NOAA Paleoclimatology Program, NCDC Paleoclimatology Branch

CA Streamflow Home - Background - Chronologies - Reconstructions - Case Study - Resources

Streamflow Reconstructions

A tree-ring reconstruction of streamflow or other hydroclimatic variable is developed by calibrating a set of tree-ring chronologies with a gage record to extend that record into the past. See the Background and Case Study pages for more information about the reconstruction process.

Several reconstructions have been developed for California watersheds since 2000. To access the reconstruction data, click on a gage name in the list below or go to the Gage Map.

For other reconstructions of streamflow and climate for California and the surrounding region, click here.

For reconstructions of streamflow for the Colorado River basin, click here.

Sacramento Basin
Sacramento River - Four Rivers Index (annual streamflow) - sum of the following gages: Sacramento River at Bend Bridge; Feather River inflow to Lake Oroville; Yuba River at Smartville; American River inflow to Folsom Lake

Feather River inflow to Lake Oroville (annual streamflow)

San Francisco Bay
San Francisco Bay Salinity

Salinas Basin
Salinas River at Paso Robles (annual streamflow)

Gage Map - Click on gage names in blue to access reconstruction data
map showing hydroclimatic reconstructions in California

map showing hydroclimatic reconstructions in California

Other Streamflow and Climate Reconstructions for California

Streamflow Reconstructions

Below are two other notable efforts in the past 20 years to reconstruct streamflow in California.

Sacramento River Basin, 400 years
In the mid-1980s, Christopher Earle and Hal Fritts of the University of Arizona's Laboratory of Tree-Ring Research were funded to develop annual streamflow reconstructions for several gages in the Sacramento basin. This work has been superseded by the more recent reconstructions for the Sacramento basin generated by David Meko and colleagues.

Earle, C.J., 1993. Asynchronous droughts in California streamflow as reconstructed from tree rings. Quaternary Research 39: 290-299.

Los Angeles, San Gabriel, Santa Ana, and San Jacinto Rivers, 300 years
In the early 1990s, Daniel Larson of California State University, Long Beach developed an annual streamflow reconstruction (1670-1961) of the average of five gaged flow records in southern California, on the Los Angeles, San Gabriel, Santa Ana, and San Jacinto Rivers. The reconstruction is based on only one tree-ring chronology, and so is not as robust as other streamflow reconstructions. But this reconstruction indicates the excellent potential for future work in these basins.

Larson, D.O. 1994. California climatic reconstructions. Journal of Interdisciplinary History 25(2): 225-253.

Precipitation Reconstructions

Because precipitation and streamflow are so closely linked, tree-ring reconstructions of precipitation can provide useful information about hydrologic variability. Many precipitation reconstructions have been developed for various parts of California and the surrounding region over the past 20 years. Below are the references in the scientific literature that describe them, roughly ordered from north to south. In a few cases, links to the reconstruction data are provided.

Northern California/Southeastern Oregon, 300 years
Graumlich, L.J. 1987. Precipitation variation in the Pacific Northwest (1675-1975) as reconstructed from tree rings. Annals of the Association of American Geographers 77(1): 19-29.

Central California, 400 years

Michaelsen, J., Haston, L., Davis, F.W. 1987. 400 years of central California precipitation variability reconstructed from tree rings. Water Resources Bulletin 23(5): 809-818.

Central coastal California, 400 years

Haston, L., Michaelsen, J. 1994. Long-term central coastal California precipitation variability and relationships to El Nino-Southern Oscillation. Journal of Climate 7: 1373-1387.

Central California (Sierra Nevada), 1000 years

Graumlich, L.J. 1993. A 1000-year record of temperature and precipitation in the Sierra Nevada. Quaternary Research 39(2): 249-255.

Central California (Sierra Nevada), 2000 years

Swetnam, T.W. 1993. Fire history and climate change in giant sequoia groves. Science 262: 885-889.

Central Coastal California, 160 years

Biondi, F., Cayan, D.R., Berger, W.H. 1997. Dendroclimatology of Torrey pine (Pinus torreyana Parry ex Carr.). American Midland Naturalist 138: 237-251.

Central and Southern California (Sierra Nevada; San Joaquin basin), 1000 years

Graybill, D.A., Funkhouser, G.S. 1999. Dendroclimatic reconstructions during the past millennium in the southern Sierra Nevada and Owens Valley, California.
In: M.R. Rose and P.E. Wigand, eds., Proceedings of the Southern California Climate Symposium: Trends and Extremes of the Past 2000 Years. Natural History Museum of Los Angeles County, Technical Report: 239-269.

Eastern California/Western Nevada (Walker River basin), 2300 years

Biondi, F., Kozubowski, T.J., Panorska, A.K. 2005. A new model for quantifying climate episodes. International Journal of Climatology 25(9): 1253-1264.

South-central California, 300 years

Gervais, B.R. 2006. A three-century record of precipitation and blue oak recruitment from the Tehachapi Mountains, Southern California, USA. Dendrochronologia 24(1): 29-37.

Southern California, 400 years

Haston, L., Michaelsen, J. 1997. Spatial and temporal variability of Southern California precipitation over the last 400 yr and relationships to atmospheric circulation patterns. Journal of Climate 10(8): 1836-1852.

Southwest Nevada (Division 3), 8000 years

Hughes, M.K., Graumlich, L.J. 1996. Multimillennial dendroclimatic studies from the western United States.
In: P.D. Jones, R.S. Bradley, and J. Jouzel, eds., Climatic Variations and Forcing Mechanisms of the Last 2000 Years. NATO ASI Series I41: 109-124.
Link to data

Arizona (all 7 climate divisions) and New Mexico (all 8 climate divisions), 1000 years

Ni, F.B., Cavazos, T., Hughes, M.K., Comrie, A.C., Funkhouser, G. 2002. Cool-season precipitation in the southwestern USA since AD 1000: Comparison of linear and nonlinear techniques for reconstruction. International Journal of Climatology 22(13): 1645-1662.
Link to data

Reconstructions of Hydrologic Drought from Relict Trees
Scott Stine of California State University, Hayward has used carbon-dating (not tree-ring cross-dating) of relict stumps rooted in modern lakes, rivers, and marshes in the Sierra Nevada to infer the occurrence of two extraordinary century-long regional droughts, in ~AD 900-1110 and ~AD 1210 to 1350. The timing of these droughts correspond well to drier periods seen in the longer precipitation reconstructions (e.g., Graumlich 1993) listed above, but the magnitude of the droughts suggested by the presence of stumps rooted up to 70 feet below the current lake surface far exceeds those indicated by the tree-ring reconstructions.

Stine, S. 1994. Extreme and persistent drought in California and Patagonia during mediaeval time. Nature 369:546–49.

Stine, S. 1998. “A Medieval Climatic Anomaly in the Americas,” in Water, environment, and society in times of climatic change. Edited by A. Issar and N. Brown. Dordrecht and Boston: Kluwer Academic.

Streamflow Reconstructions for the Colorado River basin

Among the seven basin states, California receives the largest apportionment of water from the Colorado River mainstem, and this water represents about 10% of all water used in California. So the hydrologic variability of the Colorado River is of great concern to many California water providers.

The first reconstructions of streamflow of streamflow using modern techniques were done for the Colorado River at Lees Ferry, and other basin gages, by Charles Stockton and Gordon Jacoby in 1976. Their reconstruction of Lees Ferry demonstrated that the period in the early 1900s on which the Colorado River Compact was based was anomalously wet in the context of the past 400 years, and a severe and persistent drought in the late 1500s was far worse than any in the 1900s.

Stockton, C.W. and G.C. Jacoby, 1976. Long-term surface water supply and streamflow levels in the upper Colorado River basin. Lake Powell Research Project Bulletin No. 18, Inst. of Geophysics and Planetary Physics, University of California, Los Angeles, 70 pp.
Link to data

In 2005, Connie Woodhouse, Steve Gray, and David Meko used a new network of tree-ring chronologies to generate new reconstructions of annual streamflow for the Colorado River at Lees Ferry and nine other basin gages. These reconstructions, being based on a longer calibration period, are more robust than the Stockton and Jacoby work, but show very similar variability.

Woodhouse, C.A., S.T. Gray, and D.M. Meko. 2006. Updated streamflow reconstructions for the Upper Colorado River basin. Water Resources Research 42(5): W0541.5
Link to data


http://www.ncdc.noaa.gov/paleo/streamflow/ca/reconstructions.html Downloaded Sunday, 06-Jul-2008 18:13:36 EDT Last Updated Monday, 04-Dec-2006 19:20:14 EST by paleo@noaa.gov Please see the Paleoclimatology Contact Page or the NCDC Contact Page if you have questions or comments.