Relevant bibliographies by topics / Little Blue River

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Reports

Academic literature on the topic 'Little Blue River'

Author: Grafiati
Published: 4 June 2021
Last updated: 14 February 2022

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Journal articles on the topic "Little Blue River"

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Barnes, P. L., and P. K. Kalita. "Watershed monitoring to address contamination source issues and remediation of the contaminant impairments." Water Science and Technology 44, no. 7 (2001): 51–56. http://dx.doi.org/10.2166/wst.2001.0387.

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The Big Blue River Basin is located in southeastern Nebraska and northeastern Kansas and consists of surface water in the Big Blue River, Little Blue River, Black Vermillion River, and various tributaries draining 24,968 km2. Approximately 75% of the land area in the basin are cultivated cropland. The Big Blue River flows into Tuttle Creek Reservoir near Manhattan, Kansas. Releases from the lake are used to maintain streamflow in the Kansas River during low flow periods, contributing 27% of the mean flow rate of the Kansas River at its confluence with the Missouri River. Tuttle Creek Reservoir
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Christensen, Eric, Rebecca Bushon, and Amie Brady. "Microbial Source Tracking as a Tool for TMDL Development, Little Blue River in Independence, Missouri." Proceedings of the Water Environment Federation 2013, no. 6 (2013): 7218–21. http://dx.doi.org/10.2175/193864713813726920.

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Wang, Lixin, and David S. Leigh. "Late-Holocene paleofloods in the Upper Little Tennessee River valley, Southern Blue Ridge Mountains, USA." Holocene 22, no. 9 (2012): 1061–66. http://dx.doi.org/10.1177/0959683612437863.

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Wang, Lixin, and David S. Leigh. "Anthropic signatures in alluvium of the Upper Little Tennessee River valley, Southern Blue Ridge Mountains, USA." Anthropocene 11 (September 2015): 35–47. http://dx.doi.org/10.1016/j.ancene.2015.11.005.

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Leigh, David S. "Vertical accretion sand proxies of gaged floods along the upper Little Tennessee River, Blue Ridge Mountains, USA." Sedimentary Geology 364 (February 2018): 342–50. http://dx.doi.org/10.1016/j.sedgeo.2017.09.007.

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Berhane, Fisseha, Benjamin Zaitchik, and Amin Dezfuli. "Subseasonal Analysis of Precipitation Variability in the Blue Nile River Basin." Journal of Climate 27, no. 1 (2014): 325–44. http://dx.doi.org/10.1175/jcli-d-13-00094.1.

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Abstract The Ethiopian portion of the Blue Nile River basin is subject to significant interannual variability in precipitation. As this variability has implications for local food security and transboundary water resources, numerous studies have been directed at improved understanding and, potentially, predictability of the Blue Nile rainy season (June–September) precipitation. Taken collectively, these studies present a wide range of large-scale drivers associated with precipitation variability in the Blue Nile: El Niño–Southern Oscillation (ENSO), the Indian summer monsoon, sea level pressur
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Leigh, David S. "Human and Climate influence on Floodplain Sedimentation in the Upper Little Tennessee River Valley, Southern Blue Ridge Mountains, USA." Quaternary International 279-280 (November 2012): 274. http://dx.doi.org/10.1016/j.quaint.2012.08.700.

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Tankersley, Kenneth B., and Nichelle Lyle. "Holocene faunal procurement and species response to climate change in the Ohio River valley." North American Archaeologist 40, no. 4 (2019): 192–235. http://dx.doi.org/10.1177/0197693119889256.

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This paper examines the temporal distribution of 163 distinct species recovered from 21 well-dated Holocene age archaeological sites in the Ohio River valley to determine patterns of faunal resource procurement and their response to periods of climate change. Climate change proxies include bison, long-billed curlew, pine marten, porcupine, prairie vole, and swamp rabbit. While the rice rat may be a proxy of climate change, its initial appearance in the Archaic cultural period co-occurs with storable starchy and oily seed crops such as erect knotweed, little barley, marsh elder, maygrass, and s
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Kislik, Chippie, Laurel Genzoli, Andy Lyons, and Maggi Kelly. "Application of UAV Imagery to Detect and Quantify Submerged Filamentous Algae and Rooted Macrophytes in a Non-Wadeable River." Remote Sensing 12, no. 20 (2020): 3332. http://dx.doi.org/10.3390/rs12203332.

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Imagery from unoccupied aerial vehicles (UAVs) is useful for mapping floating and emerged primary producers, as well as single taxa of submerged primary producers in shallow, clear lakes and streams. However, there is little research on the effectiveness of UAV imagery-based detection and quantification of submerged filamentous algae and rooted macrophytes in deeper rivers using a standard red-green-blue (RGB) camera. This study provides a novel application of UAV imagery analysis for monitoring a non-wadeable river, the Klamath River in northern California, USA. River depth and solar angle du
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Zhuo, L., M. M. Mekonnen, and A. Y. Hoekstra. "Sensitivity and uncertainty in crop water footprint accounting: a case study for the Yellow River basin." Hydrology and Earth System Sciences 18, no. 6 (2014): 2219–34. http://dx.doi.org/10.5194/hess-18-2219-2014.

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Abstract. Water Footprint Assessment is a fast-growing field of research, but as yet little attention has been paid to the uncertainties involved. This study investigates the sensitivity of and uncertainty in crop water footprint (in m3 t−1) estimates related to uncertainties in important input variables. The study focuses on the green (from rainfall) and blue (from irrigation) water footprint of producing maize, soybean, rice, and wheat at the scale of the Yellow River basin in the period 1996–2005. A grid-based daily water balance model at a 5 by 5 arcmin resolution was applied to compute gr
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Dissertations / Theses on the topic "Little Blue River"

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Conrad, Richard C. "Comparison of macroinvertebrate assemblages in a first- and second-order stream in Wilber Wright State Fish and Wildlife Area, Henry County, Indiana in 2000." Virtual Press, 2003. http://liblink.bsu.edu/uhtbin/catkey/1273262.

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Macroinvertebrate assemblages were semi-quantitatively sampled from the Little Blue River and an isolated headwater stream in Wilbur Wright Fish and Wildlife Area from March through November of 2000. Physicochemical conditions and qualitative habitat characteristics were recorded at each site. Each stream contained unique community assemblages based on taxa richness, composition, functional feeding groups, behavioral groups, reproductive habits, and drought tolerance/avoidance. Collections from the first-order stream contained fewer taxa and a greater proportion of non-insects and tolerant tax
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Books on the topic "Little Blue River"

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Cole, Stephen West. Quicksand and Blue Springs: Exploring the Little Colorado River Gorge. Vishnu Temple Press, 2006.

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Williams, Mark D. So Many Fish, So Little Time: 1001 of the World's Greatest Backcountry Honeyholes, Trout Rivers, Blue Ribbon Waters, Bass Lakes, and Saltwater Hot Spots. Collins, 2007.

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Williams, Mark D. So Many Fish, So Little Time: 1001 of the World's Greatest Backcountry Honeyholes, Trout Rivers, Blue Ribbon Waters, Bass Lakes, and Saltwater Hot Spots. Collins, 2007.

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Johansen, Bruce, and Adebowale Akande, eds. Nationalism: Past as Prologue. Nova Science Publishers, Inc., 2021. http://dx.doi.org/10.52305/aief3847.

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Nationalism: Past as Prologue began as a single volume being compiled by Ad Akande, a scholar from South Africa, who proposed it to me as co-author about two years ago. The original idea was to examine how the damaging roots of nationalism have been corroding political systems around the world, and creating dangerous obstacles for necessary international cooperation. Since I (Bruce E. Johansen) has written profusely about climate change (global warming, a.k.a. infrared forcing), I suggested a concerted effort in that direction. This is a worldwide existential threat that affects every living t
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Book chapters on the topic "Little Blue River"

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"Conservation, Ecology, and Management of Catfish: The Second International Symposium." In Conservation, Ecology, and Management of Catfish: The Second International Symposium, edited by DANIEL L. GARRETT and CHARLES F. RABENI. American Fisheries Society, 2011. http://dx.doi.org/10.47886/9781934874257.ch41.

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<em>Abstract</em>.—Flathead catfish <em>Pylodictis olivaris</em> and blue catfish <em>Ictalurus furcatus</em> thrive in large rivers and constitute large sport fisheries. Defining a spatial scale for new management strategies has become increasingly important due to rapid expansion of the sport fishery. To investigate life history characteristics, migratory pathways, and space use, we used telemetry to monitor the movement behavior of flathead catfish and blue catfish during two complete annual cycles. Individuals were sampled from a 97-km reach of the lower Missouri River and surgically implanted with transmitters during April 2006 (<EM>N</EM> = 77) and again in April and July of 2007 (<EM>N</EM> = 80). Acoustic tracking by boat and radio tracking by helicopter were used on the Missouri, Lamine, Chariton, Little Chariton, and Grand rivers during 2006–2008. The proportion of individuals that used a tributary during the putative spawning period (May 15–July 15) increased from 10% (8 of 77) in 2006 to 18% (14 of 80) in 2007. Flood conditions in May 2007 may have contributed to this increase. Between April 2006 and May 2007, the majority of flathead (51%) and blue catfishes (55%) moved less than 100 river kilometers from where they were tagged. The maximum linear range during 2006–2007 was 347.6 river kilometers for blue catfish and 751.9 river kilometers for flathead catfish. Seasonal structure to annual movements was evident with periods of both restricted movement (December–March; July–September) and migratory behavior (March–June; October–December). The variability in observed behaviors provides a substantial basis for managers to identify and protect distant habitats that are used by adult catfish for spawning, feeding and growth, and overwintering.
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Colopy, Cheryl. "Melamchi River Blues." In Dirty, Sacred Rivers. Oxford University Press, 2012. http://dx.doi.org/10.1093/oso/9780199845019.003.0014.

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While I lived in Kathmandu, I regularly visited the American Mission Association. Members call it Phora, while some Nepalis call it “mini America.” It’s a club, and expatriates with the right kind of visa can apply to become members. It has a pool and tennis courts, a small gym, a field for baseball and soccer, a children’s playground, movie rentals, manicures and massages, a commissary and wifi café, and very polite Nepali staff. It has a certain colonial feel to it, which bothered me at times: yet it was also a haven where on a weekday afternoon I could exercise, read the papers, and eat lunch. Phora refers to phohara durbar, which in Nepali means “fountain palace.” The extensive, welltended grounds where dozens of expats and their children gather for hours on weekends was once the site of a Rana palace, a place for parties and dances, performances and cinema. It got its name because there were fountains throughout the gardens as well as inside the building. The ornate, neoclassical palace is long gone. In serious disrepair by 1960, the palace was demolished and the land sold to the American government. But phohara durbar has other claims to fame. It was also the site of the first piped water in the Kathmandu Valley. To explain how this came about, I’ll tell you a little more about the valley’s history and culture. The Lichchhavis and Mallas kept the city from growing beyond certain limits. They prohibited building outside a ring of shrines to various mother goddesses, like Kali. They knew that disturbing the land beyond that ring would be “killing your own food, your economic base,” says Sudarshan Tiwari, the architect and cultural historian who has reconstructed aspects of ancient life in the valley. There is still some agriculture in the Kathmandu Valley, because a few of the old landowners stubbornly hold on to their fields even as a sea of “wedding cake,” multistory, pastel houses engulfs them. But daily the green plots of rice and vegetables shrink as the valley succumbs, like the ancient water channels, to unplanned urban development.
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Colopy, Cheryl. "More River Blues." In Dirty, Sacred Rivers. Oxford University Press, 2012. http://dx.doi.org/10.1093/oso/9780199845019.003.0015.

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It was not entirely clear to me why Ngawang Lama and his group wanted the intake point—the head of the Melamchi tunnel—moved to the spot that was proposed back in the early 1990s, when the World Bank was funding the revamping of Kathmandu’s water supply. But I learned that Norwegian engineers, who were then consultants on the project, had originally placed that intake upstream to provide for a hydropower plant. They saw the Melamchi project as a good opportunity to get more for the same investment of money. The Norwegians had proposed to place the intake several miles above the spot that Cholendra and I almost reached as we walked up the damaged access road. Using that intake point, called Nukute, would have allowed for a twenty-five-megawatt hydropower plant in Sundarijal, where the tunnel ended. The higher intake could give an additional three hundred meters of “head”—water pressure to generate electricity. When the Asian Development Bank took over the project, they scuttled the hydropower component. After this, the Norwegians pulled out. The proposed twenty-five megawatts of electricity would have been welcome in a country that is likely to see power outages for at least another decade. Now, with the planned intake point lower on the river, hydropower is not possible because there would be insufficient water pressure. The ADB’s reasons for dropping the hydro component are a little vague. Ratna Sansar Shrestha dismisses the economic and environmental costs the organization cites as its rationale for dropping hydropower. Ratna is a water resources specialist who is well known for wanting the Melamchi project to include hydropower. He is one of three members of the Regulatory Commission for Water Supply that oversees tariffs and quality of service throughout Nepal. To be charitable to the ADB, he says, “working with Nepal’s bureaucracy is not easy.” Hydropower projects require negotiating with an entirely different ministry from the one that oversees water supply. Cutting out the hydropower component also cut out half the administrative red tape on a project that has been drowning in it for years.
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"A Week from the Big Pigeon To the Little Tennessee River." In Blues and Roots/Rue and Bluets. Duke University Press, 1985. http://dx.doi.org/10.1215/9780822382959-042.

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"A Week from the Big Pigeon To the Little Tennessee River." In Blues and Roots/Rue and Bluets. Duke University Press, 2020. http://dx.doi.org/10.1515/9780822382959-043.

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"Invasive Asian Carps in North America." In Invasive Asian Carps in North America, edited by Leo G. Nico, Amanda Demopoulos, Daniel Gualtieri, and Carla Wieser. American Fisheries Society, 2011. http://dx.doi.org/10.47886/9781934874233.ch8.

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<em>Abstract</em>.—The black carp <em>Mylopharyngodon piceus </em>is a large (>1 m long) riverine fish from eastern Asia introduced into the United States via the aquaculture industry. A wild population has been present in the lower Mississippi River basin since the early 1990s, but little is known about the ecological effect of black carp in invaded environments. In its native range, black carp feed almost exclusively on mollusks. In U.S. waters, they likely prey on native mussels, but few wild-caught specimens have been examined by biologists and all have had empty gastrointestinal tracts. In lieu of stomach content data, we examined isotopic values (δ<sup>13</sup>C and δ <sup>15</sup>N) and mercury (Hg) concentrations in muscle tissue of black carp and 10 other large nonnative and native fish species captured in the Red–Atchafalaya River system of Louisiana, USA. Trophic position estimates derived from δ <sup>15</sup>N values ranged from 2.0 for grass carp <em>Ctenopharyngodon idella </em>to 4.8 for blue catfish <em>Ictalurus furcatus </em>and flathead catfish <em>Pylodictis olivaris</em>. Adult black carp had a δ <sup>15</sup>N value (13.2‰), indicating a trophic level of 3.5. Mean total Hg concentrations ranged from 0.02 µg/g in grass carp to 0.27 µg/g in bigmouth buffalo <em>Ictiobus cyprinellus</em>, in black carp 0.17 µg/g; Hg increased with increasing δ <sup>15</sup>N, indicating biomagnification. The limited numbers of taxa and small samples sizes, as well as constraints in methods used, do not allow confirmation that wild black carp are consuming native mollusks. However, our stable isotope results do provide evidence that its diet is similar to other large fish species inhabiting the Red–Atchafalaya system considered to be benthic invertivores, including some known to prey on freshwater mollusks (i.e., smallmouth buffalo <em>I. bubalus </em>and nonnative common carp <em>Cyprinus carpio</em>).
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Worster, Donald. "Restoring a Natural Order." In Wealth of Nature. Oxford University Press, 1994. http://dx.doi.org/10.1093/oso/9780195092646.003.0017.

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A few years ago I came down a backcountry road in Wisconsin looking for a place where a man had given his life. The road had once been the route of pioneers moving west, then a farm road running through dry, sandy, marginal fields. In the days of Prohibition it had carried illegal whiskey distilled hereabouts, some of the last trees having been cut down to cook the bootlegger’s brew. Then in 1935 another sort of settler came along. It was the time of the Great Depression, and he could buy a lot of land, 120 acres in all, land abandoned by its owners, for a little money in back taxes. The land had no economic value left in it. The man, whose name was Aldo Leopold, knew that but did not mind; he was not after gain or even subsistence. He began coming out regularly from the city of Madison, where he taught at the university, to plant trees. For thirteen years he planted and nurtured. Then, in 1948, he died fighting a forest fire on a neighbor’s land. Knowing those few details, I came wanting to know what manner of man he was and what he had died for. There was no publicity, no tour guide provided, but the dense forest of pines was a sufficient announcement that here was Leopold’s place, now all grown up again to natural splendor. I walked through an open field rich in wild grasses and forbs to a small, gray, weathered shack where he had stayed on those weekends, regaled by the smell of his new pines coming up and the sound of birdsong and wind in their branches. From the shack, I found my way down a short path to the Wisconsin River, rolling silently between its pungent banks, the warm summer sun glinting on its ripples. One August years ago Leopold, as recalled in a sketch he wrote and collected in A Sand County Almanac, found the river “in a painting mood,” laying down a brief carpet of moss on its silty edges, spangling it with blue and white and pink flowers, attracting deer and meadow mice, then abruptly scouring its palette down to austere sand.
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"Invasive Asian Carps in North America." In Invasive Asian Carps in North America, edited by Leo G. Nico, Amanda Demopoulos, Daniel Gualtieri, and Carla Wieser. American Fisheries Society, 2011. http://dx.doi.org/10.47886/9781934874233.ch8.

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<em>Abstract</em>.—The black carp <em>Mylopharyngodon piceus </em>is a large (>1 m long) riverine fish from eastern Asia introduced into the United States via the aquaculture industry. A wild population has been present in the lower Mississippi River basin since the early 1990s, but little is known about the ecological effect of black carp in invaded environments. In its native range, black carp feed almost exclusively on mollusks. In U.S. waters, they likely prey on native mussels, but few wild-caught specimens have been examined by biologists and all have had empty gastrointestinal tracts. In lieu of stomach content data, we examined isotopic values (δ<sup>13</sup>C and δ <sup>15</sup>N) and mercury (Hg) concentrations in muscle tissue of black carp and 10 other large nonnative and native fish species captured in the Red–Atchafalaya River system of Louisiana, USA. Trophic position estimates derived from δ <sup>15</sup>N values ranged from 2.0 for grass carp <em>Ctenopharyngodon idella </em>to 4.8 for blue catfish <em>Ictalurus furcatus </em>and flathead catfish <em>Pylodictis olivaris</em>. Adult black carp had a δ <sup>15</sup>N value (13.2‰), indicating a trophic level of 3.5. Mean total Hg concentrations ranged from 0.02 µg/g in grass carp to 0.27 µg/g in bigmouth buffalo <em>Ictiobus cyprinellus</em>, in black carp 0.17 µg/g; Hg increased with increasing δ <sup>15</sup>N, indicating biomagnification. The limited numbers of taxa and small samples sizes, as well as constraints in methods used, do not allow confirmation that wild black carp are consuming native mollusks. However, our stable isotope results do provide evidence that its diet is similar to other large fish species inhabiting the Red–Atchafalaya system considered to be benthic invertivores, including some known to prey on freshwater mollusks (i.e., smallmouth buffalo <em>I. bubalus </em>and nonnative common carp <em>Cyprinus carpio</em>).
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Thomson, Peter. "Blind Love Is a Dangerous Thing." In Sacred Sea. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780195170511.003.0029.

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The sky is a blinding white and blue, and the little minibus from Listvianka to Irkutsk flits over the folds of the Angara Valley like a bumblebee, slightly ungainly and, to an observer, perhaps not quite in control of its trajectory, but confident in its own path and in the completion of its journey. We’ve seen our last of Baikal. One last run alongside daughter Angara and James and I will get our final glimpse of the lake’s cobalt water, bearing northwest for the turbines and factories of the Angarsk industrial corridor and then, slightly tarnished, on to her rendezvous with her beloved Yenisei and finally the Arctic ocean, 2,500 river kilometers downstream. One last pass through Irkutsk, and we’ll be back on the beast-machine bound for Moscow and beyond, and a world more familiar if still not known. We’ve seen our last of Baikal, but I’m pretty sure that I, anyway, am not leaving it behind, that it will never quite stop flowing through me. Blood has the same salinity as the ocean, someone once told me—we never really left the sea, we just carry it around inside us. Alas, this little detail of life turns out to be just too exquisite to be true, but it sure works as metaphor—we all carry around a biological memory of where and what we come from, from the water that makes up roughly sixty percent of our bodies to the ninety-eight or so percent of our genes that we share with chimpanzees. And so it is with Baikal—the lake inseparable from the people who love it in so many complex and ambiguous ways—I’ll carry a piece of it around in every part of me, like a new strand of DNA that has spliced itself in with mine and changed ever so slightly who I am and how I live in the world. For our last couple of nights back in Irkutsk, James and I stay in a downtown hotel, for about three times the cost of the American House, where, Olga tells us, we can finally get our visas properly registered.
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Horning, Ned, Julie A. Robinson, Eleanor J. Sterling, Woody Turner, and Sacha Spector. "Working with images." In Remote Sensing for Ecology and Conservation. Oxford University Press, 2010. http://dx.doi.org/10.1093/oso/9780199219940.003.0009.

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There are two very different ways to envision a satellite image: as a photograph taken with a camera, or as a visual representation of spectral intensity data quantifying the light reflecting off of objects on a planet’s surface. In working with satellite images, sometimes the objective is to highlight and accent the information in the image using tools to enhance the way the image looks—the same goal that a professional photographer might have when working in the darkroom with film or using Photoshop to manipulate digital photographs. Another objective could be to manipulate the image using automated processing methods within a remote sensing package that rely on a set of equations that quantify information about reflected light. With either approach the goal is to gain information about conditions observed on the ground. At first glance, the image in Fig. 3.1 bears little resemblance to what most people would recognize as a terrestrial landscape. After all, its predominant colors are orange and bright turquoise. The use of colors in creating a visual image allows great breadth in the types of things one can identify on the ground, but also makes image interpretation an art. Even an inexperienced interpreter can make some sense of the image; more experienced interpreters with knowledge of the color scheme in use are able to determine finer details. For example, in Fig. 3.1 some of the more prominent features are a river (blue line on the left side of the image) a gradient of different vegetation (orange colors throughout the image that go from light to dark), and burn scars (turquoise patches). Fig. 3.2 shows a portion of landscape represented in the satellite image in Fig. 3.1. The red dot in Fig. 3.1 indicates the location where the photograph was taken. This photograph shows what a human observer would see looking south (in this case toward the top of the satellite image) from the point represented by the red dot. The view in the photograph differs from the satellite image in two important ways.
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Reports on the topic "Little Blue River"

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Huffman, Clyde W., and William F. Lowe. Multiple-Purpose Project Little Blue River Basin East Fork Little Blue River Missouri. Blue Springs Lake - Operation and Maintenance Manual. Appendix 4, Volume 2. Construction Foundation Report. Defense Technical Information Center, 1990. http://dx.doi.org/10.21236/ada229026.

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Lynch, Lori L., Francke E. Walberg, and Robert G. Dimmitt. Multiple-Purpose Project, Little Blue River Basin, Little Blue River, Missouri: Longview Lake Operation and Maintenance Manual. Appendix 5. Embankment Criteria and Performance Report. Defense Technical Information Center, 1990. http://dx.doi.org/10.21236/ada241911.

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Schmits, Larry J. Prehistory of the Little Blue River Valley, Western Missouri: Archaeological Investigations at Blue Springs Lake. Defense Technical Information Center, 1989. http://dx.doi.org/10.21236/ada216614.

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