A 963-year reconstruction of summer (JJA) stream flow in the White River, Arkansas, USA, from tree-rings
Bibliographic Data
| ID | 12265237 |
|---|---|
| Authors | Malcolm K Cleaveland (University of Arkansas at Fayetteville, corresponding author) |
| Year | 2000 |
| Volume | 10 |
| Issue | 1 |
| Pages | 33-41 |
| Publication date | 2000-01-01 |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | The Holocene (JOURNAL) |
| Journal identifiers | ISSN: 0959-6836 • E-ISSN: 1477-0911 |
| Publisher | SAGE Publishing (PUBLISHER • US) |
| DOI | 10.1191/095968300666157027 |
| OpenAlex | W1999324263 |
| Language | EN |
| Citations received | 8 |
| References cited | 22 |
An average of three baldcypress ( Taxodium distichum) ring-width chronologies was used to recon struct total summer (JJA) mean daily flow of the White River at Clarendon, Arkansas, for years 1023–1985. A quadratic transformation of the tree-ring data accounted for 68% (R 2 adjusted for degrees of freedom lost) when regressed against total summer flow 1931–1985. The distribution of the quadratic reconstruction matched the gauged distribution much better than a simple linear model which only accounted for 62% of the variance. The model was validated by comparing regression estimates against independent data. Years with summer flow below the 25th percentile occur nonrandomly, i.e., they tend to cluster, in both the reconstructed and gauged data. Hydrologic regimes have apparently varied considerably in the past on annual to century time-scales, with extended dry and wet periods that exceeded anything in the modern record. The frequency of both wet and dry extremes has varied considerably over the last millennium. The eleventh through thirteenth cen turies were not analysed due to reduced replication, but the well-replicated fourteenth and twentieth centuries both have large numbers of extremes. The twentieth century appears to have more extreme low flows than the previous centuries and also to have a large number of high flows. The practical consequences for society of variation in extremes and persistence of low flows may be considerable. Climatic change or anthropogenic changes to the watershed (e.g., widespread upland clearing for agriculture and logging of bottomland forests) may be responsible for the change in hydrologic regime during the twentieth century
Archaeology · Cartography · Climatology · Dendrochronology · Dendroclimatology · Drainage basin · Flood myth · Geography · Hydrology (agriculture · Physical geography · Streamflow · Watershed · Environmental Science · Hydrology and Sediment Transport Processes · Plant Water Relations and Carbon Dynamics · Tree-ring climate responses · Geology
The Potential to Reconstruct Manasi River Streamflow in the Northern Tien Shan Mountains (NW China)
Multi-millennial streamflow dynamics in two forested watersheds on Vancouver Island, Canada
Annual climate variability in the Holocene
Using dendroclimatic analysis of exotic deciduous conifers in an arboretum to document tree growth in response to climate change, Northeast Ohio, USA
Baldcypress false ring formation linked to summer hydroclimatic extremes in the southeastern United States
Tree-ring based streamfiow reconstruction for Ashley Creek, northeastern Utah
Palaeoflood records for the Red River, Manitoba, Canada, derived from anatomical tree-ring signatures
Modelling river discharge and precipitation from estuarine salinity in the northern Chesapeake Bay
| Citations per year | 0.31 |
|---|---|
| Citation span | 2000 - 2026 (27) |
| Highly cited | No |