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  • 2000-2004  (458)
  • 1940-1944
  • 2003  (458)
  • 1
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Routledge
    Call number: AWI A5-18-91525
    Type of Medium: Monograph available for loan
    Pages: XVI, 421 S. , Ill., graph. Darst., Kt. , 25cm
    Edition: 8. ed.
    ISBN: 0415271711 (pbk.) , 0415271703
    Language: English
    Note: Contents: Preface to the eighth edition. - Acknowledgements. - 1 INTRODUCTION AND HISTORY OF METEOROLOGY AND CLIMATOLOGY. - A The atmosphere. - B Solar energy. - C Global circulation. - D Climatology. - E Mid-latitude disturbances. - F Tropical weather. - G Palaeoclimates. - H The global climate system. - 2 ATMOSPHERIC COMPOSITION, MASS AND STRUCTURE. - A Composition of the atmosphere. - 1 Primary gases. - 2 Greenhouse gases. - 3 Reactive gas species. - 4 Aerosols. - 5 Variations with height. - 6 Variations with latitude and season. - 7 Variations with time. - B Mass of the atmosphere. - 1 Total pressure. - 2 Vapour pressure C The layering of the atmosphere. - 1 Troposphere. - 2 Stratosphere. - 3 Mesosphere. - 4 Thermosphere. - 5 Exosphere and magnetosphere. - 3 SOLAR RADIATION AND THE GLOBAL ENERGY BUDGET. - A Solar radiation. - 1 Solar output. - 2 Distance from the sun. - 3 Altitude of the sun. - 4 Length of day. - B Surface receipt of solar radiation and its effects. - 1 Energy transfer within the earth-atmosphere system. - 2 Effect of the atmosphere. - 3 Effect of cloud cover. - 4 Effect of latitude. - 5 Effect ofland and sea. - 6 Effect of elevation and aspect. - 7 Variation of free-air temperature with height. - C Terrestrial infra-red radiation and the greenhouse effect. - D Heat budget of the earth. - E Atmospheric energy and horizontal heat transport. - 1 The horizontal transport of heat. - 2 Spatial pattern of the heat budget components. - 4 ATMOSPHERIC MOISTURE BUDGET. - A The global hydrological cycle. - B Humidity. - 1 Moisture content. - 2 Moisture transport. - C Evaporation. - D Condensation. - E Precipitation characteristics and measurement. - 1 Forms of precipitation. - 2 Precipitation characteristics. - a Rainfall intensity. - b Areal extent of a rainstorm. - c Frequency of rainstorms. - 3 The world pattern of precipitation. - 4 Regional variations in the altitudinal maximum of precipitation. - 5 Drought. - 5 ATMOSPHERIC INSTABILITY, CLOUD FORMATION AND PRECIPITATION PROCESSES. - A Adiabatic temperature changes. - B Condensation level. - C Air stability and instability. - D Cloud formation. - 1 Condensation nuclei. - 2 Cloud types. - 3 Global cloud cover. - E Formation of precipitation. - 1 Bergeron-Findeisen theory. - 2 Coalescence theories. - 3 Solid precipitation. - F Precipitation types. - 1 'Convective type' precipitation. - 2 'Cyclonic type' precipitation. - 3 Orographic precipitation. - G Thunderstorms. - 1 Development. - 2 Cloud electrification and lightning. - 6 ATMOSPHERIC MOTION: PRINCIPLES. - A Laws of horizontal motion. - 1 The pressure-gradient force. - 2 The earth's rotational deflective (Coriolis) force. - 3 The geostrophic wind. - 4 The centripetal acceleration. - 5 Frictional forces and the planetary boundary layer. - B Divergence, vertical motion and vorticity. - 1 Divergence. - 2 Vertical motion. - 3 Vorticity. - C Local winds. - 1 Mountain and valley winds. - 2 Land and sea breezes. - 3 Winds due to topographic barriers. - 7 PLANETARY-SCALE MOTIONS IN THE ATMOSPHERE AND OCEAN. - A Variation of pressure and wind velocity with height. - 1 The vertical variation of pressure systems. - 2 Mean upper-air patterns. - 3 Upper wind conditions. - 4 Surface pressure conditions. - B The global wind belts. - 1 The trade winds. - 2 The equatorial westerlies. - 3 The mid-latitude (Ferrel) westerlies. - 4 The polar easterlies. - C The general circulation. - 1 Circulations in the vertical and horizontal planes. - 2 Variations in the circulation of the northern hemisphere. - a Zonal index variations. - b North Atlantic Oscillation. - D Ocean structure and circulation. - 1 Above the thermocline. - a Vertical. - b Horizontal. - 2 Deep ocean water interactions. - a Upwelling. - b Deep ocean circulation. - 3 The oceans and atmospheric regulation. - 8 NUMERICAL MODELS OF THE GENERAL CIRCULATION, CLIMATE AND WEATHER PREDICTION / T. N. Chase and R. G. Barry. - A Fundamentals of the GCM. - B Model simulations. - 1 GCMs. - 2 Simpler models. - 3 Regional models. - C Data sources for forecasting. - D Numerical weather prediction. - 1 Short- and medium-range forecasting. - 2 'Nowcasting'. - 3 Long-range outlooks. - 9 MID-LATITUDE SYNOPTIC AND MESOSCALE SYSTEMS. - A The airmass concept. - B Nature of the source area. - 1 Cold airmasses. - 2 Warm airmasses. - C Airmass modification. - 1 Mechanisms of modification. - a Thermodynamic changes. - b Dynamic changes. - 2 The results of modification: secondary airmasses. - a Cold air. - b Warm air. - 3 The age of the airmass. - D Frontogenesis. - 1 Frontal waves. - 2 The frontal-wave depression. - E Frontal characteristics. - 1 The warm front. - 2 The cold front. - 3 The occlusion. - 4 Frontal-wave families. - F Zones of wave development and frontogenesis. - G Surface/upper-air relationships and the formation of frontal cyclones. - H Non-frontal depressions. - 1 The lee cyclone. - 2 The thermal low. - 3 Polar air depressions. - 4 The cold low. - I Mesoscale convective systems. - 10 WEATHER AND CLIMATE IN MIDDLE AND HIGH LATITUDES. - A Europe. - 1 Pressure and wind conditions. - 2 Oceanicity and continentality. - 3 British airflow patterns and their climatic characteristics. - 4 Singularities and natural seasons. - 5 Synoptic anomalies. - 6 Topographic effects. - B North America. - 1 Pressure systems. - 2 The temperate west coast and Cordillera. - 3 Interior and eastern North America. - a Continental and oceanic influences. - b Warm and cold spells. - c Precipitation and the moisture balance. - C The subtropical margins. - 1 The semi-arid southwestern United States. - 2 The interior southeastern United States. - 3 The Mediterranean. - 4 North Africa. - 5 Australasia. - D High latitudes. - 1 The southern westerlies. - 2 The sub-Arctic. - 3 The polar regions. - a The Arctic. - b Antarctica. - 11 TROPICAL WEATHER AND CLIMATE. - A The intertropical convergence. - B Tropical disturbances. - 1 Wave disturbances. - 2 Cyclones. - a Hurricanes and typhoons. - b Other tropical disturbances. - 3 Tropical cloud clusters. - C The Asian monsoon. - 1 Winter. - 2 Spring. - 3 Early summer. - 4 Summer. - 5 Autumn. - D East Asian and Australian summer monsoons. - E Central and southern Africa. - 1 The African monsoon. - 2 Southern Africa. - F Amazonia. - G El Niño-Southern Oscillation (ENSO) events. - 1 The Pacific Ocean. - 2 Teleconnections. - H Other sources of climatic variations in the tropics. - 1 Cool ocean currents. - 2 Topographic effects. - 3 Diurnal variations. - I Forecasting tropical weather. - 1 Short- and extended-range forecasts. - 2 Long-range forecasts. - 12 BOUNDARY LAYER CLIMATES. - A Surface energy budgets. - B Non-vegetated natural surfaces. - 1 Rock and sand. - 2 Water. - 3 Snow and ice C Vegetated surfaces. - 1 Short green crops. - 2 Forests. - a Modification of energy transfers. - b Modification of airflow. - c Modification of the humidity environment. - d Modification of the thermal environment. - D Urban surfaces. - 1 Modification of atmospheric composition. - a Aerosols. - b Gases. - c Pollution distribution and impacts. - 2 Modification of the heat budget. - a Atmospheric composition. - b Urban surfaces. - c Human heat production. - d Heat islands. - 3 Modification of surface characteristics. - a Airflow. - b Moisture. - 4 Tropical urban climates. - 13 CLIMATE CHANGE. - A General considerations. - B Climate forcings and feedbacks. - 1 External forcing. - 2 Short-term forcing and feedback. - C The climatic record. - 1 The geological record. - 2 Late glacial and post-glacial conditions. - 3 The past 1000 years. - D Possible causes of recent climatic change. - 1 Circulation changes. - 2 Energy budgets. - 3 Anthropogenic factors. - E Model s
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 2
  • 3
    Publication Date: 2015-05-08
    Description: Upper Cretaceous strata in the type area of the Maastrichtian Stage (SE Netherlands, NE Belgium) have yielded comparatively abundant and diverse raninid assemblages (Collins et al., 1995; Fraaye & van Bakel, 1998). To date, seven species are known: Eumorphocorystes sculptus, Pseudoraninella muelleri, Lyreidina pyriformis, Raninoides? quadrispinosus, Raniliformis chevrona, Raniliformis prebaltica and Raniliformis occlusa. These occur mainly from the upper portion of the Maastricht Formation [Emael, Nekum and Meerssen members, Belemnitella junior and Belemnella (Neobelemnella) kazimiroviensis biozones].
    Keywords: Homonymy ; Crustacea ; ichnofossils ; Notopus
    Repository Name: National Museum of Natural History, Netherlands
    Type: Article / Letter to the editor
    Format: application/pdf
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  • 4
    Publication Date: 2015-05-08
    Description: Well-preserved material of Binkhorstia ubaghsii reveals some additional information that helps clarify the taxonomic affinities with the Torynommidae of this Late Cretaceous crab from the Maastricht area of Belgium and Netherland
    Keywords: Crustacea ; type Maastrichtian ; Binkhorstia ; systematic placement
    Repository Name: National Museum of Natural History, Netherlands
    Type: Article / Letter to the editor
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  • 5
    Publication Date: 2024-01-12
    Description: Upper Cretaceous strata in the type area of the Maastrichtian Stage (SE Netherlands, NE Belgium) have yielded comparatively abundant and diverse raninid assemblages (Collins et al., 1995; Fraaye & van Bakel, 1998). To date, seven species are known: Eumorphocorystes sculptus, Pseudoraninella muelleri, Lyreidina pyriformis, Raninoides? quadrispinosus, Raniliformis chevrona, Raniliformis prebaltica and Raniliformis occlusa. These occur mainly from the upper portion of the Maastricht Formation [Emael, Nekum and Meerssen members, Belemnitella junior and Belemnella (Neobelemnella) kazimiroviensis biozones].
    Keywords: Homonymy ; Crustacea ; ichnofossils ; Notopus
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 6
    Publication Date: 2024-01-12
    Description: Well-preserved material of Binkhorstia ubaghsii reveals some additional information that helps clarify the taxonomic affinities with the Torynommidae of this Late Cretaceous crab from the Maastricht area of Belgium and Netherland
    Keywords: Crustacea ; type Maastrichtian ; Binkhorstia ; systematic placement
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Economic affairs 23 (2003), S. 0 
    ISSN: 1468-0270
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Economics
    Notes: Marjorie Grice-Hutchinson, who recently died, was a leading scholar of the Salamanca school of economics. That school anticipated much of the economic thinking which helped underpin the case for liberal markets in the eighteenth and nineteenth centuries.
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  • 8
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Economic affairs 23 (2003), S. 0 
    ISSN: 1468-0270
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Economics
    Notes: Taxes on capital are economically and socially counterproductive. The economy and society would benefit from their abolition. The obstacle to their abolition is not financial or economic but a failure of political will. This article looks at taxes on capital from an economic perspective: how do they differ from other taxes, what costs do they impose on the economy, and what are the consequences of their abolition? And, even if they are a failure economically, can they be justified socially or politically?
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Berkeley, Calif. : Berkeley Electronic Press (now: De Gruyter)
    Review of marketing science 1.2003, 1, art3 
    ISSN: 1546-5616
    Source: Berkeley Electronic Press Academic Journals
    Topics: Economics
    Notes: In this paper, we study competitive response to a product innovation. We consider the dynamic interaction between a "Defender" (a firm with a first generation product) and an "Attacker" (a firm with a second generation product). The second generation product entry decision of the Defender, as well as the pricing decisions of both firms, are analyzed. Analytical results are derived by developing a 3-period pricing game, and studying closed-loop policies for a Nash equilibrium. These results allow us to identify strategies in which the Attacker can prevent (or delay) a competitive response by the Defender. Some empirical support for our analytical results is also provided by pricing data and information on the timing of successive product generation introductions in the semiconductor and personal computer industries.
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  • 10
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Ground water 41 (2003), S. 0 
    ISSN: 1745-6584
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geosciences
    Notes: This paper presents a three-dimensional, MODFLOW/MT3DMS-based reactive multicomponent transport model for saturated porous media. Based on a split-operator technique, the model, referred to as PHT3D, couples the transport simulator MT3DMS and the geochemical modeling code PHREEQC-2. Through the flexible, generic nature of PHREEQC-2, PHT3D can handle a broad range of equilibrium and kinetically controlled reactive processes, including aqueous complexation, mineral precipitation/dissolution, and ion exchange. The diversity of potential applications is demonstrated through simulation of five existing literature benchmarks and a new three-dimensional sample problem. The model might be applied to simulate the geochemical evolution of pristine and contaminated aquifers as well as their cleanup. The latter problem class includes the natural and enhanced attenuation/remediation schemes of a wide range of organic and inorganic contaminants. Processes/reactions not included in the standard PHREEQC-2 database but typical for this type of application (e.g., NAPL dissolution, microbial growth/decay) can be defined and included via the extensible PHREEQC-2 database file.
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