scholarly journals Changes in streamflow and summary of major-ion chemistry and loads in the North Fork Red River basin upstream from Lake Altus, northwestern Texas and western Oklahoma, 1945-1999

2003 ◽  
Keyword(s):  
River Basin ◽  
Red River ◽  
Ion Chemistry ◽  
Major Ion Chemistry ◽  
Major Ion ◽  
The North ◽  
North Fork ◽  
Red River Basin

Hydroclimatic Change in Southern Manitoba Since A.D. 1409 Inferred from Tree Rings

2002 ◽  
Vol 58 (2) ◽  
pp. 103-111 ◽  
Author(s):  
Scott St. George ◽  
Erik Nielsen
Keyword(s):  
River Basin ◽  
Great Plains ◽  
Red River ◽  
Tree Ring Chronology ◽  
Quercus Macrocarpa ◽  
The North ◽  
Red River Basin ◽  
Bur Oak ◽  
Dry Conditions ◽  
Hydroclimatic Change

AbstractA record of estimated annual (prior August to current July) precipitation derived from a regional bur oak (Quercus macrocarpa Michx.) tree-ring chronology indicates that southern Manitoba's hydroclimate has been relatively stable over the last 200 yr. Although this stability was interrupted briefly by pronounced wet intervals in the late A.D. 1820s and 1850s, hydroclimatic conditions since permanent Euro-Canadian settlement were much less variable and persistent than those prior to A.D. 1790. The reconstruction indicates that the Red River basin experienced extremely dry conditions between A.D. 1670 and 1775, with below-normal precipitation occurring approximately 2 years out of 3. Annual precipitation was estimated at more than two standard deviations below the mean during A.D. 1477, 1485, 1556, 1595, 1612, 1644, 1661, 1743, 1900, and 1980. Comparisons with limnological records from North Dakota and Minnesota suggest that multidecadal fluctuations in regional hydroclimate have been remarkably coherent across the northeastern Great Plains during the last 600 yr. However, individual dry years in the Red River basin were usually associated with larger scale drought across much of the North American interior.

scholarly journals Mothers’ Concerns about Children’s Exposure to Pesticide Drift in the Red River Basin of the North: A Novel Application of Photovoice

2012 ◽  
Vol 12 (2) ◽  
pp. 88-101 ◽  
Author(s):  
Maggie Stedman-Smith ◽  
Patricia McGovern ◽  
Cynthia Peden-McAlpine ◽  
Linda Kingery ◽  
Kathryn Draeger
Keyword(s):  
River Basin ◽  
Red River ◽  
The North ◽  
Red River Basin ◽  
Pesticide Drift ◽  
Children’S Exposure

Major ion chemistry, weathering processes and water quality assessment in upper catchment of Damodar River basin, India

2007 ◽  
Vol 54 (4) ◽  
pp. 745-758 ◽  
Author(s):  
Abhay Kumar Singh ◽  
G. C. Mondal ◽  
Suresh Kumar ◽  
T. B. Singh ◽  
B. K. Tewary ◽  
...  
Keyword(s):  
Water Quality ◽  
Quality Assessment ◽  
River Basin ◽  
Water Quality Assessment ◽  
Ion Chemistry ◽  
Major Ion Chemistry ◽  
Major Ion ◽  
Weathering Processes ◽  
Damodar River ◽  
Damodar River Basin

scholarly journals The Middle Caddoan Period in the Lower Sulphur River Area

1997 ◽  
Author(s):  
Maynard B. Cliff
Keyword(s):  
River Basin ◽  
Cultural Development ◽  
Red River ◽  
White Oak ◽  
Cultural Constructs ◽  
The North ◽  
Current Usage ◽  
Red River Basin ◽  
Management Area ◽  
Eastern Edge

For purposes of this review, the Lower Sulphur River in Texas includes the area of the Sulphur River basin from the Arkansas border to the eastern edge of Titus County, and encompasses the area of what is today Wright Patman Lake and the White Oak Creek Wildlife Management Area. Traditionally, the Lower Sulphur River area has been tied to cultural constructs defined in the Red River basin, to the north and east. In his ambitious overview of the Caddoan Culture Area, Don Wyckoff generally placed the Lower Sulphur River area with the cultures of the Great Bend. As defined by current usage in Texas, the Middle Caddoan period dates from A.D. 1200 to A.D. 1400, but it is actually the middle portion of a long period of indigenous Caddoan cultural development, which began anywhere from A.D. 800 to 1000 and lasted until after the arrival of the Europeans. Several researchers have suggested that the strongest (and possibly the only) evidence for continuity from the Early Caddoan period to the Late Caddoan period can be found in the area of the Great Bend of the Red River.

Photovoice in the Red River Basin of the North

2011 ◽  
Vol 13 (5) ◽  
pp. 599-607 ◽  
Author(s):  
Maggie Stedman-Smith ◽  
Patricia M. McGovern ◽  
Cynthia J. Peden-McAlpine ◽  
Linda R. Kingery ◽  
Kathryn J. Draeger
Keyword(s):  
River Basin ◽  
Red River ◽  
The North ◽  
Red River Basin

Cultural Exchange in the Red River Basin

2008 ◽  
Vol 49 (3) ◽  
pp. 4-5
Author(s):  
Siobhán M Mattison
Keyword(s):  
River Basin ◽  
Cultural Exchange ◽  
Red River ◽  
Red River Basin
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