TY - JOUR
T1 - Spatiotemporal variability of human–fire interactions on the Navajo Nation
AU - Guiterman, Christopher H.
AU - Margolis, Ellis Q.
AU - Baisan, Christopher H.
AU - Falk, Donald A.
AU - Allen, Craig D.
AU - Swetnam, Thomas W.
N1 - Funding Information:
We are indebted to the Navajo Nation, the Navajo Forestry Department, the Navajo Heritage and Historic Preservation Department, and the BIA Navajo Regional Office for supporting and encouraging this work. In particular, we thank Alexious Becenti, Frankie Thompson, Timothy Jim, Herman Yazzie, Sadie Johnson, Cathy Covington, and Andrew Cadenhead. We were assisted in the field and laboratory by Eze Ahanonu, Alex Arizpe, Erica Bigio, Royale Billy, Patrick Brewer, Rebecca Brice, Josh Farella, Charles Mogen, and especially Melissa Schwan. We thank William Tsosie, Tamara Billie, Jeffrey Dean, Ronald Towner, and Marsha Weisiger for providing their perspectives on Navajo history. Comments by Wade Campbell and two anonymous reviewers improved this manuscript. The research presented here was conducted under permits by the Navajo HHPD (#C14028) and the NFD. We were funded by the Navajo Nation (joint agreement CO1142), an EPA STAR Fellowship to C.H.G. (award F13F51318), and the Bureau of Indian Affairs Tribal Resilience Program (agreement A17AC00020). Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government.
Publisher Copyright:
© 2019 The Authors.
PY - 2019/11/1
Y1 - 2019/11/1
N2 - Unraveling 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.
AB - Unraveling 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.
KW - Diné
KW - Navajo
KW - dendrochronology
KW - fire history
KW - natural disturbance regimes
KW - pastoralism
KW - ponderosa pine
KW - transhumance
KW - tree rings
UR - http://www.scopus.com/inward/record.url?scp=85076381347&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85076381347&partnerID=8YFLogxK
U2 - 10.1002/ecs2.2932
DO - 10.1002/ecs2.2932
M3 - Article
AN - SCOPUS:85076381347
SN - 2150-8925
VL - 10
JO - Ecosphere
JF - Ecosphere
IS - 11
M1 - e02932
ER -