The Physics of Glaciers

Höfundur Cuffey, Kurt M.; Paterson, W. S. B.

Útgefandi Elsevier S & T

Snið Page Fidelity

Print ISBN 9780123694614

Útgáfa 4

Útgáfuár

3.990 kr.

Description

Efnisyfirlit

  • Front Cover
  • Title Page
  • Copyright Page
  • Table of Contents
  • Preface to Fourth Edition
  • Preface to First Edition
  • Chapter 1. Introduction
  • 1.1 Introduction
  • 1.2 History and Perspective
  • 1.3 Organization of the Book
  • Further Reading
  • Chapter 2. Transformation of Snow to Ice
  • 2.1 Introduction
  • 2.2 Snow, Firn, and Ice
  • 2.2.1 Density of Ice
  • 2.3 Zones in a Glacier
  • 2.3.1 Distribution of Zones
  • 2.4 Variation of Density with Depth in Firn
  • 2.5 Snow to Ice Transformation in a Dry-snow Zone
  • 2.5.1 Processes
  • 2.5.2 Models of Density Profiles in Dry Firn
  • 2.5.3 Reduction of Gas Mobility
  • 2.6 Hoar Layers
  • 2.7 Transformation When Meltwater Is Present
  • Further Reading
  • Chapter 3. Grain-Scale Structures and Deformation of Ice
  • 3.1 Introduction
  • 3.2 Properties of a Single Ice Crystal
  • 3.2.1 Structure
  • 3.2.2 Deformation of a Single Crystal
  • 3.3 Polycrystalline Ice: Grain-scale Forms and Processes
  • 3.3.1 Orientation Fabrics: Brief Description
  • 3.3.2 Impurities and Bubbles
  • 3.3.3 Texture and Recrystallization
  • 3.3.4 Formation of C-axis Orientation Fabrics
  • 3.3.5 Mechanisms of Polycrystalline Deformation
  • 3.4 Bulk Creep Properties of Polycrystalline Ice
  • 3.4.1 Strain Rate and Incompressibility
  • 3.4.2 Deviatoric Stress
  • 3.4.3 Bench-top Experiments: The Three Phases of Creep
  • 3.4.4 Isotropic Creep Behavior
  • 3.4.5 Controls on Creep Parameter A
  • 3.4.6 Recommended Isotropic Creep Relation and Values for A
  • 3.4.7 Anisotropic Creep of Ice
  • 3.5 Elastic Deformation of Polycrystalline Ice
  • Appendix 3.1
  • Appendix 3.2: Data for Figure 3.16
  • Chapter 4. Mass Balance Processes: 1. Overview and Regimes
  • 4.1 Introduction
  • 4.1.1 Notes on Terminology
  • 4.2 Surface Mass Balance
  • 4.2.1 Surface Accumulation Processes
  • 4.2.2 Surface Ablation Processes
  • 4.2.3 Annual (Net) Balance and the Seasonal Cycle
  • 4.2.4 Annual Glacier Balance and Average Specific Balances
  • 4.2.5 Variation of Surface Balance with Altitude
  • 4.2.6 Generalized Relation of Surface Balance to Temperature and Precipitation
  • 4.2.7 Relation of Glacier-wide Balance to the Area-Altitude Distribution
  • 4.3 Mass Balance Variations of Mountain Glaciers
  • 4.3.1 Interannual Fluctuations of Balance
  • 4.3.2 Cumulative Balance and Delayed Adjustments
  • 4.3.3 Regional Variations of Mass Balance
  • 4.4 Englacial Mass Balance
  • 4.4.1 Internal Accumulation
  • 4.4.2 Internal Ablation
  • 4.5 Basal Mass Balance
  • 4.5.1 Basal Accumulation
  • 4.5.2 Basal Ablation
  • 4.6 Mass Loss by Calving
  • 4.6.1 The Calving Spectrum
  • 4.6.2 Calving from Tidewater Glaciers
  • 4.6.3 Calving from Ice Shelves
  • 4.6.4 Calving Relations for Ice Sheet Models
  • 4.7 Methods for Determining Glacier Mass Balance
  • 4.8 Mass Balance Regimes of the Ice Sheets
  • 4.8.1 Greenland Ice Sheet
  • 4.8.2 Antarctic Ice Sheet
  • Further Reading
  • Chapter 5. Mass Balance Processes: 2. Surface Ablation and Energy Budget
  • 5.1 Introduction
  • 5.1.1 Radiation
  • 5.1.2 Energy Budget of Earth’s Atmosphere and Surface
  • 5.2 Statement of the Surface Energy Budget
  • 5.2.1 Driving and Responding Factors in the Energy Budget
  • 5.2.2 Melt and Warming Driven by Net Energy Flux
  • 5.3 Components of the Net Energy Flux
  • 5.3.1 Downward Shortwave Radiation
  • 5.3.2 Reflected Shortwave Radiation
  • 5.3.3 Longwave Radiation
  • 5.3.4 Field Example, Net Radiation Budget
  • 5.3.5 Subsurface Conduction and Radiation
  • 5.3.6 Turbulent Fluxes
  • 5.4 Relation of Ablation to Climate
  • 5.4.1 Calculating Melt from Energy Budget Measurements
  • 5.4.2 Simple Approaches to Modelling Melt
  • 5.4.3 Increase of Ablation with Warming
  • 5.4.4 Importance of the Frequency of Different Weather Conditions
  • 5.4.5 Energy Budget Regimes
  • Further Reading
  • Chapter 6. Glacial Hydrology
  • 6.1 Introduction
  • 6.1.1 Permeability of Glacier Ice
  • 6.1.2 Effective Pressure
  • 6.2 Features of the Hydrologic System
  • 6.2.1 Surface (Supraglacial) Hydrology
  • 6.2.2 Englacial Hydrology
  • 6.2.3 Subglacial Hydrology
  • 6.2.4 Runoff from Glaciers
  • 6.3 The Water System within Temperate Glaciers
  • 6.3.1 Direction of Flow
  • 6.3.2 Drainage in Conduits
  • 6.3.3 Drainage in Linked Cavities
  • 6.3.4 Subglacial Drainage on a Soft Bed
  • 6.3.5 Summary of Water Systems at the Glacier Bed
  • 6.3.6 System Behavior
  • 6.4 Glacial Hydrological Phenomena
  • 6.4.1 Jökulhlaups
  • 6.4.2 Antarctic Subglacial Lakes
  • Further Reading
  • Chapter 7. Basal Slip
  • 7.1 Introduction
  • 7.1.1 Measurements of Basal Velocity
  • 7.1.2 Local vs. Global Control of Basal Velocity
  • 7.2 Hard Beds
  • 7.2.1 Weertman’s Theory of Sliding
  • 7.2.2 Observations at the Glacier Sole
  • 7.2.3 Improvements to Weertman’s Analysis
  • 7.2.4 Discussion of Assumptions
  • 7.2.5 Comparison of Predictions with Observations
  • 7.2.6 How Water Changes Sliding Velocity on Hard Beds
  • 7.2.7 Sliding of Debris-laden Ice
  • 7.2.8 Sliding at Sub-Freezing Temperatures
  • 7.2.9 Hard-bed Sliding: Summary and Outlook
  • 7.3 Deformable Beds
  • 7.3.1 Key Observations
  • 7.3.2 Till Properties and Processes
  • 7.3.3 Constitutive Behaviors
  • 7.3.4 Slip Rate ub on a Deformable Bed
  • 7.3.5 Large-scale Behavior of Soft Beds
  • 7.3.6 Continuity of Till
  • 7.3.7 Additional Geological Information
  • 7.4 Practical Relations for Basal Slip and Drag
  • Further Reading
  • Chapter 8. The Flow of Ice Masses
  • 8.1 Introduction
  • 8.1.1 Ice Flux
  • 8.1.2 Balance Velocities
  • 8.1.3 Actual Velocities
  • 8.1.4 How Surface Velocities Are Measured
  • 8.2 Driving and Resisting Stresses
  • 8.2.1 Driving Stress and Basal Shear Stress
  • 8.2.2 Additional Resisting Forces and the Force Balance
  • 8.2.3 Factors Controlling Resistance and Flow
  • 8.2.4 Effective Driving Force of a Vertical Cliff
  • 8.3 Vertical Profiles of Flow
  • 8.3.1 Parallel Flow
  • 8.3.2 Observed Complications in Shear Profiles
  • 8.4 Fundamental Properties of Extending and Compressing Flows
  • 8.4.1 General Concepts
  • 8.4.2 Uniform Extension or Compression
  • 8.5 General Governing Relations
  • 8.5.1 Local Stress-equilibrium Relations
  • 8.5.2 General Solutions for Stress and Velocity
  • 8.5.3 Vertically Integrated Force Balance
  • 8.5.4 General Mass Conservation Relation (Equation of Continuity)
  • 8.5.5 Vertically Integrated Continuity Equations
  • 8.6 Effects of Valley Walls and Shear Margins
  • 8.6.1 Transverse Velocity Profile Where Basal Resistance Is Small
  • 8.6.2 Combined Effects of Side and Basal Resistances
  • 8.7 Variations Along a Flow Line
  • 8.7.1 Factors Controlling Longitudinal Strain Rate
  • 8.7.2 Local-scale Variation: Longitudinal Stress-gradient Coupling
  • 8.7.3 Large-Scale Variation
  • 8.8 Flow at Tidewater Margins
  • 8.8.1 Theory
  • 8.8.2 Observations: Columbia Glacier
  • 8.9 Ice Sheets: Flow Components
  • 8.9.1 Flow at a Divide
  • 8.9.2 Ice Streams
  • 8.9.3 Ice Shelves
  • 8.9.4 Transition Zone Between Grounded and Floating Ice
  • 8.9.5 Flow Over Subglacial Lakes
  • 8.10 Surface Profiles of Ice Sheets
  • 8.10.1 Profile Equations
  • 8.10.2 Other Factors Influencing Profiles
  • 8.10.3 Relation Between Ice Area and Volume
  • 8.10.4 Travel Times
  • 8.10.5 Local-scale Relation of Surface and Bed Topography
  • Further Reading
  • Chapter 9. Temperatures in Ice Masses
  • 9.1 Introduction
  • 9.2 Thermal Parameters of Ice and Snow
  • 9.3 Temperature of Surface Layers
  • 9.4 Temperate Glaciers
  • 9.4.1 Ice Temperature
  • 9.4.2 Origin and Effect of Water
  • 9.4.3 Distribution of Temperate Glaciers
  • 9.5 Steady-state Temperature Distributions
  • 9.5.1 Steady-state Vertical Temperature Profile
  • 9.6 Measured Temperature Profiles
  • 9.7 General Equation of Heat Transfer
  • 9.7.1 Derivation of Equation
  • 9.7.2 Boundary and Basal Conditions
  • 9.8 Temperatures Along a Flow Line
  • 9.8.1 Observations
  • 9.9 Time-varying Temperatures
  • 9.10 Temperatures in Ice Shelves
  • Chapter 10. Large-Scale Structures
  • 10.1 Introduction
  • 10.2 Sedimentary Layers
  • 10.3 Foliation
  • 10.3.1 Elongate Bubble Forms
  • 10.3.2 Finite Strain
  • 10.4 Folds
  • 10.4.1 Folding in Central Regions of Ice Sheets
  • 10.5 Boudinage
  • 10.6 Faults
  • 10.7 Implications for Ice Core Stratigraphy
  • 10.8 Ogives and Longitudinal Corrugations
  • 10.9 Crevasses
  • 10.9.1 Patterns and Conditions for Occurrence
  • 10.9.2 Crevasse Depth and Propagation
  • 10.9.3 Related Tensional Features
  • 10.10 Structural Assemblages
  • Further Reading
  • Chapter 11. Reaction of Glaciers to Environmental Changes
  • 11.1 Introduction
  • 11.2 Reaction to Changes of Mass Balance: Scales
  • 11.2.1 Net Change of Glacier Length
  • 11.2.2 Simple Models for Response
  • 11.2.3 Simple Models for Different Zones
  • 11.3 Reaction to Changes of Mass Balance: Dynamics
  • 11.3.1 Theoretical Framework
  • 11.3.2 Ice Thickness Changes
  • 11.3.3 Relative Importance of Diffusion and Kinematic Waves
  • 11.3.4 Numerical Models of Glacier Variation
  • 11.4 Reactions to Additional Forcings
  • 11.4.1 Response of Glaciers to Ice and Bed Changes
  • 11.4.2 Factors Influencing the Reaction of an Ice Sheet to the End of an Ice Age
  • 11.4.3 Ice Flow Increased by Water Input
  • 11.5 Changes at a Marine Margin
  • 11.5.1 Conceptual Framework
  • 11.5.2 The Tidewater Glacier Cycle
  • 11.5.3 Interactions of Ice Shelves and Inland Ice
  • 11.5.4 Forcing by Sea-level Rise
  • Further Reading
  • Chapter 12. Glacier Surges
  • 12.1 Introduction
  • 12.2 Characteristics of Surging Glaciers
  • 12.2.1 Spatial Distribution and Relation to Geological Setting
  • 12.2.2 Distribution in Time
  • 12.2.3 Temperature Characteristics
  • 12.2.4 Characteristics of Form and Velocity
  • 12.3 Detailed Observations of Surges
  • 12.3.1 Surges of Temperate Glaciers
  • 12.3.2 The Role of Water: Variegated Glacier
  • 12.3.3 Surges Where the Bed Is Partly Frozen
  • 12.3.4 Surges of Polythermal Tidewater Glaciers
  • 12.4 Surge Mechanisms
  • 12.4.1 General Evidence Relevant to the Mechanism
  • 12.4.2 The Mechanism for Temperate Glaciers
  • 12.4.3 Polythermal Glaciers
  • 12.5 Surging of Ice Sheets?
  • 12.6 Ice Avalanches
  • Chapter 13. Ice Sheets and the Earth System
  • 13.1 Introduction
  • 13.2 Interaction of Ice Sheets with the Earth System
  • 13.2.1 Processes Driving Ice Sheet Change
  • 13.2.2 Feedback Processes
  • 13.3 Growth and Decay of Quaternary Ice Sheets
  • 13.3.1 Relation to Milankovitch Forcings
  • 13.3.2 Climate Forcings at the LGM
  • 13.3.3 Onset of Quaternary Cycles
  • 13.3.4 Heinrich Events
  • 13.4 Ice Sheet Evolution Models
  • 13.4.1 Model Components
  • 13.4.2 Model Calibration
  • 13.4.3 Simulations of Quaternary Ice Sheets
  • Further Reading
  • Chapter 14. Ice, Sea Level, and Contemporary Climate Change
  • 14.1 Introduction
  • 14.1.1 Equivalent Sea Level
  • 14.1.2 Recent Climate and Sea-level Change
  • 14.2 Global Warming and Mountain Glaciers
  • 14.2.1 History of Glacier Lengths
  • 14.2.2 Worldwide Mass Balance of Mountain Glaciers and Small Ice Caps
  • 14.2.3 Sea-level Forecasts: Mountain Glaciers and Small Ice Caps
  • 14.3 The Ice Sheets and Global Warming
  • 14.3.1 Greenland
  • 14.3.2 Antarctica
  • 14.3.3 Model Forecasts of Ice Sheet Contributions to Sea-level Change
  • 14.3.4 Simple Approaches to Forecasts for the Century Ahead
  • 14.4 Summary
  • 14.4.1 Recent Sea-level Rise
  • 14.4.2 The Twentieth Century
  • 14.4.3 This Century
  • Chapter 15. Ice Core Studies
  • 15.1 Introduction
  • 15.1.1 Some Essential Terms and Concepts
  • 15.1.2 Delta Notation
  • 15.2 Relation Between Depth and Age
  • 15.2.1 Theoretical Relations
  • 15.2.2 Determination of Ages
  • 15.2.3 Difference of Gas and Ice Ages
  • 15.3 Fractionation of Gases in Polar Firn
  • 15.4 Total Air Content
  • 15.5 Stable Isotopes of Ice
  • 15.5.1 Conceptual Model
  • 15.5.2 Interpretation of Records
  • 15.6 Additional Techniques of Temperature Reconstruction
  • 15.6.1 Borehole Temperatures
  • 15.6.2 Melt Layers
  • 15.6.3 Thermal and Gravitational Fractionation of Gases
  • 15.7 Estimation of Past Accumulation Rates
  • 15.8 Greenhouse Gas Records
  • 15.8.1 Histories of Atmospheric Concentration
  • 15.8.2 Isotopic Compositions of Greenhouse Gases
  • 15.9 Gas Indicators of Global Parameters
  • 15.9.1 Global Mean Ocean Temperature
  • 15.9.2 Global Biological Productivity
  • 15.10 Particulate and Soluble Impurities
  • 15.10.1 Electrical Conductivity Measurement (ECM)
  • 15.10.2 Primary Aerosols
  • 15.10.3 Secondary Aerosols
  • 15.11 Examples of Multiparameter Records from Ice Sheets
  • 15.11.1 Deglacial Climate Change
  • 15.11.2 A Long Record of Climate Cycling
  • 15.12 Low-latitude Ice Cores
  • 15.13 Surface Exposures in Ablation Zones
  • Further Reading
  • Appendix A: A Primer on Stress and Strain
  • Index
  • Color Plates
Show More

Additional information

Veldu vöru

Leiga á rafbók í 30 daga, Leiga á rafbók í 180 daga, Leiga á rafbók í 120 daga, Leiga á rafbók í 90 daga, Leiga á rafbók í 150 daga, Rafbók til eignar

Reviews

There are no reviews yet.

Be the first to review “The Physics of Glaciers”

Netfang þitt verður ekki birt. Nauðsynlegir reitir eru merktir *

Aðrar vörur

2
    2
    Karfan þín
    Archaeological Situations
    Archaeological Situations
    Veldu vöru:

    Rafbók til eignar

    1 X 6.290 kr. = 6.290 kr.
    A Beginner's Guide to Structural Equation Modeling
    A Beginner's Guide to Structural Equation Modeling
    Veldu vöru:

    Rafbók til eignar

    1 X 11.690 kr. = 11.690 kr.