1200 years of Upper Missouri River streamflow reconstructed from tree rings. (15th November 2019)

• Record Type: Journal Article
• Authors: Martin, Justin T.; Pederson, Gregory T.; Woodhouse, Connie A.; Cook, Edward R.; McCabe, Gregory J.; Wise, Erika K.; Erger, Patrick; Dolan, Larry; McGuire, Marketa; Gangopadhyay, Subhrendu; Chase, Katherine; Littell, Jeremy S.; Gray, Stephen T.; George, Scott St.; Friedman, Jonathan; Sauchyn, Dave; Jacques, Jeannine St.; King, John
• Is Part Of: Quaternary science reviews. Volume 224(2019)
• Publication Date: 2019-11-15
• Subjects: Holocene -- Paleoclimatology -- North America -- Tree-rings -- Streamflow -- Upper Missouri River -- Reconstruction; Geology, Stratigraphic -- Quaternary -- Periodicals; Stratigraphie -- Quaternaire -- Périodiques; 551.79
• DOI: 10.1016/j.quascirev.2019.105971
• Languages: English
• ISSNs: 0277-3791

Abstract

Abstract: Paleohydrologic records can provide unique, long-term perspectives on streamflow variability and hydroclimate for use in water resource planning. Such long-term records can also play a key role in placing both present day events and projected future conditions into a broader context than that offered by instrumental observations. However, relative to other major river basins across the western United States, a paucity of streamflow reconstructions has to date prevented the full application of such paleohydrologic information in the Upper Missouri River Basin. Here we utilize a set of naturalized streamflow records for the Upper Missouri and an expanded network of tree-ring records to reconstruct streamflow at thirty-one gaging locations across the major headwaters of the basin. The reconstructions explain an average of 68% of the variability in the observed streamflow records and extend available records of streamflow back to 886 CE on average. Basin-wide analyses suggest unprecedented hydroclimatic variability over the region during the Medieval period, similar to that observed in the Upper Colorado River Basin, and show considerable synchrony of persistent wet-dry phasing with the Colorado River over the last 1200 years. Streamflow estimates in individual sub-basins of the Upper Missouri demonstrate increased spatial variability in discharge during the Little Ice Age (∼1400–1850 CE) compared with the Medieval Climate Anomaly (∼800–1400 CE). The network of streamflow reconstructions presented here fills a major geographical void in paleohydrologic understanding and now allows for a long-term assessment of hydrological variability over the majority of the western U.S. Highlights: Upper Missouri River streamflow is reconstructed using tree-rings. Persistent wet-dry cycles in the Upper Missouri track those in the Upper Colorado. Medieval, Little Ice Age, and 20th century streamflow variability differed.