Little River Experimental Watershed, a keystone in understanding of coastal plain watersheds. Issue 8 (23rd August 2021)

• Record Type: Journal Article
• Authors: Bosch, David D.; Coffin, Alisa W.; Sheridan, Joseph; Pisani, Oliva; Endale, Dinku M.; Strickland, Tim C.
• Is Part Of: Hydrological processes. Volume 35:Issue 8(2021)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2021-08-23
• Subjects: agriculture -- rainfall‐runoff response -- southeastern plains -- streamflow -- watersheds; Hydrology -- Periodicals; Hydrology -- Research -- Periodicals; Hydrologic models -- Periodicals; Hydrological forecasting -- Periodicals; 631.432
• DOI: 10.1002/hyp.14334
• Languages: English
• ISSNs: 0885-6087

Abstract

Abstract: The US Department of Agriculture‐Agricultural Research Service Southeast Watershed Research Laboratory (SEWRL) initiated a hydrologic research program on the Little River Experimental Watershed (LREW) in 1967. Long‐term (52 years) streamflow data are available for nine sites, including rainfall‐runoff relationships and hydrograph characteristics regularly used in research on interactive effects of climate, vegetation, soils, and land‐use in low‐gradient streams of the US EPA Level III Southeastern Plains ecoregion. A summary of prior research on the LREW illustrates the impact of the watershed on building a regional understanding of hydrology and water quality. Climatic and streamflow data were used to make comparisons of scale across the nine nested LREW watersheds (LRB, LRF, LRI, LRJ, LRK, LRO, LRN, LRM, and LRO3) and two regional watersheds (Alapaha and Little River at Adel). Annual rainfall for the largest LREW, LRB, was 1200 mm while average annual streamflow was 320 mm. Annual rainfall, streamflow, and the ratio between annual streamflow and rainfall (Sratio) were similar ( α = 0.05) across LREWs LRB, LRF, LRI, LRJ, LRK, and LRO. While annual rainfall within the 275 ha LRO3 was found to be similar to LRO and LRM ( α = 0.05), annual streamflow and Sratio were significantly different ( α = 0.05). Comparisons of annual rainfall, streamflow, and Sratio between LRB and the regional watersheds indicated no differences ( α = 0.05). Based upon this analysis, most regional watersheds shared similar hydrologic characteristics. LRO3 was an exception, where increases in row crops and decreases in forest coverage resulted in increased streamflow. LREW data have been instrumental in building considerable scientific understanding of flow and transport processes for these stream systems. Continued operation of the LREW hydrologic network will support hydrologic research as well as environmental quality and riparian research programs that address emerging and high priority natural resource and environmental issues. Abstract : Long‐term (52 years) of streamflow data are currently available for nine flow measurement sites in the US EPA Level III Southeastern Plains ecoregion. Hydrologic comparisons across several regional watersheds indicated few differences. Differences found for a smaller nested watershed indicate significant changes in crop and forest coverage can alter long‐term hydrologic characteristics.