The University of Arizona

AZ Climate Division 7 | CLIMAS

AZ Climate Division 7

Single-Year Reconstruction and Extremes

The graph below shows the cool season (November-April) precipitation reconstruction for Arizona climate division 7. Values are expressed as a percentage of 1000-1988 average precipitation. The adjusted 2006 and 1959 averages, the two driest years during the dry periods of the 1950s and 2000s, are plotted in orange and red, respectively, for comparison. As the reconstruction shows, many years in the past thousand years were drier than 2006.

R2 = 44%

View calibration/verification data

Reconstructed Average (1000-1988) = 125 mm

Instrumental Average (1896-2010) = 128 mm


Driest Year Wettest Year
Year Precipitation (mm) Percent Average Year Precipitaton (mm) Percent Average
1664 9.2 7.3 1816 261.0 208.5
1668 10.6 8.5 1840 259.0 206.9
1670 11.0 8.8 1200 249.5 199.2
1218 17.2 13.7 1618 248.0 198.1
1150 17.2 13.7 1839 245.5 196.1

Multi-Year Reconstructions and Extremes

The graph below shows the five-year average precipitation reconstruction for Arizona climate division 7; values are expressed as a percentage of 1000-1988 average precipitation. The adjusted 1955-1959 and 1999-2003 averages for this climate division are provided for comparison (orange and red lines, respectively). Several extended dry periods stand out, particularly the late 1000s-early 1100s, late 1200s, early 1300s, late 1500s, late-1700s, and the mid-1900s.


   R2 = 44%
View calibration/verification data

5-Year Reconstructed Average (1000-1988) = 125 mm/yr; 626 mm/5-yr

5-Year Instrumental Average (1896-2010) = 128 mm/yr; 644 mm/5-yr

Driest Five-year Period Wettest Five-year Period
Years Precipitation (mm) Percent Average Years Precipitation (mm) Percent Average
1664-1668 232.0 37.1 1837-1841 1138.4 182.0
1214-1218 295.8 47.3 1330-1334 1122.4 179.4
1778-1782 304.2 48.6 1813-1816 1046.2 167.2
1250-1254 307.5 49.2 1336-1340 1000.3 159.9
1147-1151 322.5 51.6 1200-1204 985.5 157.5


Instrumental Record and Extremes

Precipitation was below average for climate division 7 (21.0%) in 2006, making it one of the driest years in the instrumental record. Based on five-year precipitation averages, 2001-2005 was one of the driest spells in the historical record for this climate division.

Driest One-Year Period Wettest One-Year Period
    Year      Precipitation (mm) Percent Average      Year      Precipitation (mm) Percent Average
1904 15.2 11.9 1905 311.9 243.2
2006 26.9 21.0 1979 309.6 241.4
2000 32.5 25.3 1993 284.0 221.4
1921 34.0 26.5 1983 279.4 218.0
1971 43.7 34.1 1966 270.3 210.7
Driest Five-Year Period Wettest Five-Year Period
Year Precipitation (mm) Percent Average Year Precipitation (mm) Percent Average
1902-1906 374.1 58.1 1993-1997 1111.5 172.5
2001-2005 392.4 60.9 1981-1985 980.2 152.1
1900-1904 420.4 65.3 1985-1989 973.6 151.1
1948-1952 421.4 65.4 1994-1998 972.6 151.0
1945-1949 427.0 66.3 1907-1911 968.5 150.3

Calibration and Verification Data

The graph below shows a comparison between instrumental and reconstructed November-April precipitation for Arizona climate division 7. The graph shows good agreement between the tree-ring and instrumental records over most of the 20th century. The R2, in this case 44%, indicates the amount of variation in the instrumental precipitation record captured by tree rings. Higher R2 values indicate more reliable reconstructions.

How the Data Were Calculated

The 1000-year reconstruction of cool-season precipitation is presented as the combined neural network and linear regression reconstructions. The two separate reconstructions were combined in the following manner. If both the linear regression and neural network reconstructions were below the calibration in any given year, then the linear regression value was used. In all other instances, a simple average of the two reconstructions was used. The rationale for this approach is based on detailed analyses and the simple observation that the linear regression does a better job at capturing the drought years. The reconstructions for each division were “smoothed” using a centered 5-year running average.

These reconstructions were developed using millimeters as the measurement unit. However, it is sometimes easier to think of precipitation in terms of the percentage of the long term average. To convert these data to percentage of average each reconstructed value was simply divided by the average of the reconstruction. The same procedure was used to convert instrumental precipitation.

The threshold line for the most recent drought period was calculated by first determining the percentage of average precipitation received during the year or averaged over the last five years, then dividing by the long term averages. In the case of the five-year smoothed reconstructions the average is based on five year averages over the 1896-2010 period. Comparison of the most recent drought in the 2000s to the long term average is problematic, however, because these reconstructions only extend through 1988. In addition, tree-ring data do not match the variance contained within the instrumental data so an adjustment is needed to be made in order to make more reasonable comparisons. The 2006 value (or the 5 year average) was first adjusted relative to the 1896-1988 reference period by calculating the percentage of average over the entire period (1896-2010), then determining the value relative to only the common overlap period (1896-1988). For example, Arizona Climate Division 7 recorded 26.9 mm of precipitation in 2006, which is 21.0% of the 1896-2010 average (128 mm). To put this into the context of the tree-ring reconstruction in terms of millimeters of precipitation, this value (21.0% or 0.210) was multiplied by the reconstructed average over the period 1896-1988 (138.0 mm), which yields an adjusted value of 29.0 mm.

A note about dates: while a single year or range of dates is given in the data for simplicity, cool-season precipitation estimates are for November-April. For example data listed for 2002 would actually be from November 2001 to April 2002.