SYMPOSIUM ON THE GREAT PLAINS OF NORTH AMERICA. Edited by Carle C. Zimmerman and Seth Russell. Fargo: The North Dakota Institute for Regional Studies, 1968. 222 pp. $4.75

Social Forces ◽  
1969 ◽  
Vol 47 (4) ◽  
pp. 490-491
Author(s):  
S. C. Mayo
Keyword(s):  
North America ◽  
North Dakota ◽  
Great Plains ◽  
Regional Studies ◽  
The North

scholarly journals Pygmy Shrew (Sorex hoyi) in Montana east of the Rocky Mountains with comments on its distribution across the northern Great Plains

2014 ◽  
Vol 128 (2) ◽  
pp. 204
Author(s):  
Paul Hendricks ◽  
Susan Lenard
Keyword(s):  
North Dakota ◽  
Great Plains ◽  
Rocky Mountains ◽  
Riparian Vegetation ◽  
Missouri River ◽  
Northern Great Plains ◽  
Prairie Pothole ◽  
The North ◽  
Pygmy Shrew ◽  
River Bottom

Range maps for Pygmy Shrew (Sorex hoyi) show a large hiatus over much of the northern Great Plains between the Rocky Mountains and eastern North Dakota. We report a new record of the Pygmy Shrew in northeastern Montana, review previous records for the state and adjacent regions bordering Montana to the north and east, and suggest that the range boundary in the northern Great Plains be redrawn farther south to include all of Montana north of the Missouri River. This is consistent with the known range of the Pygmy Shrew in eastern North Dakota and South Dakota, where the species has been documented only north and east of the Missouri River, although records are still lacking from north of the Missouri River in northwestern North Dakota and adjacent regions of Canada. Pygmy Shrews will probably be found at additional localities in prairie regions of Canada adjacent to Montana, most likely in association with prairie pothole wetlands, river bottom riparian vegetation, and hardwood draws.

Stratospheric cirrus clouds related to deep convection over North America observed by satellite measurements

2021 ◽  
Author(s):  
Ling Zou ◽  
Lars Hoffmann ◽  
Sabine Griessbach ◽  
Lunche Wang
Keyword(s):  
North America ◽  
Formation Mechanism ◽  
Great Plains ◽  
Gravity Waves ◽  
North Atlantic ◽  
Deep Convection ◽  
Eastern Pacific ◽  
Western Canada ◽  
The North ◽  
North Eastern

<p>Cirrus clouds in the stratosphere (SCCs) regulate the water vapor budget in the stratosphere, impact the stratosphere and tropopshere exchange, and affect the surface energy balance. But the knowledge of its occurrence and formation mechanism is limited, especially in middle and high latitudes. In this study, we aim to assess the occurrence frequencies of SCC over North America based on The Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) instrument during the years 2006 to 2018. Possible driving forces such as deep convection are assessed based on Atmospheric Infrared Sounder (AIRS) observations during the same time. </p><p>Results show that at nighttime, SCCs are most frequently observed during the thunderstorm season over the Great Plains from May to August (MJJA) with maximum occurrence frequency of 6.2%. During the months from November to February (NDJF), the highest SCCs occurrence frequencies are 5.5% over the North-Eastern Pacific, western Canada and 4.4% over the western North Atlantic. Occurrence frequencies of deep convection and strong storm systems from AIRS show similar hotspots like the SCCs, with highest occurrence frequencies being observed over the Great Plains in MJJA (4.4%) and over the North-Eastern Pacific, western Canada and the western North Atlantic in NDJF (~2.5%). Both, seasonal patterns and daily time series of SCCs and deep convection show a high degree of spatial and temporal correlation. As further analysis indicates that the maximum fraction of SCCs generated by deep convection is 74% over the Great Plains in MJJA and about 50% over the western North Atlantic, the North-Eastern Pacific and western Canada in NDJF, we conclude that, locally and regionally, deep convection is a leading factor for the formation of SCCs over North America. Other studies stressed the relevance of isentropic transport, double tropopause events, or gravity waves for the formation of SCCs. </p><p>In this study, we also analyzed the impact of gravity waves as a secondary formation mechanism for SCCs, as the Great Plains is a well-known hotspot for stratospheric gravity waves. In case of SCCs that are not directly linked to deep convection, we found that stratospheric gravity wave observations correlate in as much as 30% of the cases over the Great Plains in MJJA, about 50% over the North-Eastern Pacific, western Canada and maximally 90% over eastern Canada and the north-west Atlantic in NDJF. </p><p>Our results provide better understanding of the physical processes and climate variability related to SCCs and will be of interest for modelers as SCC sources such as deep convection and gravity waves are small-scale processes that are difficult to represent in global general circulation models. </p>

scholarly journals Quality Evaluation of Flaxseed for Food Use Specifications

2016 ◽  
Vol 6 (1) ◽  
pp. 59 ◽  
Author(s):  
Anuradha Vegi ◽  
Charlene E. Wolf-Hall ◽  
Clifford A Hall III
Keyword(s):  
North Dakota ◽  
Great Plains ◽  
Quality Evaluation ◽  
Northern Great Plains ◽  
Regional Survey ◽  
E Coli ◽  
North East ◽  
The North ◽  
Colony Forming Units ◽  
Plate Counts

A Northern Great Plains regional survey of microbiological loads in flaxseed was completed for years 2008 and 2009. Effects of cleaning flaxseed on microbial loads including aerobic plate counts (APCs), mold counts (MCs) yeast counts (YCs), coliform counts (CCs), Escherichia coli counts, and Enterobacteriaceae counts (ECs) were determined. Chemical analyses including oil and linolenic acid -ALA indicated that all flaxseed had near normal oil content. This was the first reported survey for flaxseed. The pre-cleaned flaxseed had an average of 5.7 ± 0.1, 4.1 ± 0.2, 4.5 ± 0.2, 3.6 ± 0.1, and 3.0 ± 0.1 log colony forming units (CFU) g-1 of APC, CC, EC, YC and MC respectively. All counts were higher than those for cleaned seed. No E. coli was detected. The North Dakota-West (ND-W) region flaxseed had higher MC when compared to Canada, ND-North East (ND-NE) and ND-South East (ND-SE) region flaxseed. For APC, the counts were higher in flaxseed from Canada when compared to North Dakota. Cleaning the flaxseed should be considered an important step in reducing the microbial counts and also for maintaining high quality flaxseed. 

Ancestral trans−North American Bell River system recorded in late Oligocene to early Miocene sediments in the Labrador Sea and Canadian Great Plains

2021 ◽  
Author(s):  
Julia I. Corradino ◽  
Alex Pullen ◽  
Andrew L. Leier ◽  
David L. Barbeau Jr. ◽  
Howie D. Scher ◽  
...  
Keyword(s):  
North America ◽  
Great Plains ◽  
North American ◽  
Detrital Zircon ◽  
Detrital Zircons ◽  
Labrador Sea ◽  
Western Canada ◽  
Zircon Age ◽  
North American Cordillera ◽  
The North

The Bell River hypothesis proposes that an ancestral, transcontinental river occupied much of northern North America during the Cenozoic Era, transporting water and sediment from the North American Cordillera to the Saglek Basin on the eastern margin of the Labrador Sea. To explore this hypothesis and reconstruct Cenozoic North American drainage patterns, we analyzed detrital zircon grains from the Oligocene−Miocene Mokami and Saglek formations of the Saglek Basin and Oligocene−Miocene fluvial conglomerates in the Great Plains of western Canada. U-Pb detrital zircon age populations in the Mokami and Saglek formations include clusters at <250 Ma, 950−1250 Ma, 1600−2000 Ma, and 2400−3200 Ma. Detrital zircons with ages of <250 Ma were derived from the North American Cordillera, supporting the transcontinental Bell River hypothesis. Oligocene−Miocene fluvial strata in western Canada contain detrital zircon age populations similar to those in the Saglek Basin and are interpreted to represent the western headwaters of the ancient Bell River drainage. Strontium-isotope ratios of marine shell fragments from the Mokami and Saglek formations yielded ages between 25.63 and 18.08 Ma. The same shells have εNd values of −10.2 to −12.0 (average = −11.2), which are consistent with values of Paleozoic strata in western North America but are more radiogenic than the modern Labrador Current, Labrador Sea Water, and North Atlantic Deep Water values (εNd ∼−12 to −25). As a freshwater source, the existence and termination of the Bell River may have been important for Labrador Sea circulation, stratification, and chemistry.

The Archaeology of the North American Great Plains

2021 ◽  
Author(s):  
Douglas B. Bamforth
Keyword(s):  
North America ◽  
Great Plains ◽  
Resource Use ◽  
Social Groups ◽  
Human History ◽  
Archaeological Evidence ◽  
Mountain Ranges ◽  
The North ◽  
Over Time

In this volume, Douglas B. Bamforth offers an archaeological overview of the Great Plains, the vast, open grassland bordered by forests and mountain ranges situated in the heart of North America. Synthesizing a century of scholarship and new archaeological evidence, he focuses on changes in resource use, continental trade connections, social formations, and warfare over a period of 15,000 years. Bamforth investigates how foragers harvested the grasslands more intensively over time, ultimately turning to maize farming, and examines the persistence of industrial mobile bison hunters in much of the region as farmers lived in communities ranging from hamlets to towns with thousands of occupants. He also explores how social groups formed and changed, migrations of peoples in and out of the Plains, and the conflicts that occurred over time and space. Significantly, Bamforth's volume demonstrates how archaeology can be used as the basis for telling long-term, problem-oriented human history.

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