Great Basin


Reconstructions
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Introduction

The Great Basin, despite popular images of unyielding aridity and lack of surface water, has a number of rivers which drain high mountain areas. These rivers support large urban areas such as Salt Lake City and Reno, as well as unique riparian and aquatic ecosystems, like the Great Salt Lake, Bear Lake, and Pyramid Lake. These mountain ranges on the periphery of and within the Great Basin also are home to extensive stands of old and very moisture-sensitive trees—primarily singleleaf pinyon pine, and also bristlecone pine, limber pine, and Douglas-fir.

So far, the great potential for tree-ring reconstructions of streamflow in the Great Basin has gone largely untapped, but that is changing as of the past several years. In the western half of the basin, Franco Biondi of the University of Nevada-Reno and his students have developed dozens of new pinyon chronologies across Nevada to use for paleoclimate reconstructions, and have done preliminary work towards a long reconstruction of flow for the West Walker River. In the northeast part of the basin, Matthew Bekker at Brigham Young University and his students have used new limber pine chronologies to reconstruct seasonal streamflow for streams draining the Wasatch Range into the Great Salt Lake.


A merely old (~1000 years) Great Basin bristlecone pine, in Great Basin National Park, Nevada. The oldest members of this species are over 4500 years old.

Photo courtesy of the National Park Service


Great Basin Streamflow Reconstructions

No reconstructions of annual/water-year streamflow have yet been developed for the Great Basin. Those interested in reconstructions for the western Great Basin and Nevada should contact Franco Biondi; for the Wasatch Front and Utah, contact Matthew Bekker.

Other Hydroclimatic Reconstructions developed for, or including, the Great Basin:

Annual Precipitation, Northeastern Utah, 1226-2001 - Gray et al. 2004

Nevada Climate Division 3 Annual (July-June) Precipitation - Hughes and Graumlich 1996

Summer (JJA) Palmer Drought Severity Index (PDSI), covering most of North America on 2.5-degree grid

 

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Workshops

Two of our technical workshops for water managers and stakeholders have been held within the Great Basin, or locations immediately adjacent to it. These workshops included presentations relevant to the Great Basin. Click on a workshop below to access a summary report and the presentations; see the Treeflow Workshops page for general information about the workshops.

Jeff Lukas (University of Colorado, INSTAAR) presents "Tree-Ring 101" at the Boulder City, NV workshop.

 

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Lahontan Dam and Reservoir on the Carson River, Nevada.

Photo courtesy of the US Bureau of Reclamation

Applications

There are many different ways to use tree-ring reconstructions in the planning and management for water resources, from educational tools to inform stakeholders about the occurrence of severe droughts, to numerical input into water supply models to test the resilience of the system under past hydrologic conditions.

The Southern Nevada Water Authority (SNWA) anticipates using tree-ring data (in the form of precipitation reconstructions in conjunction with groundwater modeling) in a water planning application. Plans for this work were presented by Joseph Leising of SNWA at the Boulder City, NV workshop.

The State of Utah's Drought Plan, revised in 2008, contains a chapter on "Drought from a Paleoclimatic Perspective", based on the gridded summer PDSI reconstructions developed by Cook et al. The quality of the four gridpoint reconstructions within Utah indicates the potential for reconstruction of other hydroclimatic variables, such as annual streamflow.

The TreeFlow Applications page provides summaries of other applications of tree-ring data around the West.

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Great Basin References*

Hydroclimatic reconstructions and analyses

Graham, N. E., and M. K. Hughes. 2007. Reconstructing the medieval Mono Lake low stands. The Holocene, 17, 1197-1210

Gray, S.T., S.T Jackson, and J. L. Betancourt. 2004. Tree-ring based reconstructions of interannual to decadal-scale precipitation variability for northeastern Utah since 1226 AD. Journal of the American Water Resources Association 40 (4), 947–960.

Hardman, G. and O.E. Reil. 1936. The Relationship Between Tree Growth and Stream Runoff in the Truckee River Basin. California-Nevada Bulletin 141, Nevada Agricultural Experiment Station. Reno, Nevada.

Hughes, M.K. and G. Funkhouser. 2003. Frequency-dependent climate signal in upper and lower forest border tree rings in the mountains of the Great Basin. Climatic Change 59: 233-244.

Hughes, M. K. and L. J. Graumlich. 1996. Climatic variations and forcing mechanisms of the last 2000 years. Volume 141. Multi-millenial dendroclimatic studies from the western United States. NATO ASI Series, pp. 109-124.

Saito, L., F. Biondi, J.D. Salas, A.K. Panorska, and T.J. Kozubowski. 2008. A watershed modeling approach to streamflow reconstruction from tree-ring records. Environmental Research Letters 3: 024006; doi:10.1088/1748-9326/3/2/024006 (Abstract)

Smith, W.P. 1986. Reconstruction of precipitation in northeastern Nevada using tree rings, 1600-1982. Journal of Climate and Applied Meteorology 25: 1255-1263.

Solander, K., L. Saito, and F. Biondi. 2010. Streamflow simulation using a water-balance model with annually-resolved inputs. Journal of Hydrology 387: 46–53. (Abstract)

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External Links

University of Nevada-Reno DendroLab (Franco Biondi)

The Big Picture: Combining Watershed Computer Models With Historical Tree-Ring Data

Western Water Assessment (WWA)

Climate Assessment for the Southwest (CLIMAS)

NOAA Regional Integrated Sciences and Assessment Program (RISA)

 

* for additional resources, see the Other Resources page.

 

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