DOI: 10.25921/zn2x-m574
title: NOAA/WDS Paleoclimatology - Stahle and Cleaveland 1988 Texas June PDSI Reconstructions

description: A selected group of nine climate-sensitive tree-ring chronologies from old post oak trees are used to reconstruct the June Palmer Drought Severity Index (PDSI) from 1698 to 1980 for two large regions in northern and southern Texas. Analysis of tree growth and monthly climate variables indicate that the June PDSI is the most robust climate signal evident in these chronologies, and principal component analysis (PCA) reveals a north-south geographic pattern in the relationships between the regional tree-ring time series. Serially random amplitude series from the first two significant eigenvectors of tree growth, which explain 65% of the total variance in the tree-ring data, were entered into stepwise multiple regression as predictors of regionally averaged June PDSI in north and south Texas for the common interval 1931–80. The regression models explain 59% and 60% of the variance in north and south Texas June PDSI, respectively, and both reconstructions are well verified against independent June PDSI data available on a statewide basis from 1888 to 1930. The weak persistence present in the observed June PDSI series was added to the serially random tree-ring reconnections prior to verification, using autoregressive modeling procedures. The mean and variance of June PDSI during the 50-yr period of meteorological observation (1931–80) appear to be representative of the last 283 yr, but significant changes in average June PDSI for Texas appear to have occurred over both 30 and ∼90-yr time intervals. Moderate or more severe June droughts (PDSI ≤ −2.0) have an estimated recurrence probability of over 90% each decade, and the risk of extreme June drought (PDSI ≤ −4.0) is estimated at over 50% every 15 yr in north Texas and every 10 yr in south Texas. The reconstructions faithfully reproduce the frequency domain properties of the actual June PDSI, and marginally significant spectral peaks are present at 2.3 yr and between 14 and 18.67 yr in both reconstructions. Significant interannual persistence of June moisture extremes apparent in the statewide June temperature, precipitation, and PDSI data from 1888 to 1982 is also present in both regional reconstructions from 1698 to 1980. The reconstructions indicate that the risk for below average June moisture conditions increases to at least 65% in north and south Texas in the summer following a June drought (PDSI ≤ −2.0). Interannual persistence is also indicated for June wetness anomalies and may have some modest value in statistical forecasts of growing season moisture conditions in Texas.
description: Reconstructed June Palmer Drought Severity Index (PDSI). Each series is an average of 2 Texas climate divisions. North is an average of North Central and Low Rolling Plains. South is an average of South Central and Edwards Plateau. (from T.R. Karl et al. 1983, Statewide Average Climatic History: Texas 1888-1982. Historical Climatology Series 6-1. National Climatic Data Center, Asheville, NC 28801). Based on 9 post oak (Quercus stellata) chronologies. All are archived with the International Tree Ring Data Bank at the World Data Center for Paleoclimatology: 1. Quanah Mtn,OK (34d41mN, 98d38mW); 2. Mud Creek,OK (34d06mN, 97d40mW); 3. Lake Arbuckle,OK (34d26mN, 96d59mW); 4. Nichols Ranch,TX (32d59mN, 99d11mW); 5. Mason Mtn,TX (30d53mN, 99d11mW); 6. Brazos River,TX (30d56mN, 96d48mW); 7. Yegua Creek,TX (30d19mN, 96d38mW); 8.Lavaca River,TX (29d18mN, 96d38mW); 9. Coleto Creek,TX (28d46mN, 97d11mW)