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  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Physical geography. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (336 pages)
    Edition: 1st ed.
    ISBN: 9783319324494
    Series Statement: Space Sciences Series of ISSI Series ; v.55
    DDC: 551.48028
    Language: English
    Note: Intro -- Contents -- 1 Foreword: International Space Science Institute (ISSI) Workshop on Remote Sensing and Water Resources -- References -- 2 Modelling Freshwater Resources at the Global Scale: Challenges and Prospects -- Abstract -- 1 Introduction -- 2 Approaches for Modelling Global Hydrology -- 3 Challenges -- 3.1 Modelling Human Water Use -- 3.2 Uncertain Climate Input -- 3.2.1 Uncertainties in Historic Climate Information and Their Impact on Simulating Water Resources -- 3.2.2 Uncertainties in Global and Regional Climate Projections and Their Impact on Simulating Future Water Resources -- 3.3 Quantification of the Role of Active Vegetation Under Changing Climate and CO2 Concentrations -- 3.4 Understanding of Why GHMs (Including Global Irrigation Models) Respond Differently to Changed Climate Input -- 3.5 Modelling of Monthly Time Series of River Discharge and Human Water Use to Support More Meaningful Indicators of Water Stress for Both Humans and Ecosystems -- 3.6 Simulation of Groundwater-Surface Water Interaction and Capillary Rise by Gradient-Based Groundwater Modelling -- 3.7 Detection and Attribution of Observed Changes in Freshwater Systems -- 4 Prospects -- 4.1 Multi-criteria Validation Against River Discharge and Geodetic/Remote Sensing Observations -- 4.2 Multi-criteria Calibration and Data Assimilation -- 4.3 Hyperresolution Global Hydrological Modelling -- 5 Conclusions -- Acknowledgments -- References -- 3 On the Use of Hydrological Models and Satellite Data to Study the Water Budget of River Basins Affected by Human Activities: Examples from the Garonne Basin of France -- Abstract -- 1 Introduction -- 2 The Water Balance at the Scale of the Entire Garonne Basin -- 2.1 Climate and Physical Properties -- 2.2 Anthropization, Environmental Change due to Human Actions. , 2.3 Hydrological Regime of the Garonne Basin: Trends and Variability -- 3 Interest of Fine Scale Data to Validate or Constrain Models -- 3.1 Snow Cover -- 3.2 Crop Sowing Date -- 4 Explicit Modeling of Human Activities at the Scale of the Basin Using a Multi-agent Simulation Platform -- 4.1 MAELIA: A Multi-agent Platform of Social-Ecological Systems -- 4.1.1 Agricultural Processes -- 4.1.2 Hydrological Processes -- 4.1.3 Water Management -- 4.1.4 Other Socioeconomic Processes -- 4.1.5 Calibration of the Model -- 4.2 Evaluation and Impact of Changes in the Spatial Allocation of Cropping Systems in the Aveyron Sub-basin -- 4.2.1 Studied Area and Methodology -- 4.2.2 Evaluation of the MAELIA Instance -- 4.2.3 Impact Assessment of Crop Rotation Changes -- 5 Conclusions -- Acknowledgments -- References -- 4 On Creating Global Gridded Terrestrial Water Budget Estimates from Satellite Remote Sensing -- Abstract -- 1 Introduction -- 2 Data and Methodology -- 2.1 Utilized Data -- 2.2 Product Merging and Water Budget Closure -- 2.3 Design of the Budget Closure Experiments -- 3 Results and Discussion -- 3.1 Roles of Non-satellite Sources in Closing the Water Budget -- 3.2 Roles of In Situ Precipitation Observations in Water Budget Closure -- 3.3 Effects of Different Remote Sensing ET Products in the Water Budget Closure -- 3.4 Roles of CKF in Constraining the Water Balance -- 3.5 Runoff Validation Against GRDC Data at the Basin Scale -- 4 Conclusions -- Acknowledgments -- References -- 5 Lake Volume Monitoring from Space -- Abstract -- 1 Introduction -- 2 Satellite Altimetry -- 2.1 Introduction -- 2.2 Basics of Satellite Altimetry -- 2.3 Past, Present, and Future Satellite Altimetry -- 2.4 Combination of Multi-Satellite Data -- 2.5 Accuracy of Satellite Altimetry Over Lakes -- 3 Satellite Imagery -- 4 Storage Change Calculation. , 5 Case Study: The Tibetan Plateau -- 6 Results -- 7 Conclusions -- Acknowledgments -- References -- 6 The SWOT Mission and Its Capabilities for Land Hydrology -- Abstract -- 1 SWOT Mission Overview -- 1.1 The Needs for a Global Water Surface Mission and Its Requirements -- 1.2 Characteristics of the KaRIn Instrument -- 1.3 SWOT Measurements over Terrestrial Surface Waters -- 1.4 SWOT Spatiotemporal Coverage -- 2 River Studies -- 2.1 Rivers Seen by SWOT -- 2.2 Instantaneous Direct River Discharge Estimations -- 2.3 Data Assimilation and Optimal Interpolation -- 3 Lake/Reservoir Studies and Other Land Hydrology Applications -- 3.1 Lakes and Reservoirs -- 3.2 Other Land Hydrology Applications and Synergistic Land Sciences -- 4 Conclusions and Perspectives -- Acknowledgments -- References -- 7 Toward a High-Resolution Monitoring of Continental Surface Water Extent and Dynamics, at Global Scale: from GIEMS (Global Inundation Extent from Multi-Satellites) to SWOT (Surface Water Ocean Topography) -- Abstract -- 1 Introduction -- 2 The Potential and Limitation of Satellite Techniques for Surface Water Estimation -- 2.1 Visible (VIS) and Near-Infrared (NIR) Observations -- 2.2 Active Microwave Observations -- 2.3 Passive Microwave Observations -- 3 A Multi-satellite Methodology for Global Surface Water Estimation -- 3.1 The Global Inundation Extent from Multi-satellites (GIEMS) -- 3.2 Downscaling of GIEMS -- 3.2.1 Downscaling Based on High-Resolution Satellite Observations -- 3.2.2 Downscaling Based on Topography Information -- 4 The Future with SWOT -- 5 Conclusions and Perspective -- Acknowledgments -- References -- 8 Assessing Global Water Storage Variability from GRACE: Trends, Seasonal Cycle, Subseasonal Anomalies and Extremes -- Abstract -- 1 Introduction -- 2 Data -- 2.1 GRACE Data -- 2.2 Filtered Grids of Atmospheric Reanalysis -- 3 Methods. , 3.1 Signal Decomposition -- 3.1.1 Background and Previous Approaches -- 3.1.2 Seasonal Trend Decomposition Using Loess (STL) -- 3.2 Monthly Averaging of the Daily Decomposed Forcing Time Series -- 3.2.1 Limitations of the Arithmetic Mean for the Comparison of High-Frequency Anomalies -- 3.2.2. Comparing Flux and State Variables at Different Temporal Resolutions -- 3.2.3 Weights Based on Integrated Exponential Decay Functions -- 3.2.4 Shape and Properties of the Weighting Function -- 3.3 Significance Testing and Correlation Analysis -- 3.3.1 Linear Trends -- 3.3.2 Inter-Annual Anomalies -- 3.3.3 Seasonal Cycle -- 3.3.4 Subseasonal Residuals -- 3.4 Identifying Droughts in the GRACE Record -- 4 Global Hydrological Variability in the GRACE Data -- 4.1 Distribution of GRACE Variance Among Temporal Components -- 4.2 Linear Trends -- 4.3 Inter-Annual Anomalies -- 4.4 Seasonal Cycle -- 4.5 Subseasonal Residuals -- 4.6 Droughts -- 5 Conclusions -- Acknowledgments -- Appendix 1: STL for Unevenly Spaced Time Series -- Locally Weighted Regression (Loess) -- Inner Loop -- Outer Loop -- Choosing the Parameters -- Appendix 2 -- Analytical Integration of the Weighting Function -- References -- 9 Groundwater Storage Changes: Present Status from GRACE Observations -- Abstract -- 1 Introduction -- 2 Groundwater Depletion from GRACE -- 2.1 Groundwater Depletion in North West India -- 2.2 Groundwater Depletion in the California Central Valley -- 2.3 Groundwater Depletion in Southern Murray-Darling Basin -- 2.4 Groundwater Depletions in Other Regions -- 3 Major Challenges in Monitoring Groundwater Change Using GRACE -- 3.1 Uncertainty of SSS Water Storage Changes -- 3.2 Uncertainties in GRACE TWS Storage Changes -- 4 Summary -- Acknowledgments -- References -- 10 Modeling Groundwater Depletion at Regional and Global Scales: Present State and Future Prospects -- Abstract. , 1 Introduction -- 2 Human Water Use and Groundwater Pumping -- 3 Global and Regional Assessments of Groundwater Depletion -- 4 Groundwater Depletion and Sea-Level Rise -- 5 Future Projections of Groundwater Depletion -- 6 A Way Forward -- 6.1 Quantifying the Sustainable Yield with Use of Satellite Observations and Integrated Modeling Framework -- 6.2 Assessing Food Security -- 6.3 Assessing Regional Mitigation Strategies on Food Security -- Acknowledgments -- References -- 11 What Can be Expected from the GRACE-FO Laser Ranging Interferometer for Earth Science Applications? -- Abstract -- 1 Introduction -- 2 Simulation Assumptions and Strategy -- 3 Results in the Spectral and Spatial Domain -- 4 Regional Applications Using Simulated MWI and LRI Data -- 5 Error Analysis -- 6 Summary and Conclusions -- 7 Acknowledgments -- References -- 12 Subsurface Hydrology of the Lake Chad Basin from Convection Modelling and Observations -- Abstract -- 1 Introduction -- 2 Description of the Lake Chad Basin -- 2.1 Hydrology of Lake Chad -- 2.2 Geology of the Chad Basin -- 2.3 Hydrogeology of the Basin -- 2.4 Potential Permeability Field of the Basin -- 3 2D Convective Model -- 4 Discussion -- 4.1 Relations Between the Deep Convective Circulation and Thermal Data -- 4.1.1 Subsurface Thermal Data -- 4.1.2 Surface Thermal Data -- 4.2 Relation Between Deep Convective Circulation and Hydrogeology -- 4.2.1 Evolution of the Water Composition -- 4.2.2 Comparison Between Convective Velocity and Transient Variations of the Piezometric Level: Inference on Water Mass Changes -- 5 Conclusions -- Acknowledgments -- Appendix 1: Governing Equations, Parameters and Equations of State -- Appendix 2: Parameter values -- Appendix 3: Method and Boundary Conditions -- Appendix 4: Evaluation of the Hydrological and Thermal Characteristics of Our Model -- References. , 13 Water and Food in the Twenty-First Century.
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 100 (1990), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: To first order, the estimated thickness Te of the elastic part of the oceanic lithosphere increases linearly with the square root of the age of the lithosphere at the time of loading, Δt. In order to quantify this relationship in the particular case of volcanic loading, a synthesis of Te estimates reported both in this paper and in previous studies is conducted. Excluding the anomalously low estimates from the south-central Pacific, the values are very consistent for the three main oceans and follow the empirical relationship: Te (km) = (2.7 ± 0.15)½Δt (Ma). the relationship is used to predict the age of volcanoes when the age of the crust is known (for the Trindade chain in the south Atlantic Ocean) and to predict the age of the crust when the age of the volcanoes is known (for the Pacific plate east of the Tonga trench). the age estimates are in good agreement with the structural setting.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 125 (1996), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The remote-sensing satellite ERS-1, launched in 1991 to study the Earth's environment, was placed on a geodetic (168-day repeat) orbit between 1994 April and 1995 March to map, through altimetric measurements, the gravity field over the whole oceanic domain with a resolution of 8 km at the equator in both along-track and cross-track directions. We have analysed the precise altimeter data of the geodetic mission, and, by also using one year of Topex-Poseidon altimeter data, we have computed a global high-resolution mean sea surface. The various steps involved in pre-processing the ERS-1 data consisted of correcting the data for environmental factors, editing, and reducing, through crossover analyses, the radial orbit error, which directly affects sea-surface height measurements. For this purpose, we adjusted sinusoids at 1 and 2 cycle rev−1 along the ERS-1 profiles in order to minimize crossover differences between ERS-1 and yearly averaged Topex-Poseidon profiles. In effect, the orbit of Topex-Poseidon is very accurately determined (within 2–3 cm for the radial component), so Topex-Poseidon altimeter profiles can serve as a reference to reduce the ERS-1 radial orbit error. The ERS-1 residual orbit error was further reduced through a second crossover analysis between all ascending and descending profiles of the geodetic mission. The along-track ERS-1 and Topex-Poseidon data were then interpolated over the whole oceanic domain on a regular grid of 1/16°× 1/16° size. The mapping of the gridded sea-surface heights reveals the very fine structure of the marine geoid, up until now unknown at a global scale. This new data set will be most useful for marine geophysical and tectonic investigations.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 114 (1993), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Laser data analysis on the Lageos satellite for the period 1985–1989 has been conducted to recover temporal variations of the low-degree harmonics of the Earth gravity field, in particular of C̄40, the dynamical flattening, and of C̄30 Temporal variation of these zonal coefficients may represent changes in the Earth inertia tensor, hence mass redistribution inside the solid Earth and the hydrosphere (atmosphere, oceans, ground water and glaciers).No separation has been possible between C̄20 and even zonal harmonics of higher degree (e.g. C̄40) so that the solution represents an effective C̄20. We have not solved for odd zonal harmonics of degree higher than 3, hence the C̄30 solution also represents an effective C̄30.Monthly solutions for the effective C̄20 and C̄30 over 1985–1989 are dominated by a strong seasonal (mostly annual) signal. In 1989, the C̄30 solution shows an unusually large fluctuation. This fluctuation has also been reported by other investigators and is known as the 1989 anomaly’. It may be related to some mismodelled non-gravitational perturbation in the Lageos orbit at this epoch.Spectral analysis of the monthly C̄20 solutions gives annual and semi-annual amplitudes of 1.43 × 10−10 and 0.76 × 10−10 (normalized values) respectively. For C̄30, corresponding amplitudes are 1.95 X 10−10 and 0.33 X 10−10 (normalized values; annual and semi-annual terms). the year 1989 has been excluded from the C̄30 spectral analysis to avoid pollution by the ‘1989 anomaly’.At the annual frequency, most of the observed variations may result from air mass redistribution in the atmosphere. Using global air-pressure data over the same period (1985–1989), we have computed the atmospheric induced C̄20 and C̄30 variations for both inverted and non-inverted-barometer response of the oceans and compared these to the Lageos-derived monthly solutions. Comparison shows better consistency between Lageos and atmospheric C̄20 variations for the non-inverted-barometer response at the seasonal frequency. This result challenges the common assumption that the oceans respond as an inverted barometer to long-period variations in atmospheric pressure. On the other hand, if the inverted-barometer assumption is correct, then most of the annual variations in C̄20 and C̄30 have to be found in other reservoirs. Since the contribution of ground waters and glaciers is known to be small, this leaves us with the oceanic contribution. In addition, errors in modelling annual and semi-annual ocean tides may contribute to the observed seasonal signal. We have subtracted the adjusted annual and semi-annual terms in both Lageos-derived and atmospheric-induced monthly C̄20 and C̄30 solutions. Residuals show short-term fluctuations in both series but the correlation is poor. Removal in the monthly C̄20 solutions of the total atmospheric contribution (assuming non-inverted-barometer response for the oceans) leaves a long-term, interannual fluctuation, reaching a maximum in the years 1987–1988. This interannual signal is possibly associated with the oceanic El NiÑo event which occured at this epoch. A contamination of the 18.yr non-equilibrium ocean tide as well as of
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 297 (1982), S. 386-387 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] A good correlation has been established2'3 between LOD variations and either global temperature B (correlation coefficient 0.85; 0 lagging LOD variations by 5 yr, see Fig. 1) or the long period atmospheric and oceanic excitation function (//T related to near surface winds, changes in the ...
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Earth and Planetary Science Letters 77 (1986), S. 187-202 
    ISSN: 0012-821X
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Earth and Planetary Science Letters 70 (1984), S. 395-406 
    ISSN: 0012-821X
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Earth and Planetary Science Letters 75 (1985), S. 410-416 
    ISSN: 0012-821X
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Earth and Planetary Science Letters 126 (1994), S. 473-492 
    ISSN: 0012-821X
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Earth and Planetary Science Letters 91 (1988), S. 179-197 
    ISSN: 0012-821X
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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