Life History and Behaviour of the Armyworm, Pseudaletia unipuncta (Haw.) (Lepidoptera: Noctuidae), in Eastern Ontario

1961 ◽  
Vol 93 (12) ◽  
pp. 1141-1153 ◽  
Author(s):  
J. C. Guppy

The armyworm, Pseudaletia unipuncta (Haw.), has been an important pest of grasses in North America for many years, largely in the eastern half of the Continent, from the more southerly regions of Canada to the southern United States. The larvae skeletonize rhe surface of the leaf blades or rhe inner surface of the sheaths during the early instars, and later feed from the margins of the leaves, consuming all the tissues. The inflorescence is seldom damaged unless leaf foliage is scarce but in some grasses, notably timothy, the green heads are often readily consumed by the older larvae even when foliage is abundant. Normally, populations of the armyworm are small, attracting little attention, but at irregular intervals of five to 20 years widespread outbreaks have occured simultaneously in Canada and the united States; eight such outbreaks have been recorded since 1860. In some of the intervening years smaller and more localized outbreaks have occurred. During the outbreak, damage to forage grasses and cereal crops has been so severe that the armyworm constitutes one of the most important insects attacking these crops. The latest great outbreak occurred on the North American Continent in 1954; this was preceded by a smaller but severe attack in 1953, largely in the central United States east of the Mississippi River. In Canada, in 1954, all the provinces from eastern Saskatchewan to Newfoundland were involved.

1962 ◽  
Vol 94 (10) ◽  
pp. 1103-1107 ◽  
Author(s):  
C. E. Brown

The Bruce spanworrn, Operophtera bruceata (Hulst), is most common in the mid latitudes of the North American Continent; in Canada it occurs from Newfoundland to the interior of British Columbia (Prentice, In Press) and has been reported from Vermont and Wisconsin in the United States (Craighead, 1950.) Three outbreaks of this insect have been recorded in Alberta. The first occurred in 1903 (de Gryse, 1925) and was apparently of short duration. The second reported by Wolley Dod (1913) occurred in 1913 and denuded hundreds of acres of aspen poplar. Heavy defoliation in the third outbreak became evident in 1957 (Brown, 1957) but an examination of Forest Insect Survey records revealed that population buildup began about 1951. The outbreak continued to expand until 1958 and began to decline in 1959; by 1961 populations were again low except for one or two isolated areas where moderate to low populations persisted. At the peak of the outbreak in 1958 approximately 50,000 square miies were moderately or heavily infested and many more lightly infested.


2017 ◽  
Vol 27 (5) ◽  
pp. 718-730 ◽  
Author(s):  
David C. Zlesak ◽  
Randy Nelson ◽  
Derald Harp ◽  
Barbara Villarreal ◽  
Nick Howell ◽  
...  

Landscape roses (Rosa sp.) are popular flowering shrubs. Consumers are less willing or able to maintain landscape beds than in years past and require plants that are not only attractive, but well-adapted to regional climatic conditions, soil types, and disease and pest pressures. Marketing and distribution of rose cultivars occurs on a national level; therefore, it is difficult for U.S. consumers in the U.S. Department of Agriculture (USDA) Plant Hardiness Zones 3 to 5 to identify well-adapted, cold-hardy cultivars. Identifying suitable cultivars that have strong genetic resistance to pests and disease and that will tolerate temperature extremes without winter protection in the USDA Plant Hardiness Zones 3 to 5 is of tremendous value to consumers and retailers in northern states. Twenty landscape rose cultivars, primarily developed in north-central North America, were evaluated at five locations in the United States (three in the north-central United States, one in the central United States, and one in the south-central United States) using the low-input, multiyear Earth-Kind® methodology. Six roses had ≥75% plant survival at the end of the study and were in the top 50% of performers for overall mean horticultural rating at each of the three north-central U.S. sites: ‘Lena’, ‘Frontenac’, ‘Ole’, ‘Polar Joy’, ‘Sunrise Sunset’, and ‘Sven’. Five of these six roses met the same criteria at the central United States (exception ‘Lena’) and the south-central United States (exception ‘Polar Joy’) sites. Cultivar, rating time, and their interaction were highly significant, and block effects were not significant for horticultural rating for all single-site analyses of variance. Significant positive correlations were found between sites for flower number, flower diameter, and overall horticultural rating. Significant negative correlations were found between flower number and diameter within each site and also between black spot (Diplocarpon rosae) lesion size from a previous study and overall horticultural rating for three of the five sites. Cane survival ratings were not significantly correlated with overall horticultural rating, suggesting some cultivars can experience severe winter cane dieback, yet recover and perform well. Data from this study benefit multiple stakeholders, including nurseries, landscapers, and consumers, with evidence-based regional cultivar recommendations and breeders desiring to identify regionally adapted parents.


2010 ◽  
Vol 23 (6) ◽  
pp. 1477-1494 ◽  
Author(s):  
Kerry H. Cook ◽  
Edward K. Vizy

Abstract The easterly Caribbean low-level jet (CLLJ) is a prominent climate feature over the Intra-America Seas, and it is associated with much of the water vapor transport from the tropical Atlantic into the Caribbean Basin. In this study, the North American Regional Reanalysis (NARR) is analyzed to improve the understanding of the dynamics of the CLLJ and its relationship to regional rainfall variations. Horizontal momentum balances are examined to understand how jet variations on both diurnal and seasonal time scales are controlled. The jet is geostrophic to the first order. Its previously documented semidiurnal cycle (with minima at about 0400 and 1600 LT) is caused by semidiurnal cycling of the meridional geopotential height gradient in association with changes in the westward extension of the North Atlantic subtropical high (NASH). A diurnal cycle is superimposed, associated with a meridional land–sea breeze (solenoidal circulation) onto the north coast of South America, so that the weakest jet velocities occur at 1600 LT. The CLLJ is present throughout the year, and it is known to vary in strength semiannually. Peak magnitudes in July are related to the seasonal cycle of the NASH, and a second maximum in February is caused by heating over northern South America. From May through September, zonal geopotential gradients associated with summer heating over Central America and Mexico induce meridional flow. The CLLJ splits into two branches, including a southerly branch that connects with the Great Plains low-level jet (GPLLJ) bringing moisture into the central United States. During the rest of the year, the flow remains essentially zonal across the Caribbean Basin and into the Pacific. A strong (weak) CLLJ is associated with reduced (enhanced) rainfall over the Caribbean Sea throughout the year in the NARR. The relationship with precipitation over land depends on the season. Despite the fact that the southerly branch of the CLLJ feeds into the meridional GPLLJ in May through September, variations in the CLLJ strength during these months do not impact U.S. precipitation, because the CLLJ strength is varying in response to regional-scale forcing and not to changes in the large-scale circulation. During the cool season, there are statistically significant correlations between the CLLJ index and rainfall over the United States. When the CLLJ is strong, there is anomalous northward moisture transport across the Gulf of Mexico into the central United States and pronounced rainfall increases over Louisiana and Texas. A weak jet is associated with anomalous westerly flow across the southern Caribbean region and significantly reduced rainfall over the south-central United States. No connection between the intensity of the CLLJ and drought over the central United States is found. There are only three drought summers in the NARR period (1980, 1988, and 2006), and the CLLJ was extremely weak in 1988 but not in 1980 or 2006.


2021 ◽  
Vol 51 (1) ◽  
pp. 114-130
Author(s):  
Heather Corbally Bryant

This article investigates the influence of North America on Bowen's later work. After the war, Bowen traveled to America, at least once a year, until her last illness. Yet her time in the United States has often been overlooked. In the States, she lectured at colleges and universities across the country, and taught at several prestigious schools. She also wrote articles and essays for the more lucrative American journals and periodicals. In addition to touring the country, she was able to see her many American friends, such as Eudora Welty, and her publishers, the Knopfs, as well as her lover, Charles Ritchie. This new continent allowed Bowen to confront old traumas on new grounds, especially in the American element of Eva Trout, in which she displaces the central question of the relationship between mother and child onto American soil to interrogate the (literally, in Jeremy's case) unspeakable nature of trauma.


Author(s):  
Susan Elizabeth Hough ◽  
Roger G. Bilham

The Caribbean is a place of romance. Idyllic beaches, buoyant cultures, lush tropical flora; even the Caribbean pirates of yore often find themselves romanticized in modern eyes, and on modern movie screens. Yet it requires barely a moment’s reflection to appreciate the enormous resilience that must exist in a place that is so routinely battered by storms of enormous ferocity. News stories tend to focus on large storms that reach the United States, but many large hurricanes arrive in the United States by way of the Caribbean. Before it slammed into South Carolina in 1989, Hurricane Hugo brushed the Caribbean islands, skimming Puerto Rico and devastating many small islands to its east. Other hurricanes have hit the islands more directly. These include Inez, which claimed some 1,500 lives in 1966, and the powerful Luis, which caused $2.5 billion in property damage and 17 deaths when it pummeled the Leeward Islands and parts of Puerto Rico and the Virgin Islands in 1995. Hurricanes also figure prominently in the pre-20th-century history of the Caribbean—storms that had no names, the sometimes lethal fury of which arrived unheralded by modern forecasts. Most people know that the Caribbean is hurricane country; probably few realize that it is earthquake country as well. After all, the western edge of North America is the active plate boundary; earthquakes occur in the more staid midcontinent and Atlantic seaboard, but far less commonly. What can be overlooked, however, is North America’s other active plate boundary. To understand the general framework of this other boundary, it is useful to return briefly to basic tenets of plate tectonics theory. As discussed in earlier chapters, the eastern edge of North America is known as a passive margin. Because the North American continent is not moving relative to the adjacent Atlantic oceanic crust, in plate tectonics terms, scientists do not differentiate between the North American continent and the western half of the Atlantic ocean.


Plant Disease ◽  
2018 ◽  
Vol 102 (2) ◽  
pp. 292-299 ◽  
Author(s):  
Japheth D. Weems ◽  
Carl A. Bradley

Northern leaf blight (NLB) of corn, caused by Exserohilum turcicum, is a foliar disease common across corn production regions of the world, including those in the north central United States. Previous race population distribution studies identified five physiological races present in the United States, prior to 1995. For this study, 156 E. turcicum isolates were screened on corn differential lines containing Ht1, Ht2, Ht3, Htm1, and Htn1 resistance genes. Isolates were collected from fields in Iowa, Illinois, Indiana, Minnesota, North Carolina, Ohio, and Wisconsin, which included 143 isolates collected between 2007 and 2014 and 13 isolates collected between 1979 and 1985. Twenty different physiological races were observed based on the symptom response of the differential corn lines. E. turcicum race 0, 1, and 1mn were the most prevalent races, comprising 21, 27, and 13% of the 156 isolates, respectively. Race populations were diverse within states and years. Virulence to multiple Ht resistance genes within individual isolates was observed in 47% of those tested, with 3% of the isolates conferring virulence to all Ht resistance genes. Virulence to the Ht1, Ht2, Ht3, Htm1, and Htn1 resistance genes was present in 64, 20, 18, 32, and 27% of the E. turcicum isolates, respectively. Virulence to Ht resistance genes was fairly evenly distributed across states, in isolates collected after 2008. Virulence to Ht2, Ht3, Htm1, and Htn1 decreased after 2010. Variations in race population diversity are difficult to explain without knowing the level of selection pressure present in fields, and information regarding Ht resistance gene deployment in commercial varieties is not publicly available. Although virulence was observed against all Ht resistance genes, qualitative Ht resistance genes could be used in conjunction with quantitative resistance to increase NLB control.


2011 ◽  
Vol 1 (7) ◽  
pp. 20
Author(s):  
L. Bajorunas

The Great Lakes Superior, Michigan, Huron, Erie, and Ontario extend almost to the middle of the North American Continent. With their 95,000 square miles of water surface and their three navigable connections with the Atlantic Ocean and Gulf of Mexico, they affect the well-being of about 4.0 million people living within their vicinity in Canada and the United States. Possessing a shoreline of 6,600 miles, these waters have been called the fourth coast of the continent along with the Atlantic, Gulf, and Pacific coasts. This paper analyzes one of the many problems of the Great Lakes, the littoral transport problem. Littoral transport has been defined as the movement of material along the shore in the littoral zone by waves and currents. The material thus transported is referred to as the littoral drift. The littoral drift originates from the beach material, being picked up by the water and transported along the shore and deposited in another location. Shore erosion, littoral transport, and deposition of drift are all factors in the littoral process. A knowledge of the littoral process is important for many engineering projects including the construction and maintenance of shoreline harbors. The harbor breakwater extending from the shore into deep water forms a littoral barrier, and by stopping the transport action causes the depositio of drift on the updrift side. If the breakwater does not entirely stop the transport, or when the storage area on the updrift side is filled, the drift will bypass the breakwater and fill the dredged navigation channel causing frequent and expensive maintenance dredging. This problem is especially important in the small harbors on the Great Lakes planned every 25 to 30 miles as refuge for fishing and pleasure boats. These harbors have a rather small capacity for littoral drift, and the costs of maintenan dredging of so many entrance channels would be almost prohibitive. In order to provide data required for the design and economic evaluation of the small refuge harbors on the Great .Lakes, the United States Lake Survey, Corps of Engineers, conducted a study of the best method of estimating the rate of littoral transport along the shores of the Great Lakes. Although much of the data used in this paper was taken from the above study, the views and


Author(s):  
Thorkild Kjærgaard

Thorkild Kjærgaard: The Peace in Kiel, Greenland, and the North Atlantic, 1814–2014 At the peace conference in Kiel (North Germany) in January 1814, the Danish-Norwegian North Atlantic Empire that controlled an enormous area of land and water, including not only Denmark (with Schleswig-Holstein) and Norway but also Iceland, the Faroe Islands and the huge, thinly populated ice-covered island of Greenland, was dissolved by the victorious powers of the Napoleonic wars. Norway was given to Sweden as compensation for Finland, which Sweden — now in the victorious coalition — had lost to Russia in 1809. Rather surprisingly, the Kingdom of Denmark — now, without Norway, Europe’s smallest independent country — was entrusted with Greenland, Iceland and the Faroe Islands, although these three North Atlantic areas since early medieval times had been a part of the Kingdom of Norway. Without question, this was a major historical injustice. For Denmark, the outcome of the 1814 conference in Kiel was twofold: it was reduced to a very small country and it became — and still is — a polar nation, which it had not been before. The article discusses three aspects of this complex. Firstly: What happened in Kiel? Why were the three North Atlantic territories taken from Norway and given to Denmark? Was it, as it has been claimed by a majority of historians, the merit of sly Danish diplomats or was it — as the author believes — the will of the United Kingdom that was imposed on two small countries, Sweden and Denmark? Secondly, it is discussed how Denmark dealt with its new role as a polar nation. It turns out that Denmark initially was a rather hesitant, not to say, unwilling polar nation. Gradually, however, the extraordinary qualities of the North Atlantic islands, especially Greenland, were recognized. Since the end of the 19th century, Greenland has been a major subject of Danish art and literature, just as it has been a decisive dimension of Danish scientific research. The last section of the article deals with the significance of Greenland for Danish security and foreign policy. It is shown how the suffocating dependency on Great Britain after 1814 gradually was reduced thanks to a rapprochement to the new world power, the United States, which very early on showed interest in Greenland, which is, geographically, a part of the North American continent. The close alliance with the United States has saved Greenland for Denmark, just as it has been extremely helpful for Denmark in number of critical situations since 1814, but it also has its price. The price is that Denmark always follows US and never questions US actions. Relatively, Denmark, one of President Bush’s “willing nations,” has had more casualties on the American battlefields in Iraq and Afghanistan than any other of the United States’ allied nations. The Danish soldiers who have been killed on Middle East or Central Asiatic battlefields since 2001 have died for Greenland.


2016 ◽  
Vol 17 (4) ◽  
pp. 232-238 ◽  
Author(s):  
Yuba R. Kandel ◽  
Daren S. Mueller ◽  
Chad E. Hart ◽  
Nathan R. C. Bestor ◽  
Carl A. Bradley ◽  
...  

Foliar disease and insect management on soybean (Glycine max L. Merrill) in the North Central region of the United States has been increasingly accomplished through foliar fungicide and insecticide application. Data from research trials conducted in Illinois, Indiana, Iowa, and Nebraska were compiled from 2008 to 2014 to determine the impact of fungicide, insecticide, and fungicide + insecticide applications on soybean yield and profitability. In each state, field experiments occurred each year in two to seven locations. All treatments were applied at the R3 growth stage. Disease and insect pressure were very low in all states and years. A foliar application of fungicide, insecticide, or the combination, increased yield in seven out of 14 total site-years (P < 0.10). Economic analysis using an average soybean price of $0.42 per kilogram and average application cost of $62 per hectare indicated that fungicide applications were only profitable in 14% of the trial site-years. Insecticide alone and fungicide + insecticide was profitable in 39% and 45% of site-years, respectively. Effect of fungicide class on yield was inconsistent. Our results indicate that although yield increases can occur with foliar fungicide and/or insecticide treatments, current market prices and application costs may limit profitability when disease and/or insect pressure is low. Accepted for publication 22 September 2016.


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