Some Remarks on Linguistic and Lexical Change in the North Eastern Neo-Aramaic Dialects

2003 ◽  
Vol 1 (2) ◽  
pp. 179-190
Author(s):  
Geoffrey Khan
Keyword(s):  
Historical Development ◽  
Linguistic Features ◽  
North West ◽  
North East ◽  
The North ◽  
Urgent Task ◽  
Lexical Change ◽  
North Eastern ◽  
Relationship Of ◽  
The Relationship

Abstract The great diversity of the North Eastern Neo-Aramaic dialect group has only partially been studied. This is now an urgent task, since many of the dialects are now in danger of extinction. These dialects exhibit many fascinating linguistic features, which makes their investigation very rewarding. Investigation of these dialects also casts important light on some issues in the historical development of Aramaic and of North-West Semitic languages in general. Some of these issues are discussed in the paper. Particular attention is directed to the relationship of the lexicon of North-East Neo-Aramaic to that of earlier forms of literary Aramaic.

scholarly journals Evaluation of Soil Moisture Variability in Poland from SMOS Satellite Observations

2019 ◽  
Vol 11 (11) ◽  
pp. 1280 ◽  
Author(s):  
Bogusław Usowicz ◽  
Jerzy Lipiec ◽  
Mateusz Lukowski
Keyword(s):  
Soil Moisture ◽  
North West ◽  
Moisture Contents ◽  
North East ◽  
The North ◽  
Linear Distance ◽  
Classical Statistics ◽  
Ocean Salinity ◽  
North Eastern ◽  
Smos Satellite

Soil moisture (SM) data play an important role in agriculture, hydrology, and climate sciences. In this study, we examined the spatial-temporal variability of soil moisture using Soil Moisture Ocean Salinity (SMOS) satellite measurements for Poland from a five-year period (2010–2014). SMOS L2 v. 551 datasets (latitudinal rectangle 1600 × 840 km, centered in Poland) averaged for quarterly (three months corresponding to winter, spring, summer, and autumn) and yearly values were used. The results were analysed with the use of classical statistics and geostatistics (using semivariograms) to acquire information about the nature of anisotropy and the lengths and directions of spatial dependences. The minimum (close to zero) and maximum soil moisture values covered the 0.5 m3 m−3 range. In particular quarters, average soil moisture did not exceed 0.2 m3 m−3 and did not drop below 0.12 m3 m−3; the corresponding values in the study years were 0.171 m3 m−3 and 0.128 m3 m−3. The highest variability of SM occurred generally in winter (coefficient of variation, CV, up to 40%) and the lowest value was recorded in spring (around 23%). The average CV for all years was 32%. The quarterly maximum (max) soil moisture contents were well positively correlated with the average soil moisture contents (R2 = 0.63). Most of the soil moisture distributions (histograms) were close to normal distribution and asymmetric data were transformed with the square root to facilitate geostatistical analysis. Isotropic and anisotropic empirical semivariograms were constructed and the theoretical exponential models were well fitted (R2 > 0.9). In general, the structural dependence of the semivariance was strong and moderate. The nugget (C0) values slightly deceased with increasing soil moisture while the sills (C0 + C) increased. The effective ranges of spatial dependence (A) were between 1° and 4° (110–440 km of linear distance). Generally, the ranges were greater for drier than moist soils. Anisotropy of the SM distribution exhibited different orientation with predominance from north-west to south-east in winter and spring and changed for from north-east to south-west or from north to south in the other seasons. The fractal dimension values showed that the distribution of the soil moisture pattern was less diverse (smoother) in the winter and spring, compared to that in the summer and autumn. The soil moisture maps showed occurrence of wet areas (soil moisture > 0.25 m3 m−3) in the north-eastern, south-eastern and western parts and dry areas (soil moisture < 0.05 m3 m−3) mainly in the central part (oriented towards the south) of Poland. The spatial distribution of SM was attributed to soil texture patterns and associated with water holding capacity and permeability. The results will help undertake appropriate steps to minimize susceptibility to drought and flooding in different regions of Poland.

Long Term Changes in Abundance of Eggs of the Cornish Pilchard (Sardina Pilchardus Walbaum) Off Plymouth

1974 ◽  
Vol 54 (3) ◽  
pp. 641-649 ◽  
Author(s):  
A. J. Southward
Keyword(s):  
Small Scale ◽  
Personal Communications ◽  
North West ◽  
The North ◽  
History Of ◽  
Inshore Waters ◽  
Relationship Of ◽  
Hearsay Evidence ◽  
The Relationship

The inshore fishery for the pilchard in Cornish waters has existed for several hundred years, and such records as are available concerning fluctuation in catches and market conditions have been reviewed by Couch (1865), Cushing (1957) and Culley (1971). Although pilchard have been landed from Lyme Bay, from the eastern half of the Channel, and from the southern North Sea (Couch, 1865; Furnestin, 1945; Cushing, 1957; personal communications G. T. Boalch) the catches have usually been incidental to other fisheries and more sporadic than in Cornish waters. Traditionally there are three areas fished for the Cornish pilchard: on the north-west coast around St Ives; in Mounts Bay and towards the Scillies; and between the Lizard Pt and Bolt Tail in Devon (Couch, 1865; Culley, 1971). The latter region, constituting the inshore waters of south-east Cornwall and south Devon, effectively forms the eastern limits of the regular occurrence of commercial shoals. Knowledge of the breeding and life-history of the fish in this region has always been scarce and subject to much hearsay evidence (reviewed in Southward, 1963). Up to quite recently it was thought that the main spawning area lay well to the west of the entrance to the Channel, and it was not until the investigations reported by Corbin (1947,195°) a nd Cushing (1957)tnat it was conclusively shown that extensive spawning can occur within the English Channel from May to October. The relationship of the spawning in the western Channel to the other areas of spawning off the entrance to the Channel and in the northern Bay of Biscay is illustrated in a recent series of reports (Arbault & Boutin, 1968; Arbault & Lacroix-Boutin, 1969; Arbault & Lacroix, 1971; Wallace, P. D. & Pleasants, C. A., duplicated ICES meeting paper CM 1972/J: 8), and is further demonstrated by Demir & Southward (1974) in discussing the results of a study of small scale seasonal changes in spawning intensity in inshore waters.

Globally Speaking

2008 ◽  
Vol 13 (2) ◽  
pp. 137-140 ◽  
Author(s):  
Trevor Wishart
Keyword(s):  
Electroacoustic Music ◽  
Digital Recording ◽  
Recording Equipment ◽  
High Quality ◽  
Cultural Experience ◽  
North East ◽  
The North ◽  
Local Sound ◽  
Relationship Of ◽  
The Relationship

AbstractCheaply available high-quality digital recording equipment, and the ubiquity of computer music tools and the Internet make the creation of electroacoustic music in diverse localities, and its dissemination around the globe, extremely easy. This raises important questions about the relationship of local sound worlds and cultural experience to a potentially global audience. This quandary is examined through the compositions Globalalia (which deals explicitly with speech material from many languages) and Fabulous Paris – a virtual oratorio whcih uses speech in different ways to contrast our relationship to the local and personal with our relationship to the mass experience of the globalised mega-city. The problems in relating to both a local and a global audience are considered in relation to the composer's current project recording speech materials in local communities in the North East of England.

Modernization of Universities through Greater Interaction with Small Firms

1999 ◽  
Vol 13 (2) ◽  
pp. 119-126 ◽  
Author(s):  
Fiona Tilley ◽  
David Johnson
Keyword(s):  
Higher Education ◽  
Small Firms ◽  
Best Practice ◽  
Business Sector ◽  
North East ◽  
The North ◽  
The Uk ◽  
Political Economic ◽  
Relationship Of ◽  
The Relationship

This paper explores the ‘best practice’ interactions between universities and small firms in the UK. The purpose is to identify ways in which a university can build stronger and more effective links with small firms. The relationship between universities and small firms is of growing importance. There are political, economic and educational pressures which influence the behaviour and relationship of higher education toward the business sector, and small firms in particular. The wider context of the changes taking place within higher education are discussed. This is followed by the initial findings from a recently completed research project for the Council for Industry and Higher Education which investigated the foremost components in ‘best practice’ interactions and linkages between small firms and universities in the North East of England. Some preliminary ideas are suggested on how best practice can be further facilitated. These proposals are then interpreted in terms of the operational implications for universities and other strategic organizations involved in building linkages with small firms.

The Place of the North-Eastern Transvaal Sotho in the South Bantu Complex

Africa ◽  
1938 ◽  
Vol 11 (3) ◽  
pp. 265-293 ◽  
Author(s):  
Eileen Jensen Krige
Keyword(s):  
Total Population ◽  
The West ◽  
North West ◽  
Effective Barrier ◽  
North East ◽  
The North ◽  
North Eastern ◽  
Game Reserve ◽  
Olifants River ◽  
Opening Paragraph

Opening ParagraphThe Sotho of the North-Eastern Transvaal Lowveld occupy an area with fairly well-marked geographical boundaries. To the east, the Game Reserve, low-lying, unhealthy, very sparsely populated even in the old days, remains an effective barrier to contact with and further migrations from the Shangana-Tonga of Portuguese East Africa. South are the Olifants River and the towering Drakensberg range curving north-west then northwards to merge into the well-marked escarpment on the west dividing Lowveld from Highveld. On the north the Klein Letaba river roughly demarcates our area from the Venda and the Shangana-Tonga of the Knobnose Location. The Sotho-speaking Venda of Tswale and Moila, who fall well within this area, resemble in culture their Sotho-ized neighbours more than their own Venda kin to the north; but the Shangana- Tonga, who occupy most of the lower-lying eastern and north-eastern portion of the area and comprise at least one-third of its total population, are unassimilated strangers of different stock coming from the north-east and east. They have been entering since about 1840, usually in small bands, at first seeking the protection of and subjecting themselves to the Sotho owners of the land. On the arrival of the white man, some of their headmen were granted independent locations which have served as nuclei for the building up of more united tribal groups. (See accompanying map.)

Serpentinites in the North-East Ox Mountains, Eire

1966 ◽  
Vol 103 (2) ◽  
pp. 124-137 ◽  
Author(s):  
G. G. Lemon
Keyword(s):  
Fracture Zone ◽  
Additional Information ◽  
North East ◽  
The North ◽  
Relationship Of ◽  
Boundary Fracture ◽  
First Time ◽  
The Relationship

AbstractSix serpentinites occur in the Moinian granulites of the North-East Ox Mountains. Four have been known for some time and have been previously described. Additional information on these and the associated vermiculite deposits is provided. The remaining two serpentinites are described for the first time. A pyroxenite vein associated with one of these may have been produced by meta-morphic regeneration.The relationship of some of these serpentinites to the probable position of the Highland Boundary Fracture-zone in Eire is also discussed. Brief comparison is made with serpentinites occurring in the Scottish Moinian.

scholarly journals Appearance of the common paper nautilus Argonauta argo related to the increase of the sea surface temperature in the north-eastern Atlantic

2002 ◽  
Vol 82 (5) ◽  
pp. 855-858 ◽  
Author(s):  
A. Guerra ◽  
A.F. González ◽  
F. Rocha
Keyword(s):  
Surface Temperature ◽  
Sea Surface Temperature ◽  
First Record ◽  
Mature Female ◽  
Sea Surface ◽  
North West ◽  
The North ◽  
North Eastern ◽  
The Common ◽  
The Relationship

The relationship between the increase of the sea surface temperature observed off the Galician coast and the appearance of a tropical poikilotherm species Argonauta argo in these coasts is discussed. This is the first record of Argonautaargo in the north-west Iberian Peninsula. A female of this species was captured alive near the surface at dusk on 22 December 2000 in the Ria de Aldán (42°15′N–08°48′W). The specimen, a mature female of 70 mm mantle length and 96 mm shell diameter, died 36 hours after introduction in the tank.

scholarly journals Reproductive biology and diet of the grey sharpnose shark Rhizoprionodon oligolinx Springer, 1964 (Chondrichthyes: Carcharhinidae) from the north-eastern Arabian Sea

2017 ◽  
Vol 64 (4) ◽  
Author(s):  
G. B. Purushottama ◽  
Thakurdas . ◽  
V. Ramasubramanian ◽  
Gnyanaranjan Dash ◽  
K. V. Akhilesh ◽  
...  
Keyword(s):  
Reproductive Biology ◽  
Arabian Sea ◽  
Stomach Contents ◽  
Size At Maturity ◽  
Dietary Analysis ◽  
North West ◽  
The North ◽  
Northern Arabian Sea ◽  
North Eastern ◽  
Relationship Of

Information on reproductive biology is presented for the grey sharpnose shark Rhizoprionodon oligolinx Springer, 1964 (Chondrichthyes: Carcharhiniformes), collected off the north-west coast of India in the Arabian Sea. A total of 711 individuals, of 27.0 to 93.0 cm total length (TL), 180 to 2600 g total weight (TW) were used for the study. The lengthweight relationships were significantly different between the sexes. The size-at  maturity (Lm50) for females and males was estimated to be 62.3 and 59.5 cm TL respectively. Number of embryos ranged from 1 to 7 and the size at birth was estimated between 25 to 30 cm TL. Overall sex ratio favoured the females slightly at the rate of 1.27:1. There was significant positive correlation between maternal TL and number of embryos (p<0.001). Dietary analysis of stomach contents (%IRI) revealed that R. oligolinx feeds primarily on teleosts (95.5%), cephalopods (3.2%) and crustaceans (1.2%). This study presents the first detailed biological observation on size, sex composition, size-at-maturity (Lm50) and length-weight relationship of R. oligolinx from the northern Arabian Sea.

A Homestead Moat at Nuthampstead, Hertfordshire

1946 ◽  
Vol 26 (3-4) ◽  
pp. 138-144
Author(s):  
Audrey Williams
Keyword(s):  
Outer Edge ◽  
Royal Commission ◽  
The South ◽  
North West ◽  
North East ◽  
The North ◽  
North Eastern ◽  
Ancient Monuments ◽  
The Village ◽  
Western Half

A small moated site in Scales Park near the village of Nuthampstead, Hertfordshire (fig. 1), has lately been examined by the Ancient Monuments Department of the Ministry of Works. It lies just within the Hertfordshire-Essex boundary, four miles north-east of Buntingford and eight miles north-west of Bishop's Stortford. On the O.S. 6-in. sheet (Herts. 9 NE.) it is marked as The Warren, but not as an antiquity; nor is it included among the 139 homestead moats recorded for the county by the Royal Commission.Scales Park comprises something over 400 acres of well-grown woodland on the plateau which forms the watershed of the rivers Stort and Quin, both flowing south to join eventually the Thames. Its height above sea-level is 450 ft. on the northwest, declining gently to 400 ft. on the east and south. Geologically the area consists of chalky clay over the chalk.The moat of the Warren, enclosing an approximately square island about a quarter of an acre in size, varied in width from 10 to 25 ft. and at the time of excavation was filled with black boggy silt. Round its outer edge ran a low much-spread bank, 20 to 30 ft. wide but not more than 2 ft. high. The enclosure presented a puzzling combination of mounds and hollows. A large mound, 9 ft. 6 in. high, on a raised platform occupied the north-eastern half. The south-western half had centrally a similar platform, 5 ft. above the surface of the moat, with flanking mounds, 6 and 7 ft. high, at the corners (pl. xxiv b). The cavities between the mounds were practically level with the moat; slight ridges barred the western hollow and the south end of the eastern hollow.

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