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Books on the topic 'Speed of Adjustment (SOA)'

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Author: Grafiati

Published: 10 December 2022

Last updated: 28 January 2023

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1

Driffield, Nigel. Inward investment, industry concentration and the speed of adjustment. Cardiff: Cardiff Business School, 1999.

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2

Bivin, David. Multi-product firms and the speed of adjustment in inventory models. Antwerpen: Universiteit Antwerpen, 1992.

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3

Modeling wind adjustment factor and midflame wind speed for Rothermel's surface fire spread model. Fort Collins, CO: United States Department of Agriculture/Forest Service, Rocky Mountain Research Station, 2012.

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4

Nsouli, Saleh M. The speed of adjustment and the sequencing of economic reforms: Issues and guidelines for policymakers. [Washington, D.C.]: International Monetary Fund, IMF Institute, 2002.

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5

United States. Congress. House. A bill to amend part C of title XVIII of the Social Security Act to speed up by 1 year the application of risk adjustment factors under the Medicare+Choice Program. [Washington, D.C.?]: [United States Government Printing Office], 1997.

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6

M, Hyde G., Washington State University. Cooperative Extension., and United States. Dept. of Agriculture., eds. Potato harvester chain speed adjustment. Pullman: Cooperative Extension, College of Agriculture and Home Economics, Washington State University, 1990.

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7

Naseer, Abdul, S. M. Ali Abbas, and Kenji Moriyama. Fiscal Adjustment in Sudan: Size, Speed and Composition. International Monetary Fund, 2010.

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8

Naseer, Abdul, S. M. Ali Abbas, and Kenji Moriyama. Fiscal Adjustment in Sudan: Size, Speed and Composition. International Monetary Fund, 2010.

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9

Naseer, Abdul, S. M. Ali Abbas, and Kenji Moriyama. Fiscal Adjustment in Sudan: Size, Speed and Composition. International Monetary Fund, 2010.

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10

FANG, LU. Psychological adjustment Quick-speed Roms: Case practical version. China Legal Publishing House, 2014.

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11

FANG, LU. Psychological adjustment Quick-speed Roms: Case practical version. China Legal Publishing House, 2014.

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12

(Editor), Markus Zirn, and Harish Gaur (Editor), eds. BPEL Cookbook: Best Practices for SOA-based integration and composite applications development. Packt Publishing, 2006.

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13

Speed of adjustment and inflation: Unemployment tradeoff in developing countries : case of India. Ahmedabad: Indian Institute of Management, 2011.

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14

Fund, International Monetary, ed. Openness, human developmnet. and fiscal policies: Effects on economic growth and speed of adjustment. Washington, D.C: International Monetary Fund, 1993.

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15

Villanueva, Delano. Openness, Human Development, and Fiscal Policies - Effects on Economic Growth and Speed of Adjustment. International Monetary Fund, 1993.

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16

Villanueva, Delano. Openness, Human Development, and Fiscal Policies: Effects on Economic Growth and Speed of Adjustment. International Monetary Fund, 1993.

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17

Villanueva, Delano. Openness, Human Development, and Fiscal Policies - Effects on Economic Growth and Speed of Adjustment. International Monetary Fund, 1993.

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18

Räisänen, Jouni. Future Climate Change in the Baltic Sea Region and Environmental Impacts. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.634.

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The warming of the global climate is expected to continue in the 21st century, although the magnitude of change depends on future anthropogenic greenhouse gas emissions and the sensitivity of climate to them. The regional characteristics and impacts of future climate change in the Baltic Sea countries have been explored since at least the 1990s. Later research has supported many findings from the early studies, but advances in understanding and improved modeling tools have made the picture gradually more comprehensive and more detailed. Nevertheless, many uncertainties still remain.In the Baltic Sea region, warming is likely to exceed its global average, particularly in winter and in the northern parts of the area. The warming will be accompanied by a general increase in winter precipitation, but in summer, precipitation may either increase or decrease, with a larger chance of drying in the southern than in the northern parts of the region. Despite the increase in winter precipitation, the amount of snow is generally expected to decrease, as a smaller fraction of the precipitation falls as snow and midwinter snowmelt episodes become more common. Changes in windiness are very uncertain, although most projections suggest a slight increase in average wind speed over the Baltic Sea. Climatic extremes are also projected to change, but some of the changes will differ from the corresponding change in mean climate. For example, the lowest winter temperatures are expected to warm even more than the winter mean temperature, and short-term summer precipitation extremes are likely to become more severe, even in the areas where the mean summer precipitation does not increase.The projected atmospheric changes will be accompanied by an increase in Baltic Sea water temperature, reduced ice cover, and, according to most studies, reduced salinity due to increased precipitation and river runoff. The seasonal cycle of runoff will be modified by changes in precipitation and earlier snowmelt. Global-scale sea level rise also will affect the Baltic Sea, but will be counteracted by glacial isostatic adjustment. According to most projections, in the northern parts of the Baltic Sea, the latter will still dominate, leading to a continued, although decelerated, decrease in relative sea level. The changes in the physical environment and climate will have a number of environmental impacts on, for example, atmospheric chemistry, freshwater and marine biogeochemistry, ecosystems, and coastal erosion. However, future environmental change in the region will be affected by several interrelated factors. Climate change is only one of them, and in many cases its effects may be exceeded by other anthropogenic changes.

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19

Building Trust at the Speed of Change: The Power of the Relationship-Based Corporation. AMACOM, 1999.

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20

Yang, Kun. Observed Regional Climate Change in Tibet over the Last Decades. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.587.

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The Tibetan Plateau (TP) is subjected to strong interactions among the atmosphere, hydrosphere, cryosphere, and biosphere. The Plateau exerts huge thermal forcing on the mid-troposphere over the mid-latitude of the Northern Hemisphere during spring and summer. This region also contains the headwaters of major rivers in Asia and provides a large portion of the water resources used for economic activities in adjacent regions. Since the beginning of the 1980s, the TP has undergone evident climate changes, with overall surface air warming and moistening, solar dimming, and decrease in wind speed. Surface warming, which depends on elevation and its horizontal pattern (warming in most of the TP but cooling in the westernmost TP), was consistent with glacial changes. Accompanying the warming was air moistening, with a sudden increase in precipitable water in 1998. Both triggered more deep clouds, which resulted in solar dimming. Surface wind speed declined from the 1970s and started to recover in 2002, as a result of atmospheric circulation adjustment caused by the differential surface warming between Asian high latitudes and low latitudes.The climate changes over the TP have changed energy and water cycles and has thus reshaped the local environment. Thermal forcing over the TP has weakened. The warming and decrease in wind speed lowered the Bowen ratio and has led to less surface sensible heating. Atmospheric radiative cooling has been enhanced, mainly through outgoing longwave emission from the warming planetary system and slightly enhanced solar radiation reflection. The trend in both energy terms has contributed to the weakening of thermal forcing over the Plateau. The water cycle has been significantly altered by the climate changes. The monsoon-impacted region (i.e., the southern and eastern regions of the TP) has received less precipitation, more evaporation, less soil moisture and less runoff, which has resulted in the general shrinkage of lakes and pools in this region, although glacier melt has increased. The region dominated by westerlies (i.e., central, northern and western regions of the TP) received more precipitation, more evaporation, more soil moisture and more runoff, which together with more glacier melt resulted in the general expansion of lakes in this region. The overall wetting in the TP is due to both the warmer and moister conditions at the surface, which increased convective available potential energy and may eventually depend on decadal variability of atmospheric circulations such as Atlantic Multi-decadal Oscillation and an intensified Siberian High. The drying process in the southern region is perhaps related to the expansion of Hadley circulation. All these processes have not been well understood.

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21

Kamat, Deepak M., Henry M. Adam, and Rebecca A. Baum, eds. Quick Reference Guide to Pediatric Care. 2nd ed. American Academy of Pediatrics, 2017. http://dx.doi.org/10.1542/9781610021128.

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Significantly revised and updated, the second edition of this popular quick reference guide provides information and advice on 190 areas of current pediatric care, everything from abdominal pain and ADHD, to headache and herpes infections, to weight loss and wheezing. This indispensable resource delivers practical, action-orientated, clinical solutions for healthcare professionals to use during or between patient encounters. Authoritative content is presented in a concise outline format that helps speed and simplify decision-making. Regardless of the patient presentation you're confronted with, you'll have quick access to the help you need to Efficiently evaluate signs and symptoms. Order the right screening/diagnostic tests. Implement approved therapeutic strategies. Prescribe safe and effective medications. Recommend proven prevention measures. Confidently respond to parent questions. 35 new chapters including Adjustment disorder Anxiety Ataxia Coagulation disorders Cyanosis Dental problems Depression Drug interactions and adverse effects Fetal alcohol spectrum disorder Fragile X syndrome Hemangiomas Hypocalcemia, hypercalcemia, and hypercalcuria Inattention Inflammatory bowel disease Klinefelter syndrome Learning difficulty Learning disorders Metabolic disorders beyond the newborn period Munchausen syndrome by proxy: medical child abuse Neural tube defects Oppositional defiant disorder Pancreatitis Papulosquamous disease Pierre Robin syndrome Prader-Willi syndrome Screening for genetic-metabolic diseases Self-harm Sexual abuse of children Sleep disturbances Speech and language concerns Substance use Symptoms of emotional disturbances in young children (birth to 5) Temper tantrums and breath-holding spells Turner syndrome and Noonan syndrome Vitamin D inadequacy

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