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  • English  (8)
  • 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
    Publication Date: 2021-06-14
    Description: In 2018 we celebrated 25 years of development of radar altimetry, and the progress achieved by this methodology in the fields of global and coastal oceanography, hydrology, geodesy and cryospheric sciences. Many symbolic major events have celebrated these developments, e.g., in Venice, Italy, the 15th (2006) and 20th (2012) years of progress and more recently, in 2018, in Ponta Delgada, Portugal, 25 Years of Progress in Radar Altimetry. On this latter occasion it was decided to collect contributions of scientists, engineers and managers involved in the worldwide altimetry community to depict the state of altimetry and propose recommendations for the altimetry of the future. This paper summarizes contributions and recommendations that were collected and provides guidance for future mission design, research activities, and sustainable operational radar altimetry data exploitation. Recommendations provided are fundamental for optimizing further scientific and operational advances of oceanographic observations by altimetry, including requirements for spatial and temporal resolution of altimetric measurements, their accuracy and continuity. There are also new challenges and new openings mentioned in the paper that are particularly crucial for observations at higher latitudes, for coastal oceanography, for cryospheric studies and for hydrology. The paper starts with a general introduction followed by a section on Earth System Science including Ocean Dynamics, Sea Level, the Coastal Ocean, Hydrology, the Cryosphere and Polar Oceans and the “Green” Ocean, extending the frontier from biogeochemistry to marine ecology. Applications are described in a subsequent section, which covers Operational Oceanography, Weather, Hurricane Wave and Wind Forecasting, Climate projection. Instruments’ development and satellite missions’ evolutions are described in a fourth section. A fifth section covers the key observations that altimeters provide and their potential complements, from other Earth observation measurements to in situ data. Section 6 identifies the data and methods and provides some accuracy and resolution requirements for the wet tropospheric correction, the orbit and other geodetic requirements, the Mean Sea Surface, Geoid and Mean Dynamic Topography, Calibration and Validation, data accuracy, data access and handling (including the DUACS system). Section 7 brings a transversal view on scales, integration, artificial intelligence, and capacity building (education and training). Section 8 reviews the programmatic issues followed by a conclusion.
    Language: English
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 3
    Publication Date: 2020-02-12
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 4
    Publication Date: 2022-07-13
    Description: Time-variable gravity measurements from the Gravity Recovery and Climate Experiment (GRACE) and GRACE Follow-On (GRACE-FO) missions have opened up a new avenue of opportunities for studying large-scale mass redistribution and transport in the Earth system. Over the past 19 years, GRACE/GRACE-FO time-variable gravity measurements have been widely used to study mass variations in different components of the Earth system, including the hydrosphere, ocean, cryosphere, and solid Earth, and significantly improved our understanding of long-term variability of the climate system. We carry out a comprehensive review of GRACE/GRACE-FO satellite gravimetry, time-variable gravity fields, data processing methods, and major applications in several different fields, including terrestrial water storage change, global ocean mass variation, ice sheets and glaciers mass balance, and deformation of the solid Earth. We discuss in detail several major challenges we need to face when using GRACE/GRACE-FO time-variable gravity measurements to study mass changes, and how we should address them. We also discuss the potential of satellite gravimetry in detecting gravitational changes that are believed to originate from the deep Earth. The extended record of GRACE/GRACE-FO gravity series, with expected continuous improvements in the coming years, will lead to a broader range of applications and improve our understanding of both climate change and the Earth system.
    Language: English
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 5
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-05-19
    Description: The rotation of the Earth changes in response to the action of torques acting on the Earth from both gravitational effects of other bodies of the solar system and interactions with all the geophysical fluids. The response of the Earth to these torques can be described using angular momentum conservation involving mass distribution in the Earth in a frame of reference fixed to the Earth. The long-term, interdecadal, intra-decadal, and decadal variations in length of day (LOD) could have several possible driving mechanisms. On the one hand, there is the external forcing such as the gravitational attraction from the Sun, Moon, and other planets acting on the solid Earth mainly explaining long-term variations, and on the other hand, there exist torques induced by the atmosphere, ocean, and hydrology circulation, mainly causing small-period changes in the Earth rotation. Using the atmosphere, ocean, and hydrology observations, it is possible to model their contributions to the Earth’s rotation change through the angular momentum approach. Furthermore, the large-scale surface mass transport such as the glacial isostatic adjustment and polar icecap melting, etc. all slightly modify the global shape of Earth, as well as alter the rotation speed in a linear way at the long-term and decadal time scale. In addition, the core-mantle processes must be involved to explain the decadal oscillation measured in LOD, typically processes involving large-scale fluid motions in the liquid outer core. We study the various periodical oscillations in the historical data and the IERS C04 LOD products as well.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 6
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-07-18
    Description: In the context of the ESA CCI Coastal Sea Level project, a complete reprocessing of high resolution along-track altimetry data of the Jason-1, Jason-2 and Jason-3 missions over January 2002 to January 2020 was performed along the world coastal zones. This reprocessing has provided valid sea level data in the 0-15 km band from the coast. A total of 750+ altimetry-based virtual coastal stations have been selected and sea level anomalies time series together with associated coastal sea level trends have been computed over the 2002-2020 time span. These virtual stations offer a unique tool for estimating sea level change close to the coast (typically up to 3 km to the coast but in many instances up to 1 km or even closer), especially in the coastal regions devoid from tide gauges. Results show that at about 90% of the virtual stations, the rate of sea level rise at the coast is similar to the rate offshore (15+ km away from the coast). In the remaining 10%, the sea level rate within 4-5 km from the coast is either faster or slower than offshore. In this presentation, we focus on a few coastal sites where the rate of sea level rise differs from that offshore. We discuss potential small-scale coastal processes (e.g., changes in shelf currents, waves, fresh water input from river runoff in deltas and estuaries, etc.) able to explain the observations.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 7
    Publication Date: 2023-06-22
    Description: The Gulf of Guinea (GoG) reports high vulnerability to coastal flooding caused by relative or climate-induced sea level rise, which is an example of how coastal sea level changes remain poorly understood, in contrast to the global and regional average sea levels measured by satellite altimetry missions. The relationship between equatorial Atlantic Ocean variability and the 1° coastal band off the coast of the GoG is investigated at interannual time scales from 29 years from recent altimetric products in order to understand its mitigation to sea level rise in a region where there is no reliable tide gauges data. The study focuses on the (extreme) warm and cold events that occur in both the GoG and the Atlantic Ninos and links them to the well-known Benguela Ninos occurrences that occur off the coast of Angola and Namibia. A correlation between signals observed along the GoG with significant events depicted along the Angola-Namibian coastlines as the extraordinary Equatorial Atlantic Warming in 2010, 2012, and 2021 with the 2019 events depicted as the warmest in the last 40 years, which has never been reported in this region, using both altimetric monthly Sea Level Anomalies and Sea Surface Temperature Anomalies. Interannual SLA along the equatorial domain are systematically analyzed, and it is found that they advance the West African coastal ones by 1 month, supporting the idea that equatorial wave dynamics are responsible for their creation and the northward propagation observed on the SLA attributed mainly to the Kelvin coastal trapped waves.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 8
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-08-09
    Description: To understand the complex functioning of the Earth system and its evolution under natural and anthropogenic forcings, as well as global change impacts on natural systems and human societies, a wide range of space-based observing systems routinely monitor for more than three decades, the Earth and its environment. This allows better understanding of processes causing global changes and their mutual interactions, and helps validating models that simulate future evolutions. Space observations are particularly important since the measurements are global and cover regions difficult to access. They provide a synoptic view of the phenomena and allow quantifying long-term changes. But in some instances, in situ observations are also highly useful, for example to measure physical and biogeochemical parameters inside the ocean. In Europe, the Copernicus Programme provides a wide range of Earth observation data and elaborated products, intended to be used not only by the international scientific community but also by the public and private sector and by policy makers, for a broad variety of applications, including mitigation and adaptation to global changes. In this presentation, we focus on physical changes occurring in the oceans under current climate change, in particular sea level rise and its coastal impacts, as well as on water resources, two topics where space observations provide invaluable information that greatly contribute to SDG6 and SDG13.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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