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| The southwestern U.S. has experienced severe drought for much of the last four years. Record or near-record dryness occurred in some areas during the summer of 2003, with New Mexico having the driest July since statewide records began in 1895. The 1950s drought stands out as the most severe and longest-lasting drought for the state in the last 100 years. In the longer historical perspective, however, paleoclimatic data (primarily tree-rings) indicate that more severe and longer-lasting droughts have occurred in the region during the last two thousand years. |
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Dr. Henri Gissino-Mayer, of the University of Tennessee, has analyzed paleoclimatic data from the El Malpais site in New Mexico (see map to right) to provide a climate reconstruction going back to 136 B.C. The El Malpais site is especially suitable for the reconstruction of past climate because the Douglas-fir trees growing at this site are isolated from destructive environmental and human forces by protective lava fields. The site is described in further detail at the web page here.
The El Malpais tree-ring record is most closely associated with precipitation over a 13-month period covering July through the following July. The top graph in the image below right shows the close association between the tree-ring reconstruction and observed 13-month July-July precipitation for the Southwestern Mountains of New Mexico (Climate Division 4) for the last 100 years. The comparison shows that the droughts of the 1950s and early 1900s are well represented by the tree-ring reconstruction of precipitation. The bottom graph to the right shows the 10-year moving mean of the precipitation reconstruction for the last two millennia. While the 20th century dry events were quite severe, the reconstruction shows that several earlier droughts were more severe and lasted much longer. A number of the severe droughts of the past spanned several decades, the most recent occurring in the second half of the 16th century. Other notable examples are the dry spells in the middle of the 15th century, in the 12th and 13th centuries, in the middle of the sixth century, and the prolonged period of dryness which stretched across most of the fourth and fifth centuries. Overall, this reconstruction suggests that severe, long-duration (longer than 10 years) droughts are a common feature of New Mexico's climate.
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Dr. Thomas Swetnam and colleagues from the University of Arizona have collected samples from fire scarred trees for a large number of sites in New Mexico and Arizona. From these collections, Dr. Swetnam and Merrick Richmond have developed a set of maps that compares large fires for 2002 and 2003 with fires in the tree-ring record for 1748 - see the maps here. Their analysis of tree-ring data from 55 forest and woodland sites in Arizona, New Mexico and northern Mexico provides a wildfire chronology for the last 400 years. As noted by Dr. Swetnam and his colleagues, investigating the fire regimes of the United States during pre- and post-Euro-American settlement periods can give important clues to current and future fire activity for the region. It can also help explain current fire behavior, and help inform future management decisions. Fire regimes can be described by creating fire histories: the actual record of fires for a particular geographic area. A variety of techniques can be used to compile fire histories, including building chronologies from fire scarred trees, forest age and stand structure reconstructions using dendrochronology, repeat photographs, historical writings, and early land survey records.
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In the graph to the left, composite fire scar chronologies from 55 forest and woodland sites in Arizona, New Mexico and northern Mexico (AD 1600-Present) reveal how synchronized wildfires have occurred across the Southwest region. (Each site consists of at least four trees and up to 56 trees at some sites, with an average of 19 trees per site.) In the upper chart, each horizontal line represents the composite fire chronology from a different site, and the yellow tick marks are the fire dates recorded by 10% or more fire-scarred trees ( with at least 2 trees showing fire scars ) within that site. The long red tick marks are fire dates recorded by at least 10 sites in the 55-site southwestern network.
As seen in the bottom time series, large, regional fire years were common during the pre-settlement era. Typically, years with wildfires across much of the region are dry years that follow a sequence of one to three wet years. The year 1748 stands out with nearly two-thirds of the sites showing evidence of wildfire, followed by 1851 and 1861 as particularly volatile years. The long periods of time without fire during the 20th century are anomalous for many of the sampled forest types in the region. However, fire severity has increased in many forest types in recent decades, at least in part due to the high forest fuel load resulting from fire suppression starting at the turn of the last century. |
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References:
Grissino-Mayer, Henri D. 1995. The climate and fire history of El Malpais National Monument, New Mexico. Ph.D. dissertation, The University of Arizona, Tucson. 407 pp. Grissino-Mayer, Henri D. 1996. A 2129 year annual reconstruction of precipitation for northwestern New Mexico, USA. In Dean, J.S., Meko, D.M., and Swetnam, T.W., eds., Tree Rings, Environment, and Humanity. Radiocarbon 1996, Department of Geosciences, The University of Arizona, Tucson: 191-204. Grissino-Mayer, Henri D., Swetnam, Thomas W., and Adams, Rex K., in press. The rare, old-aged conifers of the malpais. In Zidek, J., ed., The Natural History of El Malpais. Santa Fe, NM: National Park Service, Southwestern Region. Swetnam, T. W., C. D. Allen, and J. L. Betancourt. 1999. Applied historical ecology: Using the past to manage for the future. Ecological Applications 9(4): 1189-1206. The WDC Paleoclimatology archive contains the El Malpais Precipitation Reconstruction Data and Data Description.
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