localized, early (1830s) decline in fire activity was geographically widespread across higher human‐use sites. In contrast, fires continued to burn uninterrupted through this period at the lower use sites. Though the 1830s included significantly wet and cold periods that could have contributed to fire regime decline, human factors pose a more spatiotemporally consistent explanation. A rise in Navajo pastoralism in the 1820s–1830s was concentrated seasonally in the heavy use sites. By the 1880s, livestock numbers more than doubled, grazing became far more spatially widespread, and frequent fire regimes of Navajo forests collapsed. The last widespread fire recorded on either landscape was in 1886. In the Chuska Mountains, livestock and fire coexisted for over 50 yr between the initial 1832 fire decline and the end of frequent fires after 1886, an exceptional pattern in the western United States. Though unique in its timing, character, and spatial dynamics, the collapse of historical fire regimes in Navajo forests contributed to now over a century without frequent surface fire, leaving Navajo forests at risk for large, uncharacteristic high‐severity fires.

Highlights

  • Recent increases in wildfire activity have triggered devastating impacts on human communities and natural resources, raising awareness that anthropogenic climate change combined with past fire management is increasing the vulnerability of western U.S forests (Stephens et al 2013)

  • The goal of this study is to evaluate the relative roles of human land use and climate on spatial and temporal variability of forest fire regimes on the Navajo Nation

  • Tree-ring chronologies extend longer than one millennium, with the earliest tree dating to 735 Common Era (CE), the earliest fire scar is in 817 CE, and the most recent scar is in 2011 (Table 1)

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Summary

Introduction

Recent increases in wildfire activity have triggered devastating impacts on human communities and natural resources, raising awareness that anthropogenic climate change combined with past fire management is increasing the vulnerability of western U.S forests (Stephens et al 2013). High-severity fire has been increasing in recent decades in many regions (e.g., southwestern United States; Singleton et al 2019). These changes highlight the influence of both humans and climate on fire regimes (Abatzoglou and Williams 2016, Balch et al 2017) but represent only a small snapshot in time for understanding interactions of multiple complex processes. Paleo records of fire provide multi-century insights into human–fire–climate dynamics that can inform current fire management and restoration and help to calibrate projections of future fire regimes

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