Books: 'Pattern grading'

1

Merryweather, John. Pattern cutting: Grading : Module 9. Rossendale: Footwear OPEN TECH Unit, 1986.

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2

K, Mullet Kathy, and Young Margaret Prevatt, eds. Concepts of pattern grading: Techniques for manual and computer grading. New York: Fairchild Pub., 2001.

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3

L, Moore Carolyn, Young Margaret Prevatt, and Moore Carolyn L, eds. Concepts of pattern grading: Techniques for manual and computer grading. 2nd ed. New York: Fairchild Books, 2009.

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4

Bernard, Zamkoff, ed. Grading techniques for modern design. New York: Fairchild Publications, 1990.

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5

British United Shoe Machinery Company Ltd. Instructions for coset grading: August : universal pattern grading machine, symbol BUPG. Leicester: British United Shoe Machinery Co., Ltd, 1986.

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6

Price, Jeanne. Grading techniques for fashion design. 2nd ed. New York: Fairchild Publications, 1996.

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7

Pattern grading for women's clothes: The technology of sizing. Oxford: BSP Professional, 1990.

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8

Cooklin, Gerry. Pattern grading for children's clothes: The technology of sizing. Oxford: BSP Professional, 1991.

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9

Cooklin, Gerry. Pattern grading for men's clothes: The technology of sizing. Oxford: Blackwell Scientific Publications, 1992.

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10

Cooklin, Gerry. Master patterns and grading for women's outsizes. Oxford: Blackwell Science, 1995.

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11

Taylor, Patrick J. Grading for the fashion industry: The theory and practice. 2nd ed. Cheltenham: Thornes, 1990.

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12

Gebbia, A. Modern method of women's & children's garment design: Measurement charts, pattern drafting, grading. Chicago: Master Designer, 1987.

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13

Gebbia, A. Modern method of women's & children's garment design: Measurement charts, pattern drafting, grading. Chicago: Master Designer, 1987.

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14

Chansarkar, B. A. Valuation patterns in an interdisciplinary course. London: Middlesex Business School, 1991.

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15

Microevolutionary patterns in Aboriginal Australia: A gradient analysis of clines. New York: Oxford University Press, 1993.

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16

Skifstad, Kurt D. High-speed range estimation based on intensity gradient analysis. New York: Springer-Verlag, 1991.

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17

Skifstad, Kurt D. High-speed range estimation based on intensity gradient analysis. New York: Springer-Verlag, 1991.

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18

High-speed range estimation based on intensity gradient analysis. New York: Springer-Verlag, 1991.

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19

Barrs, Myra. Patterns of learning: The Primary Language Record and the National Curriculum. London: Centre for Language in Primary Education, 1990.

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20

Crampton, G. R. Residential density patterns in London: Any role left for the exponential density gradient?. Reading: University of Reading, Department of Economics, 1990.

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21

Cooklin, Gerry. Pattern Grading for Childrens Clothing. Blackwell Science, 1991.

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22

Moore, Carolyn L., Kathy K. Mullet, and Margaret B. Prevatt Young. Concepts of Pattern Grading: Techniques for Manual and Computer Grading. Fairchild Books & Visuals, 2000.

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23

Concepts of Pattern Grading: Techniques for Manual and Computer Grading. Bloomsbury Publishing Plc, 2015.

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24

Lininger, Michele. Patternmaking and Grading Using Gerber's AccuMark Pattern Design Software. Pearson, 2014.

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25

Cooklin, Gerry. Pattern Grading for Womens' Clothes: The Technology of Sizing. Blackwell Science, 1990.

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26

Professional Pattern Grading for Women's, Men's, and Children's Apparel. Fairchild Books & Visuals, 2003.

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27

The Essentials of Pattern Grading: The Projection of Cartesian Coordinates Into a Spherical Geometry of Fractal Order 2.5 Using Collinear Scaling As the Algebraic Matrix..... Clarified. Hanover Phist, 2003.

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28

Warmkessel, L. H. Modern Shirt Drafting for Stock Patterns: Shirt Drafting and Grading. Master Designer, 1994.

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29

Barrs, Myra. Patterns of Learning. Centre for Language in Primary Education, 1991.

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30

Editors, Interweave Interweave. Gradient Style: Color-Shifting Techniques and Knitting Patterns. Interweave Press, LLC, 2019.

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31

Ohmann, Janet L. Regional gradient analysis and spatial pattern of woody plant communities in Oregon. 1995.

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32

Skifstad, Kurt D. High-Speed Range Estimation Based on Intensity Gradient Analysis. Springer, 2011.

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33

High-Speed Range Estimation Based on Intensity Gradient Analysis. Springer, 2012.

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34

Roberts, Ian S. D., Philip Mason, and Agnes B. Fogo. The renal biopsy. Edited by Christopher G. Winearls. Oxford University Press, 2015. http://dx.doi.org/10.1093/med/9780199592548.003.0018.

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This chapter describes the indications for renal biopsy, the procedure, processing of the specimen and the diagnostic method applied by the nephropathologist, and illustrates the spectrum of pathologies seen. The terminology used in renal pathology is explained and illustrated. Diagnostic algorithms are presented. More detailed descriptions of the various pathologies, and in particular the rarer entities, are provided in specific chapters. The focus will be on native renal diseases. The renal biopsy is an invasive procedure associated with a risk of serious complications. The decision to perform a biopsy is based on a careful risk: benefit assessment. The final diagnosis is usually derived from combining clinical and histological data; it is therefore essential that the nephrologist includes all relevant information on the pathology request form. Discussion of the biopsy findings at a multidisciplinary meeting is an important part of the diagnostic and management decision-making process. The essential starting point for histological diagnosis is to define the morphological abnormality at light microscopy, the ‘pattern of disease’. In only a minority of cases will this be sufficient to provide a firm diagnosis; more frequently the morphology provides the basis for formulating a differential diagnosis. Supplemental information from immunohistology and electron microscopy, in addition to clinical, biochemical, and serological data, are used to reach a precise diagnosis. In addition to diagnosis, the renal biopsy may provide prognostic information and be used to guide therapy. For inflammatory renal diseases in particular, the biopsy report will include measures of disease activity and chronicity. In some instances the diagnosis may already be clear, and the biopsy is performed for grading and staging purposes or to assist in decisions about treatment.

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35

Publishing, RB-Modernio. One Big Fat Notebook: Texture Background Pattern Gradient Cover - 200 Pages Gift Ruled Journal Modern Professional Notebook Ruled - Notebooks for Men and Women. Independently Published, 2020.

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36

O'Donnell, Ian. Undoing Death I. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198798477.003.0008.

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Capital punishment has been described as a ‘lottery’, implying that it operates at random; but in Ireland a pattern can be discerned. Murderers who avoided execution fell into one of six categories, with a clear gradient in how sympathetically they were viewed, as indicated by the duration of their coercive confinement and the likelihood that mercy would be recommended. At one end of the scale were those who destroyed an unwanted child, 92 per cent of whom aroused the sympathy of judge and jury and who were denied their liberty for 44 months, on average. At the other extreme were those whose treatment was capricious, only 20 per cent of whom received recommendations to mercy and whose average period of coercive confinement was 115 months. This chapter explores cases where the death penalty was imposed for the murder of an infant (usually, but not always, by the mother), romantic entanglements that had lethally soured, and sexual violence resulting in death.

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37

Gossai, Anala, Dorothea T. Barton, Judy R. Rees, Heather H. Nelson, and Margaret R. Karagas. Keratinocyte Cancers. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780190238667.003.0058.

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Keratinocyte cancers (KC) include basal and squamous cell carcinomas that arise from keratinocytes or their precursors. KCs are the most common malignancies in humans. Basal cell carcinoma (BCC) has higher incidence rates, but squamous cell carcinoma (SCC) causes most deaths. Despite increasing incidence rates, the mortality rates have not changed markedly in recent years. The geographic and demographic features of these tumors have remained consistent over the past several decades, with a gradient of increasing incidence rates with proximity to the equator, predominantly affecting fair-skinned populations. Risk increases with age, is higher in men than women, and is associated with artificial as well as natural exposure to UV light. There is emerging evidence that these malignancies, particularly BCCs, may be increasing in younger adults and among women. While basal and squamous cell carcinomas share etiological factors, the relative importance of these factors, pattern of exposure, molecular alterations, and even the factors themselves differ.

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38

Jacobsen, Dean, and Olivier Dangles. Ecology of High Altitude Waters. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198736868.001.0001.

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This book brings together current knowledge on patterns and processes in the ecology of streams, lakes, and wetlands situated at more than 3000 m above sea level. The alpine headwaters of the large Asian rivers and Lake Titicaca are both well-known and iconic examples. High altitude waters include more than these systems—they are both numerous and cover many habitat types, organisms, and specializations. The book provides an overview of the variety of aquatic ecosystems and habitats, their environmental features, prominent species, and their functional adaptations to the harsh aquatic environmental conditions through to global diversity patterns along altitudinal gradients, community dynamics, species interactions and dispersal, trophic relations, and energy flows. High altitude waters are ideal systems to address a broad range of topical themes in ecology because patterns and processes are both diverse and singular. The book highlights how key concepts in ecology (e.g. the stress gradient hypothesis, the biodiversity–ecosystem functioning relationship) could find relevant study models in high altitude waters. The usual perception of pristine mountain waters is far from true, particularly in the case of high altitude waters at low latitudes where human population density is often high, and local communities live in intimate contact with, utilize, influence, and exploit these aquatic systems. Climate change effects, extinction risks of mountain populations due to vanishing glaciers, multiple human impacts, management, and conservation are also treated thoroughly. The book is richly illustrated with diagrams and numerous pictures of these poorly known systems and species.

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39

Kroenke, Candyce, and Ichiro Kawachi. Socioeconomic Disparities in Cancer Incidence and Mortality. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780190238667.003.0009.

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The relationship between socioeconomic status (SES) and cancer is complex, dynamic, and evolving. Associations depend on SES measures, cancer type, sociodemographic factors including race/ethnicity, and historical trends. However, socioeconomic disadvantage is often associated with a higher risk of cancer, particularly cancers diagnosed at a late stage, as well as worse prognosis once diagnosed. Research on secular trends over the past 70 years has shown reversals of the socioeconomic gradient for lung and colorectal cancer consistent with differential trends by SES in patterns of smoking, diet, and obesity. Rates of these cancers are now currently higher in socioeconomically disadvantaged groups. SES is considered to be a “fundamental” determinant of health outcomes, and this appears true throughout the cancer spectrum—from cancer incidence to detection, treatment, and survival. Investigations over the past decade have increasingly considered the simultaneous impact of individual SES and area-level SES (as a contextual influence) on health outcomes.

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40

Books, Bee. For I Too Have Knucked and Bucked and Been Ready to Fight : Patterned Gradient: Journal / Diary / Sketchbook / Notebook / 120 Pages / Graph Paper / Gag Gift / Rap Music / Funny / Teacher Gift. Independently Published, 2020.

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41

Behera, Swadhin, and Toshio Yamagata. Climate Dynamics of ENSO Modoki Phenomena. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.612.

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The El Niño Modoki/La Niña Modoki (ENSO Modoki) is a newly acknowledged face of ocean-atmosphere coupled variability in the tropical Pacific Ocean. The oceanic and atmospheric conditions associated with the El Niño Modoki are different from that of canonical El Niño, which is extensively studied for its dynamics and worldwide impacts. A typical El Niño event is marked by a warm anomaly of sea surface temperature (SST) in the equatorial eastern Pacific. Because of the associated changes in the surface winds and the weakening of coastal upwelling, the coasts of South America suffer from widespread fish mortality during the event. Quite opposite of this characteristic change in the ocean condition, cold SST anomalies prevail in the eastern equatorial Pacific during the El Niño Modoki events, but with the warm anomalies intensified in the central Pacific. The boreal winter condition of 2004 is a typical example of such an event, when a tripole pattern is noticed in the SST anomalies; warm central Pacific flanked by cold eastern and western regions. The SST anomalies are coupled to a double cell in anomalous Walker circulation with rising motion in the central parts and sinking motion on both sides of the basin. This is again a different feature compared to the well-known single-cell anomalous Walker circulation during El Niños. La Niña Modoki is the opposite phase of the El Niño Modoki, when a cold central Pacific is flanked by warm anomalies on both sides.The Modoki events are seen to peak in both boreal summer and winter and hence are not seasonally phase-locked to a single seasonal cycle like El Niño/La Niña events. Because of this distinction in the seasonality, the teleconnection arising from these events will vary between the seasons as teleconnection path will vary depending on the prevailing seasonal mean conditions in the atmosphere. Moreover, the Modoki El Niño/La Niña impacts over regions such as the western coast of the United States, the Far East including Japan, Australia, and southern Africa, etc., are opposite to those of the canonical El Niño/La Niña. For example, the western coasts of the United States suffer from severe droughts during El Niño Modoki, whereas those regions are quite wet during El Niño. The influences of Modoki events are also seen in tropical cyclogenesis, stratosphere warming of the Southern Hemisphere, ocean primary productivity, river discharges, sea level variations, etc. A remarkable feature associated with Modoki events is the decadal flattening of the equatorial thermocline and weakening of zonal thermal gradient. The associated ocean-atmosphere conditions have caused frequent and persistent developments of Modoki events in recent decades.

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42

Benestad, Rasmus. Climate in the Barents Region. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.655.

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The Barents Sea is a region of the Arctic Ocean named after one of its first known explorers (1594–1597), Willem Barentsz from the Netherlands, although there are accounts of earlier explorations: the Norwegian seafarer Ottar rounded the northern tip of Europe and explored the Barents and White Seas between 870 and 890 ce, a journey followed by a number of Norsemen; Pomors hunted seals and walruses in the region; and Novgorodian merchants engaged in the fur trade. These seafarers were probably the first to accumulate knowledge about the nature of sea ice in the Barents region; however, scientific expeditions and the exploration of the climate of the region had to wait until the invention and employment of scientific instruments such as the thermometer and barometer. Most of the early exploration involved mapping the land and the sea ice and making geographical observations. There were also many unsuccessful attempts to use the Northeast Passage to reach the Bering Strait. The first scientific expeditions involved F. P. Litke (1821±1824), P. K. Pakhtusov (1834±1835), A. K. Tsivol’ka (1837±1839), and Henrik Mohn (1876–1878), who recorded oceanographic, ice, and meteorological conditions.The scientific study of the Barents region and its climate has been spearheaded by a number of campaigns. There were four generations of the International Polar Year (IPY): 1882–1883, 1932–1933, 1957–1958, and 2007–2008. A British polar campaign was launched in July 1945 with Antarctic operations administered by the Colonial Office, renamed as the Falkland Islands Dependencies Survey (FIDS); it included a scientific bureau by 1950. It was rebranded as the British Antarctic Survey (BAS) in 1962 (British Antarctic Survey History leaflet). While BAS had its initial emphasis on the Antarctic, it has also been involved in science projects in the Barents region. The most dedicated mission to the Arctic and the Barents region has been the Arctic Monitoring and Assessment Programme (AMAP), which has commissioned a series of reports on the Arctic climate: the Arctic Climate Impact Assessment (ACIA) report, the Snow Water Ice and Permafrost in the Arctic (SWIPA) report, and the Adaptive Actions in a Changing Arctic (AACA) report.The climate of the Barents Sea is strongly influenced by the warm waters from the Norwegian current bringing heat from the subtropical North Atlantic. The region is 10°C–15°C warmer than the average temperature on the same latitude, and a large part of the Barents Sea is open water even in winter. It is roughly bounded by the Svalbard archipelago, northern Fennoscandia, the Kanin Peninsula, Kolguyev Island, Novaya Zemlya, and Franz Josef Land, and is a shallow ocean basin which constrains physical processes such as currents and convection. To the west, the Greenland Sea forms a buffer region with some of the strongest temperature gradients on earth between Iceland and Greenland. The combination of a strong temperature gradient and westerlies influences air pressure, wind patterns, and storm tracks. The strong temperature contrast between sea ice and open water in the northern part sets the stage for polar lows, as well as heat and moisture exchange between ocean and atmosphere. Glaciers on the Arctic islands generate icebergs, which may drift in the Barents Sea subject to wind and ocean currents.The land encircling the Barents Sea includes regions with permafrost and tundra. Precipitation comes mainly from synoptic storms and weather fronts; it falls as snow in the winter and rain in the summer. The land area is snow-covered in winter, and rivers in the region drain the rainwater and meltwater into the Barents Sea. Pronounced natural variations in the seasonal weather statistics can be linked to variations in the polar jet stream and Rossby waves, which result in a clustering of storm activity, blocking high-pressure systems. The Barents region is subject to rapid climate change due to a “polar amplification,” and observations from Svalbard suggest that the past warming trend ranks among the strongest recorded on earth. The regional change is reinforced by a number of feedback effects, such as receding sea-ice cover and influx of mild moist air from the south.

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Books on the topic 'Pattern grading'

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