The western Sandhills of Nebraska contain many shallow lakes and wetlands that interact strongly with groundwater and the overlying atmosphere. The region is semi-arid, and most of the lakes are saline, supporting a wide range of ecosystems. Water levels and salt concentrations are highly sensitive to variations in precipitation, evaporation, and groundwater fluxes, making the Sandhills an excellent laboratory for examining the effects of climate on the water balance of interdunal lakes. In this study, we investigate the atmospheric controls on evaporation rates, as well as the water balance of Alkali Lake, one of the more saline lakes in the western Sandhills. The Bowen ratio energy balance and mass-transfer methods are applied over a thre...
The Great Salt Lake is a closed basin lake in which level and volume fluctuate due to differences be...
Lakes are integral parts of groundwater flow systems in many environments. Yet, few exceptions exist...
Reliable evaporation data are an essential requirement in any water and/or energy budget studies. Th...
Despite potential evaporation rates in excess of the local precipitation, dry climates often support...
Interaction between surface water and groundwater is an important component of the water cycle that ...
Interaction between surface water and groundwater is an important component of the water cycle that ...
Between the Platte and Niobrara Rivers in western and central Nebraska lie over 25,000 square kilome...
The Sand Hills of Nebraska are typified by dunes separated by broad valleys, many of which contain l...
Evapotranspiration (ET) is an important component of the water and energy balance, yet it is also on...
Study Region: The Nebraska Sand Hills consisting of four major land cover types: (1) lakes and wetla...
Study region: The Nebraska Sand Hills (NSH) lies in the western part of Nebraska, United States. We ...
Analyzing the dynamic hydrologic conditions of the Sandhills is critical for water and range managem...
Freshwater and hypersaline lakes in arid and semi-arid environments are crucial from agricultural, i...
The Great Salt Lake is a closed basin lake in which level and volume fluctuate due to differences be...
Lakes are integral parts of groundwater flow systems in many environments. Yet, few exceptions exist...
Reliable evaporation data are an essential requirement in any water and/or energy budget studies. Th...
Despite potential evaporation rates in excess of the local precipitation, dry climates often support...
Interaction between surface water and groundwater is an important component of the water cycle that ...
Interaction between surface water and groundwater is an important component of the water cycle that ...
Between the Platte and Niobrara Rivers in western and central Nebraska lie over 25,000 square kilome...
The Sand Hills of Nebraska are typified by dunes separated by broad valleys, many of which contain l...
Evapotranspiration (ET) is an important component of the water and energy balance, yet it is also on...
Study Region: The Nebraska Sand Hills consisting of four major land cover types: (1) lakes and wetla...
Study region: The Nebraska Sand Hills (NSH) lies in the western part of Nebraska, United States. We ...
Analyzing the dynamic hydrologic conditions of the Sandhills is critical for water and range managem...
Freshwater and hypersaline lakes in arid and semi-arid environments are crucial from agricultural, i...
The Great Salt Lake is a closed basin lake in which level and volume fluctuate due to differences be...
Lakes are integral parts of groundwater flow systems in many environments. Yet, few exceptions exist...
Reliable evaporation data are an essential requirement in any water and/or energy budget studies. Th...