Treesearch

Evapotranspiration (ET) is an essential component of the water balance and a major consumptive use of irrigation water and precipitation on cropland. Any attempt to improve water use efficiency must be based on reliable estimates of ET for irrigation scheduling purposes.

The New York – New Jersey Harbor Estuary is the biggest public space in the nation's largest metropolitan area. Access to its waters – whether for swimming, boating, fishing, or just enjoying the spectacular views – is an amenity that impacts quality of life and drives spending and investments by residents, visitors, and businesses. Park access and use have been positively correlated with physical activity levels and public health. Further, access is critical for fostering a connection with and stewardship of the estuary, especially for young people. For all these reasons, ensuring and...

Over the last several decades, many lakes globally have increased in dissolved organic carbon (DOC), calling into question how lake functions may respond to increasing DOC. Unfortunately, our basis for making predictions is limited to spatial surveys, modeling, and laboratory experiments, which may not accurately capture important whole-ecosystem processes. In this article, we present data on metabolic and physiochemical responses of a multiyear experimental whole-lake increase in DOC concentration. Unexpectedly, we observed an increase in pelagic gross primary production, likely due to a...

We report on the current status of a long-term study of Cerulean Warbler (Setophaga cerulea) response to silviculture on a 58-ha tract in Desha County, Arkansas. The work involved a 10 year premanipulation monitoring of the birds on the tract, followed by implementation of a split plot comparison of alternative treatments, each applied to a randomly selected half of the original plot. We present results of the alternative treatments on warbler species occurrence, distribution and standing crop of canopy and subcanopy trees, and composition and abundance of advanced regeneration resulting...

Evapotranspiration (ET) is the largest watershed water balance component only next to precipitation in the United States. ET is closely coupled with ecosystem carbon and energy fluxes, affects flooding or drought magnitude, and is also a good predictor for biodiversity at a regional scale.Thus, accurately estimating ET is of paramount importance to quantify the effects of land use change and climate change on watershed ecosystem services in water supply, water resources management, carbon sequestration, and biodiversity conservation.

In forested watersheds, changes in climate and forest structure or age can affect water yield; yet few long-term observational records from such watersheds exist that allow an assessment of these impacts over time. In this study, we used long-term (~80 yrs) observational records of climate and water yield in six reference watersheds at the Coweeta Hydrologic Laboratory in the southern Appalachian mountains of North Carolina to determine whether water yield has changed over time, and examine and attribute the causal mechanisms of change.

Drought and resulting water-limiting conditions can result in negative ecological impacts such as reduced plant growth and increased stress that can make plants more vulnerable to threats such as insect infestations. The long-term dataset at Panola Mountain Research Watershed, a small 0.41-hectare forested watershed near Atlanta, Georgia, U.S.A., was used to better quantify the important factors leading to water-limiting conditions.

Hydrology is the driving force of sediment, nutrient, and pesticide movement. Separation of streamflow hydrographs into rapid surface runoff and baseflow can vastly improve our understanding of chemical transport. In addition, characterizing these two components of streamflow can also greatly improve overall watershed hydrologic budgets which are critical for accurate evapotranspiration estimation. For validation of hydrology in model simulations, direct runoff and baseflow components of the streamflow hydrographs typically need to be separated. Incorrect representation of baseflow...

Long-term studies on paired-research catchments have often showed periods of changes to water yields and peak stormflow after forest harvesting. Most studies have focused on wholecatchment or downstream responses. In contrast, few studies have ever been established to measure and investigate specific pathways of water routing through catchment soils or how sub-catchment hydrological flowpaths respond to experimental vegetation manipulations, as well as common metrics of annual water yields and stormflow magnitudes.