Книги з теми "Current climatic conditions"
Щоб переглянути інші типи публікацій з цієї теми, перейдіть за посиланням: Current climatic conditions.
Оформте джерело за APA, MLA, Chicago, Harvard та іншими стилями
Ознайомтеся з топ-30 книг для дослідження на тему "Current climatic conditions".
Біля кожної праці в переліку літератури доступна кнопка «Додати до бібліографії». Скористайтеся нею – і ми автоматично оформимо бібліографічне посилання на обрану працю в потрібному вам стилі цитування: APA, MLA, «Гарвард», «Чикаго», «Ванкувер» тощо.
Також ви можете завантажити повний текст наукової публікації у форматі «.pdf» та прочитати онлайн анотацію до роботи, якщо відповідні параметри наявні в метаданих.
Переглядайте книги для різних дисциплін та оформлюйте правильно вашу бібліографію.
1
Bells, Youlsau. Republic of Palau current and projected impacts of climate change. [Melekeok]: Office of Environmental Response and Coordination, Office of the President of the Republic of Palau, 2001.
Знайти повний текст джерела
2
Porter, Julia. The vulnerability of Fiji to current climate variability and future change. North Ryde, N.S.W., Australia: Climate Impacts Centre, School of Earth Sciences, Macquarie University, 1994.
Знайти повний текст джерела
3
José de Fátima da Silva. El Niño: O fenômeno climático do século. Brasília, DF: Thesaurus Editora, 2000.
Знайти повний текст джерела
4
Mastrandrea, Michael D. Current and future impacts of extreme events in California: Final paper : a paper from California Climate Change Center. Sacramento, Calif.]: California Energy Commission, 2009.
Знайти повний текст джерела
5
Drought and climate change on water resources: Hearing before the Committee on Energy and Natural Resources, United States Senate, One Hundred Twelfth Congress, first session, to receive testimony on the current drought conditions affecting New Mexico and the status of reports to be issued pursuant to sections 9503 and 9506 of the Secure Water Act regarding a review of the current scientific understanding of the impacts of climate change on water resources and an assessment of the risks associated with climate change on water resources in certain river basins, Santa Fe, NM, April 27, 2011. Washington: U.S. G.P.O., 2011.
Знайти повний текст джерела
6
Winckell, Alain. Los efectos de El Niño en Tijuana, 1997-1998. Tijuana, B. C., México: El Colegio de la Frontera Norte, 2006.
Знайти повний текст джерела
7
WaterWatch: Maps and graphs of current water resources conditions. [Reston, Va.?: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.
Знайти повний текст джерела
8
WaterWatch: Maps and graphs of current water resources conditions. [Reston, Va.?: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.
Знайти повний текст джерела
9
Geological Survey (U.S.), ed. WaterWatch: Maps and graphs of current water resources conditions. [Reston, Va.?: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.
Знайти повний текст джерела
10
E, Welsh Susan, Coastal Marine Institute (Baton Rouge, La.), and United States. Minerals Management Service. Gulf of Mexico OCS Region, eds. Numerical simulation of Gulf of Mexico circulation under present and glacial climatic conditions. New Orleans: U.S. Dept. of the Interior, Minerals Management Service, Gulf of Mexico OCS Region, 1997.
Знайти повний текст джерела
11
Numerical simulation of Gulf of Mexico circulation under present and glacial climatic conditions. New Orleans: U.S. Dept. of the Interior, Minerals Management Service, Gulf of Mexico OCS Region, 1997.
Знайти повний текст джерела
12
E, Welsh Susan, Coastal Marine Institute (Baton Rouge, La.), and United States. Minerals Management Service. Gulf of Mexico OCS Region., eds. Numerical simulation of Gulf of Mexico circulation under present and glacial climatic conditions. New Orleans: U.S. Dept. of the Interior, Minerals Management Service, Gulf of Mexico OCS Region, 1997.
Знайти повний текст джерела
13
Ragland, Meg, and Sarah Keene Meltzoff. Listening to Sea Lions: Currents of Change from Galapagos to Patagonia. AltaMira Press, 2012.
Знайти повний текст джерела
14
Pagè, Fréric, Dominique Maison, and Michael Faulde. Current control strategies for infectious diseases in low-income countries. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198789833.003.0002.
Повний текст джерелаАнотація:
The burden of communicable diseases is ten times higher in low- and middle-income countries (LMICs) in terms of mortality rate and of years of life lost. Most of the LMCIs are in tropical or subtropical areas with vector-favorable climate conditions and poverty impeding access to improved water supply, sanitation, and efficient health care coverage. Public health strategies to control infectious diseases can be sorted by prevention level. Infectious diseases control strategies often combine actions from different prevention levels according to the stage of a disease. At the individual level, actions and interventions are succeeding in a logical cascade following the stage of the disease as community-level actions are implemented. We present strategies that have been implemented to control infectious diseases, their limits and the needs to attain successful control of infectious diseases in LMICs.
15
Armstrong, Christopher. Climate Change and Justice. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228637.013.231.
Повний текст джерелаАнотація:
Understanding the complex set of processes collected under the heading of climate change represents a considerable scientific challenge. But it also raises important challenges for our best moral theories. For instance, in assessing the risks that climate change poses, we face profound questions about how to weigh the respective harms it may inflict on current and future generations, as well as on humans and other species. We also face difficult questions about how to act in conditions of uncertainty, in which at least some of the consequences of climate change—and of various human interventions to adapt to or mitigate it—are difficult to predict fully. Even if we agree that mitigating climate change is morally required, there is room for disagreement about the precise extent to which it ought to be mitigated (insofar as there is room for underlying disagreement about the level of temperature rises that are morally permissible). Finally, once we determine which actions to take to reduce or avoid climate change, we face the normative question of who ought to bear the costs of those actions, as well as the costs associated with any climate change that nevertheless comes to pass.
16
Schmidt-Thomé, Philipp. Climate Change Adaptation. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.635.
Повний текст джерелаАнотація:
Climate change adaptation is the ability of a society or a natural system to adjust to the (changing) conditions that support life in a certain climate region, including weather extremes in that region. The current discussion on climate change adaptation began in the 1990s, with the publication of the Assessment Reports of the Intergovernmental Panel on Climate Change (IPCC). Since the beginning of the 21st century, most countries, and many regions and municipalities have started to develop and implement climate change adaptation strategies and plans. But since the implementation of adaptation measures must be planned and conducted at the local level, a major challenge is to actually implement adaptation to climate change in practice. One challenge is that scientific results are mainly published on international or national levels, and political guidelines are written at transnational (e.g., European Union), national, or regional levels—these scientific results must be downscaled, interpreted, and adapted to local municipal or community levels. Needless to say, the challenges for implementation are also rooted in a large number of uncertainties, from long time spans to matters of scale, as well as in economic, political, and social interests. From a human perspective, climate change impacts occur rather slowly, while local decision makers are engaged with daily business over much shorter time spans.Among the obstacles to implementing adaptation measures to climate change are three major groups of uncertainties: (a) the uncertainties surrounding the development of our future climate, which include the exact climate sensitivity of anthropogenic greenhouse gas emissions, the reliability of emission scenarios and underlying storylines, and inherent uncertainties in climate models; (b) uncertainties about anthropogenically induced climate change impacts (e.g., long-term sea level changes, changing weather patterns, and extreme events); and (c) uncertainties about the future development of socioeconomic and political structures as well as legislative frameworks.Besides slow changes, such as changing sea levels and vegetation zones, extreme events (natural hazards) are a factor of major importance. Many societies and their socioeconomic systems are not properly adapted to their current climate zones (e.g., intensive agriculture in dry zones) or to extreme events (e.g., housing built in flood-prone areas). Adaptation measures can be successful only by gaining common societal agreement on their necessity and overall benefit. Ideally, climate change adaptation measures are combined with disaster risk reduction measures to enhance resilience on short, medium, and long time scales.The role of uncertainties and time horizons is addressed by developing climate change adaptation measures on community level and in close cooperation with local actors and stakeholders, focusing on strengthening resilience by addressing current and emerging vulnerability patterns. Successful adaptation measures are usually achieved by developing “no-regret” measures, in other words—measures that have at least one function of immediate social and/or economic benefit as well as long-term, future benefits. To identify socially acceptable and financially viable adaptation measures successfully, it is useful to employ participatory tools that give all involved parties and decision makers the possibility to engage in the process of identifying adaptation measures that best fit collective needs.
17
Olivera Villaroel, Sazcha Marcelo, and Gustavo Sosa Núñez((Coordinador). Impactos del cambio climático : una visión desde México. "UNIVERSIDAD AUTÓNOMA METROPOLITANA- INSTITUTO DE INVESTIGACIONES DR. JOSÉ MARÍA LUIS MORA", 2022. http://dx.doi.org/10.24275/9786072824638.
Повний текст джерелаАнотація:
"Climate change is the most important problem facing humanity. Evidence on the effect of human activity on the basic conditions of the climate has permeated the national level, and states seem to be willing to formulate strategies to counter the problem, either through mitigation or adaptation measures. Recognizing that climate change is a multifactorial, interdisciplinary problem and transversal to public policies, this project brings together contributions from academic specialists in the subject and its purpose is to explore the current state of the art in Mexico, present research advances, as well as propose paths to explore."
18
Lykholat, Yuriy. Effects of pollution and climate change on the ecosystem components. OKTAN PRINT s.r.o., 2021. http://dx.doi.org/10.46489/eopacc-1204211.
Повний текст джерелаАнотація:
The book contains the study results of the environmental and soil conditions of the transformed territories, the ecological patterns of woody plants natural communities’ formation as well as the features of the herbaceous communities’ succession in flooded areas. The current state of forest areas is highlighted, the problems of forest management and their exploitation in Ukraine are outlined. Aspects of anthropogenic impact on natural aquatic ecosystems are shown and various biotesting methods of negative effects are characterized. The relationship between the presence of exogenous biologically active chemical compounds in the environment and damage to the endocrine system of animals has been revealed. The scientific manuscript is intended for ecologists, specialists interested in environmental management and environmental protection. The book may be useful for graduate students and scientific researchers.
19
Brindza, Ján, and Olga Grygorieva, eds. Book of Abstracts of the 5th International Scientific Conference Agrobiodiversity for Improving the Nutrition, Health, Quality of Life and Spiritual Human Development. Slovak University of Agriculture in Nitra, Slovakia, 2021. http://dx.doi.org/10.15414/2021.9788055224015.
Повний текст джерелаАнотація:
International conference aims to create more space and conditions for a broader discussion and search for all available solutions for the conservation and use of agrobiodiversity within the possibilities that research teams in individual countries and workplaces have. Research teams usually focus only on solving a specific biological problem of a plant species. That's right. But it would be appropriate for research teams to go beyond the research barriers and connect research results to practical applications, conditions and current societal challenges not only to improve nutrition, health and quality of life, but also to areas related to spiritual human development, and of humankind.Therefore, the conference organizers included in the program lectures focused on ethics in biological research, the use of plant species and nature for human healing, the use of agroforestry systems for food production with the current solution of adverse climate change, practical use of plants for new therapy and rehabilitation of humans and other specific and unusual areas.
20
Busuioc, Aristita, and Alexandru Dumitrescu. Empirical-Statistical Downscaling: Nonlinear Statistical Downscaling. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.770.
Повний текст джерелаАнотація:
This is an advance summary of a forthcoming article in the Oxford Research Encyclopedia of Climate Science. Please check back later for the full article.The concept of statistical downscaling or empirical-statistical downscaling became a distinct and important scientific approach in climate science in recent decades, when the climate change issue and assessment of climate change impact on various social and natural systems have become international challenges. Global climate models are the best tools for estimating future climate conditions. Even if improvements can be made in state-of-the art global climate models, in terms of spatial resolution and their performance in simulation of climate characteristics, they are still skillful only in reproducing large-scale feature of climate variability, such as global mean temperature or various circulation patterns (e.g., the North Atlantic Oscillation). However, these models are not able to provide reliable information on local climate characteristics (mean temperature, total precipitation), especially on extreme weather and climate events. The main reason for this failure is the influence of local geographical features on the local climate, as well as other factors related to surrounding large-scale conditions, the influence of which cannot be correctly taken into consideration by the current dynamical global models.Impact models, such as hydrological and crop models, need high resolution information on various climate parameters on the scale of a river basin or a farm, scales that are not available from the usual global climate models. Downscaling techniques produce regional climate information on finer scale, from global climate change scenarios, based on the assumption that there is a systematic link between the large-scale and local climate. Two types of downscaling approaches are known: a) dynamical downscaling is based on regional climate models nested in a global climate model; and b) statistical downscaling is based on developing statistical relationships between large-scale atmospheric variables (predictors), available from global climate models, and observed local-scale variables of interest (predictands).Various types of empirical-statistical downscaling approaches can be placed approximately in linear and nonlinear groupings. The empirical-statistical downscaling techniques focus more on details related to the nonlinear models—their validation, strengths, and weaknesses—in comparison to linear models or the mixed models combining the linear and nonlinear approaches. Stochastic models can be applied to daily and sub-daily precipitation in Romania, with a comparison to dynamical downscaling. Conditional stochastic models are generally specific for daily or sub-daily precipitation as predictand.A complex validation of the nonlinear statistical downscaling models, selection of the large-scale predictors, model ability to reproduce historical trends, extreme events, and the uncertainty related to future downscaled changes are important issues. A better estimation of the uncertainty related to downscaled climate change projections can be achieved by using ensembles of more global climate models as drivers, including their ability to simulate the input in downscaling models. Comparison between future statistical downscaled climate signals and those derived from dynamical downscaling driven by the same global model, including a complex validation of the regional climate models, gives a measure of the reliability of downscaled regional climate changes.
21
Xue, Yongkang, Yaoming Ma, and Qian Li. Land–Climate Interaction Over the Tibetan Plateau. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.592.
Повний текст джерелаАнотація:
The Tibetan Plateau (TP) is the largest and highest plateau on Earth. Due to its elevation, it receives much more downward shortwave radiation than other areas, which results in very strong diurnal and seasonal changes of the surface energy components and other meteorological variables, such as surface temperature and the convective atmospheric boundary layer. With such unique land process conditions on a distinct geomorphic unit, the TP has been identified as having the strongest land/atmosphere interactions in the mid-latitudes.Three major TP land/atmosphere interaction issues are presented in this article: (1) Scientists have long been aware of the role of the TP in atmospheric circulation. The view that the TP’s thermal and dynamic forcing drives the Asian monsoon has been prevalent in the literature for decades. In addition to the TP’s topographic effect, diagnostic and modeling studies have shown that the TP provides a huge, elevated heat source to the middle troposphere, and that the sensible heat pump plays a major role in the regional climate and in the formation of the Asian monsoon. Recent modeling studies, however, suggest that the south and west slopes of the Himalayas produce a strong monsoon by insulating warm and moist tropical air from the cold and dry extratropics, so the TP heat source cannot be considered as a factor for driving the Indian monsoon. The climate models’ shortcomings have been speculated to cause the discrepancies/controversies in the modeling results in this aspect. (2) The TP snow cover and Asian monsoon relationship is considered as another hot topic in TP land/atmosphere interaction studies and was proposed as early as 1884. Using ground measurements and remote sensing data available since the 1970s, a number of studies have confirmed the empirical relationship between TP snow cover and the Asian monsoon, albeit sometimes with different signs. Sensitivity studies using numerical modeling have also demonstrated the effects of snow on the monsoon but were normally tested with specified extreme snow cover conditions. There are also controversies regarding the possible mechanisms through which snow affects the monsoon. Currently, snow is no longer a factor in the statistic prediction model for the Indian monsoon prediction in the Indian Meteorological Department. These controversial issues indicate the necessity of having measurements that are more comprehensive over the TP to better understand the nature of the TP land/atmosphere interactions and evaluate the model-produced results. (3) The TP is one of the major areas in China greatly affected by land degradation due to both natural processes and anthropogenic activities. Preliminary modeling studies have been conducted to assess its possible impact on climate and regional hydrology. Assessments using global and regional models with more realistic TP land degradation data are imperative.Due to high elevation and harsh climate conditions, measurements over the TP used to be sparse. Fortunately, since the 1990s, state-of-the-art observational long-term station networks in the TP and neighboring regions have been established. Four large field experiments since 1996, among many observational activities, are presented in this article. These experiments should greatly help further research on TP land/atmosphere interactions.
22
Holmes, Jonathan, and Philipp Hoelzmann. The Late Pleistocene-Holocene African Humid Period as Evident in Lakes. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.531.
Повний текст джерелаАнотація:
From the end of the last glacial stage until the mid-Holocene, large areas of arid and semi-arid North Africa were much wetter than present, during the interval that is known as the African Humid Period (AHP). During this time, large areas were characterized by a marked increase in precipitation, an expansion of lakes, river systems, and wetlands, and the spread of grassland, shrub land, and woodland vegetation into areas that are currently much drier. Simulations with climate models indicate that the AHP was the result of orbitally forced increase in northern hemisphere summer insolation, which caused the intensification and northward expansion of the boreal summer monsoon. However, feedbacks from ocean circulation, land-surface cover, and greenhouse gases were probably also important.Lake basins and their sediment archives have provided important information about climate during the AHP, including the overall increases in precipitation and in rates, trajectories, and spatial variations in change at the beginning and the end of the interval. The general pattern is one of apparently synchronous onset of the AHP at the start of the Bølling-Allerød interstadial around 14,700 years ago, although wet conditions were interrupted by aridity during the Younger Dryas stadial. Wetter conditions returned at the start of the Holocene around 11,700 years ago covering much of North Africa and extended into parts of the southern hemisphere, including southeastern Equatorial Africa. During this time, the expansion of lakes and of grassland or shrub land vegetation over the area that is now the Sahara desert, was especially marked. Increasing aridity through the mid-Holocene, associated with a reduction in northern hemisphere summer insolation, brought about the end of the AHP by around 5000–4000 years before present. The degree to which this end was abrupt or gradual and geographically synchronous or time transgressive, remains open to debate. Taken as a whole, the lake sediment records do not support rapid and synchronous declines in precipitation and vegetation across the whole of North Africa, as some model experiments and other palaeoclimate archives have suggested. Lake sediments from basins that desiccated during the mid-Holocene may have been deflated, thus providing a misleading picture of rapid change. Moreover, different proxies of climate or environment may respond in contrasting ways to the same changes in climate. Despite this, there is evidence of rapid (within a few hundred years) termination to the AHP in some regions, with clear signs of a time-transgressive response both north to south and east to west, pointing to complex controls over the mid-Holocene drying of North Africa.
23
Williams, Jacqueline, and Paul Martin, eds. Defending the Social Licence of Farming. CSIRO Publishing, 2011. http://dx.doi.org/10.1071/9780643104549.
Повний текст джерелаАнотація:
Issues including climate variability, water scarcity, animal welfare and declining biodiversity have led to increasing demands on farmers to conduct and communicate their farming practices so as to protect their ‘social licence to farm’. Farmers are increasingly expected to demonstrate their social and environmental responsibility as a pre-condition to being allowed to carry out their preferred farming and commercial practices. Current examples include the live animal export trade, battles over protection of aquifers from mining, and contests over rural carbon emissions.
In Defending the Social Licence of Farming, authors from Australia, the USA, Europe and Iceland document the diverse issues associated with the 'social licence to farm'. They provide examples of different sectors’ strategies and experiences, and give specific indications of what is involved in coping successfully with this political and legal dimension of farming.
As resources become scarce and society’s expectations more diverse and demanding, farming can expect that social licence issues will become both more difficult and more important. The book suggests that the old models of response, largely focused on defensive positions, will often be insufficient to protect the interests of both farmers and the community. This book will provide a useful stimulus for innovation and proactive policies to defend the social licence of the farm sector.
24
Jacobsen, Dean, and Olivier Dangles. Ecology of High Altitude Waters. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198736868.001.0001.
Повний текст джерелаАнотація:
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.
25
Anderson, Michael, and Corinne Roughley. Scotland's Populations from the 1850s to Today. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198805830.001.0001.
Повний текст джерелаАнотація:
The last book-length study of Scottish population history was published in 1977, and it stopped in 1939. This book uses much hitherto unexploited material to throw new light on many topics. It sets current and recent population changes in their long-term context, exploring how the legacies of past demographic change have combined with a history of weak industrial investment, employment insecurity, deprivation and poor living conditions to produce the population profiles and changes of Scotland today. A major argument of this book is that Scotland has had multiple population histories, with great variability in population change, migration patterns, nuptiality, fertility, and mortality, and that these can be directly linked to its wide diversity of topography, climate and natural resources, which are in turn significantly linked to the many differences in local agrarian systems, settlement patterns and housing, transport accessibility, and local industries and other employments. This diversity and these linkages are explored throughout the book. However, the book also shows that, on all the major demographic variables, there have been features that stand out as making Scotland different both from England and Wales and from other parts of Europe. Emigration was higher, nuptiality lower, marital fertility higher until the 1980s, and mortality persistently higher, especially in the West Central Belt of the country; the only exception, in a comparative context, was low infant mortality in the later nineteenth century. The reasons behind these differences are extensively explored.
26
Wang, Bin. Intraseasonal Modulation of the Indian Summer Monsoon. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.616.
Повний текст джерелаАнотація:
The strongest Indian summer monsoon (ISM) on the planet features prolonged clustered spells of wet and dry conditions often lasting for two to three weeks, known as active and break monsoons. The active and break monsoons are attributed to a quasi-periodic intraseasonal oscillation (ISO), which is an extremely important form of the ISM variability bridging weather and climate variation. The ISO over India is part of the ISO in global tropics. The latter is one of the most important meteorological phenomena discovered during the 20th century (Madden & Julian, 1971, 1972). The extreme dry and wet events are regulated by the boreal summer ISO (BSISO). The BSISO over Indian monsoon region consists of northward propagating 30–60 day and westward propagating 10–20 day modes. The “clustering” of synoptic activity was separately modulated by both the 30–60 day and 10–20 day BSISO modes in approximately equal amounts. The clustering is particularly strong when the enhancement effect from both modes acts in concert. The northward propagation of BSISO is primarily originated from the easterly vertical shear (increasing easterly winds with height) of the monsoon flows, which by interacting with the BSISO convective system can generate boundary layer convergence to the north of the convective system that promotes its northward movement. The BSISO-ocean interaction through wind-evaporation feedback and cloud-radiation feedback can also contribute to the northward propagation of BSISO from the equator. The 10–20 day oscillation is primarily produced by convectively coupled Rossby waves modified by the monsoon mean flows. Using coupled general circulation models (GCMs) for ISO prediction is an important advance in subseasonal forecasts. The major modes of ISO over Indian monsoon region are potentially predictable up to 40–45 days as estimated by multiple GCM ensemble hindcast experiments. The current dynamical models’ prediction skills for the large initial amplitude cases are approximately 20–25 days, but the prediction of developing BSISO disturbance is much more difficult than the prediction of the mature BSISO disturbances. This article provides a synthesis of our current knowledge on the observed spatial and temporal structure of the ISO over India and the important physical processes through which the BSISO regulates the ISM active-break cycles and severe weather events. Our present capability and shortcomings in simulating and predicting the monsoon ISO and outstanding issues are also discussed.
27
Beerling, David. The Emerald Planet. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780192806024.001.0001.
Повний текст джерелаАнотація:
Global warming is contentious and difficult to measure, even among the majority of scientists who agree that it is taking place. Will temperatures rise by 2ºC or 8ºC over the next hundred years? Will sea levels rise by 2 or 30 feet? The only way that we can accurately answer questions like these is by looking into the distant past, for a comparison with the world long before the rise of mankind. We may currently believe that atmospheric shifts, like global warming, result from our impact on the planet, but the earth's atmosphere has been dramatically shifting since its creation. This book reveals the crucial role that plants have played in determining atmospheric change - and hence the conditions on the planet we know today. Along the way a number of fascinating puzzles arise: Why did plants evolve leaves? When and how did forests once grow on Antarctica? How did prehistoric insects manage to grow so large? The answers show the extraordinary amount plants can tell us about the history of the planet -- something that has often been overlooked amongst the preoccuputations with dinosaur bones and animal fossils. David Beerling's surprising conclusions are teased out from various lines of scientific enquiry, with evidence being brought to bear from fossil plants and animals, computer models of the atmosphere, and experimental studies. Intimately bound up with the narrative describing the dynamic evolution of climate and life through Earth's history, we find Victorian fossil hunters, intrepid polar explorers and pioneering chemists, alongside wallowing hippos, belching volcanoes, and restless landmasses.
28
Meijers, Tim. Justice Between Generations. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228637.013.233.
Повний текст джерелаАнотація:
A wide range of issues in moral, political, and legal philosophy fall under the heading of “intergenerational justice,” such as questions of justice between the young and the old, obligations to more-or-less distant past and future generations, generational sovereignty, and the boundaries of democratic decision-making.These issues deserve our attention first because they are of great social importance. Solving the challenges raised by aging, stable pension funding, and increasing healthcare costs, for example, requires a view on what justice between age groups demands. Climate change, resource depletion, environmental degradation, population growth, and the like, raise serious concerns about the conditions under which future people will have to live. What kind of world should we bequest to future generations?Second, this debate has theoretical significance. Questions of intergenerational justice force reconsideration of the fundamental commitments (on scope, pattern, site, and currency) of existing moral and political theories. The age-group debate has led to fundamental questions about the pattern of distributive justice: Should we care about people’s lives considered as whole being equally good? This has implausible implications. Can existing accounts be modified to avoid such problematic consequences?Justice between nonoverlapping generations raises a different set of questions. One important worry is about the pattern of intergenerational justice—are future generations owed equality, or should intergenerational justice be cast in terms of sufficiency? Another issue is the currency of intergenerational justice: what kind of goods should be transferred? Perhaps the most puzzling worry resulting from this debate translates into a worry about scope: do obligations of justice extend to future people? Most conventional views on the scope of justice—those that focus on shared coercive institutions, a common culture, a cooperative scheme for mutual advantage—cannot easily be extended to include future generations. Even humanity-based views, which seem most hospitable to the inclusion of future generations, are confronted with what Parfit called the nonidentity problem, which results from the fact that future people are mostly possible people: because of the lack of a fixed identity of future people, it is often impossible to harm them in the comparative sense.
29
López, Ivan, ed. Aftershocks: Globalism and the Future of Democracy. Universidad de Zaragoza, 2021. http://dx.doi.org/10.26754/uz.978-84-18321-12-2.
Повний текст джерелаАнотація:
This digital publication consists of a selection of 56 papers presented at the 16th International Conference of the International Society for the Study of European Ideas (ISSEI), held at the University of Zaragoza, 2-5 July 2019, the general theme of which was ‘Aftershocks: Globalism and the Future of Democracy’. Sponsored by The Aragonese Association of Sociology, the conference was well-attended – 170 participants from 28 countries met to discuss a wide variety of topics in 29 workshops. The feedback we received from participants confirmed that they had greatly enjoyed the venue of the conference, that they appreciated the warm welcome they had received and the congenial social atmosphere and opportunity to attend workshops on subjects that were not only in their own field of expertise. No one, of course, could have predicted that our world – our work and life as individuals, as communities and as nations – would change so suddenly and radically eighteen months after the conference, with the rapid and devastating spread of the Convid-19 pandemic. The current deepening global crisis along with the challenge of climate change and growing international tensions are a stark reminder of how vulnerable our societies, our civilization, and our species are. The shocks and aftershocks of these crises are felt today in every corner of the world and in every aspect of our global and local economies, and most obviously in the sociopolitical arena. As several of the conference workshops on the multiple crises Europe and the world face today – from the migrant crisis to the rise of populism and deepening inequality between rich and poor – showed – and as the Covid-19 pandemic has so cruelly brought home to us – we simply cannot take the achievements of human civilization for granted and must find ways to meet the fundamental social and political needs of human beings not only in our own neighborhoods, cities and countries, but ultimately in the world as a whole: their living conditions, livelihoods, social services, education and healthcare, human rights and political representation. Several of the workshops, as I mentioned, directly addressed these issues and emphasized the need for building social resilience based on tolerance, solidarity and equity. This too is why, as academics, we should continue to initiate and engage in collective reflection and debate on how to foster and strengthen human communities and human solidarity. Finally, I want to thank the participants and workshop chairs for their contribution to the success of the conference. It was a pleasure for me to work with the university organizing team and with ISSEI’s team in bringing this about, and I am particularly proud that my university and the city of Zaragoza hosted this conference.
30
Wojewodzic, Tomasz. Procesy dywestycji i dezagraryzacji w rolnictwie o rozdrobnionej strukturze agrarnej. Publishing House of the University of Agriculture in Krakow, 2017. http://dx.doi.org/10.15576/978-83-66602-31-1.
Повний текст джерелаАнотація:
The turn of the 20th and 21st centuries has been a very dynamic period of change in Poland and around the world; also a period of change in thinking about the economy and agriculture. The present work is a study of the decline, divestments and development of agriculture in the areas of fragmented farming structure. The reflections presented herein, upon the processes of the remodelling of agrarian structures, of divestments in farming, and disagrarisation, are mostly anchored in the achievements of the theory of spatial economy (land management), and the microeconomic theories of choice, including the theory of an agricultural holding (farm) and land rent theories. The work focuses on the economic issues of remodelling the agrarian structure, but due to the nature of the issues discussed herein, specifically in relation to family-owned farms, the social and environmental aspects also needed to be taken into account – in response to the need for a heterogeneous approach, which is increasingly stressed in economic sciences today. The main objective of the research was to diagnose and assess the scale and scope of the mechanisms and processes that inform the decline and growth of agricultural holdings in the areas with fragmented farming structure. The study covered the area comprising four regions (provinces) of south-eastern Poland, which – according to the FADN nomenclature – form the macro region of Małopolska and Pogórze. The study of subject literature has been enriched with an analysis of available statistics; data from the Farm Accountancy Data Network (FADN); information obtained from the Department of Programming and Reporting at the Agency for Restructuring and Modernisation of Agriculture; and author’s own research conducted among farm owners. The information thus obtained made it possible to: • Determine the theoretical premises for the spatial diversity of agriculture, and the role of small farms in the shaping of agrarian structure. • Adapt the concept of “divestment” for the description and analysis of the phenomena occurring in agriculture. • Indicate the role and importance of the processes of divestment and disagrarisation in the restructuring of agriculture. • Assess the natural, social and economic determinants of the process of restructuring agriculture in areas with fragmented farming structure. • Assess selected aspects of economic efficiency of agriculture in areas with fragmented farming structure, with the focus on small and micro farms. • Carry out an ex ante evaluation of the impact of agricultural policy instruments on the process of restructuring of agriculture in the macro region of Małopolska and Pogórze. • Identify the indicators of decline and fall, and barriers to the liquidation of farms. • Assess the relationship between the level of socio-economic development, the structure of farming, and the quality of agricultural production space in a given territorial unit, versus the intensity of the economic and production disagrarisation processes in agricultural holdings. • Propose targeted solutions conducive to the improvement of the farming structure in areas with a high framentation of agriculture. Observation of the processes occurring in agriculture, and the scientific theories created on the basis thereof, have shown that even the smallest farms have a chance to continue in existence, provided that we are able to positively verify their adaptation to the changing conditions in the environment. Carrying out farming activity is a prerequisite for implementing the economic, social and environmental functions associated with family farms. At the same time, based on the analyses performed, we need to assume that the advanced processes of the production and economic disagrarisation of agricultural holdings are to a greater extent determined by the anatomical features of agriculture, and by the natural conditions, than by the level of socio-economic development of the given territorial unit. In the current economic climate, the remodelling of the agrarian structure is only possible with the active participation of the institutions responsible for the creation of economic growth and agricultural policy development. It is extremely important from the point of view of environmental protection, and the viability of rural areas, to support small farms engaged in agricultural activities, and to introduce such instruments that will enable the replacement of an economic collapse with divestments, carried out in a planned manner, and allowing for thus released agricultural resources to find alternative application in units with a higher development potential. The area of theoretical research requiring further exploration includes the issues such as transactional costs of the liquidation of agricultural holdings, and the assessment of the economic effectiveness of conducting divestments.