Devils Lake, a terminal saline lake in eastern North Dakota, has experienced catastrophic flooding over the past two decades producing direct damages in excess of $1 billion ($USD). We use three long-term datasets to examine the temporal coherence between historical lake fluctuations and basic hydroclimatic drivers. Monthly precipitation and mean monthly air temperature data are used to characterize long-term precipitation delivery and evaporative demand. Monthly water balance data for a representative location are used to assess basin soil moisture conditions. A lake volume time series documents lake volume fluctuation in response to long-term precipitation and regional soil moisture conditions. Three variables are derived from the dataset...
Devils Lake, a terminal, saline lake in North Dakota has experienced a 24~ foot rise in lake elevat...
Varved sediments from a lake near the present forest-prairie border in northwestern Minnesota provid...
This paper analyzes the effects of geology and geomorphology on surface-water/-groundwater interacti...
Proxy variables from palaeolimnological studies of lakes in the Prairie Pothole Region of North Amer...
Since the spring of 1993, the water surface elevation at Devils Lake, a terminal lake in eastern Nor...
Reconstructions of lake-water salinity at decadal resolution for the last 2,000 years are compared a...
Devils Lake is a Closed Basin Lake (CBL) located in northeast North Dakota, and is a sub basin of th...
Diatom assemblages preserved in sediment cores from closed-basin lakes can provide high-resolution r...
The Devils Lake Basin is a 3,810- square-mile subbasin (fig. 1) in the Red River of the North Basin....
Six high-resolution climatic reconstructions, based on diatom analyses from lake sediment cores from...
Evaluation of current climatic trends and reconstruction of paleoclimatic conditions for Devils Lake...
The Devils Lake Basin is a sub-basin of the larger Red River Basin located in east-central North Dak...
During the AD 1990s the Waubay Lakes complex in eastern South Dakota experienced historically unprec...
High-resolution paleohydrological reconstructions were carried out in five shallow lakes in the Nebr...
Estimates of past lake-water salinity from fossil diatom assemblages were used to infer past climati...
Devils Lake, a terminal, saline lake in North Dakota has experienced a 24~ foot rise in lake elevat...
Varved sediments from a lake near the present forest-prairie border in northwestern Minnesota provid...
This paper analyzes the effects of geology and geomorphology on surface-water/-groundwater interacti...
Proxy variables from palaeolimnological studies of lakes in the Prairie Pothole Region of North Amer...
Since the spring of 1993, the water surface elevation at Devils Lake, a terminal lake in eastern Nor...
Reconstructions of lake-water salinity at decadal resolution for the last 2,000 years are compared a...
Devils Lake is a Closed Basin Lake (CBL) located in northeast North Dakota, and is a sub basin of th...
Diatom assemblages preserved in sediment cores from closed-basin lakes can provide high-resolution r...
The Devils Lake Basin is a 3,810- square-mile subbasin (fig. 1) in the Red River of the North Basin....
Six high-resolution climatic reconstructions, based on diatom analyses from lake sediment cores from...
Evaluation of current climatic trends and reconstruction of paleoclimatic conditions for Devils Lake...
The Devils Lake Basin is a sub-basin of the larger Red River Basin located in east-central North Dak...
During the AD 1990s the Waubay Lakes complex in eastern South Dakota experienced historically unprec...
High-resolution paleohydrological reconstructions were carried out in five shallow lakes in the Nebr...
Estimates of past lake-water salinity from fossil diatom assemblages were used to infer past climati...
Devils Lake, a terminal, saline lake in North Dakota has experienced a 24~ foot rise in lake elevat...
Varved sediments from a lake near the present forest-prairie border in northwestern Minnesota provid...
This paper analyzes the effects of geology and geomorphology on surface-water/-groundwater interacti...