Devils Lake is a Closed Basin Lake (CBL) located in northeast North Dakota, and is a sub basin of the Red River of the North drainage system. It is a CBL in that, although it lies within the Red River drainage system, no water has naturally left the Devils Lake Basin in recorded history (since the 1830s). Instead, the basin\u27s surface runoff flows through many small coulees (streams) and lakes and is collected by Devils Lake or Stump Lake (located to the east of Devils Lake). There it remains until it evaporates, enters the groundwater, or overflows naturally into the Red River via Stump Lake and the Sheyenne River. The natural state of Devils Lake is one of fluctuation. There is no “normal” lake level or natural footprint for it to occup...
Devils Lake is nominally part of the Hudson Bay basin (Figure 1), but is located in a closed sub-bas...
Evaluation of current climatic trends and reconstruction of paleoclimatic conditions for Devils Lake...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/94725/1/eost16649.pd
The Devils Lake Basin is a 3,810- square-mile subbasin (fig. 1) in the Red River of the North Basin....
The Devils Lake, North Dakota, region has experienced a dramatic wet cycle since 1992 that has cause...
Proxy variables from palaeolimnological studies of lakes in the Prairie Pothole Region of North Amer...
Devils Lake, a terminal saline lake in eastern North Dakota, has experienced catastrophic flooding o...
The views expressed in this report are those of the authors and not necessarily those of the Natural...
Devils Lake, a terminal, saline lake in North Dakota has experienced a 24~ foot rise in lake elevat...
Since the spring of 1993, the water surface elevation at Devils Lake, a terminal lake in eastern Nor...
From the Executive Summary: The closed basins area, which includes parts of Day, Marshall, Roberts, ...
Interbasin water transfers present particular environmental risks. Concerns over invasive species an...
Devils Lake is a terminal lake located in northeast North Dakota. Because of its glacial origin and ...
Background Water level fluctuations in endorheic lakes are highly susceptible to even slight changes...
The Devils Lake Basin is a sub-basin of the larger Red River Basin located in east-central North Dak...
Devils Lake is nominally part of the Hudson Bay basin (Figure 1), but is located in a closed sub-bas...
Evaluation of current climatic trends and reconstruction of paleoclimatic conditions for Devils Lake...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/94725/1/eost16649.pd
The Devils Lake Basin is a 3,810- square-mile subbasin (fig. 1) in the Red River of the North Basin....
The Devils Lake, North Dakota, region has experienced a dramatic wet cycle since 1992 that has cause...
Proxy variables from palaeolimnological studies of lakes in the Prairie Pothole Region of North Amer...
Devils Lake, a terminal saline lake in eastern North Dakota, has experienced catastrophic flooding o...
The views expressed in this report are those of the authors and not necessarily those of the Natural...
Devils Lake, a terminal, saline lake in North Dakota has experienced a 24~ foot rise in lake elevat...
Since the spring of 1993, the water surface elevation at Devils Lake, a terminal lake in eastern Nor...
From the Executive Summary: The closed basins area, which includes parts of Day, Marshall, Roberts, ...
Interbasin water transfers present particular environmental risks. Concerns over invasive species an...
Devils Lake is a terminal lake located in northeast North Dakota. Because of its glacial origin and ...
Background Water level fluctuations in endorheic lakes are highly susceptible to even slight changes...
The Devils Lake Basin is a sub-basin of the larger Red River Basin located in east-central North Dak...
Devils Lake is nominally part of the Hudson Bay basin (Figure 1), but is located in a closed sub-bas...
Evaluation of current climatic trends and reconstruction of paleoclimatic conditions for Devils Lake...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/94725/1/eost16649.pd